THE TO CONNECT THE ATLANTIC & PACIFIC OCEANS. WITH A HISTORY OF THE ENTERPRISE From its first Inception to the Completion of the Surveys, INCLUDING THE INSTRUCTIONS FROM F. M. KELLEY, ESQ., TO WILLIAM KENNISH, ESQ., CIVIL ENGINEER- REPORT OF MR. KENNISH S SURVEY, WITH ACCOMPANYING PLATES, AND A PAPER UPON THE THEORY OF THE TIDES-CONFIRMATORY REPORT OF E. W. SERRELL, ESQ., CONSULTING ENGINEER —AND AN ESSAY UPON THE IMPORTANCE OF THE CANAL IN ITS RELATIONS TO THE COMIMERCE OF THE WORLD. NEW-YORK: GEORGE F. NESBITT & CO., PRINTERS AND STATIONERS, Corner Pearl and Pine Streets. 1855, REPOORTS, ETC. INSTRUCTIONS TO CIVIL ENGINEER. NEw-YORK, November 2d, 1854. WILLIAM KENNISH, ESQ., Cdivil Engineer. DEAR SnR: Be pleased to form a party forthwith for the purpose of malking -explorations for a ship canal in New Granada, and proceed at once to Panama, via. Aspinwall, by the next regular steamer. At Panama charter such a vessel as, in your judgment, will best suit the purpose, and follow down the coast to the southward, with a view of discovering a good harbor in the vicinity of latitude 7 deg. north. Having found such a bay as will admit the largest class vessels, make a regular hydrographical survey of the same, noticing in particular such improvements (if any are required) that can be made, to render it perfectly safe under all circumstances. 5While passing down the coast, observe closely the mountain ranges, and look for any decided breaking down of the Cordilleras that occurs. From the bay (if you are fortunate enough to find one), proceed eastward towards the dividing ridge of the country, and search for such a line as will admit the construction of an open cut, without locks, for a ship canal that shall connect the waters of the Pacific Ocean with the Atrato River, near its confluence with the Truando River, in latitude 7 deg., longitude 77 deg. west from Greenwich. The researches which have heretofore been made at my instance, and those made by distinguished travelers, indicate that the summit of the country in this general direction is very low; and in order to establish the lowest pass —having reached the ridge between the waters flowing into the Pacific and those discharging into the Atrato River in anopposite direction -you will ruin an instrumental line of levels along the summit of this ridge, in a direction transverse to your general line. By so doingm the lowxest point will be determined, and into this:: gap, from the Pacfic, direct your researches. It is important, lien the general direction is approximacely determinedl, that a regular transit line should be run, and carefully measured, and all the inequalitiesof thie surface ascertained by level in the usual manner. When you have crossed the dividing ridge in the best place,; proceed to the Atrato River, on the most practicable- route, and then descend to the Atlantic Ocean, continuing your exiaminations of direction, currents, soundings, &c., &c. At the mouth of the Atrato make the necessary examinations for harbors, &c. The more immediate object of these surveys being to determine the approximate cost of an open cut, without locks, from ocean to ocean, having thirty feet depth of water at extreme low tide, and sufficiently wide to pass two of the largest steamers afloat, you will fill up the details of the examination with reference to this purpose. All particulars that your time and circumstances will permit you to record, of climate, and the natural productions of all kinds, of the country, be pleased to note. The sanitary condition of this region requires your special attention. As it is of the greatest consequence that whatever is done should be most thorough, please provide yourself with all instruments and apparatus that will ensure exactness. Report to me by letter, from time to time, as opportunity offers, and when you have finished, please return to New-York as expeditiously as possible. Herewith I hand you such letters of credit and introduction as are necessary, and will facilitate you in the prosecution of the enterprise. Wishing you and your party health, and a safe return, and confiding in your ability, energy, and faithfulness, I remiain, yours truly, F. M. KELLEY. REPORT OF CIVIL ENGINEER. F. M. KELLEY, EsQ. SIR: In compliance with your order, bearing date November 2d, 1854, directing me to proceed to the Province of Choco, in the Republic of New Granada, South America, and explore a route across the Cordilleras, from 7 deg. north latitude, on the Pacific, to 7 deR'. north latitude, 77 deg. longitude west of Greenwich, on the Atrato River, for the purpose of locating a line for an inter-oceanic ship canal, without locks, I have the honor to REPORT: That, accompanied by my first assistant, Mr. Norman Rude, I started, in the steamship George Law, for Aspinwall, on the sixth November, 1854, and arrived there on the fourteenth day of the same month, whence we proceeded across the Isthmus, and arrived at Panama the next night, where I was joined by my second assistant, Dr. R. G. Jameson. December 10, 1854.-We sailed from Panama for the Island of Tobago, and arrived there the next day. Here we remained, in order to get necessary alterations and repairs made to a bungo, which we purchased for the voyage down the coast. December 13.-Sailed at one o'clock, A. M., for the Pearl Islands, which were in our course; the wind liaght. December 14. —We laid to all night, and reached the pueblo of San Miguel, on the Island San Miguel (one of the Pearl group); the weather clear and pleasant. December 15.-At San Miguel. The 16th, 17th and 18th were occupied in the voyage from the Pearl Islands to the Boca Chica, the smallest of the two nmouths that connect the harbor of Darien with the Gulf. xWe stopped the night of the 18th at Palma, a pueblo, or village, of five houses, built of cane, and situated just inside the harbor of Darien. Decemrber 19.-Arrived at two o'clock, P. M. at Chapigana, and landed at the residence olf Iessrs. Hossack and Nelson. Here the Alcalde and village Judge called upon us, and offered their services, and gave us information of a very encoura ing nature respecting the country between thle Jurador River and the river Atrato. They expressed nmuch apprehension of being attacked by their neighbors7 the San Blus Indians, who, ever since the memorable and unfortunate expedition of the Virago, and of the American party, under Lieut. Strain, have been more inveterate than before against foreigners. The object which we had in view in visiting this place, was to obtain the aid of Mr. Nelson, and one or two sailors acquainted with that portion of the Pacific coast which extends from the Gulf of San Miguel to the river Jurador. Skillful and experienced pilots are very necessary for this voyage, as the coast is bold and rocky, with numezrous reefs and strong currents. The thermom-eter was 82 deg. at noon. December 22.-AWe obtained two sailors one of whom engoaged for the voyage; the other would not go further than Gairachine. Mir. Nelson also agreed to accompany us. Here our cook deserted, but was retaken, and sent on board by the Alcalde. \We returned from. Chapigana to Palma, which we reached in the afternoon, and found the tidal currents of thne harbor of San Miguel very strong. /December 23. —Left Palma for Garachine, passing the Boca Chica; emerging from this narrow and remarkable passage, we steered for Garachine, and reached it about 5.30 o'clock, P. M. -ere we found that it would be impossible to obtain the services of any sailors until after Christmas, and were therefore constrained to remain until the 2?7th. Decemzber 24.-0We took altitudes, &c. in order to determine the longitude of Garachine. December 27.-Obtained a pilot; also another to replace the one who left us at Garachine. At Garachine we noticed a lofty range of mountains, one of which, immediately behind the village, rises to the height of 3,000 feet; and from this the range passes southwards, following -the coast to Puerto Pinas, where it is but little diminished in altitude. December 28.-WVe made sail and rounded Cape Garachine, and being apprehensive of not having water enough on board, we put in at Puerto Escondido, a small boat harbor, very inaccessible, with narrow entrance, through which there rushes a furious tidal current, causing a heavy swell and formidable surf. When safely anchored inside, we obtained excellent water; and suspending our hammocks from the branches of trees, passed a comfortable night. December 29.-Sailecl again; the wind being light and baffling, we were compelled to anchor during the night. There are few situations along the Pacific, in this latitude, where good anchorage is obtainable. The coast all the way from Garachine, is rocky and bold, and has but little beach. The hills, from the margin of the sea to the higaest visible mountain ridges, are covered with dense forests, rarely traversed by any human being. This is true of the coast all the way fiom Punto Garachine to Puerto Pinas, and from thence to Punto. Ardita. ~With the exception of Puerto Pinas, there is no harbor of sufficient depth for vessels larger thane those used for coasting, (which are small,) on all this line of coast. Puerto Pinas, however, is capacious, and deserves a more extended description, which is given hereafter. December 30.-We arrived within a mile and a-half of the entrance of Puerto Pinas, but were baffled by the winds, and were compelled to anchor in a dangerous situation, exposed to a heavy swell, 1which threatened to drive us ashore. December 31.-We weighed ancho.r at daylight, and, after four hours' heavy pulling against a current, made the entrance of Puerto Pinas, near which there are several remarkable detached roces, which mark the position of the harbor very distinctly. We entered the harbor about eight o'clock, A. M., and followed closely the rocks on its northern margin, until we reached the mouth of a river which flows into it froiA the direction of the Sierra, which is lofty, and limits the view towards the interior. At the time of landing, tIre thermoimeter siood at 88 deg. A rancho was speedily erected on the sandy neck, between the river and the bay. This harbor is two miles and a-half wide at the mouthl and extends inwards, to the cro-17wn of the bay, about five miles. It is closely hemmed in by mountains, which are densely wooded, and rise to the altitude of from five hundred to one thousand feet. The more distant ranges, in the interior, appear to have av n altit;ude from three thousand to four thousand feet. The shores, on both sides, are indented with bays, which would shelter a vessel against )allI winds. These are of limited extent, but have deep water close to the shore. The Rio de Pinas is an inconsiderable stream, liable to sudden a1nd heavy freshets, during one of which, outr bunio dragged her anchor, and was with great difficulty prevented from driftling out into the bay. The playa, or beach, which margins the crowan of the harbor, is very smooth, with a gradual slope, but, owing to the tidal current, is at all times beaten by a succession of breakers, rendering it difficult, and even dangerous, to land upon from boats. Landing-places can only be found at the mouth of the river, or in the various inlets which indent its northern and southern shores..J~anuzary 1, 1855.-I started from the rancho at half-past eight o'clock, A. M., and, accompanied by the Doctor, walked towards the crown of the harbor, intending to ascend one of the hills. -We were attended by our pilot and the sailors, armed with hatchets, to cut the brushwood in our ascent. After walking' three miles along the beach, we reached a cool and shaded rivulet, falling in a cascade. Here we breakfasted, and then comnmenced the ascent. We took with us one aneroid barometer and detached thermometer; the other aneroid, with thermometer, being left at the rancho, with Captain Rude, who was directed to note, every hour, the baronmeter pressure, and register the atmospheric temperature. When we reached the summit of the hill, which was very steep, and difficult of ascent, and, moreover, extremely slippery from the clayey nature of th e surface, we observed the instruments, and found the atmospheric pressure diminished 45-100 of an inch, indicating, with the correction for the temperature, a height of nearly 500 feet. Jctnucary 2.-We took angles of elevatiomn, to ascertain, t;rigonometrically, the height of te hi;ll wnh ich we ascended yesterday; but the angles obtained weTre necessarily, very acute, and consequently, unsatislfactory. In ascending andCt measurting the altitude of thais hill, we had two objects in view: First, to test the accuracy of a barometrical observation, as compared with a trigonometrical one; and, secondly, to obtain a view, from an elevated summit, over the neighboring country. But in the latter we were completely disappointed; the foliage being so dense, that it wtas impossible to see to a greater distance thaen a few yards. This difficulty we had to contend with during all our subsequent travels, from the Pacific to the Atrato. Hence, all statements respecting views from the tops of hills in iNew GQranada, are to be received with caution and. distrust. No extensive prospects are obtainable from anty nloutain seen by our expedition in New Granada. January 3. —At'uerto Pinas, we became acquainted with a resident of Jurador, who gave us a very intelligent account of the country between the mouth of that river and the Atrato. January 6.-This evening, at seven o'clock, we got under way, and stood out of the harbor? with light, unsteady winds. We passed a row of remarkable detached rocks, seven in number, which mark the southern head of the harbor. Janusary 7.-We reached.Punto Ardita, after two days of difficult, harassig, anld tedious navigation; making sail when the wind was favorable, and anchoriag when it was calm, or foul. The coast between Puerto Pinas and Punto Ardita, is bold, rocky, and dangerous. There are two remarkable pronontories. The most northerly is called Punto Muerto; the more southerly, Punto Caracoles. In the vicinity of these points, the sinall coasting canoes and piraguas find anchorage. Punto Cocalito is another similar promontory, within about six miles of Punto Ardita. At this last-named promontory commences the remarkable and important bay, which encloses the outlet of thq Jurador and Paracuchichi rivelrs'besides others of lesser note; and here we perceived, at a glance, that depression of the Cordilleras, (from the altitude of thousands to that o0 hundreds of feet,) -where we have determined to effect a hitherto unexplored route from the Pacific to the Atrato. This important bay terminates, towards the south, in the remarkable promontory of Punto Marzo, An extent of not less than thirty-five miles, with a depth of fifteen miles. from the crown of the bay, to a straight line, connects the two headlands. This line of coast presents three great playas, or beaches of sand, the first of which, forming the segment of a circle, intervenes betweer Punto Ardita and the mouths of the Jurador; the second runs nearly ir a straight line, from the Jurador to the mouths of the Paracuchichi, a dis tance of ten miles; the third extends from the month of the last-named: river, in a semi-circular direction, to the mnoutlh of the Corredor River, a distance of fifteen miles. The waves of the Pacific break in long continuous lines of surf against these elongated beaches, from whence the water deepens very regularly and gradually, afifording anchorage of frorm ten to thirty fathomns, within two or three miles of the shore. The bottom is of sand, deepening very gradually from the shore outwards. Off thne points of Ardita, Jurador, and Mar-zo, there are detached rocks; but all other parts of the bay are free from these dangerous obstructions. At Corredor, there is an indentation of the coast, forming a saie an.chorage and harbor, where ships of large size can be protected from nearly every wind, within seven or eight miles, running distance, from the mouth of the River P-araoC uchichi, the importalnce of which will hereafter be pointed out. The coast between Punto A.rdita and Marzo is dieserving of an especial description. First: towards the sea, is a beach skirted with innumerable cocoa-nut trees; more interiorly, a level expanse thickly covered with mangroves, and traversedc by canoes or canals formled by nature in a network, in which the tide rises and fa.lls, showing thSre to conmunicat with the Jurador and Paracuchichi rivers. Beyond this level, or " manglade," the surface rises into gentle elevations, of inconsiderable altit-ude, the highest of which does not appear to exceed a few hundred feet. Thronughout its entire extent, the country, far and near, is covered with trees. Froi Coorredor to Jurador, and even to Ardita, it is possible to go on foot along' the beaches excepot a- hibgh water, when the tide reaches the bushes. This being the only partt of the coast at which a depression of the Cordilleras is visible, the character of the coast line itself requires an especial deseription, viith r-eference to the existence of a harbor at which a canal might ternlina e. Hitherto we had not heard of th e existence of a-ny natural harbor in this vicinity, except Coi edor. It was necessary for us to enter the moutuh of the Paracuchichi, through its rows of breakers, ere vwe became aware of the wide and beautiful expanse of sheltered water, which was hidden from our sight as we passec along by the long peninsula of Paracuchichi. To resume the narra-tive of events: we reached, as already observed, Punto Ardita, and brought up in a small anchorage, only accessible to canoes or bungos. Fromn this point our pilot pointed out the entrance of the Jurador, about five miles distant, and he wwas of opinion that the surf was too heavy to attempt to enter; nevertheless, about five o'clock, P. M., he changed his mind, and ran across the bay of Ardita to within a few hundred yards of the mouth of the river; here we anchored, as it was getting dark, in about eight fat-homs. JazuaCry 8.-We got under way at daylight, and pulled close to the northern mouth of the Jurador; but the surf was so heavy and formidable, that to have attempted an entrance would have been madness. The passage is only a few yards wide, and can only be approached at certain times. Formidable rocks break the heavy rollers into foam,'which is dashed upwards in clouds of spray. Steering on for about one mile and a-quarter, we passed the island which separates the two mouths of the Jurador; it is level at each extremity, and rises in its central part to a height of about thirty feet. The surf, as we sailed along, forbade any attempts at landing, and when we reached the southern mouth, the same difficulty met us; in fact, we had no alternative but to steer along the coast froml the Jurador in search of a landing-place, but which we could not find nearer than Corredoro There we brought up in a finely sheltered harbor about two o'clock P. M. Janzuary 9.-At Corredor there are no inhabitants. The hills rise abruptly from the beach, and are, as everywhere else in this country, thickly wooded from base to summit;. This day we took a lilne of soundings across the harbor, at a cable's length from the shore, and the result was a medium depth of three fathoms. Leewardly there is a safe anchorage for large ships protection against the prevailing winds being afforded by the neighboring coas's. Jaznucary 10.-VWe took bearings of important points from Corredor. Mouth of the Parucalchihi N. 25 deg. Wi.; Cocalito, 1N. /W.; AMouth of Jurador N. -W. and by AV. In the evening', having obtained the services of a mrore trustworthy pilot, who came down fron Jurador on purpose to see us, we weighed anchor and stood across the bay, steering -for the mouths of die Paracuchichi. Jancuary 1 i. —This m1orning, ulder the pilotage of a skillful seamail, we approached the nmouths of the iivel, from our anchorage off Paracuchiclli. The surf was, as usual, high andt continuous; there was no passage except through the breakers, and there being no wind, it was necessary to trust solely to the three oarsmen. The pilot, keeping -the boat's head at right angles to the line of surf, which afordecl our only chance of effecting a safe passage, urged the sailors, by every possible effort of voice and gesture, to pull through vigorously. Three heavy breakers followed us up in suecession, and tthe fourthl brought us into suloother water. In a few mllintes more we found ourselves floating on the surface of a river, which wound witl a slow current through a level space, covered with mangroves of great height. Firom thence we proceeded in smaller canoes, furnished by a native resident, to the pueblo or village of Eurachichi, which we reached about haltf-past twelve o'clock, noon, leaving our bungo to be taken after us, when dismasted. Arrived at the pueblo, which contains about six houses, widely scatterecl, we beheld with pleasure a fine andc spacious inlet, extendin-g inorthwards froil the mouth of the Paracuchichi River, from three and a-half to fourl miles in length, and from two hiundllred and fifty to five hundred yards in breadth. Seen from its southern extremity, it appeared likle a fine inland lake, with a pesilbectly smooth surface, protected fiom the minds of the Pacific by an iiltervenilng peninisula, which supports an abundant vegetation of cocoa-nuts, pallm and othier tropical plants, growingm so densely, that, unless by following a beaten triack, it is quite impossible to traverse it. On the other side of the inlet, the vegetation is of a nmore soiibre aspec t, consisting chiefly of manglacde or nimagrovei whichl, although selkdom attaining great thickness, is distinguished by the extrenme htardness and durability of its wood. This wood would, no doubtl be suitable for piles, and may be obtained iln any required quantity. This inlet is not aicd down on any chart; it is situakted in latiltude 6 deo. 57 nin.n 32 sec. nort. NWe fcun'd the temperature cool and agreeable, and heardc of no sickness, except a little fever and ague among the natives of t'he vicinity. 2 10 The thermometer ranged from 84 deg. at noon to 70 deg. at night. The barometer from 29 35-100 inches to 29 42-100 inches; determined by the aneroid. The highest tide observed at Paracuchichi, at spring and neap, was twelve feet six inches, and the lowest ten feet eleven inches. The soundings of this inlet, taken at low water, were from two and a-half to three fathoms, in mid-channel. The bottom is mud and sand, easily excavated to any necessary depth. Towards the north the inlet narrows to the breadth of twenty yards, and winds intricately. In this direction it can be navigated in canoes for nearly two-thirds of the distance to Jurador; but by degrees the channel becomes narrower and shallower, until it finally loses itself in mud, which prevents any further progress in that direction. In full states of the tide canoes can advance considerably further, so as to meet a creek that is sent off from the southern channel of the Jurador, thereby converting the Peninsula of Paracuchichi, for the time being, into an island. The breadth of this peninsula varies but slightly throughout its whole length of ten miles; the average distance from the margin of the sea to that of the inlet, being from three hundred to five hundred yards. Its surface is several feet above the highest reach of the sea. The inhabitants informed us that on no occasion, within their recollection, had it been overflowed. I saw no drift-wood, or any similar indications of its having been inundated within any recent period. If to these reasons, we add the well ascertained fact, that violent storms are almost unheard of occurrences in this region of the Pacific, we shall readily arrive at this important conelusion, viz.: that this peninsula constitutes a permanent barrier, or breakwater, sheltering from the sea a beautiful and tranquil inlet, almost fashioned by nature to serve as a dock or harbor, of ample extent, and suitable in every respect for the terminus of an inter-oceanic canal. The surf which I have described is a common feature of the [Pacific coast of South America; I have noticed it to prevail everywhere, except in situations sheltered from the westerly winds. It is far more formidable in appearance than in reality, especially in a bottom of sloping sand: a boat with sufficient headway can pass through it ~with safety at any time at Paracuchichi; but a bungo, such as our own, being too large to be adequately impelled by oars, runs much risk of being swamped. The line of surf extends outwards, about one hundred yards. The manner of connecting the inlet with the ocean, by a cut through the peninsula, so as to obviate the inconvenience fiom the surf, is represented in Fig. 10, Plate IV.'Before entering upon the description of our overland route to the Atrato, I consider it necessary to point out the various important conclusions that are established by the preceding narrative, and observations of the coast from Garachine to the Promontory of Punto Marzo. first.-That the coast between Punto Garachine and Punto Ardita is everywhere bold and mountainous, and the interior more so, and that it contains only one good harbor, viz.: that of Puerto Pinas, which, however useful and interesting in some respects, is of no importance with reference to an inter-oceanic canal. Second.-The very remarkable depression of the Cordilleras, which is seen opposite that portion of the coast between Punto Ardita and Punto 11 Marzo. In this interval the country loses the mountainous character entirely, and assumes the appearance of a gradual rise or slope, with hills of little elevation in the distance. This space is bounded on the north by a range of mountains running in a north-easterly direction from the vicinity of Punto Ardita. On the south it is limited by another lofty range of mountains, following a similar course, and terminating at Punto Marzo. Third. —Because opposite to this depression of the Cordilleras I have discovered anrinlet, which, I believe, is hitherto undescribed, presenting ample extent and perfect shelter, capable of being deepened to any required extent, and of being connected with the ocean so as to constitute a terminus to the canal, and which will need, comparatively, but a small outlay in order to render it complete in every respect. Fourth.-Because there is safe anchorage within a mile or two, as we proved, of this inlet, and also a valuable harbor of refuge at Corredor, distant only seven miles, in a straight line. Fifth.-Because severe gales or hurricanes seldom occur on this coast. On this voyage, and on four previous occasions, when in this vicinity, in open canoes, sometimes with the gunnel only a few inches above the water, I never experienced any state of the weather at all approaching the nature of a storm, or what is called a gale of wind; gusts of short duration frequently rush down the valleys that open upon the sea-shore, and these would sometimes endanger the small schooners and canoes used in this navigation, but for the precaution taken of steering with the sheet in hand. In ordinary ship navigation, these temporary gusts, seldom of more than five minutes' duration, would cause no danger, or even inconvenience. In confirmation of these statements, it is also to be remarked, that the loss of a canoe, or other vessel, on this coast is an extremely rare occurrence: yet the anchor commonly used by the natives is only a large stone, with a cable made of the vejuce, or vine tendrils, so abundant in the forests of New Granada. Vessels equipped in this wretched manner, and at the same time badly manned, as they generally are, would, doubtless, be lost, stranded upon the rocks, or blown out to sea, in very numerous instances, but for the absolutely stormless character of this section of coast. A gale of wind capable of causing a ship to drag her anchor on this coast, would assuredly be considered a singularly rare occurrence. Weighing all the preceding considerations, the manifest capabilities of the inlet of Paracuchichi,h the existence of good anchorage in the offing, and at Corredor, in its immediate vicinity, rendering this inlet in every respect available as the terminus of a canal; the abundance of available hard wood timber in the neighborhood, the absence or extreme rarity of storms in this portion of the coast, and encouraged, moreover, by all the information we could obtain respecting the character of the country in the interior, I determined to make my arrangements for cross~ ing from this point to the Atrato, by the shortest and lowest route that can be found. January 14.-Accompanied by Dr. Jameson and Mr. Nelson, I this day started for the Jurador River, intending to confer with certain persons residing there respecting the route across from Paracuchichi to the Atrato, and also, if possible, to obtain peons for the journey. 12 WN/e were two days absent on this expedition., during which time we examined the two mouths of the river, and also noticed the windings and other features of the river itself. The disposition of the mouths of the Jurador is laid down in my remarks on the facilities for rendering them suitable for a canal terilinus. HavingT ascertained that several days must elapse before the necessary number of peons could be procured at Juraclor, but placing full confidence in the activity and. inte!ligence of the inldividual enmployed to effect the arrangements on our behalf, we were content to wait patiently until he shoulld report hiinself and his people to be in readiness for departure. Jancuavry 21.-We left ourT rancho at Paracucihichli this monting at half-past ten o'clock. I was accompanied on the occasion by the Doctor and nl r. Nelson, with our guide, Alexancldro, and peons to paddle the two canoes, and carry the baggage on the route. I left Captain Rude at Paracuchichi, with directions to continue his baromletrical observations at certain intervals, and to watch over the safety of the heavier and luore valuable baggage, including nmoney and provisions, with which he was directed to followv as soon as we should report the possibility of crossing to the Atrato by this route. To one or two of the muost trustworthy peons was confided the duty of carrying the surveying instruments. Wte crossed the inlet in a south-easterly direction, steering for the mouth of a small river, which falls into it about half a mlnile froim the nearest luouth of the Paracuchichi. cWe found the iiouth. obstructed by a bar of sand; interiorly of the bar it assumed the character of a sluggish and tortuous stream, about twenty yards in width, and closely hemmed in by the forests of imalngrove trees, which generally cover the level spaces, close to the sea-shore, on this coast. A few fallen trees retarded our progress. The banks of the creek on each side consist of a black alluvial soil, easy to cut through. The highest tides reach to two miles from the mouth of the river; here the banlks consist of alluvium, but beiig less subject to overflows, present a different vegetation —the mangrove being entirely absent. Large spaces are covered with plantain walks, the fruit of which constitutes the main depelndence of the native population; it grows with unbounded profusion. From this point the river beconmes quite shallow, with a bottom of sand and pebbles; the latter consisting chiefly of the rolled fragmnents of clay slate. Six small rapids occur in this part, varyingg in height from six to eighteen inches, and estimated to amount to six feet in the aggregate. At the distance of a mile and a-quarter above the tidal reach, we entered the mouth of a tributary called Pie de Nerqua, on the bank of which, about fifty yards from the confluence, we halted at three o'clock, P. M., for the night, and erected No. 1 Rancho, or station. It had now conmmencecd to rain heavily, and continued without intermissiol throughout the afternoon and night, causing a rise of only a few inches in the river. The general course from Paracuchichi to No. 1 Rancho, is north-east. January 22.-Rancho No. 1 being situated on a point or tongLue of land, formed by a bend of the Pie de Nerqua, I measured by level, the height of the -iver at opposite points, above and below, and found a difference of two feet six inches (2 ft. 6in.) The run of the current I found to be eighteen yards in ourteen seconds in the small rapid, and four yards in fourteen seconds in a piece of still water contiguous. We the n crossed, in succession, three other tongues of land, inclosed by the bends of the river between the crossings; so that our general course lay, as before, north-east rather easterly. The necks of land were from ten to twenty feet above the level of the river, and consisted entirely of clay. Only at one or two points did the indurated rock present itself, and then rose no higher than the bed of the stream. The depth of the river was about one foot, so that we had no difficulty in wading through it. Two other measurements of the flow of the current gave, respectively, nine yards in fourteen seconds, and four yards in fourteen seconds. The distance measured in this part of our course was one thousand yards, when we reached the confluence of a small tributary of the Pie de Nerqua, at a spot called by the natives Dos Bocas. Here we left the Pie de Nerqua, and followed the ridge of a hill which is inclosed between the two rivers, still steering' north-east. The ascent of the hill was gradual, with occasional depressions; and on each side, separated only by a breadth varying from twenty to fifty yards, was a deep ravine. The detached thermometer stood 84 deg. at 11 o'clock, A. M. Our distance from the Dos Bocas was one hundred and thirty-eight yards. We thlen found the ridge to descend from this point, until it suddenly dipped down to the level of a small, sluggish quebrada or brook, which crossed our road, and marked the termination of the first of a series of remarkable elongated hills, moderate in elevation, and consisting of clay entirely, stretching in a north-east direction, from within a few miles of the Pacific to thle valley of the Nerqua. After crossing this brook, which flowed into the valley on the righthand side of our route, I ascended another elongated or haystack shaped hill, much lower than the preceding one; and following it, under a heavy rain, still steering north-east, we reached the spot where I determined to halt for the night. This spot is situated on the bank of the river Chupipi, and is designated in the Field-Book as!ancho No. 2. (See Plates 1 and 3, where the dotted line shows the top of the ridge and where the line of level was run, and the termination of the dotted perpendicular lines shows the bottom of the valley.) The distance measured from the Dos Bocas was one thousand eight hundred and thirty yards, to the Quebrada, and nine hundred yards from thence to the Chupipi. Here the aneroid barometer, at 1 o'clock, P. M., stood at 29 20-100, and the thermometer at 79 deg. The Chupipi will cross the line of the canal, as it flows from a northerly direction and passes away to the south-westward to join the Paracuecichi. From its small size, it will form no impediment to the construction, but will be useful as a feeder. Its average breadth is about twenty feet, with a medium depth not exceeding two feet. Its bottom is pebbly, and here and there a stratified rock of clay slate presents itself in the bed, dipping at an angle of 20 deg. towards the north east: the banks, for a considerable space above the level of the water, and suppoprting a heavy vegetation, with trees, fron sixty to seventy feet high. 14 These marginal spaces of alluvial soil are frequent along the rivers of this country, and are of great importance to a public work requiring large bodies of men, from the immense profutsion with which they yield the plantain, and other kinds of food. January 23.-We remained at Rancho No. 2, awaiting communications from Captain Rude. On the same day, the party at the rancho at Chupipi started at seven o'clock, A. M., the thermoimeter at 80 deg., and, passing over a level space of alluvial soil, began the ascent of another hill, of the same form of the others we hlad previously passed over; still keeping in a north-east direction, and havi-ng close on our right hand a deep valley. At nine o'clock, A. M., being on the summit of the hill, we observed the aneroid 28 82-100, and the thermometer 79 deg. Here the course becomles east by north, the ridge exceedingly narrow, and we could hear the waters of the Chupipi at the bottom of the ravine on our left, falling over a cascade. At forty-five minutes past ten, a heavy thunder-shower, but of short duration. We continued our journey, alternately ascending and descending, according to the -form of the ridge, until a rapid descent brought us to the bank of a quebrada or brook, where, the daily rains having already set in, we erected Rancho No. 3, having passed over, since we left the last rancho in the morning, the distance of two miles and a-half, in the general direction of east north-east. It again rained very heavily throughout the afternoon and night, accompanied with much thunder and lightning. Aneroid barometer stood at 28 60-100, and the thermometer at 75 deg. The small quebrada on which Rancho No. 3 was erected, is of no imnportance, being only three or three and a-half feet wide, with high banks of clay, and a muddy bottom. During' very heavy rains it would carry a considerable body of water down to the canal, and would be of some use as a feeder. The hills and ravines continued to be thickly wooded. 1 have here to remark again, that in passing successively over the three preceding longitudinal hills of clay foundation, we had invariably observed an uninterrupted valley of great depth on our right-hand side. We look attentively for any transverse ridge or other obstacle to the passage of a canal through this elongated and continuous valley, as it seemed to me, but no such impediment could be discovered. I have also to point out the important fact, that, although sleeping nightly in the open air, sheltered from the rain only by th'e sloping roof of palm-leaves, which our peons erected for us in half an hour, our beds consisting of India rubber blankets spread over pahlm-leaves, none of our party suffered the least in health. Januzary 25.-We left Rancho No. 3 at nine o'clock, A. M., and commenced the ascent of another elongated hill of the haystack form, consisting, like the preceding ones, of clay in the soft state. At some points, the summit was a mere shell in thickness; in other respects presenting no difference, except in being of much lower eleva'tion: its course is northeast, and the distance to the Chuparador River, which crosses at its northeast foot, is twelve hundred and sixty-five yards. The Chuparador is a tributary of the Paracuchichi, and is here four feet wide, six or eight inches deep, with banks of clay, and flows southwest, with a very slow current. Then we gradually ascended another low hill, until we reached a 15 remarkably large tree, (as compared with the others, which are generally of small size on these hills, although of great height.) From thence we steered on about thile same course, and crossed another very small brook, or, rather, ditch, falling into the Chuparador. This was the last trace of water flowing into the Pacific, that we crossed. We then ascended the next in succession of this series of hills, It was of a low elevation, with a table or plateau at the top. On our left hand there was a valley, through which flows the Hingador, a tributary of the Nerqua, and, therefore, the first water hithle-rto encountered flowin' to the Atlantic. The valley of the Hingador is separated from that on our right hand, which is drained into the Pacific, by the hill or elevated ground which we were then traversing. The distance between the two valleys, in some places, is not more than one hundred and thirty feet. Descending very gradually north-east, -we crossed two small branches or tributaries of the Hingador, and reached a large branch of this river, at its junction with one of the small tri'butaries already mentionedr aCnd erected thereon Rancho No. 4. In the afternoon the rain fell heavily, and continulted until midnight. No rise of the small river before us took place; aneroid barometer 28 6-10. This branch of the Hingador is a clear, pleasant brook, half a foot in depth, eight feet wide, pebbly bottom, and flows from the westward with a moderate current. I have to point out that, from the last station or rancho, we carried along with us on our right the same continuous valley; but have to observe that, in approaching the Hingador, the country becomes more intricate, and several ridges proceed from this vicinity as from a centre, in different directions. Two form between them a deep and narrow gorge, through which the Hingador descends to the Nerqua, over a series of water-fallsthe first of which I ascertained to be of the height of hundred and sixty feet; the others, seven in number, averaging in height from three feet to twenty-four feet, This formation of the country will cause a deflection or bend in the line of the canal, in order to bring it to the level of the Nerqua. The length of the gorge of the Hingador, fron the great fall to the Nerqua in a direct line, is not more than one mile and a half. A parallel line from the valley in which it is proposed to bend the canal (the righthand valley so often mentioned) -o near the mouth of the Hingador, would but little exceed that length. Jzanuary 26.-Leaving Rancho No. 4 at nine o'clock A.., we crossed successively two bends of the tributary, and then the main body of the Hingador, which we found to be considerably swollen and muddy from the rain of last night. A fallen tree across thae stream served us for a bridge; the current was too strong and deep to ford: the bottom is rocky, and formed by ledg'es of gray slate,~ From Rancho No. 3 to this crossing, the distance is sixteen hundred and sixty yards; but as this is not within the limits of the canal, I do not enlarge the details. The great fall is but a short distance below this crossing, and in favorable states of the atmosphere can be heard easily. From this point we continued our journey along another elongated hill in the plain of the Nerqua, itc; foot being crossed by a small stony brook leading into that river. The peons had provided a couple of small canoes, belonging to the only Indian living on the Nerqua, and in these we descended the river a mile, to the house of this Indian, in whose neighborhood, at a point two-thirds of a mile above the mouth of the Hingador, we erected Rancho No. 5. Here it was necessary to await the arrival of Captain lRude, from Paracuchichi, with the remaining baggage and provisions, as I had determined to continue our journey fr'om this point to the Atrato, by the Nerqua and Truando. It was afterwards ascertained that the canoes belonging to the Indian would be much too small to carry the expedition and baggage; it therefore became necessary to have one built of sufficient size ibr that purpose. The Nerqua is about the average width of twenty yards. At the fords, which are numerous, it is not more than knee deep; the intervening pools are from three to six feet deep. I ascertained, by measurements, the rate of its flow to be two miles per hour; its water, like that of all the strea ms crossed on our route, is very sweet and cool, and perfectly salubrious. It flows through a wide alluvical valley, finely timbered and extremely fertile, capable, if cultivated, of supporting a vast population. On our arrival at the Nerqcua, we found the aneroid, at half-past eleven o'clock, A. M., stoodc at 29 25-100, and the thermometer at 80 deg. Jcanualry 31.-Captain Rude and Mr. Nelson, with the remainder of thle baggage, arrived this day from the Paracuchichi, having performled tLhe journey across in nine hours' traveling time, although the peons carried full loads. Last night a freshet raised the river three feet and a-half, so that the playa, or pebbly beach, in front of our encampment was overflowed; before morning it had quite subsided. February 1.-In coiapany with the Doctor, I examined the mouth of the Hingador, and ascended seven hundred yards. It has two mouths, one of whicl is dry, except in flood; they inclose between them a triangular space of alluvial soil. Februcary 2.-An Indian, whom we had dispatched to see another Indian living up the Truando, and the only inhabitant on that river above the Nerqlua, (or below it, as I afterwards ascertained,) camne back, and said that the man we wanted (Juan Domingo) could not conme to assist us in descending the Truando, in consequence of his being sick. He returned an answer to our special inquiry, that " no white man had ever been up the Truando, above the falls, or he mlust have known it." 2February 5.-A good tree was obtained for a large canoe, and the Indian and one of his sons, with two of our peo-is, commenced wor1king on it. February 7 cand 8.-VVe examined the Hingador, from the cataract to the Nerqua; during these dclays. At two turns below the Tree crossing, the river falls over a horizontal ledge of clay slate, perpendicularly fifteen feet. It then falls at an angle of 45 deg., over large and irregular rocks, of a black and dark color, heavy and indurated, until it reaches the bottom of the descent. The quantity of water, in ordinary states of the river, is but small; but, when flooded, this cataract must present a most imposing spectacle, from its great height. As already stated, two spurs, or ridges, forml bet7ween themr the deep and narrow gorge through which this river flows, from the fails to the Nerquia. The walls of the gorge generally rise almost perpendicularly, so that, in following the stream, it is necessary to wade nearly the whole of 17 the way, except where a cataract, or rapid, compels an ascent on the face of the rocks. The heights, on each side of the river, are from seventy to three hundred feet in perpendicular height. They consist of the black indurated rock, already described. This rock has a ready cleavage, and may be eascily excavated. In only one part of the gorge were observed indications of a land slip, and this had recently taken place. A mass of clay had become detached from near the summit of a hill, on the left hand, and had carried down with it one or two large trees to the bed of the stream. About one-third of the distance from the great fall, there is another, twenty-four feet hig'h. A little lower down, one of twelve feet, and five o'thers, varyinL from eight to three feet in height. Besides these catafacts, there are numerous rapids, caused by the descent of the river, and the bottmn is strewn with rounded and water-worn masses of rock of all sizes, from that of ithe smallest pebble, to boulders many tons in weight. About t1hree-qua-l ers of the distance down the gorge, there are numerous hot springs in the bed of the river, which are highly sulphurous, anld raise the tempercature of the surrounding water to 110 Fahr. Below the hot springs, the valley widens out considerably; the river becomes tortuous, 1rminmg bends with level tongues of land, in which the veoetation is raink and dense. Finally, as already described, it enters the Nerqua by two mnou+hs, oane of which is dry, except during freshets. ebrzcargy 1. —Ve measured the IHingador Falls by a line, as follolws: -— Lenigt, fiorm ftop to base, two hundred and thirty feet; angle of depression, 45 dlego; resulting hetiglht of perpendicular, one hundred and sixty-six feet. laebrcuary 15o=-We entered,a brook, or river, falling into the Nerqua about one-half of a mnil belov the Hingador, and followed up the same for three hours. Like the Hingador, it passes through a deep and narrow gorg-e, hemnmed in betwveen t-wo ridgies. In size, it nearly approaches the Hingador. No cataracts were met with in the bed of the river, as far as we examined it; but there were numerous small rapids. The distance to which the rliver was followed up, is computed at one and a-half miles. It is impossible to asdeend these rivers, as they are so full of natural obstacles, faster than at thie rate of half a mile per hour, on foot, and they are nmuch too shallow even for the smallest-sized canoe. Another gorge was also examinedc, opening upon the Nerqua, close to our encampment. It was obound to give passage to a small brook, which, at one part, descended in- a cataract, ninety feet in height. Our workmen havingo reported the canoe ready for service, it appeared, on inspection, adequate in size, and liglt, lbeing built of cedar, and was, therefore, better for navigating rivejrs in vwhich one of the principal obstacles to be contended sagainst consists of fallen trees. Alexandro Domno o rriirved fiom Juractor,,nct Paracuchichil and brouoght with him two youno but active Indians, with whose assistance, and that of the two residing' on the Aerqlia, wve proposed dlescending to the Atrato. ]tebrucry 1(6.-At half-past ninep o'cnock A. M., we commenced the descent fiom'the mlouth of the Hinamador towIards the Truando.'The Nerqua, below the Hingadcor, is apparently but little increased, as will be seen by refer ence to the rTable of Stoppax.es. It presents a great many obstacles, suc'h as shaOT1,o and f allen tmee-;. 18 W'_e passed the following tributaries, which the river receives on the right bank, viz.: at lO10. 30mr. the Chupachavi —the one which was examined on the 14th. At 1lh. 20m., the Pavarando, which we entered on the left bank; it is a stream rather larger than the Hingador. At 2h. P. M. we passed the mouth of the Equebrador, a tributary of the right bank - equal in size to tohe Hingador; at 2h. 15m., the Tuniando, a small branch on the left bank. The banlks of the river are alluvial, presenti;ng clay in various stages of induration; generally very soft, but at other times moderately hard, and everywhere much perforated by land crabs; sometimes strata of leaves are observed between thick beds of clay, and there are numerous deposits of a kind of blue clay, which the natives use i m aking their pottery. The general course of the river was north-eilst. We reached our rancho at four o'cloc1k P. M. Tile day, vlich lthad been beautiful in the early part of the journey, bceamuie raiy -oitowards the afternoon. The barometer stood at 29 2-10; t]le thermonometer at 9 de'. Febrzcuary 17.-We started from Ralancwho No. 6 at fortty-five mninutes past six, A. M. The heavy rains of last nionht caused a rise of the river of about one foot, which had quite subsid(ed this orninoill'. The bed of the river here consists of shelving clay rock. At ten minutes past seven o'clock the barometer stood at 29 2 7-100C and the tiermo-leter at 75 deg. There are few or no obstacies in this pa1 t of the river; it assumes a slow regular current, with Iong' reaches, the depth beingo about four feet. At twenty minutes past seven o'clock we passed the mouth of the O'odor, or Oodor, opening on the igoht bankT with a channel about a quarter the size of the Nerqua, x which it enteris fiom about north by west. At thirteen minutes past eiolht o'clock we reached the confluence of the Nerqua and Truando; the direction of the Nerqua being east by north at the point of junction. The aneroid baronmeter at this point stood at 29 3-10, and the thermomeeter at S5 d-leg.; but during our stoppaoe here -the barometer rose to 29 34-1.00. At the confluence we found the T'ruando tio be five feet deep, and thirty-five yards wide, flowing i between alluvial and level banks, elevated some eight feet above t he river, and everywhere closely covered with vegetation. It appeared about one-third largrer than. the Nerua, in the lower part of its course, and, like that river, its banks are a mere wilderness, inhabited by only one Indian and his family. It flows with a slow current, sixty feet in thirty-five seconds; and its bottom consists of rolled fragmients of a clay slate, and associated deposits similar to those found in the channel of the Nerfqua!, with about the same proportion of pebbles of quartz, or indurated clay-stone streaked with qcuartz. We left the confluence of the Nerqua and Truando at forty-five minutes past eight o'ciock, A..M., anld at twenty-five minutes past ten, after traversing some fine smnooth reaches of the river, of a depth of five to six feet, bottom of shelvingo stratified rock, inclined at an acute angle, we arrived at the heatd of the first of the series of saltos, or rapids, which constitute the mlain difflicu-lty and danger tlhat we had to encounter in descending the Trurando. Five hours and twuenty miniutes were occupied by oulr people in bringing the bagoage and thie two canoes over the first four rapids. The operation was one of immense labor and difficulty: it became necessary for them to unload the canoes three times, and carry the cargoes by land, past the most dangerous places; and in bringing down the empty canoes, especiaIly the large one, every effort of strength and skill was required in order to prevent them f'oln beilag dashed to pieces against the rocks. The valley through which this defile passes is very narrow, and hemmed in oal either side by precipices of irreguflar unstratified rock. At the foot of the fourth rapid we erected Rancho No. 7, on a rock close to the streamn andm h'gl enough to be beyond the reach of any sudden rise of'the riverx The barometer stood, at seven oeclock, P.., 29 22-100, and the the.rmlomleler at 78 deg. Betwveenl t-he second and thrd rapids the river receives a tributary on the right bank, of ineonsiderable size, not exceeding at its junction four feet in width, and only a few inches deep. Aneroid stood, at half-past seven o'clock, at 29 25-100; the thermometer at 78 deg. Februacry 18.-At eight o'clock, A. M.i we crossed the river in thle large canoe, just above te the ifth rapid, and made our way along the rocks which mnargin the river for the distance of half a mile, in which space there is a r'ec3tainoulan bend, and reached -the niain faill which was twenty-six feet. It, rained very hea ily, diTlino, which the people were employed at their difficult and hazlardous occupai;on; they first emptied the canoes, and carried the things down by land to the foot of the rapid, and then brought down the empty canloes over rocks, by sliding them over pieces of wood, in which operation all our party coeeriflly assisted. Below the main fall, we passed three ot;he rapids in the same manner. About five o'clock P. M. th oleole work s completed without the loss or damage of a single articie. _I must here state that ti'he manner in which this task was accomplished by Alexandro and his Indilans elicited the warmest thanlk]s, ancld the approbat-ion of our whole party. The barometer, at IRancho N0o. 8, at six o'cloclk, P. 1M. stood at 29 30-100. I ascertained the heig'ht of the main fall, by level, to be twenty-six feet four inches, and bv acneroid, the samne. At the head of the last rapid, the river receives a tr-ibutary from the left bank..February 19.0It was my intention to have continued the descent of the river this day, but heavy rains had caused a rise of four or five feet; and as the channel was still narrow and rocky, Alexandro did not consider it prudent to venture, although another turn of the river would have brought us into perfectly smooth water. February 20.t-Last nigit the river very quickly subsided to its usual depth; but afterwards there was a heavy rain-storm, with thunder and lightniing, and this morerino' it was higher than before, and much drift-wood floated down. During our residence at this rancho, the aneroid bcarometer ranged from 20 25-100 to 29 40-100. February 21. —The river lTars fallen, and at six o'clock A. M. we left Rancho No. 8, and dropped down the stream, and in a few minutes had cleared the na-rrow and rocky part of the channels and reached the first of the wide anid smooth reaches tihrouoh ~vlwhich the T ruando flows, after leaving the rapids. At twenty minutes past severe, I observed on the left hbank the stratified clay slate, inclined north-east at an anghle of 40 deog.; from this point the banlis again became fiat and alluvial. 20 At thirty-five minutes past seven, we passed the mouth of a river called Salida; opposite to its mouth is an island. The Salida enters the left side of the river, flowing south-east. The Truando now passes through the fiat alluvial plain of the Atrato. Itts banks consist of alluvium entirely, and are, doubtless, very fertile. At seven o'clock, A. AM., we passed the brazo, or arm, called Chuparador, which forms an island, and at twenty-five minutes past eleven we passed another island. At half-past eleven we arrived at the head of the Pallisadas or series of islands, which owe their origin to the accumulation of dlrift-wood carried down by the floods. The branches of the river diverge, and inclose, like a net-work, the numerous wooded islands which compose this group, extending to a distance of four miles. At the head of the Pallisadas, it was necessary to d-rag the canoes over a barrier of drift-wood several yards in breadth; but after this obstacle was overcome, we encountered no other in the deseent of the river, except single trees crossing the channel, one or two of which wse were compelled to cut through with the axe. At twenty-five imniutes past three, we cut through the last tree, and then continued the descent -without stoppage, until dark, when we halted for the nig'ht at a part wherie the river's banks were overflowed, which compelled uls to pass the n-ight in the canoes, in the best manner we could. The breadth of the river here is about twenty-five -yards, with a forest of lofty trees on each side. We passed about half a dozen uninhabited rauchos, built by Indians and others filom the Atrato, who occasionally ascend the Truando on fishing and hunting excursions, as far as the Pallisadas, andr even to the falls. The distance run during the day, com1puting stoppages, flow of current, and rate of passage through the water, is shown on the accompanying table. February 22. — VNe left our Rancho, No. 9, a; ten minutes past six o'clock, and resumed our voyage down the Tru' ando passing a succession of slow and smooth reaches. At fifty minutes past sevena, A.M., we entered the first of the lagoons, and found a wide and open space, oblong in uorm, and ten miles in diamleter. The whole of this open, circular space, is covered with the lagoon grass or sedge, which takes root below the surface of the water, and rises to the height of several feet above it. Through thiis green expanse flows the Truando, and other streams and brazos —the mnargins of the rivers being -frequently rather above the level of the surrounding llagoon, supporting narrow belts of trees. A rang'e of mountains is seen about twenty miles distaant, to the north, and running norlth-east and south-west. At half-past nine we passed the first lagoon, and there the Truando reentered a forest and assumed its previous forml' no open space being visible on either side. PAt forty-five minutes past eleven, we passed the mouth of the Chuparador, about twenty yards wide, and flowing north-east and south-west. At half-past one we entered the second lagoon, which closely resembled the first one in its general aspect and configuration. The Truando firom this lagooni resumes its former course, precisely. Owing to the swollen state of the Atrato, the Truando, duringl the latter part of this day, had no perceptible currenrt; consequently, our canoes were paddled along leisurely. Finally, at five o'clock, P. IM., we reached the Atrato. The mouth of the Truando is about fifty yards in width, but owiLng to the peculiar appearance of the banks of the Atrato, it is scarcely visible from the latter river. The Truando is of the depth of twenty-seven feet inside of the bar; on the bar there are but eighteen feet. The width of tlhe bar is thirty feet.,At Iorty-five minutes past five o'clock we reached the small pueblo, wThich is situated about two hundred yards below the mouth of the Sucio. H- ere ihe aneroid barometer stood at 29 37-100, at 6h. 45m., P. M. From the mouth of the iruandco to that of the Sucie, is one _mile and a-half. From this point we prioceeded to Quibdo, the capital of the Province of Cbhoco where we arrived on tihe tentLh of MEarcn; a nd having remainecd there a month and four days, on business not connected with the researehes of thhis expedition, we proceeded down the river Atrato, and arrived at its confluence with the Truando, st 6h. 30O., A.M., April 18th, 1855, froi' which point I began that pari of my survey which remained unfinished, viz,: Tv'he river Atrato from the Truando confluence to its moutIh. I sounded the river A.trato at its junction with the Truando, and found it-s depth to be fifty-eight feet; its width at this point is three hundred and fifty yards. The reach of the Atrato, at the Truando, runs due north. At'7h. 1Omi, A.M A., I arrived at the river Sucio. A sail was set on the vessel at 1Oh. 30m., A. M., which added to her speed. She went at the rate of eighbty-eig'ht feet in fourteen seconds, for thirty minutes. (See tables of Atrato.) At 11lb. 4L5m. we passed the river Salaqui, which river is called by the natives Leonda or Yegenta; it is shallow at its mouth, but opens into a large riveri. c h. 50m., P. NI., passed the mouth of the river Chercarita. _Az4ril 19.-4h. we passed the river Leondas, on the eastern bank. At 8h. A.M i. we entered the first mouth of -the river called Chocorita, and at 10h. 31m., A.AI., we entered the Gulf of Darien, through the nmouth of the Cocuito. After my arrival in Nerw-'York, on the 27th of IM ay, 1855, I reduced my notes to nmathematical calculations and drawings, and find, that not only a canal without locks is practicable, friom the Pacific to the Atrato, but a navigable river can be turned, from the lagoons of the Atrato, into the Pacific, of sufficient mnagnitude to convey the comnierce of the whole world. My endeavors to point out the practicability of such an operation are expressed in the five Plates, with explanilations of the samne, which I have thle honor to transmit herewith. As regards the salubrity of the route, I have only to call your attention to my meteorological observations, and to the fact, that neither my — self nor any of the party were sick, with the exception of a slight attack of fever and ague that I experienced while on thme Nerqua, brought on, 10 doubt, from exertion and exposure; but friom that time until my return to New-Yorlk, I enjoyed excellent health. In respect to obtaining laborers, the four adjacent provinces can supply a great numnber of men to carry out the project, some of whom, in the province of Carthagena, have been employed on the Panama Railroad. I would suggest that, the undertaking be carried on in six divisions, stationed thus:The First Division at the mouth of the river _Atrato. The Second Division at the Truando. The Third Division at Townsend Station. The Fourth Division at the eastern mouth of the tunlnel. The Fifth Division at the western mouth of the tunnel, and The Sixth Division at Kelley's Inlet. To provide accommodation for such a number of men as will be necessary to construct this work, houses must be built. The facilities offered for this purpose is the palm-tree, which grows most abundantly in this part of the country..Ranchos built of palm are applicable to the Third, Fourth, Fifth andl Sixth Divisions. Those required for the Second Division (on the Truando), and for the First Division (on the Atrato), must be constructed to float, as there are no banks on those rivers on which ranchos, or houses, can be erected. The dredging machines to be used on the river can be made sufficiently capacious to accommodate all the men in each division. East of the summit the best sites for the erection of work-shops and provision warehouses, are, Turbo, near the mouth of the Atrato, and Townsend Station, near the proposed junction of the canal with the Truando. Communication could be kept up between these two points, in twelve hours, by means of steamers drawing six feet of water. WAest of the summit I would propose, as the best locations for erecting provision magazines, &c., the Gooding and Emma Josephine Stations to supply the Fourth and Fifth. Divisions, and Kelley's Inlet to supply the Sixth Division. All the vegetables required could be raised along the shores of the Pacific, and in the valley of the Nerqua, after about a year's cultivation. The plantain, which is the chief food of the natives, grows here in great abundance; also the Indian corn and rice, to some extent, in the vicinity of the route, together with nearly all the fruits and eseulent roots of the tropics. Breadstuffs can be procured from Peru and Chili, as well as fi'om San Francisco. Cattle, pork, &c., can be conveyed from Chiriqui to Kelley's Inlet in three or'four days. Thus a sufficient supply of victuals could be obtained on the Pacific Coast for the use of the NWestern Divisions. -Previous to the construction of a lnule road across the summit, by which means fresh provisions, &e., could be carried over to the river Truando, from the same source as that at the mouth of the Atrato, namely: from the Provision M agazine at; Turbo, which Depot would be supplied from New-York, vie, Carthagena. As before stated, a steamer can make a trip to Townsend's Junction, friom Turbo, in twenty-hours; and from Tturbo to Carthagena in sixteen hours, even in the present condition of -the country. From my long experience, I am quite satisfied that colored labor is by far the most advantageous and preferable, as white men cannot perform the same amount of work in this country. Before concluding, I have much pleasure in statino that my assistants, Mr. Norman Rude, Dr. R. G. Jameson and AMr. Robert Nelson, rendered me most valuable assistance during this arduous undertaking. Having thus given you a full and detailed account of my journey, as well as my opinion of the practicability of the enterprise, and believing that it will sustain, and hoping that it may meet with, an impartial investigation, I have the honor to subscribe myself, Your obedient servant, WILLIAM KuENNTIS11, Chief YEnyFineer., Nw-YomRIC August Ith, 1855. 23 PANAMA, 25th Art1il, 1855. WM. KENNIS, EsoQ. DEAR SIR: As I have no doubt but that you will have arrived in the city of NewYork by this time, and be astonished that you have received no letter from me, I am sorry to say that, unfortunately, I have been detained in Jurador much longer than I either wished or anticipatedC, whlence I arrived here only yesterday, which will account for the delay. According to the instructions which you gave me wheln we parted at the falls of Truando, after iesting a few days at Paracucchihi, I proceeded to Jurador River, to examine it and the. Indian pat'n across the mnountains to the Salaqui River, which flows into the Atrato. Feb ruary 28, 1855.-At Alexandro's house the barometer stood at 29.38, and the thermometer at 76 deg., at seven o'clock, A. M.; and the rest of the day the barometer at 29.45, and thermometer at 81 dog. March 1. —Same place, at six o'clock, A. MI., the barometer stood at 29.46, thermometer at 78 deg.; and a-Lt noon barometer stood at 29.50, and thermometer at 85 deg. Mfarch 2.-At- six o'clock, A. MI., bavronmeter stood at 29.42,9 and the thermometer at 74 deg. At seven, A. M., accompanied by a guidcle and two Indians, I started up the river in a small canoe, at the rate of about a mile an hour. Current runs at froin tvo to three knots; course Nr. by NV. At 3 o'clock, P. M., arrived at Dos ]ocas (or the two mouths), so called from the junction of another river with the Jurador, of about the same size. Here we stopped for the night, hbaving traveled about eight miles by river, or six in a straioht line. B3arometer 29.4; thermnometer 82 deg. Six o'clock, P. t., barometer 29.41; thermometer 78 deg. /tfacrch 3.-Barometer 29.4; thermo meter 72 dleg. Started at sevenl, A. M., and traveled until three, P. Pa, wheil we arrived at a small river called Antado-general course N. by E.; distance twelve miles by rliver, or seven and one-half in a straiglht line. River much more -winding, and only about half the size it was the day before —mountains on each side. Barometer 29.3; thermometer 82 deeo. Six o'clock, P. M., barometer 29.25; thermoimmeter 80 deo. tarch 4.-Six, A. 1., barometer 29.2817; thermometer t75 deg.'he -iver Antado is sabout the saime size, and just such another river as the Hi-ingador, near the Nerqua. The bed is full of stones and rocks, and as it is too small for canoes, we had to abandon them, and travel on foot, which we did for one mile 2,425 feet, general course east, until ewe came to a smiall brook, up which we went 2,000 feet, course northerly, when we arrived at thoe road to Salacui. Barometer 29.22; thermometer 82 deg. WNe then ascended a higph and pretty steep mountain, for about one mile, which is the summit. Barometer 28.5; thermonmeter 82 deg. Traveled.along the ridge N. E., three miles or more, ~when we descended a quarter of a mile to a river called Mojando. Twelve o'clock M'. barometer 28.95; thermometer 84 deg. From Mojando to the Salaqui River (4 1-2 miles N. E.) is a perfect level, with scarce an elevation-in some places swvampy. At Salaqui barometer 28.95; thermometer 82 deg. 24 l~arch/ 5.-Six ocilock, A. M., barometer 28.92; thermometer 13 deg. Aftter the Indians had brought an old boat they had hidden somewhere in the river, we started dovwn alnd arrived at the rapids next clay about ten o'clock, A. M. —general course easterly; distance, in a straight line, about twelve miles. The Salaqui River, in everything, has the same appearance as the Truando. It has the samne depth, and runs throufh a beautiful valley like the Nerqua. Barometer 29.06; thernmomneter 85 deg. As the canoe was too large to dcrag down the rapids, we left it at tihe tIop, and walkei or crept down the side of the river for about three miles more, but did not see any fall, such as the great TfalHs on the Truando, and!lave been informed that there are none but rapiis. Haviong come to a part of the river that we could not pass writlhout a canoe, wve were obliged to return. Baro1mieter 29.1;'thermometer 82 deg. IThe mountains on each side of the rapids have the sanime appearance, and are of about the same heligohts as tose on the Truando; bult a- they recede at ain angle of about 25 to 40 de), i t hinik they could be cut down so as to n micake sufficient room for bothi canal anid river. Marchlch 11. —\Ve again arrived at A lexaudro's ho se. Thus T have given you. an account of my jurney to Salaqui, -it 1 l oservatioins, and leave you to Eorm your own opinion, havinl no d oubt lmt you will agree it Ah me in preferrin,g th-e-?erqeua rold beingc by uch the shortest and easiest. I inquired at Santiago about the sho-rt road that Ale-andiro said i'e kinew, but he protesteci that there vwas no sutilh ro'i], (SEigned ) RO'313r1' B iT S O,. 25 THE RIVERS JURADOR AND SALAQUI. Cour'ses and -Distances. Names of Places. i Course. Distance. oMiles. Feet. From Alexaundcro's house to Dos Bocas................ N. by WVr 8 Dos Bocas to river Antado...................... N. by E. 12 " River Antado to Summit....................... N.E. 1 2,425............................. N.. - 2,000 Ascent of Summit. 1 From Summit to Mojando.................. N. E. 3 1.320' Mojando to Salaqui............................E. N. E. 4 2,640 130 3,105 Descent of Salaqui to Rapids....................... E.;12..... ".below Rapids...................... E. 3.... 15.... THE RIVERS JURADOt AND SALAQUI. Baccometrical Observations. Place of Observation.. Day and Hour. Bar. Ther. Alexandro's House,............. Feb'y 28th, 7 A. lM., 29.380 760............. Rest of day, 29.450 81o................March 1st, 6 A. M1., 29.460 78' "; "............. 1.2 2M., 29.500 85o............ " 2d, 6( A. M., 29.425 74 Dos Bocas..................... " d, 7 A. M, 29.400 72: River Antado,.................... " 3 P. M, 29.300 2::: i.................. 6 P. L., 29.250 S 8; "' I wi............... 4th, 6 A.'M., 29.2 287 75 Road to Salaqui............... 8. M., 29.225 82 Summit,...................... 10 A. M., 28.500 82C Mojando,...................... " 12 M., 29.950 84C Salaqui........................ 3 P. M., 28.950 > 82-:'...................... 5th, 6 A. TM., 28.925 3:....................... 10 A. M., 29.06)0 85 -,..........................." 4 P. M., 29.100 82: (Signed,) ROBERT r ANELsoN. 4 26 THE INTER-OCEANIC AQUEDUCT. WM. KENNISE, Chief -Engineer. EXPLANATION OF PLATES. Plate 1-.-This Plate shows a section of the Inter-Oceanic River, from Kelley's Inlet on the Pacific, to the junction of the rivers Truando and Atrato. The distance and elevation of the tidal influence on the Mary River was measured, and the line of level sprung from that point, allowing for the fall of the tide (the level being taken at high water), from thence to Rancho No. 1, and on to Dos Bocas, without interruption, as shown on the Section and Plate 3; but meeting at the last-named point with a densely wooded valley-through which to cut a path to afford an opportunity to get a clear sight, would have consumed more time than could then be afforded-it was thought advisable to run a line of levels along a ridge of oblong hills (shown in Plate 3), nearly north-east and south-west, leaving a valley on either side-the valley on the right being the deepest. On this ridge of hills, represented by a dotted line from Dos Bocas, over the summit, is shown the height of leveling at each number; and the true profile of the proposed route was determined by offsets transverse to the general direction; the angles being taken, and a measurement by tape, from each reduced level to the bottom of the valley, as shown by the perpendicular dotted lines-the distance being calculated in the usual manner. At the Chupipi the level agreed with the barometer. (See Barometrical Observations.) From the summit to the river Nerqua is an abrupt descent; the angle of depression was taken, and the distance from the summit to the Nerqua measured accordingly. At Rancho No. 5 a series of barometrical observations were taken, and compared with the Chupipi, or Rancho No. 2, to endeavor to check the elevation; which two points were found to be on a level within a few feet. The distance and descent from Rancho No. 5 to the junction of the Truando with the Atrato, was ascertained from the different rates of current. (See Tables.) The red coloring, on Plate No. 1, shows the cutting to be made from the Pacific to the junction of the New River and Truando; the same color, shown at the bottom of the Truando, represents the dredging required to deepen that river to an uniform depth of thirty feet. Of the two lines represented on Plate 1, as running over the Truando, the black line shows the present surface of the river, and the red line the proposed surface, when deepened: on the bottom of the Truando, the black irregular line shows the present depth, and the straight red line the proposed depth. 2' The blue line passing from the Pacific to the Atrato, is the datum, or mean level line, of the two oceans. The height of the tide on the Pacific at that point is 12 ft. 6 in., that is to say, 6 ft. 3 in. above, and 6 ft. 3 in. below the mean level; which latter would be the 36 ft. 3 in. above the bottom of the canal at this point. The fall from the summit level to the Pacific would be, at low water, 15.2 feet plus 6.25 feet, and at high water, 15.2 feet minus 6.25 feet. The red perpendicular lines show the depth of cutting, divided into sections, and the black figures standing on an angle from the datum-line show the distances from the Pacific to each point indicated. It was thought advisable to recommend two tunnels in lieu of one, for the following reasons: the width of the tunnel must be equal to that of the river (200 feet), to prevent an increase in the current, and one arch sprung over this immense width would be too expansive to ensure safety; therefore two arches were substituted. This division will also prove advantageous to the transit, as it would preclude all danger of collision, by the ships observing the present law of navigation, viz.: that of keeping to the right. As to the heights of the proposed tunnels, they are quite sufficient to allow a line-of-battle-ship to pass through, with her top-mast and topgallant mast struck, and her yards braced to within the limit of the width of the vessel. Sailing frigates, and merchantmen generally, need only lower their top-mast, or slack it away a little, in the mast ropes. All steamers can pass through without altering any of their gear. By referring to the Table of Calculation for ascertaining the solid contents of matter to be removed in cutting the bed of the river, it will be seen that almost two-thirds is rock, which will form a permanent wall on either side, and preclude the necessity of forming an embankment of masonry, and at the sanme time save an immense quantity of cutting, as the sides of the river-bed need not exceed an angle of 30 deg. from the perpendicular, and the rock beinfg of a primitive formation, or trap, it will yield easily to the blast: at the same time rock is easier to be removed to the adjacent valleys than a softer material. There is sufficient water in this vicinity to erect hydraulic works, for hoisting rock and other material over the bankl. A height of from five hundred to six hundred feet of water can be obtained at each end of the tunnel; this, led through pipes to the canal, would work machines sufficient to perform any required operations. WILLIAM KiNNIShl, Chief -Enitneer. AUGUST 7, 1855. 28 A DESCRIPTION Of the proposed New 1iver Aqueduct, which is intended to flow from the lagoons of the river Atrato into the Pacific Ocean, thus forming an uninterrupted communication wvith the Atlantic Ocean, through which the largest ships may pass, and wi.th a current of not more than two miles per hour. The principles on which this desideratum is to be effected, are: First.-That the mean level tide of both oceans is the same. Second.-That the tidal wave at the mouth of the New River, on the Pacific shore, oscillates twelve feet six inches at spring tides, and ten feet eleven inches at neap tides; while at the mouth of the river Atrato (the' terminus of the passage on the Atlantic), the tidal wave does not exceed two feet at any phase of the moon. Third.-That the waters of the Atrato, at the points of junction with the New River, are fifteen feet, two-tenths, above the mean tidal level of either ocean. Fourth.-That the junction or summit of the New River, is, therefore, nine feet above the Pacific at the highest tide, and thus the water will flow down it with a velocity equal to that head; while at the lowest tide the velocity will be equal to twenty-one and forty-five hundredths feet head. (See Explanation of Section.) The length of the river Atrato from the proposed junction to its mouth, is sixty-one miles six hundred and sixty five yards, and that of the New River, sixty-three miles ten hundred and sixteen yards; their rate of current will, consequently, be nearly the same. The time and power, therefore, expended in ascending the Atrato will be compensated in descending the New River, and contra-wise; making it equal to sailing a distance of one hundred and twenty-fiv&e miles on a level surface. The summit formed by the Atrato and the head of the New River, being of the same height from the mean level of either ocean, the tidal influence of the Pacific will ascend the New River, nearly to the summit at every high water, and cause an irregularity in the current, whose average rate will be nearly equal to that of the Atrato, (two and a-half miles per hour.) As this river is intended to flow continually into the Pacific, without obstruction, so that vessels may at all times pass through, it may be necessary to state whence the source from which a sufficient supply of water is to be obtained. In the first place, it may be proper to point out the geographical position of the country. The Cordilleras of South America run parallel with the Pacific coast in the vicinity of the head waters of the Atrato, in a N. W. direction, toward the mouth of that river; and from these, springs another range of high hills, called the Antiochian Mountains, running in a N. E. direction. Between these two ranges of lofty mountains lies the vast alluvial valley of the Atrato, which river, during the lapse of ages, has formed for itself 29 a deep and spacious bed, running about midway between the hills, and for a distance of three hundred miles. The width of the Atrato Valley, opposite the proposed junction, is about fifty miles. This vast area may be said to be covered with water, with the exception of here and there a few islands, thrown up by the currents of the various smaller streams in their winding course to the great artery. The rivers flowing firom the Antiochian Mountains invariably preserve a north-west, and those from the Cordilleras a north-east course, pouring all their waters into the Atrato River, which, in its turn, overflowing its banks, inundates the surrounding country, forminug deep and widespread lagoons on either side. It is known as an established fact, that 4the clouds seldom pass over the Cordilleras, toward the Pacific, but are attracted by the mountains, and disgorge themselves on the Atlantic side; hence the reason of the perpetual rain, thunder, and lightning in the Atrato Valley, while on the Pacific coast there is scarcely any rain for eight months in the year-thus accounting for the absence of rivers on that coast, in this section of the country. (See Plate 6.) Froml the fact that the greater portion of this rain falls above the proposed junction, and is carried into the Atrat;o by upwards of fifteen large tributaries, besides numerous small streams, and also from the fact that these lagoons, or immense lakes, covering hundreds of acres, and maintaining an undiminished supply through all seasons of the year, are likewise above this level, it is sufficiently obvious that a superabundance of water may be constantly depended on. This most important point being established, it only remains to prove that the place selected on the Atrato is the most practicable for the purpose. In the first place, therc is no point of junction with this river, by others flowing from the Awest, so near the level of high water on the Pacific, as that of the Truando, which is just three feet above that line, and thus of sufficient height to prevent the Pacific, at high water, from flowing to the Atrato, and not so high as to cause a too rapid current through the New River at low water; in fact, just preserving a preponderating balance on the side of the former. Should either of the rivers Pocador or Napipi be selected, the forner being twenty-eight feet above the mean tidal level, and the latter thirty feet, and the rise and fall of the tide in Capica Bay being sixteen feet, the Pocador would, consequently, be thirty-six feet above low-water level, and twenty feet above high water, and the Napipi thirty-eight feet above low-water level, and twenty-two feet above high water. A canal therefore made in the vicinity of these rivers, -would have a tidal current of about five miles per hour. The Atrato, at the junction of the Salaqui, is only one foot above the level of high water on the Pacific; but the dividing ridge is one thousand and sixty-three feet high, and thirty miles in width, from the Jurador to the opposite side of the Cordilleras. (See Plate.) This line was partly run by myself, and afterwards finished by Mr. Robert Nelson, my assistant. (See Nelson's letter, annexed.) Again; should. any of the rivers at the mouth of the Atrato be selected, without reference to the height and width of the dividing ridge, I may observe, that the tidal wave on the Pacific is twenty-three feet at high water above the Atlantic, opposite the mouth of the Atrato, in a southwest direction, which would be in the vicinity of the river Sugra, or its tributaries, Maria, Balsa, Yarisa, &c., all emptying into the Gulf of San Miguel. The tide also rises from twenty-five to thirty feet at Chipagana, a small town situate eight or nine miles above the mouth of the river Savanna; while at the mouth of the Atrato, as before observed, the rise and fall are but two feet. Takincl the maximum of the tidal wave on the Pacific, then, to be twenty-five feet, and that on the Atlantic two feet, the tide at high water would flow from the Pacific to the Atrato, with a current equal to a head of eleven and one-half feet, and at low water on the Pacific the water would flow from the Atlantic with a current also equal to eleven and a-half feet. In other words, the Pacific would flow into the Atlantic for six hours, and the Atlantic into the Pacific for six hours. Notwithstanding the dividing ridge has never been explored, I have heard extraordinary stories frnom the natives concerning that region of the country. During- mny three visits to the Gulf of San Miguel and vicinity, I was told the San Bias Indians communicated with those of the Arquian territory, and that in an extraordinarily short time. But my opinion of this matter is, that all information derived from the natives is to be received with great caution: the truth or falsity of their assertions can only be proved by actual survey. Here I would mention, for general infbrrnation, that, in the so (lately) called Darien harbor, (an armnn of the sea, passing through Boca Grande and Boca Chica,) two small inlets from the Gulf of San Miguel, passing up the river Savanna for about twenty miles, and the Sugra as far as Yarisa, some twenty or thirty mniles, that the action of the tide is such on ships at anchor, that while I was on board of H. P. M.'s steamship Virago, Capt. Prevost, the first and only ship that ever entered that inlet, she dragged both anchors ahead, and was only'brought up by paying out nearly all the cable she hiad. There is scarcely a place within the two inlets above mentioned where a ship can anchor with safety, owing; to the action of the tide. WILLIAM KENNISI-, (C/7ie/f Engineer. AUGusT 7, 1855. THEORY Of the United Action of the Tide on the Pacific and the Summzit Level of the New River, at the Lagoons of the Atrato. This is a scientific problem that alone involves practical knowledge, inasmuch as there is no formula given by any writer on hydraulics, extant, to elucidate the required results. Therefore t~his most inportant subject must be treated firom analogieal inferences alone. The points to be demonstrated are these: —'Will the fresh water fromll the summit continue to flow toward the Pacific, at the top of high water, 81 with a velocity due to a head of nine feet-the height of that summit being nine feet above the high-water line on that coast l Although the tide on the Pacific has risen twelve feet six inches from the low-water mark, will the current in the river run with the velocity that a head of twenty-one feet would give it at low water? Or, will the salt water from the ocean, by the influx of the tide, maintain the lower regions of the river, in consequence of its superior gravity, and lift the fresh water, without materially commingling, (being of an inferior specific gravity,) to the height of the tides, without interfering with the current of the river more than the difference of the heads presented at the summit to the different stages of the flux and reflux of the tide on the Pacific? To answer the above queries, reference must be had to such natural rivers as are similarly situated with regard to the tide. London, on the Thames, is situated about fifty miles from the Nore, or'the mouth of that river. The tidal wave reaches London Bridge three hours and thirty minutes after passing Dover harbor, about seventy-two miles from London; from which fact it is evident that the tide, at the mnouth of the river, is half ebb when it is high water at London Bridge, and that, when it is low water at London Bridge, it is half flood at the Nore, or mouth of the river-thus preventing that current that would otherwise exist in the river at low water, should the tide begin to fall at London Bridge at the same time as it does at the Nore. But the tide in the Thames is acted on by two contrary ocean tides, viz.: that flowing southerly, along the eastern shores of Scotland, and that flowing northerly, through the Straits of Dover, which, meeting, send the flood up the Thames with great force. All tidal rivers more or less partake of these qualifications, according to the features of their adjacent shores; but, in the case of the proposed New River, it is materially altered, inasmuch as its bed is to be uniform in width and depth, from end to end; therefore, the current from the summit to the Pacific will (unobstructed by tortuous bends, which invariably exist in natural rivers) preserve a uniform flow, on known hydraulic principies, and at the same time admit the passage of the tide under the fresh water coming down the river, without antagonistic commotion either at the flood or ebb. The river will flow with a smooth current of about two miles per hour, and which, as far as theory can elucidate the tidal influence, will extend to the'Townsend Junction nearly. From thence to the summit the water will flow toward the Pacific nearly at the same rate of current as the Atrato to the Atlantic. That part of the river between Townsend Junction and the Pacific will be slightly agitated by the rise and fall of the tide, but the velocity of the current will be scarcely affected. As this portion of the country has never before been visited by a white man of any nation, mly route is here, doubtless, open to more minute exploration, and a more careful survey may suggest Humboldt's Bay as the Pacific terminus; in which case the only obstacles to be encountered in connecting the river with that, or the Corredor, are the expense of excavation from thence to Kelley's Inlet, and the crossing of the river Paracuchichi. As far, however, as hydraulic principles are concerned, I believe what I offer to be as true as instrumnents and scientific formula can effect it. As this is the grand basis upon which I have endeavored to raise my structure for accomplishing the object in view, viz.:-to join the two 32 great oceans by a never failing river, any small discrepancies in my given heights or distances, are obviously unimportant; for the difference of a few feet, more or less, in my elevation of the summit, of either ocean, could easily be met by a slight modification of the line, and would in no way prejudice the plan of connecting the twio great waters by a canal without locks. In my proofs of the practicability of this I allow of no discrepancy, the data being founded on that immutable law of nature, gravitation. WILLIAM KIENTNuSes, Chief ~a)gineer. NT w-Yoacu, August 7, 1855. }Onmitted on page 11, after the fifth paragraph.] The winds oil the PaeifiCe cotst are periodical, viz., blowing firo'r the south from Marehl to September, and foi'm the north firom September to March; and durcing the whole year it is calm f.om 6, P.M. -0 10, to. M.1 a fentle gale beginning at 101 A. M., which i:n-creases to a topgallant-sail breeze until noon, when it gradually dies away to a calim at 6, P. P`. Consequently, a vessel, once towed to as fair oling', can depend on.a breeze of four knots per hour fbr six hours during the twenty-four, which will bring the vessel into the general trade winds, clear of call head winds, in a few d ays. ER RATA. On page 6, fifth line fromil bottom, for " hatchets," read mrachietels. On page 8, on twenty-fifth line fromin top, for " it is possible,"' read, it; is'not possible. On page 9, on tenth line fiom top, for'" Leewasrdly," read Seat' wardly. 33 HEIGHT OF THE ATRATO AT ITS JUNCTION WITHE THE TRUANDO. The mean central current of the river is zabout 2.7 miles per hour, with a nmean hydraulic denpth of 53 feet, and the formu'la upon which the calculation is based is, that the square root of the mean hydraulic depth, multiplied by thlll in feet-will give the neal velocity of the current, in miles, per 7hour, under a deduction, according to the volueue of the stream, the directness of its course, and the nature of its banks. This course oil0 aeulation has been thought preferable to that of adopting any of the,mIore learned formulre, as there are now so many well ascertained facts relative to most of the chief rivers of the world, that the proper deduction can be ascertained with much precision. In Beardmore's tables of the -isc.enarge by water-courses of large area, the deduction is froml 1-9th'to 1-8th. In the case of the Nile, the iects are not entirely reliable, but, as far as they go, would give a deductiot oi a ot low water of 1-3d, and in flood of 1-6th. The Neva, at St. Pete-rsburgh, o -has a mean hydraulic depth, at a low state, of about 60 feet, and is, in many respects, simhnilar to the Atrato. The facts relative to it have been well established, and the greatest deduction which the observations give is 2-Sths. In the Ganges the deduction would be nearly -3d. In the English rivers the deduction is rarely above 1-5tlh: and that only at a low state, i. e., the greatest dceduction. And this refers to nearly all the large strecams. In applying the formula to the Atrato, and taking the observed current as the mean velocity of the water, the rise would be only 9 1-2 feet: the correction in this case becomes an addimtion, as the current is one of the data. After much calculation, and a ccareful consideration of many observations of the Atatoa, J have fixed the height at 15.2 feet. To apply the correction from the Neva, the height would be only 13 1-3d feet, and the corrections from any of the other rivers would make the height still less. WILLIAM KEN'NISH, Chief Engineer. 34 CALCULATION Of the discharye of the River Atrato, and the quantity of water required to saupply the proposed RIVER AQUEDUCT. RIVER ATRATO. Cross Section at Truando. Cross Section at 99 miles Section at Cano Barbacoa. 1,546 yds. on Longl. Section. Lengths, Depths, I Areas, Lengths, Depths, Areas, Lengths, Depths, Areas, Feet. Feet. Sq. Feet. Feet. Feet. Sq. Feet. Feet. Feet. Sq. Feet, 17 29 14 70 2j065 61 2,928 74 1,554 42 67 28 75 3,468 73 5,584 194 6838 50o2 86 42Y 128 E 6,656 124 10,974 108 4,536 53%' 91 41'' 150 8,137 123 11 808 119 5, 95 55'1101 471 110 6:215 223 22,634 96 4.584 58; 102' 48 168 9,408 94 9,306 224 10,192 54 9 96 43 211 10,233 97 8,584 196 7,840 43 81 7 24 2,867 80 5,400 136 4.148 34', 54 24 64 1,424 60 2,490 28 532 10 1 29 14 1,000 i j50,473 935 19,708 1,175 45,519 SUMIMARY. GRFATEST DEPT'IHS. AREAS. Feet. Sq. Feet. 58 50,473 102, 79,70( 48 45,519 208 j 175.700 The mean depth of the Atrato, from the Truando to its delta, being 78 feet:-if 208: 75,700:: 78 —=65,800 feet area, mean. SECTION OF THE ATRATO. The mean average surface current of the Atrato is 2.6 miles per hour, and the mean sectional velocity will therefore be 1.92 miles per hour, or 10,137 feet, which gives a discharge per hour of 667,014,600 cubic feet. RIVER AQUEDUCT. AT LOWV WATER. Fall,... 21.45 feet,} Fall petr mile, 0.382 feet. Length,. 56.08 miles, V P Sectional area, 5,000 sq. feet; mean hydraulic depth, 22.22 feet: hence surface velocity would be 2.549 miles per hour, and mean velocity 1.9 miles per hour, or 10,032 feet, giving a discharge of 50,160,000 feet per hour. AT HIGH WATER. Fall,.. 9 feet, Fall per mile, 0.16 feet. Length.. 56.08 miles, mile, 0.16 feet. During this state of the river aqueduct, the lower portions would be increased in sectional area; but as the upper part would remain nearly the same as at low water, the section there would give the ruling depth for discharge. The surface velocity would be equal to 1.7 miles per hour, and mean velocity, 6,864 feet, giving a discharge of 34,320,000 cubic feet per hour. The mean discharge of the river aqueduct, per hour, would be about 42,000,000 of cubic feet; and supposing the whole of this quantity had to be got from the bed of the Atrato, it would reduce the discharge of that river one-sixteenth, and the level of the surface of the water about three feet and three-quarters. But, in fact, the greater portion of the water required would be got from the lagoons, which at present chiefly ooze out in numerous channels into the deltas of the Atrato, and partly pass off by evaporation. The volume of water in the river aqueduct at high water, above that at low water, will be about 150,000,000 cubic feet; while the discharge, durinog the rise of the tide, would be about 250,000,000 of feet. CUTTINGS IN BED OF TRUANDO. Section K..... Mean of extreme sections taken for Soil Cuttings, and'greatest section of Rock by 1-3 the length for Rock Cutting. Greatest Cross Least Cross Diffcerence of Yertre ths, Section. Section. Bections. ceStre Deths i perfootof of Sections. difference. Sq. Yds. Sq. Yds. Sq. Yds. | Feet. Sq. Yds. Section L.. 860 745 115 16.5 7.' M *...1. 743 619 1.24 17.0 7.3 N...... 618 474 144 14.5 10. 0...... 419 269 150 13.5 11.1 ( 8................. TABLE OF DISTANCES, Fr om Zero, on Pacific Ocean, alon, linze of proposed Aqueduct. Distances Distances between f lon Stations. Zero.:Miles. Yds. Miles. Ydcs. From Zero to tidal influence,......... 2 0 2 0 T'idal influence to Rancho No. 1,.......1 440 3 440 Rancho No. 1 to Dos Bocas,................... 0 1000 3 1440 Dos Bocas to Rancho No. 2,.................. 1 970 5 650 Rancho No. 2 to Rancho No. 3,............. 26 888 1 7 1538' No. 3 to Chuperador,... 0 1257 8 1035 Chuperador to its Branch.................... 0 1360 9 635 Branch of Chuperador to Rancho No. 4,... 1 115 10 750 Rancho tNo. 4 to Rancho No. 5............... 1 880 11 1630 ll 1630 NOTE. —The above distances, taken by actual measuremlnent, correspond with those given in amy daily journal, with the exception of that from Rancho No. 4 to No. 5, the distance having ceased to be taken in my line of survey, as stated in the above joanrnal. After arriving at No. 5, the distance was measnred backward to I:ancho No. 4. LINE OF LEVELINGS, F,'om Ze7 o to the Summit. Heights of Measured Heeights in Distances leveled points depths fromI line of from along raidge i leveled pts. Section STATIONS. Zero. above da atm-! to line of aboave line. I Section. daturnmline. MIiles, Yds. t. ec Feet. dec. F eet. dec. 2 0 11.4 11.4 Tidal influence extends. 3 440' 222: 222 INo. 1 Rancho and No. 1 of points on 3 1440 48.0 20.0 28.0 Dos Bocas, No. 2. [ridge, 4 780 103. 53.0 50.4 No. 3. 4 1300i 128.5 5,5.0 73.5 No. 4 65 G 172. 79.0 93.8 No.2 R cho, No. 5. 6 160 232. 1 11.0 121.5 No. 6. 6 1520! 301.0 150.0 15 1.0 Io. 7. 7 680 43. 0 284.) 159.0 N2,'o. 8. 7 15383 386.0 222.0 14.0 No. 3 Rancho, No. 9. 8 1035; 458.0. 8.0 400.0 Rio Chuperador, No. 10. 9 635 528.0 75.0 453.0 Branch do. No. 11. 10 750 540.0 40.0 500.0 No. 4 Rancho iNo. 12, and sumnmit point of section. - ~ - - - - - - -- --''~ 37 RIO NERQUA,.Froim Ranchlo Vo. 5 to N'o. 6. STOPPAGES, RATE OF CURRENT, &C., &C. TIME. STOPPAGES. RATE oF CURRENET.! DEPTH. WIDTH. Honrs. Min. Mlinutes, Feet in seconds. Feet. Yards. 9.m15 5. 20 15 4 20 9.30 9.52 1i 20 45 18 10.2' 5 20 20 10.10 3 17 10.20 8 10.46 20 36 6 16 11.2 16 11.10 2 8 17 11.33 5 19 11.35 1 2 19 11.55 2! 6 20 12.13 9 20 1.23 25 1.535 I7. 21 2.30 23 3.25 5 4.0 48 6 16 9 i 22 Total time,..............405 minutes. " Stoppages,..........184 " Remaining time.......... 221 cc Mean current............75 feet per minute, gives whole distance 3 miles and 245 yards. RIVER NERQUA, lFrom rRancho No. 6 to confuence with Ti5ruando. TIME. STOPPAGE. RATE OF CURRENT. DEPTH. WIDTI. ----- i __- _ _______________________ Hours. min. Hours. min. Feet in seconds. Feet. Yards. 6.4-5 60 16 7.10 5 60 16 9 22 7.39 2 60 16 _ Mean current................ 225 feet per minute. Time,.................. 88 minutes. Stoppages,............. 7 " 81 X225 fr. =3 miles 795 -ds. RIVER TRUANDO. From confiuence to first Salto. TIME. RATE OF CURRENT. DE PTIT. PT WIDTH. Hours. min. I Hours, Mlin. Feet in seconds. Feet. Yards. 8.45 60 35 10 23 9.25 60 35 10.25 60 35 i 12 30 Mean current............. 100 feet per rinute. Time...100 minutes. 1 mile, 1573 yards. The distance from first Salto to Rancho No. 7 was ascertained by actual measurement to be two miles. From Rancho No. 7 to No. 8 was 2' miles. Whole distance front first Salto to Rancho No. 8, 4 n miles. 39 RIVER TRUANDO,.Iom Rancho N io. 8 to No. 9.']TrIME, RATE OF CURRENT, &C. Time. Stoppage. Depth. Width. lMean Rate of M 3ean Rate of Boat Current. through WVater. Hours. Min. Hours. Min. Feet. Yds. I Feet in Sec. Feet in See. 6.27 9 30 6.58 1 2 7.17 10 33 28 3. 28 3 7.35 32 8.5 i t 9.00 18 40 35 20 9.15 9.25 15 37 3-4 15 5 34 20 10.00. 10.6 10 40 28 15 28 15 10.7 U 10.27 8 18 45 2 10.52 9,' 11.15 15 44 28 15 18 15 12.25 a 55 12.52 24 39 I 1.15 2 1.30 5 K 22 10 18 15 1.50 20 U 2.10 6 2.33 10 J 2.50 16 15 2 3.10 2 18 3.15 5 40 3.25 25 3.48 26 4.10 15 41 22 10 1 8 15 5.00 18 I1 5.16 21 5.45 24 40 6.00 I 18 6.20 16 6.24 20 ~ T7.00 23 ji Time,............,.'753 minutes, Stoppages.......1..... 197 " Remaining time,........... 556 Mean current between Rancho iN~os. 8 and 9, 95 feet per mminute. Miean rate through water, 75 feet per minute. W5hole distance from Rancho No. 8 to No. 9, 17 miles 1,586 yards. 40 RIVER TRUANDO, From Rancho Nlo. 9 to Atrato.'IBME, RATE OF CURRENT, &C. Time. Stoppage. Depth. Width. MJean Rate of Rate of Boat Current. through Water. lours. Min. I Iours. Min. Feet. Yds. Feet in Sec. Feet in Sec. 6.10 18 41 24 15 7.00 16 30 10 t 18 15 7.40 22 40 26 15 22 15 7.45 14 20 15 18 15 8.40 15 38 20 i.5 16 ]15 9.15 16 30 15 26 15 10.40 20 32 15 16 15 11.45 18 40 22 15 16 1 12.15 21 20 15) 22 15 1.15 20 39 17 15 24 15 2.00 26 15 15 26 15 2.12 23 39 16 15 22 1 3.14.1 21 7 15 38 1) 4.00 26 39 Ii. 38 15 5.00 27 40 Time......... 10 h. 50 m. Stoppages,..... 15 m. _10 h. 35 m. X 1721x feet = 27 m.160 yds. MAean rate of current, 172}2 feet per minute..4... through water, 1721. feet per minute. RIVER ATRATO. TIME, RATE OF CURRENT, CALCULATED DISTANCES, &C. Time. Mean Depth. Calculated Distances Distances Current. Distances. from Truando. from Zero on Pacific. Hrs. Min. Ft. per min. In Feet. Miles. Yds. Miles. Yds. Miles. Yds. Stoppage, 6.30 58 63 1216 0 h. 45 m. 7.10 207 78 1 1011 1 1011 65 467 8.43 207 120 1 1566 3 817 67 273 9.20 253 66 1 1358 4 415 68 1631 Width, 10.30 245 54 3 620 8 1035 72 491 340 yds. 11.00 212 78 2 251 10 1286 74 742 1.00 233 78 4 1445 15 971 79 427 3.15 207 84 5 796 20 1717 84 1173 4.00 232 84 1 1743 22 1700 86 1156 4.30 306 66 1 318 24 258 87 1474 4.45 285 68 0 1232 24 1.490 88 946 Width, 5.00 212 I 66 0 1532 25 1266 89 718 400 yds. 6.00 201 1 75 3 420 28 1682 92 1138 9.00 169 102 7 408 36 330 99 1546 12.00 197 90 6 1525 43 95 106 1311 2.00 197 78 3 1491 46 1586 110 1042 7.00 197 69 11 354 58 180 121 1396 Width, 7.30 197 54 1 1068 59 1248 123 704 350 yds. 8.00 197 48 1 1068 61 556 125 12 To delta of Atrato....... 61 556 61 556 125 12 of Coquito........ Cano Coquito to Gul f of 892 Darien............... 2 000 6 TABLE OF BAROMETRICAL OBSERVATIONS. PLACE. DAY AND IIOUR.:BAR. 1Tnr~r,. DAY AND ttOUR.:BArn Tn~_-. RIEMAF, KS. Paracuchichi.......... JA~. ]5, 6 P.M. 29.350 78o J:t~. 16, 6 A.M. 29.300 8~ "......... " 17, 6A.M. 29.350 74o " 17, 6 I~.M. 29.300 0o "......... " 18, 6 " 29.350 75o " 18, 6 " 29.300 8o "......... " 19, 6 " 29.350 75o " 19, 6 " 29.300 8~ " ~........ " 20, 6 " 29.300 75o " 20, 6 " 29.300 8~ "......... " 21,10 " 29.350 78o " 21, 6 " 29.300 8~ " ~........ " 22, 6 " 29.350 76o " 22,10A.M. 29.400 6o "......... " 23, 6 " 29.400 76o " 23, 8 " 29.450 0o "......... " 24, 6 " 29.350 750 " 24, 8 " 29.370 4o "......... " 25, 6 " 29.350 74o " 25, 8 " 29.400 7o "......... " 26, 6 " 29.35 73o " 26, 8 " 29.400 0~ " ~......... " 27, 6 " 29.35 730 " 27, 8 " 29.4@0] 0o....31,1P.M. 29.410 80~ " 31,61~.M. 29.35,, 31, 4,, 29.385,,,, 29.385 ChupipiR. No. 2......,, 31, 4 " 29.115', 31, 6A.M. 29.150 Rancho [No. 3........ i~EB. 1, 8A.M. 28.600 Chupipi, 6 " 29.13 60 " [No. 4........ " 1,10 " 28.6501 ]qing Falls, top........ - 8,11 " 28.680 Heavy rains every afternoon, attended wilh bottom....,, I 8,11.15" 28.830 [Nerqua,..............,, 1, 6 " 29.225 80o [F~. 1, 10 A. i~. thunder and lightning. 29.300 80o Ranch 1~o. 5......... " 3, 6 " 29.225 75~ " 3, 4 P.M. 29.200 78~ " [No. 5......... " 4, 6 " 29.200 76~ " 4, 4 " 29.200 78~ " [No. 5.......... " 5, 6 " 29.150 760 " 5, 4 " 29.200 770,,.......,, [Netqua,?.:No. 5..... " iool 10, 6A.M. 29.200 74~ " 10,10 A.M. 29.154 [No. 5.....I " 11, 6 " 29.200/ 72o " 11, noon. " 29.172 820 [:No. 5..... 1 "!1, S1/~P.M 29.170i 75o " 11, 8~/~o A. 1~][. 29.250 S2o I)uring these days the mornings were cloudy, " No. 5.....I " 12, 5~ " 29.175 70~ " 12, 6}/0 " 29.200 720 and no rain fell day or night; apparently the " [No. 5,.....] " 12, 6 " 29.1751 72o " 12, 6 ~ " 29.175 71c ~erana was setting in. The observationsof TABLE OF BAROMETRICAL OBSERVATIONS.-CONTINUED. PLACE. DAY AND HOURI. BAR. TIIEE.I DAY AND HOUR. |BAM. TER.n REMARKS..,. _...,. ~ol. Nerqua R., No. 5,.... FEB. 13, 10 P. M. 29.200 notd FEB. 14, 6 A. M. 29.150 710 Mason's Hygrometer, taken nearly every day, No 5,.... " 14, 6 A. Ml[. 29.150 710o " 14, noon. 29.118 850 indicated a difference between the two therNo. 5.... 15, " 29.1251 70o 15, 1012A. M. 29,175 800 mometers of from 10o to 50, and in one inNo. 5,... " 15, noo00. 29.150 820 " 15, 9 P. M. 29.200 Not stance of 7~. 4 NO. 5... 16, 7 A.. 29.175 noti. " 16, 8 A.M. 29.200 Descending Nerqua,... " 16, 10 h. 20 ni. 29.300 88 " 16, 11 h. 20 m. 29.300 88~1 Ranch No. 6 " 16, 4 P. M. 29.200 17, 7"'A.M. 29.365 770 I Mouth of Nerqua. " Nerqua,...." 17, 7 A. M. 29.275 750 " 17, 8.13P.M. 29 300 850o Mouth of Nerqua,.... " 17, 8.45"c 29.345 85" Bottom of Rapids. First Truando Rapid.. 17, 10.45" 29.365 82~ 17, 12 h. 25 m. 29.375 Rancho No. 7,.. " 17, 3.30P.M. 29.225 84 " 17, 7 P. H. 29.225 78 Top of Main Fall.' No. 7." 1, 7.30A.M. 29.250 780 18, 10 A. M. 29.312 Measurement of rain fall by Aneroid. I Bottom of do. 18, 29.337 Truando Lower Rapid, "18, 3.55P.M. 29.275 IRancho No. 8,. 19, 6 A........ 29.250 " 19, 1.30. 29.265 No. 8,.. 19, 29.300Q 20 8 A. M. 29.300 No. 8,.........' 19, 8.4 P.M. 29.400 " 20, 8 " 29.3001 No. 8........ 20, 2 " 20, 6 P. M. 29.300 Atrato R., Sucio. " 22, 7 " 29.375 Qiibdo....... 16, 10 A.. 29.278 i80 MARCH 17, 10 A. H. 29.275 800i............ " 20, 10 " 29.324 800 " 21, 4 P. M. 29.175 85~......... " 31, 10 " 29.2751 790 APRIL 3, 10 A. M. 29.265 80o _ _. _~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ 44 TIDE TABLE-PARACUCHICHI. Time of HighlHeightof Day of Month. Water. Tide. Phases of the Moon. 1855. h. m. Ft. in. January 17, 3.30 A. M. 10 11 New moon, 17d. 20. " 19, 4.00 P. M. 1. 8 " 20, 6.30 " 12 6 " 21, 6.30 "!12 2 22, 7.15 " 11 9 Highest tide, three days after change. CALCULATED CUTTINGS, &C. SECTION A. From Kelley's Inlet to Rancho NVo. 1. ROCK CUTTING. SOIL. Length, Depth, Area of Cubic Contents, Breadth, Depth, Cubic Contents, X Section, Yards. | Ft. Sq. Yds. Cub. Yards. Ft. Ft. Cub. Yds. 33.596 210 10 3,190 2,075,095 735,194 37 705 215 10 2,200 1,754,500 525,800 447 890 215 10 3,829,595 I 1,260,994 Section A carried forward. SECTION B. Frfom Rancho NXo. 1 to Pancho NVo. 2. ROCK CUTTING. SOIL. _, j t 1 Depth Area of Length Depth. Const. Mean ]Whole Cubic Br'dth, D'pth Cubic 0c0.Sect'n. Br'dth. X Sect., Contents, Contents, ds. Ft. Ft. Ft. Sq. Yds. Cub. Yds. Ft. Ft. Cub. Yds. e _.d.49 49 200'/ 950 a); P 1,o000" \1,022,500 213 8 189,333 C) 5 5 Y2 1 0'2 201 1,095 2, 730! 5,084,625 227 8 548,851 cc,-' 121 76 20912 2,630 __ v _ _i 7 6,107,125 738,184 Section B carriedforward. 45 SECTION C. Front Rancho N.o. 2 to Miouth of Tunnel. ROC1K CUTTING. SOIL. Depthl Area of!'Length Depth, Const. Mean Whole I Cubic Br'dth, D'pth Cubic Sect'n, Br'dth, X Sect.,' Contents. Contents, Yds. Ft. Ft. Ft. Sq. Yds. Cub. Yds. Ft. Cub. Yds. 1241 80 210 2,712 1,280 3,897,600 228 62,134 151/ 107 213 3,37 12134 ~ 1 407, 1,374,846 236 5 53317 151 107 _13 3, 378.t z 1l 974 1 3,650,069 239 5 129,321 =~; 180i 136 216Y/ 4,117 - 1,747 7,487,642 244 5 235,845 v i 193! 149 218 4,455 _________i____ _ _______ l 16,410,157 580,617 Section C carried forward. SECTION D. TUNNEL. Central Section- One Tunnel. Feet. Areas, Ft. 78X92.9X30 2,561 Low Water Section. 2 92.9"X12.4 1,144 To Level of Roadway. 39.9X102.9 4,084 To Radii of Arch. Arch Radii: 63' 6" L 128~20 4,522 9. 12,311 1,368 Sq. Yards 6,4170 Yds. = 8,850,960 Or in both Tunnels........... 17,701,920 Section D carriedforward. 46 SECTION E. From Rancho NVo. 5 to ilouth of Tunnel. ROCKI CUTTING. SOIL. Depth Area of Length,I Depth, Constant Mean Whole Cubic [Br'dth, D'pth Cubic Section, Breadth, X Section, Contents. Contents, Yds. Ft. Ft. Ft. Sq. Yds. Cub. Yds. Ft. Ft. Cub. Yds. 233 19114 224 5,560 662 I 2,757,230 Nil. Nil., 126 8414 210ot 2,770 Constant Section, 800 yards. Depth, 4134 feet. Section E carried forward. SECTION F. From Rancho NYo. 5 to Rancho No. 6. ROCK CUTTING. SOIL. Depth Area of i Length, Depth, Constant Mean Whole Cubic Br'dth, D'pth Cubic Section, BBreadth, Section, Contents, Contents, ~-ds. Ft Et. Ft. Sq. Yds. Cub. Yds.. Ft. Cub. Yds. - 126 8 412 210', 2,771 - 5,525 1 I 2 14,845,675 232 17 1996,952 119 77, 210 i 2,6033 8 Constant Section, 795 yards. Depth, 41. feet. Section F carried forward. SECTION G. From -Rancho NVo. 6 to confutence of Nertqua and Truando. ROCK CUTTING. SOIL. Depth Area of Length, Depth. Constant MIean Whole Cubic Br'dth, D'pth Cubic Section, Breadth, X Section, Contents, Contents, iYds. Ft. Ft. Ft. Sq. Yds. Cub. Yds. Ft. IFt. Cub. Yds. 119 79 210 2,608 6,07- i 5 1,5,324,1871 232 8 1,252,800 Constant Section, 765 yards. Depth, 40 feet. Section G cartried forwvard. 47 SECTION HI. From the confluence of Rios NVerqua and Truando to 1st Salto. ROCK CUTTING. SOIL. Depth Area of Length, Depth, Constant Average Whole X Cubic Br'dth, Depth. Cubic Section, Breadth, Section, Contents, Contents, Yds. Ft. Ft.t.. Ft. Yds. Cub. Yds. Ft. Ft. Cub. Yds. 112 73 209 2,440 3,333 18,015,865 230 7 596,607 109 70 209 2,370 Section H carried forward. SECTION I. From 1st Salto to Rancho No. 8. ROCK CUTTING. SOIL. Depth Area of Length. Depth. Constant Average Whole X Cubic Breadth. Depth. Cubic Section. Breadth. Section. Contents. Contents ids. Ft. Ft. Ft. Sq. Yds. Cubic Yds. Ft. Ft. Cub.Yds. 122 84 21osL 2,689 1,130i 2,957,210 Nil. 116 78 210 2,545 1,716 1!3,851,52 Nil. 91 53 207 1,944 3,410' I 5,865,200 Nil.! 72 i4:- 204 1,496 1,645 1 2,048,025 Nil. 50 12 202 994 __ __' 1 14,721,997 Section I carriedforward. SECTION K. From Rancho NXo. 8. Depths. Section. Mean Section. Quantity. Lengths. Alluviall Rock. Alluvian Rock. Alluvian Rock. Alluvian. Rock. Yds. Ft. Ft. Sq. Yds. Sq. Yd. Sq. Yds.Sq. Yds. Cubic Yds. Cubic Yds. 1,416 776 1,098,816 4,248 564 2,395,872 Section K carriedforward. 48 SECTION L. Lengths. Depths. Section. Mean Section. Quantity. Alluvian Rock. Allauvian Rock. Alluvian Rock. Alluvian. Rock. Yds. \ Ft. Ft. Sq. Yds. Sq. Yds. Sq. Yds. Sq. Yds. Cubic Ydq. Cubic Yds. 29 815 1,9705 1 89 822 1,619,340 31 829 3,266 844:2 2,758,137 ~35~ 860 1,550 829 1,284,950 26' 798 1,290 805 1,038,450 28' 812 3,085 7781/ 2,401,672 19 745 1,812 790 6 1,432,386 32 836 10,534,935 Section L carriedforward. SECTION M. To Rancho lVo. 9,. Length. Depths Section. Mean Section Quantity. Alluvian Rock. Alluvian Rock. Alluvian Rock. Alluvian. Rock. Yds. Ft. Sq. Yds. Sq. Yds. Sq. Yds. Sq. Yds. Cubic Yds. Cubic Yds. 2,11-2 749 1,582,944 2 2714 710 396' 697 276,012 625 21 6 673 420,625 21 662 1,312 25 678Y 890,192 695 2,580 684 1,764,720 22i2 673 978 661/ 646,947 19-4 650 1,772 6349 1,124,334 15 619 920 639 587,880 ],208 6 664' 802,716 22 670 250 655'2 163,875 1'SY2 641 2,089, 605' 1,26L4,889 Section 11 carried forward. 49 SECTION N. To Summit Level. Depths. Section. Mean Section. Quantity. Length. Ant' Illuviani Rock. Alluvian Rock. Allanj Pock. Alluvian, Rock. _Yds. ds. Sq. Y ds.AB Sq. Yds. Cubic Yds. Cubic Yds. 4,630 57919 2,683,085 20~ V589 2,325 14 524 i. 1,293,862 14 524 308 5 611,' 17 2,942 599 2,825 2 593k9 1,675,225 2,142' 619 603 1,291,626 t23 9 619 6,530 1 556~/2 3,633,945 11 _ 494 3,3341 1 04 ) 499 1,663,666 12 504 1,205 452 544,660 9 400 -jj L.- __ __ __ _ __ __ _ ___ _ __ 1 12,959,011 Section N ca'~rried forward. SECTION O. To Atrato. Depths. Section. - Mean Section Q uantity. Length. Alluvian Rock. Alluvianl Rock. AlluvianI Rock. Alluvian. RPock. Yds. Ft. Ftt. Sq. Yds. Sq. Yds. Sq. Yds.i Sq. Yds. Cubic Yds. Cubic Yds. 9 400 2,560 390 998,400 10 380 2,350 34614 814,275 4 313 650 330 214,500 7 3417 2,920 358 1,045,360 9 369 1,800 13 394 709,200 13'2 ~ 419 2,464 344 847,616 0 269 484 294 142,290 319 t__ __ _ _ _ _ _ __ _ _ _ __ _ _ _ 4,771,64 7 Section 0 carried forwcard. 7 50 RECAPITULATION. ALLUVIAN. ROCK. TOTAL. Section A.................... 1,260,994 3,829,595 5,090,589 " B.................... 738,184 6,107,125 6,845,309 " C..580,617 16,410,157 16,990,774 Extra Cutting mouth of Tunnel, 1 62,460 62,460 Tunnel........................ 17,701,920 17,701,920 Extra Cutting of Tunnel,........ 73,260 1 73,260 Section E..................... 2,757,230 2,757,230 F" F,.................... 996,952 1 14,845,675 15,842,627 " G.................... 1,252,800 15,324,187 16,576,987,................. 596,60 8,015,865 8,612,472 I,.. 14,721,997 14,721,997 ".... 2,395,872 1,098,816 3,494,688 L,.................... 10,534,935 10,534,935 " M,............. 9,525,134- 9,525,13.4 N................... 12,959,011 12,959,011 O,................ 4,771,647 4,771,647 45,612,753 100,948,287 146,561,040 WILLIAM KEPNNISH, Chief ]Eqfineeff. Translation of a paper by a celebrated New Granadian engzineer, given by his Excellency Nicomedes Conto, Governor of the province of Choco, to iMr. Kennishl:Quibd6 is situated in latitude 50 36' 42" T., longitude 2~ 39' 16," W., of the -meridian of Bogota, at an altitude of 42.8 metres above the level of the sea. Mean temperature 29~ of the Centigrade; the maximum of heat 32~, minimum 26~. The hydrometer of Saure makes the average humidity of the atmosphere 95~. From 90 to 100 inches of rain fall annually. The sea is distant, in a straight line, 145 maritime miles, or say 50 Granadian leagues, that is, from the extreme point of the Gulf of Uraba to the Bay of Candelaria, 55 leagues. The length of the river Atrato, from Quibd6 to the Bay of Candelaria, is 91 leagues. DISTANCES. 1 2 leagues to Bete. 59 leagues to Murind6. 20 " Bebard. 98 " Turb6. 37' Tebada. 10 " Llor6. 38 " Fuerte MIurrf. 19' San Pablo. 42 " Mouth of Capica. The highest part of the Isthmus of San Pablo has an elevation of 100.3 metres. Height of Tambo on Santa Helena, looking to the north, is 71.4 rmetres (the metre is 39 English inches.) Height of San Pablo, looking to the south, 60.7 metres. Width of Isthmus of San Pablo, 1 league, 1,000 varas. Llor6 lies in latitude 4~ 22' 40" north, longitude 2~ 34' 22" west of Bogotaf, at an elevation of 69.1 metres above the level of the sea. Urrao is situated almost due north of Quibd6; and the ravine or passage, between Farrallones and Cerro Platiado, is almost in a line with Quibd6. From Quibd6, a good road could be made, by following the line running from the head of Cabl to the Capon Hill, crossing the river Bebaramd at its sources, in order to strike the road from the heads of Titiribi. 51 CONFIRMATORY REPORT OF E. W. SERRELL, ESQ., CONSULTING ENGINEER. NEW-YORK, 23d August, 1855. TO FREDERICK M. KELLEY, ESQ., OF NEW-YORK. DEAR SIR: Agreeablyr to your request, I have examlined with great care the general subject of connecting the Atlantic and Pacific Oceans, by means of water communication within the tropics; more particularly, however, upon the routes that have been surveyed, at your instance, during the past four years. The task has been undertak1en while appreciating its magnitude, and acknowledging an inability to master it properly. Vast as the enterprise is, bearing directly or indirectly upon the political, commercial, social and moral relations of the civilized world-destined, when accomplished, to reduce space, by shortening the time of transit to and fiom the ends of the earth-the field of research, however, occupies comparatively a limited extent. The excessive colds of the high northern latitudes, causing the uninterrupted presence of great masses of ice, together with the ever prevailing storms of a southern passage, long ago directed men's minds to a route through a more genial region. Thus, for more than three centuries, almost superhuman exertions have been made by the best and most enlightened in their generation, to track out a path through the dividing slopes which separate the two great valleys of our planet. Since the configuration, geographically, of the Western Continent has been known, but little reflection was required to determine that any water communication that should be established artificially, must be made within the parallels of 3 deg. south, and 20 deg. north latitude. Within these limits many positions, at various times, have been indicated for making the desired connection. The most prominent points, however, are as follows:-'ehucontelpec -Route. Commencing at the north with the route via. Tehuantepec, upon which, although it never was seriously contemplated to connect the oceans at this point by water, many very interesting explorations and surveys have been made, one of which is recorded by J. J. Williams, Esq., Principal Assistant Engineer to Major J. G. Barnard, who conducted an examination for the Tehuantepec R. R. Co., of New Orleans. 52 These explorations were very ably managed, and a vast amount of information was collected respecting the topography, geology, climate, local geography, productive industry, furnia and flora of the region. The distance from ocean to ocean, by this route-from the sea near Tehuantepec, on the Pacific side, to Coatazacoalcos, on the Atlantic-is 186 miles. The summit at Nisi Correjor pass, is 865 feet high, and the general configuration of the country is a great gradual slope from either side towards the centre. The summit is more towards the Pacific side, than central. No water exists in sufficient quantities, at the requisite level, to render this route at all practicable for a canal by lockages, and the enormous depth and length of any prism that could be formed by a thorough cut, precludes the possibility, commercially, of such an undertaking. It is proper to remark that, although the explorations elicited other important and valuable information, they were undertaken with reference to a railway, and not water communication. The direction of this route is nearly a south course from the Bay of Vera Cruz to the Pacific. The latitude is between 16 1-2 deg. and 18 1-2 deg. north, and the longitude is about 21 deg. west of Washington. Many other surveys have been made over this Isthmus; that of Senor Moro justly deserves consideration-the essential features, however, are all given by Mr. Williams. Honduras Route. The Honduras Route, explored under the direction of E. G. Squiers, Esq., in the year 1853, lies eastward of the Peninsulas of Yucatan and Balize. The direction of this line is also nearly south. It commences at Puerto Cabello, in the Caribbean Sea, and terminates at the Bay of Fonseca on the Pacific. The length of the route is one hundred and sixty statute miles. It lies wholly within the State of Honduras. Here the valleys of the Humuya and Goascoran and the plain of Comayagua constitute a transverse depression from sea to sea, through the mountain range of the Cordilleras. Here, also, as with the Tehuantepec route, however favorable the line may be for railway connection, it is utterly impracticable for adequate lockage for an inter-oceanic transit by canal. Although the waters of the Rio Humuya, Rio Ulua, and Rio Goascoran interlock, and even pass by each other several miles on their course, from the interior to the great oceans, in either direction, the necessary summit water does not exist, by which lockages could be formed for a trade of any considerable extent. The summit on this line, ascertained by the sum and length of the gradients given by Mr. Squiers, is 2,681 feet in elevation above the two oceans, and it is situated, topographically, somewhat similar to that on the Tehuantepec, that is, south-westward of the centre. The latitude and longitude of this line, as determined by Mr. Squiers, is as follows: Puerto Cabello, latitude 15 deg. 49 min. N., and long. 87 deg. 57 min. west of Greenwich; Bay of Fonseca, on the Pacific, 13 deg. 21 min. N., and long. 87 deg. 35 min. west of Greenwich. 58 Good harbors are said to exist at the termini of both these routes, preference being given to one or the other, by different writers. The next important line of communication between the two oceans, occurs by way of the Lake Nicaragua. Several very trustworthy surveys have, at various times, been made of this route, undertaken at the instance of different or the same interests. The description of it here given is obtained from Col. Childs' Report, made to the American, Atlantic and Pacific Ship Canal Company, in the year 1852. This line commences in the Bay of San Juan de Nicaragua, on the Atlantic, in lat. 11 deg. N., and long. 83 deg. 45 min. west of Greenwich, and runs in a north-westerly direction across the Continent. Starting at the harbor of San Juan de Nicaragua, near the village of San Juan, or Greytown, it crosses several lagoons, and entering the valley of the river San Juan de N7icaragua, crosses the river at Juanillo, and ascending either in the bed of the stream, through slack-water navigation, produced by locks and dams, or by open cuts, through an independent prism, it was proposed to reach the summi-t by fourteen lockages, in a distance of one hundred and nineteen miles. This summit level is the Lake Nicaragua, and the surface, at ordinary stages of water, is 105.24 feet above low tide in the Atlantic. From the Lake Nicaragua, after cutting tThrough a considerable ridge, the descent was proposed to be made to the Pacific at Brito, by another flight of fourteen locks, in a little over nine miles. The entire length of this route, from the Atlantic to the Pacific, is as follows:-from the harbor of San Juan de Nicaraoua to Port San Carlos, one hundred and nineteen miles; from San Carlos to Rio de Lajas, fifty-six and one-half miles; fioln Rio de Lajas to Brito, eighteen and one-half miles-making the whole distance one hundred and ninetyfour miles. This transit, for rnany years, lhas been considered very desirable, in consequence of the abundant supply of water on the summit, in the Lake Nicaragua. Col. Childs, in his Report, suggested a canal having- a prism fifty feet wide in the bottom, seventy-eight feet in the top, in rock cuttings, and one hundred and eighteen feet wide, in earth cuttings and lines of embankment, and having seventeen feet depth of water the entire distance from ocean to ocean. It was proposed that the locks should be two hundred and fifty feet long, and sixty feet wide-averacge lift of lock, eight feet. An artificial harbor of thirty-three acres was contemplated, at the Pacific, seventeen feet deep at low tide, and formed almost entirely by excavation in solid material, at the mouth of the Rio Grande. Although comparatively of such small dimensions, and being intended for the transit of but one vessel at a time, except at the turn-outs, and that vessel only drawing less than seventeen feet of water, the estimated cost of this work, as computed by Col. Childs and his assistants, Messrs. Fay and Richmond, was thirty-one million, five hundred and thirtyeight thousand, three hundred and nineteen dollars and fifty-five cents. ($31,538,319 55c.) Mr. James Walker and Col. Ed. Aldrich, English engineers of eminence, who were designated by the British Government, at the request of the 54 parties in interest, in the main, corroborated the views as expressed by Col. Childs, in respect to the cost of the work. The ability of this work, as proposed by Col. Childs, having. such a depth of water, width of prism, width and length of lock-chamber, &c., to accom'modate that portion of the trade of the world, for which any inter-oceanic canal might be intended, is hereafter referred to. South-east of Nicaragua is the celebrated route of the Isthmus of Panama. This line for ages was the favorite transit between the oceans; and having been known to Pizarro and Cortes, became afterwards the highway of the buccaneers. For the seventy years preceding the discovery of gold in the playas of California, at the close of the war between Mexico and the United St-ates, it occupied almost exclusively all the attention that the civilized nations of the world devoted to an inter-oceanic junction. Expeditions were fitted out at various times by the Spanish, French, English, Dutch, and Portuguese governments, to explore this wonderful and then almost fabulous region. The most reliable and important of these expedit-ions were conducted, on the part of t-he Frenchi by iapoleon Garila wi'Nth a corps of sappers and iminers, and by Major Lloyd, an eminent English engineer. The former of these gentlemen made a very elaborate report on the subjeut, contemplating a connection by railway and canal; and a grant was obtained from the New Gmranadian Governmennt, authorizing the construction of a workl of either character, and nxilgo the time for its commencement within a limited period. The very great estiLmatled cost, ho-wever, put upon this worlk precluded its adoption in i tl ehe forin, as contemplated by M. Gariila, and the period fixed for its commencement went by'wi'hou ainyh'in'; being done. Major Lloyd's triangulations and hydrog'aphical observations added a great deal of infoirmation upon this interesting subject, and won for himself lasting renown; but it was not ultil our own lamented Stephens, (returning from the travels in Central Ameriic, Chiapas and Yucatan, which filled the world with his name,) entedred boldly and determinedly upon the project of connecting the bay of Panama with a point near the mouth of the Chagres River by iron rail. Some observations, made by James L. Baldwin, Esq., at Mr. Stephens' instance, settled a disputed point in reference to the gradients on the Pacific slope; and an expedition was fitted out in 1848, by a company of New-York mlerchants, of which \Win. d-i. Aspinwall, Esq., took an active and prominent part, to attempt a location for a railroad. This expedition was headed by Brevet Lieut. Col. Geo. G. Hughes, U. S. Topographical Engineer. Messrs. mnm. H. Sidweil, ~rm.cNorris, Lloyd Tilman, Edward A. Serrell, James L. BEaldwin, John May and J. J. Williams, conducted the surveys; and a location was made, upon which general line the present Panama Railroad has since been constructed, under the direction of Colonel Totten and.Mr. John C. rrautivine of Philadelphia, as principal engineers. The length of this route, from th"e city of Aspinwall, on Manzanilla Island, in the bay of Limon, on the Atlantic, to the city of Panama, on the Pacific, is forty-seven and a half miles. Commencing at the Atlantic, passing inland, the line traverses a swampy region, on either side of the Gatun River, which it crosses; thence follow 55 ing the base of the ridge Boho Soldado, in the valley of the Chagres, which latter it crosses a few miles below Gorgona; thence takes the high ground, through the valley of the Rio Obispo, it reaches the summit at an elevation of two hundred and fifty-seven feet; thence descending in the valley of the Rio Grandce, crossing several unimportant streams, it enters Panat ala. The very considerable length through the base of the water-shed of this country, together with the fcet that no adequate sources exist for the supply of a summit level and lockages, if contemplated, must for ever preclude the possibility of connecting the two oceans at this point by water communication, artificially, though a worlk of commercial value, notwithstanding the very great facilities that exist for maintaining a railway. South of Panama, a great many explorations and surveys have been made. Besides those conducted by Col. Hughes in the country of the San Blas or Mandingo Indians, Dr. Cullen, Mr. Gisborne, Capt. Prevost, of H. Al. S. S. Virago, Mr. Kennish, Lieut. Strain, U. s. N. 0Col Codazzi, Capt. Joureiguiberry, and others at the head of private expeditions, or parties sent out by the governments of Newv Granadla 9 France, England arid the United States, whose researches, from tilme to time, have been made public, have thrown more or less light upon the possibility of connecting the two oceans by water communication tfh ough the territory lying between -the Atrato River and the Panama Railroad. These researches have demonstrated that the Sieiras Lloranas, or coast range on the Atlantic, extends from the westward of the gulf of San Blas, in longitude about 79 deg. 30 min. west of Green-wich, in an unbroken chain, to the Gulf of Uraba, or Darien. It has been thonught that depressions existed in the range, through which an open cut, without locks, from ocean to ocean, might be made; but to this time nothimnn of lhe sort has been shown to be practicable. On the contrary, the exopedition under Commander Prevost, which ascended the valley of the Savana, in 1853, from the Pacific, from the Gulf of San Miguel, in the hope of reaching a very low pass to the Atlantic, after attaining an altitude which they estimated at about twelve hundred feet, and discovering no indications which confirmed them in the belief that they had reached the summnit, turned back to the Pacific. Similar attempts were made about the same time by the parties headed by Colonel Codazzi and Captain Joureiguiberry, from the Atlantic coast at various points, and resulted equally unsatisfactorily. The expedition headed by the brave, though unfortunate, Lieut. Strain, U. S. N., after traversing the valleys of the Savana and Chucunaqlue for several weeks, terminated fatally to a number of his party, but without demonstratinSg even the probability of the existence of any passes through which the desired communication could be made. It may, therefore, be concluded that it is not within the limits of probability that a feasible line should be found, between the most westerly mouth of the Atrato River and Porto Bello, notwithstanding the comparative narrowness of the Isthmus. Entering the broad valley of the Atrato on the 77th degree of west longitude, a new neld of research is presented. It is to this region that particular attention is now directed. South of this point, although the valley of the Magdalena, the lake 56 Maracaybo, the Orinoco, and the great Amazon, all occur within 10 deg. of latitude, all of which, with the exception of the lake Maracaybo, cross transversely, very nearly, the entire northern portion of the Continent of South America-and some of them, with their head waters, are navigable more than nineteen-twentieths of the distance which separates the two oceans-yet the Cordillera range presents an impassable barrier. Upon this range occur some of the highest summits of the globe. The Atrato River, designated, nearly half a century ago, by the great Humboldt, as one of the'most probable routes by which to connect the two oceans, has been very minutely explored. Upon it, and the river San Juan, Mr. John C. Trautwine made an elaborate examination, and set forth the result of his labors, in a report made to Messrs. Belknap, James, and other gentlemen, in November, 1852. He has also published more detailed statements of these explorations, which were made with direct reference to an inter-oceanic canal, in the Journal of the Franklin Institute, of Philadelphia. James C. Lane, Esq., of N1ew-York, also made very extended explorations, in the years 1853-4, from the mouths of the Atrato to the isthmus of San Pablo, near the head waters of the Rio San Juan, including the tributaries of the Atrato; as did also Capt. Wfilliam Kennish about the same time, and subsequently at your instance, whose labors are hereafter more fully referred to. These gentlemen, with their assistants, among whom were Dr. HEalstead, Mr. Brown, Capt. Rude, and Mr. Nelson, agree in the general features of the district which they passed over. The Atrato River empties into the Gulf of Darien, by nine mouths, called by the inhabitants of the country'" Bocas," and named as follows: Tarena, Candelaria, Pabo, Matuntubo, Coquito, Coco-Grande, Pantana, Uraba, and Leon. Navigation into these mouths is impeded by sand-bars, and about ifeet of water, at low tide, is all that is usually found in the deepest, while some are dry. Within the bars the water deepens suddenly, which is also the case seaward; and sixteen to eighteen fathoms of water is found at a comparatively short distance from the shore. The harbor is represented as safe, and accessible in all weathers. The several streams which form the mouths of the Atrato, are called Cafios. They vary in depth; but the Caro Coquito and Barbacoas, which form a cross connection with the other mouths, have a depth of thirty feet within about two miles, or less, from the ocean. From the Carfos, seventy miles up the river, the least depth of water is represented at forty-seven feet. Above this point to Quibdo, a distance of two hundred and twenty miles from the mouth of the Atrato, the least depth of water is from eight to ten feet, according to. the seasons. The entire length of the Atrato is over three hundred miles, following the sinuosities of the river. Above the Caros it varies in width, from one-quarter of a mile to a mile and a-half, and even two miles in some places, for sixty-five or seventy miles. Above this point, to Quibdo, its least width is from five hundred to nine hundred feet; while a greater part of the way it is broader, with the exception of one narrow pass, a few miles below Quibdo. The valley of the Atrato is nearly 3~ in length, or about 170 miles, and varies in width from 1~ to 1 1-2g. The entire formation of the bottoml oi' the valley is a great alluvial plain, The banks of thle river are in no case high. They are generally levees, formed from -the sedimnieitar deposit broughlt down by the current, and precipitated. The banks of the tributaries, in many instances, from the continuation of this process through loio' periodos of years, have raised considerably above the surrounding country, and, in some cases, the surface of the water is above t-he l-and on eothenr side. This is said to be true of somne portions of the Pocoedor, Napipi, Boiaya, Sucio, Truando, and the Leon. In the vicinity of the. iCranco and Sucio, 7wlah were'both ascended and explored by Ir. eae nii CaQtcaini is-nnish in detail, vast lagoons, or plains covered with water anl trees were discovered. These lagoons, in many places, are f-on exwentyv to one hlundred fd eet deep of water, with mud of unkno-win depth in the booi;. A dense overshado'wing' foreist of enorrmrous trees, of very gfreat variety, is saidc to cover the wihole communtTry. -lnder1ibrush aind impenetrable thickets are said to aboundi. o erok or saone of aiy kindl excepti1ng' small detached, water-worn plebbles, iias'been discovered in any of the bottonm lands of the Atraora Thoe soil, holwever, is auriferous, and produces gold and platinum, which is -rashed in. smcall quantities by the natives. Coal mines are said to exist ii tibe initiochian rauie, ew hich forms the eastern slope. No cuitVvaiioni or bu1Lt ti'tle, has been attempted. Theare is but little current in the.tauiateo ldiriver It is said never to exceed two and. a-ha1lf ilies "er mio.-,;11- ny1 paiit of it', below thle comlune:ce of the Napipi. The elevationL or tule rivaer a' Lthe m blouth of thoe Trand1iiuo, h -ich is sixtythree miles froul tile Atl2ant is a o- fifteen fe6 oGr f~rom fifteen -to seventeen feet,above eallv-n ]e-el ) ie o (i t. t aries incoisiderably at a1y season of the yea': one and one-half: set is te. freatest range recorded by any of the explorers hebre reflc-Pl elr. t'. Froml the Truando to the Napipi, tlhe ascent in the river is lnot quite so gradual as lower down, ie aioutlh of the Napipi beineg fronm 42 to 45 feet in elevation bove thOe lrou.ti of nhe Atirato. The river at (Quibdo, uwo hundred and twenty rmiles fromn the Atlantic, is represented at severity-five tfeet aOve the oceans. Rain falls iii g'reat labunda-nce thlroug'lout the wVhole vralley of the lAtmato; andc although there are dliilerenes o:f opinion as to the exact quanti.v, there can be little tdoubt than as mainy inches descend here, in the course or a year, cas in ahnost ally other part of the globe-but few cdays, consecutively, ever pass withomut soime showers. Excessive storms of thunoder and lightning somletimes prevail,:for a week or imore at a time, wuithout interruption. Brigiht sunshine sutcceeds tle stoiorm, but tlle thernmal chaiges a-re less considerable than in most other localities~ a few degorees only, beiig the grea.test rang'e that ever occurs. I.especting these general physical:ieatures, topoora-illicail,:, ihydiog'rcphically, geologicai]yv, nmlineralo:icahlly, botanically and. mleteorologica'l]y, there are lro esseintial diffferences of opinion between thme observers who are here cited; and m-any others whlo have been referred to, whose names are not given, also agree with them. Accordiong to the surveys of' Capt. Keanlnish and Mr. Lane, the Trineiado g is navigable from its mouth, upwards, about thirty-eight miles for craft drawing ten feet of water. This river, as has already been remarked, has its sources on the Cordilleras of the Pacific Coast range, and after traversing a rocky bed, over several rapids and falls, for a distance of about thirteen miles, enters the low country and passes through swampy lagoons and marshes to its confluence with the Atrato. The drainage of the Truando and tributaries is about four hundred square miles. The banks of the stream are frequently overflowed, and are levees, in some cases, above the surrounding country. The sources of the Truando, the Nerqua and Hingador, rise on the hills to the westward of the valley of the Atrato. The Cordilleras, of which these hills are spurs, are at this point extremely low, and are very near the Pacific. So much for the physical features of this country, generally. The.Line via the Atrato and Yrcuando Rivers. This route commences at the estuary of the Atrato, and, as designated by Capt. Kennish, it is proposed to enter the Caflo Coquito, one of the mouths or Bocas. Here, at low tide, there is about four feet of water at the deepest point on the bar. The water gradually deepens as the river is ascended, and, at about two miles, is thirty feet deep. From here to the mouth of the Truando, the Atrato is nowhere less in depth than forty-seven feet, and most of the way it is much deeper. It varies in width, from a quarter of a mile to two miles, as has been stated in the general physical description. It would thus afford, when the bar at its mouth shall be removed, the most ample facilities for navigation, by the largest class of steam seagoing vessels and sailing ships. The Truando forms an angle with the general direction of the valley of the Atrato, of about seventy degrees. Its confluence is about sixtythree miles from the Atlantic, by the meanderings of the Atrato. The Truando is here taken as the line of the proposed channel, and followed for thirty-six miles. At its confluence with the Atrato there is a small bar, and the water is only eighteen feet deep. A few yards up, however, it deepens to thirty feet, and maintains this depth for a mile and a-half, or more. Above this, for thirty-eight miles, it has an average depth of about fourteen feet, and is ten feet deep at the shallowest point. At thirty-six miles from its confluence with the Atrato, the line diverges into the valley of the Nerqua, which is followed on solid ground. This part of the line, and all the remaining distance to the Pacifictwenty-six miles —is to be through solid rock cutting. The line, from the valley of the Nerqua to the Pacific, passes over a summit 506 feet above mean tide in the oceans, which summit is about three and one-quarter miles through at its base. This it is proposed to tunnel. From here to the Pacific it follows the valley of a small stream, and debouches, at the coast, at Kelley's Inlet. The distinctive features of this route are: First. —That the oceans call here be united by canal, through an open cut, without locks, guard gates, or impediments of any kind. Second.-That while it is one hundred and twenty-five miles from ocean to ocean, more than one-half of the distance is, by nature, ready for the passage of the largest class vessels. Third. —That the remaining distance is either excavations of bars, or river bottoms, under water, or solid rock, with slight earth covering. Fourth.-That excellent harbors exist at either terminus, requiring but little improvement to make them as desirable as any in the world. Thus it is proposed to form an open cut fromn ocean to ocean, without locks. Of the MIeans and Facilities of Construction. Under this head is included,lst.-The materials for mechanical works and other structures. 2d. —The opportunity that exists for obtaining workmen. 3d.-The ability to maintain a supply of provisions, clothing, &c. 4th.-The sanitary condition of the country. 5th.-The organization of proper executive departments. gMaterials for.Mechanical WVorks. But few mechanical works have to be erected in comparison to the magnitude of the undertaking as a whole. The first work is the projected jetty or line of pilings on either side of the entrance to the mouth of the Atrato, in the Carlo Coquito. Mr. Kennish sayvs abundant timber can be easily obtained, at a short distance, of good quality, and that stone may be had in abundance at the quarries of Turbo, and boated to the works across the bay. The excavation of the bar, being in sand and mud deposit, can easily be done by any of the several kinds of dredging machines now in use. From the month of the Atrato to the confluence of the Truando no work of any kind will be required. On the Truando, no bridges or aqueducts are needed, and nothing is to be done but the deepening of the stream, and the construction of such works as may be found necessary to prevent the wash of sedimentary particles into the main prism by the small streams; for these purposes, abundance of material exists within a short distance. Beyond the works on the Truando, an open cut in earth and mica-slate rock is contemplated, and here, up to Rancho No. 5, no mechanical work will be required. At or near Rancho No. 5, the river Nerqua must be turned, and some mechanical work is wanted. But, according to the evidence, there is abundance of stone and timber of good quality. At the great tunnel, proposed between Ranchos Nos. 3 and 5, some masonry may or may not be required. It is, however, stated, that good stone can probably be had within the line of the works, which is in basalt, if the same is wanted. Timber for all kinds of temporary works abounds on this division. From the mouth of the proposed tunnel, at Rancho No. 3, to the Pacific, no mechanical work is wanted, except at the Chupipi River, where good material is found. At Kelley's Inlet, anl ftiroml there to the ocean out;side the breakers, somle works must be built, such as guarlds, probal)ly jetties and lighthouses, but the material can readily be founcl near Rancho No. 2. II fact, on so longi a line o works, it is extraordinarvy o find so nearly everything required upon the gu1'ou1nd; nothting to be used in the wvorks need be bl1ought from a cistanc%, but cecl e int,ad lthte m4t;alPs. hls Oyc tpo~tvU.c,)t- tit t.aists fO t tatuai-n'yl' To0r9lemen.ze The natives of this rerion, and imgore 1aTicrieui]afry those that can be obtained -from the interior of the province of Carthacgena, are said to be faithful, industrious, sober and prudent men, inuaed by nature to the climate and food of the country, reo uiriing butt little clothing(, and thriving on the plantain. and wiid po-isr thati abouttd and tihe rice of colmmerce, whiclh is readily obtained. Very careful inquiries have been imade of a number of gentlemen, rliable, in respect to the resources of the ineiTghboTingo provinces, and friom their opinions the conclusion is t-obmed that at least six thousand mlen can be counted upon as a COnstant- Supuply, if'reqirLedC It is a very clifferent ting' f rom having to transport I1en froi'o great distances, when they can be had in their nlative country. The Jamaica negroes too, wiil do well in this country, and niay be relied upon in great nuimibers. Germans, irlish, Englis-1 miners, ontd Allericans obr the tunnel, and Chinese, mnay be importedC and coifortably sustained and maintained, as will more fully be seen by reerence to to the othete executive departments.* It may, and probabhly will, be necessarly to institute a regular system of emigration fomn om he olde-r cou-tries of Europe ancid Asia; and as the diffliculties of distant 1hland carriiage cwill not be felt here as in o-ther places iwhere attemllpts have beenl mlade to bring' tog ether la-g'e foreign populations, success in so Co:li0 wnill "c less questionabif. c The healthiness of th e country is aClso, very m ichl in fvor of the wo'k. At New-Yorlk, about one thousain c day arrive -romin Europe alone, to settle iln lhe Unitedf Sftates; utpwards of three hundred thousand have landed here in a year, Tvhil, probably, when tOhe wor!k at the canal is once organized, cnd smcient numibers are on the ground, from five to si: thousand per year wilv b slnfeienl to sulpply tIle places of those who niay, remove, or beco.e di.saf-eced, or die in the country. T7c6 AbrZiiy to 1i}lt c.,7t2Xp;i oj"S u'o vi.sm o nso Clothing, cc. Good harbors existing on either sidem, will adLuilt an unlimited commierce to be carried on, to the coast. From the shores of the Atlatic, steamboat navigation already exists tc Ranclho No. 8, on tihe Truando. * Since writinlg the above, the chief engineer of the Panama Railload lhas publishec a report, by which it appears that the mortality on the Isthmus is much less than ha, Ibeen supposed. It appears that only 293 wrhite men died in five years, out of 6,00( that were constantly engageed on the -Nork. T'he coolies fared worse; the Jamaice negroes and natives of th.e Isthmnmu?, bette,.l C.iec, from tize Yew- Y-ork7 Times of 23c duzg., 1.855.-E. 5. 1S. ci Supplies can be brought to the mouths of the Atrato from all parts of the world, and transhipped up the river, when the bars at the mouths are deepened, whichl could be in about two years —large vessels could carry their supplies all the way to the confluence of the Atrato and Truando. On the Pacific slope, the facilities are very great,. The harbors being- accessible for large vessels and all kinds of steamers, supplies could be brought -from Chili, Peru, the Sandwich Islands, California and Oregon. All the breadstuffs call be delivered here as cheap as at New-York or Liverpool, and many articles of consmnmption at less prices: certain things, such as some kinds of clo0thing and luxuries, would cost more, but the average would compare favorably with any port on the Atlantic. The valley of the Nerqua and the Pacifi slope, are said to be fine producing countries. Plantains and n-uts of various k-inds grow wild in gieat profusion, and tile opinion of those who have devoted time anld attention to the subject, is (in wlhich severaal agree), that the counatry between the Rancho No. 7 and the Pacific, will sustain as lalge a population ts the same extent of country in the best parts of Cuba. It is said to be particularly we!! adaplted to raising cattle and hogs: the latter f1'ur.nish the favorite meat of the natives. 2[le Sctziiha'y Co,)ditiolu of ie o 2f' omt'r-. From the Atlantic to the h-igh country on the T'ruando, the climate is uniform, but excessively moist. The thlermal ranoe of a.g't many observations, by different persons, spread over several mon ths indicated fluctuations of only 15 deg. The T very frequent and heavy rains, however, are unfavorable; and owing to t;he overflow of'he rivers, the country is almost uninhabited, and uninhabitable. But few natives are found anywhere lthouglh this region,'but it fortunately happens that, with the exception of subaqueous excavations, no work, but a small anolunt of piling'1 has to be done on any part of this division. From the high ground to the Pacifce, over the valley of the Nerqua, and the water-shed on the westward side, the climat;e is as salubrious as the soil is productive, and men from all parts of the globe can work here, and live as well and comfortably as in any part of the tropics. Those who are compelled to labor on and about the excavating machines, on the rivers eastward of the high ground, and at the mouth of the'Atra;o, must be provided with arks, or floating houtses, made cornfortable.,te,rxecutive Deptr:nteS. It is probable that the work can be carried on in the best and most satisfactory manner, by regular departments, or bureaux. These should include a chief executive or president, with an executive staff. The president to be the supreme head of the worLk, and to manage the whole general business. His staff should be the heads of the other departments. 62 An engineer department, consisting of chief engineer, one principal assistant engineer on the ground, and three other assistant engineers, heads of divisions, together with the necessary subordinate field and office assistants and draftsmen as may be necessary. To the engineer department should be intrusted all the general and detailed plans of the work, according to the usual methods. The advice of the most able and eminent engineers in the world should be obtained on the general plan in particular, and such a system of construction should be devised, that the details may be executed in the best way, at the least cost, and in the shortest possible timhne. The burden of the work will fall on this department. A medical staff should be organized, and proper hospitalary arrangements mnade for the sick. The medical staff might be constituted similar to the corresponding department of an army in quarters. In consequence of the very great number of men that must be elmployed to do the work in such a time as the wants of the trade of the world require, and as the climate is hot, although generally healthy, the medical deparment should be organized in tche most efficient manner, so that prompt and ample relief may be afforded at all times, on any part of the line. A paymaster's department will also be required. This bureau should take cognizance of all the expenses of every kind and nature whatever, and having suitable disbursing officers, should regulate the entire fiscal system of the enterprise that relates to the construction. A commissary department is also needed. The supplies of such a number of men as must be engaged on this work, will at first tax the energies of an experienced merchant; but with the progress of the enterprise, facilities will be created, towns will spring up, and merchandise will be brought into the country by persons not in the organization; but, at first, very great efforts should be made to subdue the natural wilderness, and to bring under cultivation large districts in the vicinity, in order that the best system of supplies may be maintained at the least cost, and without importation. It is said that the district through which the heaviest portion of the work is to be constructed, will, with proper cultivation, maintain a much larger population than will be required upon the line of the canal, and those not engaged upon it, such as the families and friends of some of the workmen, who will follow, and will, in a short time, form a civilized community. The readiness with which provisions, clothing, &c., can be had on the line of the works, may be judged from the fact that most of the labor will be expended on about thirty miles in length-one end of which rests on the Pacific, and the other at the head of steamboat navigation, on the Truando River, But little over six miles is, therefore, the average haul for supplies, which at first may be carried from either end to the centre, by mules, over the mountain roads, and, in course of time, good. wagcon roads, or even a railway or tram-road could be constructed. A department of machinery and repairs will also be required. De6pts should be erected on the Pacific, and at suitable points along 63 the line, and at the mouth of the Atrato, where the boats and machinery employed may be repaired, and where the business of obtaining the necessary materials for the work for the dwellings, stores and hospitals, can be conducted. A quartermaster's department, charged with producing suitable and healthy habitations for the men, and generally to care for their comfort, seems very necessary. Provision must also be made for supplying the work with laborers and mechanics. This, perhaps, can be done best by a bureau attached to the engineer department, or by a, separate organization. The facilities for obtaining men, have been heretofore referred to. As the laws of the land provide for the judiciary, no police regulations are necessary on the part of the organization constructing the work. It is believed that a system of contracting, in the usual way for works of less magnitude, would not here be judicious, as the profits in such a plan would be very great, and should be realized by the original organization, while the advantages of separating the responsibility (the only argument in favor of the contract system that could apply here), may be obtained by the proper execution of the functions of the different departments. It by no means, however, follows that great advantages may not arise from contracting distinct portions of the work or supplies. Of the Cost of the (anal. The work at the mouth of the Atrato consists of piling, crib-work, and dredging. Only an approximate idea of the cost here can be arrived at, until some more definite surveys have been made, and fixed upon. By the data hereto annexed of the work of dredging machines, it may be safe to estimate the cost of the improvements at the mouth of the Atrato, at $50,800. The excavations upon the Truando will depend very mnuch on the facilities afforded by the natural condition of the bottom; but the following figures show that twenty-five machines, working for eight years, may probably accomplish -the work. But as the material will, in some cases, have to be carried a long distance-say, 300 to 500 feet, and deposited, it is not safe to estimate less than an increase of 100 per cent. on this sum, although a liberal per-centage for contingencies and breakages has been made. ESTIMATE Of amount of alluvial deposit to be taken out of the bottom of the Truando, and the number of machines that will be required to do the work in eight years:QUANTITIES. Cubic Yards. Section K...................................2......... 2,395,872................................................. 10,534,935 M"............................................ 9,525,134 N............................................... 12,959,011 " 0................................................. 4,771,647 Total amount................................ 40,186,599 64 Twenty-one dredging machines, working at the rate of 800 cubic yards per day, for eight years, of three hundred days each, would be sufficient to take out the above; but allowing for breakage, &c., 20 per cent., it would require twenty-five machines. ESTIMATE On the cost cf.Dredyinzy ce-achnees to be uzsed on the vwo2r'h: — Nunlber of Machilnes on Truando....................25 25 Machines at $10,000 each..................8 250,000 Interest on 8250,000 at 7 per cent., for 8 years, amounts to..... $:40,000 Cost of working 25 Machines for 8 years, or 2,400 days, at $;9 per day............................................. 540,000 q'otal cost............................0, 0.... T otal cost...c o680,00o These machines are worked by about five or six ]mren, and employ steam power. The above contemplates the destruction of the machines in the time of service, which does not necessarily follow as a consequence. ESTIMATE Of -th'e amol.nt of' subcqueoz', excavation of tle Cano Coqquito of the Rio Takig tlhe avera,'e depth of cutting 15 feet 6 inches, and the le&ngth of cut at 19,200 feet, andl the average -vidthl of cult at 200 feet, the amount of excavation is 2,204,444 cubic yards. Number of cubic yards of excavaction, 2204,444. Five dreclging machines, or subaqueous excava;tors workino 3800 days in a year, and taking out cdaily eight hundcred cubic gyards of nmaterial, each, would excavate the above in less than two years. The bar here, however, might be excavated by jetties, as pSoposed by Mr. Kennish, and by opening only a small channel t;rough the centre, and allowing the current of the r]ivier to remove tlhe remainder into deep)er water. ESTIMATE Of' nzmzber o/q' ueonz'eqti'ed to worh/ on the sectionzs betwveen Keflley's Inlet anzd Townsezd's Junctionz, seupposing each mian to ta/ce out 400 cubic yards per year, for twzelve yeacs'8:AMOUNT OF EXCAVAT''IOi. Cubic Yards. Section A........................................... 5,108,589 " B....................................... 6,845,309 C...................................... 16,990,777 Extra at Mouth of Tunnel................ 62,460 Tunnel............................................... 17, 01,920 Extra at Mouth of Tunnel............................. 73,260 Section E........................................... 2, 57,230 F.......................... 15,842,627 ".......................... 16,576,987 Ix[........................................................ i.8,612,472 It A......................... 14,21,997 Total Amount......................... 105,293,628 Allowing 4,800 yards for eanch man in -twelve y-ears, there would have to be.21,934 men employed. On this basis it aiay be sae to S y that an establishment of 259000 men can perforrl the wor k in twelve years, aund that thlis number must be kept constant. The cost of unaintaminig such a number will glreatly depend upon the efficiency of the departments of the E~ecautive; but if they can be procured and maintained a n average e of one dollar per day bor the laborers, wil-li mechlanics, -fore-mnen, &c., in proportion, the cost of rock work, in the character of material here to contend with, slhould not, in open cut, exceed seven-eigh'ths of a dollar per cubic yard. The tunnel will not cost near so much per cubic yard as oine of a small section, owing to the proportion luhat exists between the heacding, always costly, and the remainder to be elxcavated. It is believed that Labout 0;2 per- yard will do it, -which would be, say-ten dollars per yard foi t le hieading, and over 81i 70 for the remainder in the foot wail.t. The works at the conifuence o1 itje Tv riando and open cut, and the necessary mwa2ste -eins and overflow-s, an construetions to prevent sedimentary deposits being precipitated into itle canal finom the small strealms, including the ltu7rnlig of the INe quna anid Chuplipi, can only be approximately determined in the nmost g'eierail way. it ts, hovever, believed that ample allowance has been nmade to cover conthigeneies. The cost of the improvemelnls nLecessai'ry nt elley's Inlet must be also euncerin, nil further survrs havre been madel; but an approximate quantity has been fixed upon, belierved suffcient. The great bulk of the wor ik being the rock excavation, a imore satisfactory conclusion is arrived at relaltivye to it.L The following figures sho-, as nearly as circumstances will at present permit, A SUMMAIPY OF THE 1ESTIMATED COST OF THE CANAL, AND APPURTENAN,,CES. WVorks at the mouth of thie traito........................... 0 50,800 iExcavations under wvater, in rurando....................... 1,360,000 Excavations at the conunuence of the Truaxndo and Canal, including ofier-damas anq pumnpin-o............................. 0,000 Excavations between conluence, ats a nbove, and Paeific, (exceptiDg Tu'ne!.) The quantities'are ail called rock; the excess by these leasures being aiwd f or grrubbinug and clearing at (2 s per cuic yard.................................. 7,83,994 Tunnel a't 2, being 1i0,O or heading, c.,........................ 25,403,840 Harbor and.elley's inlet., 150,000 Light-houss.............................................. 35,000'Pieprs.................................................... 20,000 Depots, (Pa 0ci0Ec) 5,0..........,000.............. I......... )5(,00O Depots and hospitals o -n lme..3............................... 3.5,000 Depot and Hospital, Towi nslsenls Junction,..................... 15,000 Depot.at arbo, ann iniprovenierits necessary................. 0,000 $105,1113,634 66 Amount brought forward,.... 6105,113G634 Executive department, 12 years,............................. 180,000 Enginee r departmentl..................................... 562,000 Medical department,...................................... 120,000 0Pay depaqrtnmenti,........................ 140,000 Commissary department,.................................. 260,000 Quartermaster' s clepartmnent................................ 150,000 Supplies for do.,.......................................... 550,000 Twenty-five pumping and hoisting engines, for t1he work in the 1 2000 Treateub,.,250,000 great cut............................................. Contingencies, 25 per cent.,................................ 27,081,408 $135,407,042 If the rock is estimnated at $1, this would be with contingent 10,000,000 allowance about, extra,....... pi45,407,042 It is not pretended that the above is more than asn approximate estimate. It is, however, believed to be ample. The dredging work is generally done for one-half what is here allowed, and rock worL iII this character of material for much less. In order to show that the great num ber of men necessary can wovk to advantage, a very simple calculation will sufnceo The line of the heaviest wori is spread over twenty-five ]niles, so that about one thousand men are allowed to CDa mile. Now, if the excavations are worked in teraces, comamencing a q.arter of a mile apart, and are carried forward in egular lift's of'five or six faces each, according to the nature of the particular pit and its stratification, only about forty or fifty men need work at face, which, being two hundred feet wide, and from twenty to thirty feet highb with the cross cuts, will afford ample room for the nullnmber proposed. In fact, many more may be employed, if necessary. Machinery for taking out the material, and delivering it on the spoil -banks, on either side of the cut, is estimated for, a ls wel as pumpinU engines for keeping the work free from water, which will runi in from the surface. The tunnel must be driven fron either end in the heading and the foot work. The heading can probably be worked, also, from at least one shaft, if it is found necessary, in order to do the work0' in time, and when once completed, the remainder will be similar to the other parts of the open cut, except that it may be worked both day and night, and in all weathers, which is in its favor. It may be proper to remark, in connection with this estimate, that this prism is intended to pass the largest class vessels, abreast,,and without locks. That a saving of many millions of dollars m-ay be effected by changing the plan, there is no doubt. Thus, by constructing the canal with a width sufficient for one ship at a time, with frequent turn-outs, a saving of about one-half of the above estimate would be made, reducing the entire cost to say 72,'703,521; and by introducing one lock on the Pacific side, the depth of cutting through the rock would be correspondingly reduced, ensuring thereby a still further mnaterial saving in the cost. A11 this, however, would not produce a perfect vork, and is not here estimated for. CALCULATI ON6 RELATIVE TO THE COMMERCIAL VALUE OF THE CANAL. The freight paid at San Francisco on Goods from the Atlantic, in 1853 alone, being on only a part of the trade, as some, freights were paid beoore shipping, was $9,911,432. At least tlhee-quar-ters of this charge would be saved —;$7,433,574 — or the interest, at 6 per cent., on........................ 4123,892,900 The foreign trade to San Francisco that would be benefited onehalf saving oL freight, paid at port in 1853, 81,840,650. One-half of which is $920,325, or a sum equal to the interest, at 6 per cent., on.........o.o....... 15,338,5'50 The United States Foreign Facific Trade wvas ctarried on, in 18 54, in 961 vessels bound out, and 895 entered home, showin' that the trade is equal to over two-thirds that o oour domesItic California trade, and would therefore, by passing this Canal, make a corresponding saving, or a sum equal to the interest Con......................................... $99,450,5i 0 Thus shosvwing that the Canal would save to the United Stal-es alone, the interest on the sum o......................... 238,682,220 The trade of France with the Pacific, which would pass through the Canal, and be benefited about one-half, is a little over,930,000,000. Our foreign Pacific trade being a little over $4133,000,000, the ratio of saving is in the direct proportion, or a sum equal to the interest, at 6 per cent., on..............$90,000,000 The British trade through this Canal would be, if no increase was estimated,,$180,000,000; which, by the same rules of saVino,' in comparison to the distance sailed, as goverl the calculations rellative to the United States,,would be equal to the interest, at 6 per cent., on the sum of $540,000,000. 3ut as the trade has facilities via the Cape of Good Hope, say to be benefited by Canal..................................... 300,000,000 The statement would then be --- United States,................ 8................ 6,2 03,682,220 France,................................................90,000,000 England............................................... 00,00,000 Other countries............................. 100,000,000 $728,682,220 isx per cent. on.................................... s,200,000,000 1for cost of Canal. And the interest, at 6 per cent., on.......................... 5t28,662,220 saving to the world. Or, twelve pem cent. profit on the cost of the Canal, at $200,000,000, and a benefit to the world at large of the saving of interest, at 6 per cent., on $528,682,220 annually. The above figures~, athough made fiora the official returns, are only approximate, as they do not include many iterns of trade that nlo-w exist, and no allowance is made for the increase of trade, whatever. The data is from Mr. Stone's Commercial Statenent,,. 68 CO CLUSIO So It will be borne in mind that the conclusions here arrived at relative to the practicability of this enterprise, and, consequently, its commercial value, are based main ly on tlhe data furnished by Mr. Kennish, partially confirmed and corroborated by MIessrs. Lane and Trautvwine-" The field notes and surveys of,1r. Kennish have been very carefully examined in this connection, and it is only justice to him to say that they are consistent with themselves, and present the appearance of care and truthfulness. Where so much depends on the accuracy of observation and faithfulness of record, too much calre cannot be takeln to gurard against errors. in this case, however, there seems to be every probability that the surveys represent faithfully what they piurport to, and may be taken for such, unhesitatinglyv. It was not intended by them to represent -the muinut'l of details. In my opinion, no other route yet discovered, by which to connect the two great oceans by water, can at all bear any comparison with this. The Londuras and Tehuantepee routes are impracticable for water intercommunication, and the Isthmus of Panama is not phlysically constituted to admit the coinstruction of a Canal within the liits of coumercial availability. The Nicaragua route, although possessing[ water o'n the summit, to be made as large and convenient for the business as that proposed at the Atrato, would cost considerably more, and in many other respects would be less favorable, inasmuch as it is sixbty-nine miles longer, and has twenty-eight locks upon it. A corresponding width and depth of prism would produce more quantities on this route than the Atrato route. And it is no less remarkable than true, that the Atrato route was indicated by Baron Humboldt, the greatest of modern observers, when in the country, and that, although referred to by such high authority, was comparatively neglected until the subject was taken up by yourseelf Opinions have at times been expressed that ships could be taken from ocean to ocean by railway, and that this method woulci preclude the use of a canal. There is, however, no foundation for such a position. If the ships could be taken out of the water, carried on a railway fifty or one hundred miles without injury to them or their eargoes, and then returned to the water again in as good condition as -when taken up, (all of which is very problemnatical,) the expenses of maintaining such a road, and the cost of working it, estimating only one-half cent per ton per mile for powe~r and expenses, would exceed the interest on an investment * But it is due to Mir. Kennish to say, that he is the first engineer who has ever proposed to unite the two oceans by a passage up one mouth and down anothler, of a never-failing river, without any locks, which is the feature that distinguishes this route from all others. 69 twice as great, as here proposed for an open permanent canal, without any impediment, as free to pass through as the oceain and safer. It is worthy of especial notice that the mouth of the Truando is situated relatively to the Atbrato and the two oceans, within a very short distance of where, theoreticallyv it NV ould be best to leae e Atrato River to enter the Pacific Ocean. If the tides on the Pacific coast were in cll p1aces alike, this remark would not apply; but as the tide rises mRntch higher- and falls lower, above and below mean level, at the Gulf of San /igc uel than at Kelley's Inlet, anud as the rise in the Pacific along this entire Coas6 is vreryiueh greater Jhan along thne correspondimgoy opposite Atlantic cocs' in the propoition of abo-ut twelve to one, i i is eviclent that if oat open cut wee inade tflrough the Isthmus at SaRn Mioguel Bay the acifie (Oceai Iould floaw through i-nto the Atlantic at hig wiater, and he t-'ant 7oulci pour. in the ciut at low'atter on the Pacific; thul producing sul -"rea't — id1 cturi'cts'i that the work would lbe useles s un les.s ]?oft.ecCi- at either i en byv.u.'.r locks. Wv hile,;f a conollietion should be att;'e nrted aboe Lie onthe l c. of' th Napipi with the Atrato,'the difference in ailt-tlide between thiis >oin't and the Pacific beilng about f"orty-five feet,'led the di-stance atbolt csi-."y miiles9 at least three locks would be recjuired e to thesA to re Pa-cic v; while in the present location, by the wray of the Tr1 uhaldo, tflie desent to the Pacific from the confltence witll the AtratL o beig -about equal to the descen t of the Atrato to the Atlantic, and -the distaive hein essentially the saile the current on both sides of the sum-it wold be a )bout equaiS exceptino the effect of the rise of -avter in -the Pasciflc whicl will oscillate in the open cut, anc flow to the lagoons iea;r the su1m1"'mit bleve-l The very permanent character of th' c orlk lpropos3eci must commend it to every one; no destrulctible mateiial hi ne: f used and no atteintion being, required forever aftert, to Eeep.i' orLder' other than tll,,hat rnus't froni time to tine be givren to t;he bars at the har1bors, shorulc'it e N found necessary to dredge them. The dis-ances t-at will b saed to the -0aic e of the -o ld by this route, being preseinted approxima telly i1 P i. Stones collmeroiia statements, now In your possession, no occasion eists io repeat; thelr Tiey would otherwise be givern While submitting this memoir I' ac'knowledge my obligations to ar. Kennish for the fi'aan-k and open m ann1er 1' -hiceh Le has replied to the 3most milnute and searobhing questions propounded to him, respecting the surveys, and the country, acnd ie facilities afforded for constructing the Wortk as well as to James C. Lane, Esq., who wuas in charge of one of the ield poaities on a formuer occasion, and to Horatio Allen, John B. Jervis and A. a. Edwards, Esq., eminent Civil Engineers, and Col. J. J. Abert, U. S. Topograplhica! Enlineer, fromn wholn valuable suggestions ha.ve been received. Wcishing you and the great enterprise in which you are so nobly engaged, all success, I remiain, your ohte. serv't., DV-An,.D -WTS SERRELL, CiviZl Engineer. 70 THE AQUEDUCT, IN ITS INFLUENCE UPON THE CO~MMERCE OF THE WORLD. HAVING thus shown fhe feasibility of the proposed route, we may be allowed to add a few statements bearing upon the importance of this enterprise, in its relation to the commerce of the world, kindly furnished by David M. Stone, Esq., one of the editors of the N'ew-York Joaernc of' The project for a ship canal at the isthmus was origlnated many years ago, before the discovery of goldc in California and Australia hadl given such importance to the commierce of the Iacifiic. Even the early Spanish adventurers sought for a praccicable rouee, and almo t everyimportant state or government on this cont inenh anld in uEurope, has, at one time or another, entertained the hope of findring i. Any one who will cast his eve upon the Map o' the world cl ill see at a gloance by what a tedious and daongerous route thei comerce of the Enast ldices, China, Japan, Australia and the settlements on the 7Western acoast of the American Continent, %must reach the principal mnarkets of: Europe and the United States. Th.e extreme leniigth of South AmLerica is -iour thousand si.x hundred miles, and at certain seasons of thl:e year, the passage around Cape HoC'rn is not only protracted, but; highly dangerous. Most of the European vessels bound for the East Indies take the eastern routte nld dIouble the Cape of Good Hope; but this is also a lonog andcl dangerous voyage. To show the saving of time which would be effected in voyages from New-York to the Pacific, by a ship canal at the Isthmius, we esxtract the following table, prepared for -lhis purpose by Lieut. Maury, and embodied in a Report of a Select Committe of the House of Representatives, presented in Congress Feb. 20, 1849. PrtgrJC3 co 01 oO 01 O 1 -5 e - e'. K 0 1 c o 010 1 0 01 01 I- C.:C ~1o.'n e; mS O O -oi1 C.D t1 > a CO~%O'-~ C~ ~ ~ o __ C ~ u CC C. ~ o CO O ~ C c CDO C~ o Co CO co -. q Q " CCW CO | CO CO CO CO CO CO C ~> @,2..: c Gi j | C CO CO C CO O OI C,:) 9 0-a) 00 _ I CID 01 % CO -H HC r4 ~ c~ r, 3 ~ r'.' o.' oc CCC) CO CO CO:) -) C= CO 01 CC) C)'C=$ C-9-~ C~ C X > >> r......::::. ~o' ~ C)5~~ CO CO CO CO CO CO C) CO CO CO All C C CC CO - CO r, j attention of a inteested i CO eC since he Ameican continet was ever ready to listen to any suggestio fo its acomplishment CO lo d C and oter near' ports, has increased from three millions of dollars to seveny-,fivemillion s dollar0s; when C alf ornia Ohas opened to the comC nerce of the world her glden g ates~ and japan is'eady to renew~ on a C) 1l -a~ C 0 Cr, m.r ca CS C" The trade between California and Atlantic ports -will soon be almost sufficient, of itself, to support such an enterprise as we propose. The total amount of freight money paid at Sa1n Francisco, for the yeajr ending 1853, was f$1,752,084, nearly all of which was for cargoes that went from northern ports, around Cape Horn. The followijng is a summary of these payments:_ Payg/ee-ts as Freight voZoney at /the Port of ~S'an Francisco dcurirb the ycear 1853. I FzOL I Fromi Itrorn;~ Thorn T~~'i'o tal.:astern Dom. Forts. Foreignr Ports. January... o.......,773 $2, 2 8$1,185,945 February........... I (11,600 i 8, 56 800,365 ar ch............. 92'7.670 254,079! 1,1 49 k.pril................ 1 2,~203 91, 1 < j i8,3c1' April.....'727,203 191,1 74 918 377 MAay................ Si, 9 1 39077 950,805 Julne..............'6,0 1473941 923,453 July.......... i. 1O,341 78,668 1,519,00.9 August.......... ~ 99s,9117 i 188,813 117,1730 September.......... 894,649 i 105,185 999,834 0 ctober........... 797,575 12 7, 62 92 5,247 JNovember.......... 506,311 1 9,267 665, 78 December........... 4 437,587 5 6,395 493,982 Total $......... c9,911,432 $!.840,652 1 11,'752,084 The above only shows the freig-l:t m"oney actually collected at the port of San Francisco. Vessels i'vorn Europe, and ma.ny froml domestic ports, r-eceived a great portion of their ifreight money at thre porti of clearance, and his, Of ours i no inclued This is trTi to a still greater exteni, of the commerce of 1854; a large portion of t1.e f-reiglt rmoney not being collected at San Francisco, and yet thle totatl thus collected in that year amounted to $5,3 i1,032, as will appear fronm the -folowing summrary: Paynents as Freight K3ooney at the Porlt of Stan'Fancisco during the year 1 1854. frm therchandie -. Oth.-r AtlantiC or i from Boston. Ports. I reign orLs. Total. 2New-Y~orPk.ot January........ i 482,458 $1 i9,603 $i7,466.-149,983; $846,510 February....... 23s,336 1 321,9 32t So80 164,861 7,5 73 March.......... 160,1811 20,180O 4-',36 152,34,7 473,072 Apri........ 0 14 O,200 J433,000 l3,981 388,95+ April 193,776 14-t200 tOGO 100 " 90 39 May..,,.',195,4331 i35,93 9 9,5(: 50,913 391,389 June............ 134, 0001 09 5811 28',611 1 04,5031 374,695 July.13798 I 103,485,Oi 32,41 21'7,13 L............ 03, 09.1.. oI 2 42 2,9 3, Aug.ust. 2231,536, 8,6 I 9,70 102.837i 122,93 Septemabe-:...... 1,716 1,4 3,0001 75,037 435,50 October......... I 02,103 6,24:8 4 65,0 6,71 50,3 Novembe....... -6,98a' 96,1 0 l 1 56,628 3001,437 Decembr....... 119,327i 67,31.....3,866 290,510 Total....... $2,472,S37 1,543,019 $245,068 $1,050,1058 $5,311,032 The tonn-age en'ga'ed in thle Califobrnia trade is'very large, the arrivals at San Francisco in 1853,:)beingo 1,028 vessels allnounting to b58,755 tons, and the clearanies 1,(653 vrssel s, aniounititin to 640 072 tons. In 18o4 the arrivals were 620 vessels of 406,114 tons, al.ll the clearances 1 193 vessels, of 515,861 tons. (1)f the above, l very lark'e proportion came fronl the -tlantie?ia Cape ornl. 3ut the trade of California, lrge ls thatl; is sl-lown to be, is Ilot the chiet reliance ofl the fiiends of the prolposed cntlul. TlThe trale between tle Unitedl Sttes andcl fo'eign Pacific ports h s 1beel, in a great lneasure, overlooked by those not directly eno'aged in i t, alndl its inmportanece has never been slfiCiently estnilated. \We hca-e ol-tained i'olL the Departm tent t \'Washino ton somle reliable inlotrmation upon this suljeCt, which w7ill )e found fll. of interest. These stateluents show that the tot.a;L ot cleatlraiaees firoil thle Unitedl Sttes to foreig'n PI eifi ports, tnil ar'rivals friom the same, blve iincreased s:bout two orhuniled pe cent. siince 1849 (tlhe tocnage showing a still larger increase, owing' to tlhe liroger vessels enployeld), wlile the total imports and exports thave doubhled dluring the s:ame space of time. This will app)ear fi ont t1he tlbowin sunllmar'y taikein ifrom official Conirionerce beltwlc~ /te l:1itlcl ted.S'tcts a.tm, 1Fo'rCeigclt Pfjic Ports'. Fiscal Year. No. [of Vessels. Tonnage. Vatlue of Imports & Exports, 1849 i 0!) (i(5. l. 7,001,320 8158(0 1:(3,54 1- 184,42,10 (3 1851 _ 2t0 ( (6 1 "1,375,428 i_:85:;)- I, 7 {0;1,91'I7,013,11.0I t1 8 53_ 18(,;; ST 87, 07 3[ L,5: 54:, 3 185 -t _85 5 (), - 33,953,4156 The ahbove is totaly -.xclsiv Co te to clol lec himremr_ tlbh Atlautic porfits,and Cailif'orniti, 1a1d presatt, al lit Jls ( oI d( s1:, nio:d truly stois hing. in order to slhow thlo w Im' rials:I(toi1l thic 1l(c, xt.}(';ic us c:l i npkiied, (:e an"nex [the de(thailes 1i01r tl t i,sea r:1tc'nt ionot. ComeerKce [;l, tet'lic /l't il' 1(1!(,S i(;t, (Sx(c,!t. l iz: /('.l l 1; Jc;.! / ]ctcce. ]orlts', /ib // ElroreI fiot. Cleared to.'iE sports Ixmports. )uateh'FLatst Inies. 2: S8,(3 1I8 7.5)1 84, 4 7i 81.;041,609 Br'itish liSt; It ndines',; I, [4 0 it-3'7 6j 412' 5,'378,30J uist ialii.........) 8: 1 L4.:10',149.07 14,' 1Xanll1......... 3; "I4'9 2) I41 4 121 219 "65t )"82 hili............ 107 -1. 1 11,7 93. 59: 332,167 P eru........... 8 L 5:. 080 I,,40 China............ 395I 1T7046,-. i. O,'06,2 2. Cynnl ~in107 70, (;i 191 87.20) 1,'..080f 10,506 9329 Miinor Pacifitc PIorts 1') 4.,264 _ 1 1 5 O 5 0, 95),,815 10,10_1 t)o. Indian Ocea-n t 1,,9 (; 3.814 "00i {:0,730 apan........... 00 Sandwich Islands. 3: 27o 8 C) )1,2 529 5,891 11 130 Northw est Cost.U.'9 6,490 0 8;951 I., 0 9,,..a........' L) 65,3163I'>9061 4.)l, 6.8.S'f,3, 1 3 J I 463,4?7,6 1 t'} 74 Of this, 1856 vessels, *amnounting to 95'7,599 tons, and carrying $33,953,456, value of' merchandise, it is evident that nearly every sail would pass through the Ship Canal at the Isthmuls, if such a one were constructed. In further confirmation of this, we can see vwhat preference was given t6 the clippers over ordinary sailing vessels-time being reckoned of so much value. We can hardly conceive it possible fbr a ship, clearing from 5New -York:for San8 Francisco, to prefir C. voyage of 19,000 miles, when_ by the use of a Ship Canal, withoult 1lanoer or detention, it could shorten the distance to 5,000 miles! The interest upon the ship a:nd upon the value o' the. cargo. and the cost of victualing a.nd sailing the vessel, to say nothina of the dangers incident to a protracted voyage around the southern point of -the Conti,nenat, would determine every vessel making a voyiage fiom any AmlTerican port on. the Atlantic to any port on the Pacific, to adopt the advatntages offered by the canal. The trade between the various European Sta;tes alid the Pacific is large, and much of it would, undoubtedly, pass through the canal, it' such a channel of communication were completed. The following will show the number of ship;s, the t.)ollnage, a1nid the im — ports and exports, between France and the Pacific paorlts, during the yTear 18.52:No. of Ships. Tons, Imports and Exports, British India....... 54 1]8,250 45,200,000 Society Islands,,..81 23,66 6 40,300,000 Peru............,. 211,051 25,200,00( Chili,......... 2,178 1 9,300,000 French India,...... 25 7,886 1:3,400,000 Dutch India,....... 5,0 7,300,000 Philippine Islands,. 14,252 i 1,700,000 China,... 912 i 1,100,000 Bolivia,......... 1 500 1.00,000 Total.......... 223 70,77]1 Ifs. 153,600,000 A total of 223 vessels, 70,771 tonrs and imports a'rd exports amounting 1t t53,600,000 francs, or over $30,000,000, for the trade of a single year. In turning to thle trade of Great Britain, we hardly know -where to draw a, line as to the portion of her imm1ense commnierce likely to avail itself of ethe advantages of tihe new lro-te. -Her direct carrying business between her own East Indiapossessionss. a.lnd the hiome nc ports, is nearly $8100,000,000 per annum, wlhile to that is to be aclded the China and other East India commerce. Her traffie between the ports in -te United Kingdlom. and the Westor( co4 st of Northi an Southll Anerica, would certainly seek the new (ciha ne an md this, lreckonino the cargoes both ways, now i aounnts to upwards of $30,000,000. The most important branch of Br3itish trade certaini to pass throuogl thel'Canal, is -that connected with Australica; and here, lest we rrighi; be accused of exaggeration, we propose 0( give the,oeicial. i.'ures, The /bllowiny are theI declacred va/,ahe /' of.,Jim'ports a~nda.Kr;p:orts a.t t/,, Colony of YTctoriajbr the yea'Cs 18 53 So.ad 1854. IMPORTS. 11.853. 1.854, 1Building Materials......00.................C2,004, 9 ~2,2436,01 Dry Goods.......................... 869,54 3592,09J Iron and iron larnumiactures............. 26 L 1, 34, 653 L'eather and ILeather M[anufactures.......... 1994 527,31 I Provisions and Groceries,................. 460, 24 101,20 Specie,........ 3.............. 3 7,I 40 Spirits.................................. OI 15, 0 04 Spuito.1~~~~~~~~ ~~~~~~ 010 19 0 Sugar aind Molasses............8......... 186614 427061 TJea,.................................. 205,364 92 83' Tobacco...........................257,39 991441 Wine...................... i.......... 33,552l 409,05: Miscellaneous,...........,........... 385,502 5,85 8,396 Total Imports....................15.)842,632 ~IJ317,720,307 The ibllowing will show fromi what counl'vies the above were, inmported 1.853. 185'4. Great Britain....................... 8,088,226 ~C11,050,329 British West Indies....................... 14,973 20 British North America.................... 13,560 60,238 Other British Colonies..................... 5,036,311 4,394,933 United States............................ 1,668,606 994,692 Other Foreign States..................... 820,961 1,220,092. 1.5, 842,632 ~ 17,720,307 EXPORTB FROM VICTORIA. 1853. 1854. Gold..............~ 64........ ~8,6,4,529 2 ~8,255,550 Wool,.I....6................ 1,651,871 1,018,1] 4 Miscellaneous,. 61,1.4-3 1,901,540 ITotal Exports.............. 11,0. 543:11,775,204 The following will show to what countries the above were cxpoorted... 1853. 1854. To Great Britain...................~.... ~9,875,624 ~10,270,213:British Colonies.......................... 942,741 1,378,107 United States,........... 19,646 50,933 Other Foreign States,.................. 223,532 75,951 Total Exports......... 11,057,543 11,775,204 These statements showilng a total of -~08,495,511 imports and exports for a single year, would be almost incre(dible, welre they not taken froin the official returns.'VWe might go iul ther, andl give ini deta.il the commerce of each of the South American States bo-derinag on tlhe Pacific, where trade has wakened into new life withil in the last twNo ao' rtltree y-ears, lut) the foregoing will serve the purpose of illustI raton. These arie not estimnates of a commerce likely to be created by the const'ruction of,l cal ld, bltt st.ttements of a commlnerce nlow in being', a large portion of which would avail itself at onlce of this inter-oceanic commuinication. WVith such a business before us, the contemplated cost of the canal sinks into comparative insignifieance. A very small tax upon such an immense amount of' tonnage, woull keep the works in repair, and pay a large interest upon the capital expended. To saTy nothinll of' the lessened risk, and the consequent reduction in cost of insurance,'the colnvenience to the world of such a speedy transit tiom ocean to ocean, xwithout breaking' bulk or unbendingo a sail, can hardly be over estimated. The advantages to be gained by a vessel in pasisinc tdhrough the canail over the route.arounid the orin, are so apparent, that ally shipowner or merchlant can calculate them froml the clata above given. To those interested in this enterprise, who are not practically flamiliar with nautical matters, it imlay be well enougnh to give Ca simple statistical statement, by way-: of illustration. This is a utilitarian age, luad iany may ask"Apart fi'om the lessened riskls of -navig-ationl, whi t will the sav:ing of time by the Isthmus route b)e IIo'tAo,iz ndollat i.s