IN THE SUPREME COURT OF THE UNITED STATES. GEORGE C. BATES, vs. THE ILLINOIS CENTRAL RAIL ROAD COMPANY. The facts of this case are very briefly as follows : Kobert Kinzee, under the act of Congress of May 29, 1830, and the subsequent amendment of the same, claimed as pre-emptor the north fraction of section ten, on town 39, north of range fourteen east, being part of what is now Chicago. At that time there was a sand bar stretching across the mouth of tho Chicago river which bounded the harbor on the south. This sand bar was the result of a current on the westerly coast of Lake Michigan from the north southward, coming in contact with the river current coming into the lake. The lake cur- rent being the largest in volume and the most powerful, pre- vailed, and sweeping the river current southward, but in some measure slackening the lake current arid creating some eddy, caused a deposit of sand, which stretching down the shore formed a bar, which was a narrow strip of sand stretch- ing southward from the north fraction claimed by Kinzee, outside of the current of the river along the whole lake front of the south fraction of the same section, and along the lake front of the next section, south of that sometimes a mile, sometimes a mile and a half, and sometimes only three- fourths of a mile, depending upon the winds and currents and freshets which might take place in the Chicago river, sometimes lengthening it out, sometimes cutting it off, and always more or less aifecting its length southward, and to some extent its dimensions in other respects. The diagram will give an idea of the position and nature and character of the bar and its form. At the time of the survey by the Government surveyors in 1820 or 1821, the river ran directly out straight into the lake in an easterly instead of a southerly course. At that time the ingress and egress for boats into and out of the river was at the point, and which in the government survey was de- signated as the mouth of the river. At that point is the call mentioned in the government survey as the mouth of the river, and at that point was the then actual mouth of the river, through which its waters passed into the lake. It so remained during that season until fall or winter, when the downward current of the lake, carrying with it ice and drift- ing sand, filled it up ; but in the spring when the freshet of the river came down it cut through the bank there again, and continued to pass out there during the next season, when the same causes again filled it up. It was probably opened in the spring of 1820 or 1821, the year of the survey when the river was high, by shoveling out a small trench on the top of the bar, across it, so as to enable a small current to run across, which in a few hours cut it out to such width and depth, that the whole current of the river found its outlet there. The same thing had been done in 1811, and again in 1816, and again once or twice afterwards, but certainly once in 1829. When this was done the result was that sometimes the downward current of the lake acting upon the current of the river, and forcing it southward, would wear away the sand bar south, and by the same process add to the north side, until the bed of the river should have passed over and worn away the entire sand bar gradually, and as gradually formed a new one by accretion or deposit of sands on the north side. The result was the old sand bar entirely wearing away, and an entirely new one forming, but the causes being always the same, invariably in the same posi- tion. This is a sketch of the history of the bar, but it is ma- terial as showing where and what was the actual mouth of the river at the time of the government survey, and as show- ing that that actual mouth, and the call made by the govern- ment survey, and designated by the style of, and as the mouth of the river, was at that time its actual mouth. In other words, that the call in the survey designated as the mouth, and the location of the mouth, or the position of the mouth on the land or earth, were the same. There was therefore no discrepancy between the survey and the monu- ments called for in the survey. A material question arises here on this point, which in itself may be decisive of the whole case. What was the southern boundary of the north fraction at the time of the govern- ment survey, and as fixed by the courses and distances, and actual monuments called for by that survey. Was it the river as it then actually was, as it it is described in the sur- vey, or was it the river as it ran at other times and in other years, outleting three-fourths of a mile, a mile, or a mile and a half below, according to the circumstances ? If it was the river as it then was emptying, and as the survey lixed it then, all that was gained to the north fraction was what was added to it by accretion subsequently, under the well known law relative to accretions. If the river, as it then was, was the southern boundary, and we think it must be so beyond controversy, then the sand bar south of it belonged to, and was a part of the south fraction of section ten, because the survey of that fraction bounds the east side of it by the Lake Michigan, and the courses and distances running from its 4 south-east corner on Lake Michigan, call for the lake shore all the way up as its eastern boundary, being a distance of half a mile, until they reach the part then designated as, and what was actually, the mouth of the river, and the call or natural monument then being the lake, of course carried the south fraction to the lake, and included within it all the land, sand bars, and shore, south of the then mouth of the river, to the lake. If this be so, then the locality of the sand bar was in the south fraction. It might be worn away by the gradual action of the waters, and the title to it lost to the owners of the south fraction, and it might, after having gradually worn away, be added to the north fraction by the gradual for- mation of land added to it by accretion, which accretion would gradually extend over the place where the sand bar formerly was, and thus add that locality to the north fraction. It will be observed, however, that though the river ran out there then, and for two years, and though it was then beyond a doubt the actual mouth of the river at that place, so recognized and designated by the surveyors as the monu- ment which bounded the north fraction on the south, and thus locating the whole situs of the sand bar south of it in the south fraction, yet some time anterior, human agency had co-operated with the current of the river to turn its waters out there and form that channel; that the channel having been formed there, in some degree, by human agency co-operating with the force of the waters, it was to some extent, at least, an artificial channel, and it was in conse- quence of the waters running out there where the downward current of the lake would not permit them to remain, but kept crowding them southward, that the sand bar south was gradu- ally washed away and a new one formed from the north, gradually stretching over the same locality, and thus adding to the north fraction the locus in quo which had formerly be- longed to the south fraction. These reflections become material in the view Judge McLean took of this question. He holds, that because Kinzee, or his grantee, could designate the situs of the sand bar and its extent, that, therefore, the title could not be lost to it by the gradual action of waters wearing it away gradu- ally and imperceptibly. He holds, also, that when human agency and artificial means have co-operated with the cur- rent to wear away the soil, the title cannot be lost. Though we do not agree with him on these points, as will be here- after seen, yet upon his principles the title to the locus in quo could never have been transferred from the owner of the south fraction to the owner of the north fraction. The cur- rent which wore away the south fraction was not the natural current, but was a current or channel formed there to some extent by artificial means. The testimony showed, that if the sand bar washed away twenty times, it would reform ex- actly in the same position, the causes being the same and acting in the same way. The site of the old sand bar could therefore be determined as exactly as that of the new one. According to Judge McLean, therefore, it could not by decre- tion or accretion be transferred, so far as title and legal right is concerned, from the south fraction to the north fraction by the action of the river and lake, as the testimony shews them to have operated. If his positions be true, therefore the title was always with the owners of the south fraction, and, as the defendants own all the lake shore of the south fraction, is in them. Again, upon any view we take of this case, we think this sand bar has never been included in the north fraction, even though the river had not ran straight into the lake when it O O was fixed and designated as the monument which bounded the north fraction on the south. In its more ordinary and natural position this sand bar stretched south of the north fraction from three-fourths of a mile to mile and a half, ex- tending far south of the whole section, and lay outside of the main shore of the south fraction and between it and the 2 waters of the lake, and with the water of the river between it and the main shore. Now the courses and distances call for the lake as the eastern boundary of the south fraction. They commence on the south-east corner on the shore of lake Michigan and run thence north on said shore of the lake un- til it reaches the point designated as the mouth of the river, thence across the said mouth to the north shore, thence along the lake shore north till it reaches the northerly line of the section. Now, upon the supposition that the said sand bar was then there, and the water did not run out where the call makes it to have done, but to have run out a mile below, we have a discrepancy between the courses and distances, and calls or monuments, called for by the surveyors, and the natural monuments as they existed. There was no lake shore on the east side of the south fraction at all, but a liver and sand bar between it and the lake. The mouth of the river, instead of being where the courses and distances and calls fix it, was a mile, or a mile and a half, south of that point, and the discrepancy is such in the circumstances, that it is impossible to ascribe it to error in admeasurements in courses, or calls. The survey is as the surveyors intended, and is without error, and the question is, what is to govern the boundaries of the north fraction according to the govern- ment survey. What was the southern boundary of the north fraction? "Was it the line designated by the courses and dis- tances and calls of the surveys, or are all these to be thrown away and the southern extremity of the fraction to be brought a mile and a half south, because one of the calls is the mouth of the river, which ordinarily was at the southern extremity of this bar, sometimes longer and sometimes shorter ? It is a case of a discrepancy between the locus of the call and that fixed by courses and distances. And the question is, to ascertain the intention of the surveyors and what they intended to fix as the south boundary, because it is by their survey that the government grants. There are certain rules established to control, or rather to enable the court to arrive at the meaning of words used in a deed or conveyance of lands. Sometimes the number of acres mentioned will be resorted to to control a given course, sometimes a given course will give way to and be controled by distance, and distance will give way to be controled by the calls or monuments upon the land, and especial- ly if it be a natural monument, as a tree, a water course, or lake, the rule being, that when all the words of description do not agree with each other, but some are repugnant to the rest, those shall be retained where there is less liability to er- ror, and those rejected where men are most liable to make mistakes. But all these maxims and rules are laid down to be followed only as the most certain rules and maxims, by which the intention of the deed can be ascertained. There- fore, it is that in some sets of circumstances the courses will give way, in others acres, in others distances, in others calls or natural monuments. Sometimes one of these elements, in combination with other facts, furnishing more certainty to the mind than others, or even all the others. For authorities bearing upon this point see the following cases. 19 Pick., 466. 6 Cowen.717, 281. 3 How. U. S., 193. 4 Wend., 313. 17 Mass., 210. 14 Barbour, 438. 8 N. H.. 404. 19 Johns., 449. 32 Maine, 80. ,.. 9 How., 4H5. 10 Ohio. 316. 4 Wheaton, 447. 2 Wheaton, 316. 3 Pick.. 277. 11 Conn.. 332. 13 Wendell. 303-5. 8 Wend., 190. 9 Yerger, 55. 2 Spear., 628. 8 These cases present a great variety of examples, those in New York and Massachusetts especially, where every ele- ment of description has been rejected which has been usu- ally denominated the most certain, because others combined with circumstances in these particular cases became more certain. The case in 17 Mass, is a very remarkable one, where calls became less certain than distance, and gave way to it. The whole go to show that there is no certain rule, but that in each case those elements, which in that case furnisli the most conclusive convictions upon the mind, of the boundaries intended, will prevail, and all other repugnant elements will give way before them. Apply the principles to this case, and there can be no doubt that the courses and distances must govern here so far as to fix the south boundary of the north fraction. The fact that those courses and distances and calls, for natural bound- ary of lake on south fraction, show that there could be no error in course and distance, because they arc each of them fortified by the great natural boundary with which they agree and correspond. There can be no error here on south frac- tion, it has the lake on the east for half a mile in the direc- tion of the courses and distances, at the end of half a mile those courses strike the river and cross it, whether that were the mouth or not. So far everthing agrees. Thence it crosses and goes on the north side following the lake shore up. Un- less the courses and distances are to govern, then there can have been no survey of the east side of the whole section. The mouth of the river may have been misnamed, but there can be no doubt where the point was. The object called the mouth was where the Jacob's staff was set. This is beyond all controversy. That was the point by them called the mouth of the river, and intended, both by them and the govern- ment, as the southern boundary of the north fraction. The sand bar was considered not as being on the north side of the river, and except where it lay across the raoutli-of the river 9 was on the south fraction, and a part of it. This is very ap- parent Now, should any construction be put upon this grant made upon this survey, which should not only defeat the manifest intent of it, but should destroy the whole survey, and now after thirty years transfer $2,000,000 of property from the south fraction to the north fraction, from the owners of one to the owner of the other ? I am aware that by the general principles of law a bound- ary by a water course generally although the courses and distances would not carry the boundary to the water will prevail, and the courses and distances will give way to it. This is the general rule as above described, because that is the presumed intention. It is the same with the general rule that where land is conveyed bounding on a fresh river, the title passes to the middle of the river. But in such case, where there are circumstances or words to do away with this presumption and rebut it, and showing a contrary intent, a contrary rule prevails. And so in this case we think that the south boundary of the north fraction was and is at the point where the courses and distances establish it. But, passing from this, in 1830 the pre-emptor entered the land and paid his money for it. He did so in a land office having no jurisdiction, and secured no title. It was entered at Palestine 7th May, 1831. Chicago had been set off from that land district February 19, 1831, three months before. He got no patent. In June, 1836, the land office at Wash- ington decided his entry to be void. Hall's opinions of Altornies General, vol. 3, 131. 13 1'eterg, 511. 7 Wheat., 210. 5 Branch., 92. 6 Peters, 676. 2 How.. 284, 318. But in July, 1836, an act passed by Congress confirming 3 10 these entries and authorizing patents to issue upon them. Under that act, in March, 1837, a patent issued to Kinzee of the north fraction, according to the map or plan in the Sur- veyor GeneraFs office of said fraction. Some questions arose upon this, as to the time when the title passed and the pre-emptor became owner. Does the confirmation relate back to the entry of May 7, 1831, or to the time of the act of Congress? I do not discuss this point, but the following authorities bear upon it: Jacob's Dictionary. Title Confirmation, 8 How., 293. 4 How., 463. 2 How., 319. 8 Cow., 285. 5 Cruise, 275. 16 Johns, 110. 13 Peters, 514. Coke Lit., 609. At the time of the passage of this act of Congress, the Government of the Union had constructed the piers at Chi- cago and opened the harbor. This was done by cutting a channel through this sand bar in an easterly direction across it and where the river was passing out when the lands were surveyed in 1820 or 1821, and where, by the survey and plat made thereupon, the mouth of the river is located, and where the courses and distances of the survey locate it, and where, at different times, from 1811 up to 1833, the river had, at va- rious times, passed out after making for itself a passage, or aided by some little help of man by a trench across it with shovels. If the title relates back only to the act of Congress, then the survey, plan in Surveyor General's office, description in the patent, and the river in its mouth, all correspond and agree exactly together as they did in 1820 or 1821, when the lands were surveyed and the government plans or maps were made, and there can be no question in the case. The pre- 11 emptor took bounded by the river. If it related back to the entry, then if this sand bar was a part of the north fraction the government, by that act of Congress, must be held to have conveyed away all the government works and harbor constructed by it. The Harbor was built in 1833-4. The channel was opened through where it now is and has ever since been, in Marchj 1834, and the permanent mouth or entrance to the harbor there established. The piers were in after years extended perhaps one thousand feet out into the lake. The effect of this was to interrupt the downward current on the shore of the lake, turn it a little from the shore and prevent the drift- ing sands from depositing upon the shore below the pier, as they had formerly done. The current striking against the pier was of course, at that point, to some extent arrested and caused to strike out into the lake a little, below the piers. The consequence was a deposit of the drifting sand on the north side of the pier, where many acres have been made, until the angle between the pier and shore was full; when, there being a curved shore formed in that angle, the water or current passes along more easily and without eddies by the end of the piers, but still turned from the shore south, and is depositing its sands south of and forming a new sand bar across the present mouth of the river, and stretching south a mile or more, and nearly but not quite parallel to the old one, which was upon the site in question. The prevailing winds are from the north-east, and the waves strike the whole western shore of Lake Michigan in a quartering or angling manner, and are, for a hundred and fifty miles north and south of Chicago, gradually encroaching upon and wearing away the land. The drift of sand being stopped by the piers and turned outside the old bar, the supply which before had been constant, and enabled it to maintain its battle with the waves by addi- tions of new material as fast as it wore away, was cut off and turned elsewhere the action of the waves continued, and 12 every particle of sand they carried away was lost, with no* new acquisitions. The consequence was, the old bar south of the piers was gradually worn away, and in three or four years disappeared beneath the waters. It had never been more than about eighteen inches high. It disappeared be- neath the surface of the water in 1836-7, but it was several years before the mass was washed away so that the lake ac- quired there its full depths, ranging from four feet near the piers to ten feet at the southern line of the section, near a half a mile below. In 1836 it mainly went under water gradually and imperceptibly, as the jury find. The water there became deep, and was for many years an open road- stead for rafts, boats and vessels. It remained so from 1836 to 1852, abandoned by all claimants, and forgotten. The Railway Company located its depot there, filled it up and expended $2,000,000 of money there. In 1857, twenty years after its disappearance, the plaintiff goes and buys up the claims which the pre-emptor of the north fraction might have to it as a part of that fraction for a small sum, and brings this suit. Now the question is admitting in this place that it once belonged to the north side did the title wash away with the sands which composed the bar ? If lands wash away by the gradual and imperceptible action of water, does the title to the locus remain f Does it make any difference that the place where the land once had been can be accurately identified ? Does it make any difference that the artificial construction of the piers by the government acting upon the current in the manner above described had an agency in causing it to wash away? That the general rule of law is that where, by the gradual and imperceptible action of the waters land is worn away the title goes with it; and where in the same manner land is gradually added the title spreads over it is indisputable, and is established by many striking cases; and the reason as- 13 signed in the Books is that the party owning on the water is subject to the contingencies there, and being liable to lose and having a chance of gain, the one is a compensation for the other, and his title shall be good to the accretion because he is liable to lose his title to the land worn away. This princi- ple is stated by the Supreme Court of the United ' States, McLean giving the opinion thus: "The question is well settled at common law that the per- " son whose land is bounded by a stream of water which " changes its course gradually by alluvial formation shall " still hold by the same boundary, including the accumulated " soil ; no other rule can be applied on just principles. Every " proprietor whose land is thus bounded is subject to loss by "the same means which may add to his territory, and as he " is without remedy for his loss in this way, he cannot be " held accountable for his gain." 10 Peters, 717. This, it will be noticed, is stated by the Supreme Court of the United States as the well settled rule of the common law, and the reason given is a common law reason. The doctrine, however, was taken from the civil law, and was incorporated into the common law in and subsequent to Bracton's time, who copied into his work on the Law of England as being the law of England, the paragraphs in the Institutes upon the subject word for word and comma for comma, as the cases cited by me below show, and ever since his time has been unquestioned law. See Angel on Tide Waters, 257-8, note 266, 9, 255, 256. Angel on Water Courses, 43, 53. 2 Black. Com., 262-3. 3 Barn. There the question was as to the property in lands formed by the accretion, and the position was taken, that the accre- tion was caused by the erection of a wharf into the river, which caused a deposit by the water by reason of a change in the current. The court said that it did not think much of the position, and that it mattered not whether the accretion was wholly by natural, or partly by natural, and partly by ar- tificial, means. This is the only authoritive case directly on the point, though the reason upon which the law is based, and all its principles, tend to that direction. So much for the general question, and I think it a clear one. There is a special question as to land formed under 'the lee of the pier in front of land owned by the govern- ment, about two hundred feet in length; this accretion ex- tended across the old bed of the river, and would occupy a small space where the sand bar had formerly been. It was formed by accretion during a space of fifteen years. The peculiarity as to this is, that it formed in front of the land of the government occupied as an hospital. The government built the pier. The consequence was, the old sand bar wore away, accretion formed in front of main shore on land of government. Does any diiferent rule apply to this than to lands owned by individuals ? Can the government who built the pier, the remote consequence of which was accretion in front of its own land, claim the accretion, and sell it? It is the case above cited from the .Roman law, with the additional element, that the remote cause of the accretion was created by the owner of the land upon which the accretion formed. There is no decision on this point, though it is alluded to in a case by a judge in New York. 4 Smith's Court of Appeals, 151. Upon the best consideration I have been able to give to it, the title to this accretion will rest upon the same principle as would that which formed upon the next lot belonging to a private owner. I can see no reason for any distinction. All my reasoning above applies as well to that land as to the rest, and I think it must be governed by the same rule. JAMES F. JOY.