riS ^, ' . . 5 ' A >« .%^ fe>, --....' »':-^v^ "^..-^^ ^'km>>. V..^ ;:^iv. ^.../ ^^z*^:. -t ...a • ■ t) ^y ^ * A- <^ A '^ O 5 • • ^ "^ 4 o ,0 ^^ '>'-^^r.' ^^ V-. '° "b >'0^ o V .. -.. , , 5- ■?■ . , vv' --^i , -, * ■■> ^.' ■ _• ,•■' ■\ A' ■>•. V ■■'.- ' / ,■'> o • . . -S o ;■ ,-. '-' ■^■'' i\:''%:~.. •>>-■ A , '•■ ^. '^ •/\^ ^. J'" ■ .. s ' " . ''^. ^ 'V-._ ■;> u. • "'•"/> S'' '■<- \ ./■ r -.' ^ X. * <;=" '■-., • V ,■ " ,, ' ""^y- 0*^ v.- • - " -' ^ ' '^. .c^" '' ' ^ ^ ■ •'■ % c^ ^^ ' ^- ' >^ .s^— ~ » „ , '^ '"' •/^ X .x^- > ■\ ^•^ ■^ I .^^ * ■> ■ \- • >'- ^1/t. C-'^->' -'-'-/ ■^. GEOGRAPHY OF CONNECTICUT By Henry T. Burr Principal, Willimantic Normal School, WiUmiantic, Connecticut EARLY HISTORY The first settlement in Connecticut was made about 1614 by the Dutch, who sailed up the Connecticut River and establisiied a trading post where the citv of Hartford now stands. Thev chose this location because it was near the head of navigation on the river and therefore convenient for their purpose as traders. In 1633 English settlers from Mas- sachusetts began to come to the same region. They were attracted by the strips of fertile land which border the river on both sides at this point. The first English settlements were made at Windsor, Wethersfield, and Hartford, and soon afterward the interven- ing territory was occupied. There was con- stant friction between the English settlers and the Dutch traders. The latter were soon outnumbered and finally withdrew, leaving the English in full possession. English settlements were independently made at Saybrook in 1635 and at New Haven in 1638. Saybrook was chosen because of its situation at the mouth of the Connecticut E. p. 6 Copyright, 1916, 1921, by American Book Company. River, which provided a harbor and offered easy access to the interior. New Haven was selected for its excellent harbor and also be- cause of the broad lowland which lay to the north of it. Other settlements soon de\eloped along the shore both east and west of New Haven as well as in the central lowland. In 1662 these settlements were all united under the name of the Connecticut colony by a charter granted by King Charles II. The influence of geographical conditions in determining the location of the settlements of the colony is indicated by the fact that, of the first twenty settlements, ten were on the coast, six on the river, and two on both coast and river. 1 he uplands were not settled until later, after the more favorable locations were largely occupied. Connecticut undoubtedly owes its inde- pendent existence as a colony and later as a state to its geographical conditions. The fertile lowland which attracted the early settlers was separated from the Massachu- setts Bay colony by over a hundred miles of ©CI.A617605 66 GEOGRAPHY OF CONNECTICUT / r. rough wilderness, which, at rliat time, offered no inducement to settlers and was without roads other than Indian trails. Thus the Connecticut settlers soon became used to governing themselves, and Massachusetts made no determined effort to exercise author- ity over them. POSITION, FORM, AND SIZE Position and Form. — Connecticut is the southernmost of the New England states. It IS roughly rectangular in shape, its length from east to west being nearly twice its breadth from north to south. Size. — Connecticut is one of tlie smallest states. It occupies but one degree of lati- tude and a little less than two degrees of longitude. An automobile can easily go from Rhode Island on the east to New York on the west in less than a day, and the fast express trains running from Bos- ton to New \'ork cross it m about three hours. It IS about four times the size of the neigh- boring state of Rhode Island, which is the smallest in the country. It is less than one sixth the size of Maine, the largest New England state, and it would take nearly fifty-four states the size of Connecticut to equal the area of 1 exas. RELIEF Uplands and Lowland. — Connecticut is divided into three parts, — an eastern up- land, a western upland, and a broad lowland lying between. In a general way the uplands are alike. Each consists of numerous hills, rounded and smooth of slope for the most part but occasionally broken by rugged cliffs. Neighboring hills rise to the same general level. Very rare]\' does a single hill overtop the others near it. In general, the eastern upland is lower than the western. In both the heights increase gradually from the shore northward. The greatest altitudes of Connecticut are in the northwest corner of the state. Bear Mountain, in the extreme northwest, with a height of 2355 feet, is the highest peak. The central lowland is underlain by softer rocks than those of the uplands, and by weathering and erosion this region has been reduced to a nearly level plain. Some layers of trap, a la\'a rock, in the soft sandstone are harder and stand up as ridges above the general level. East Rock and West Rock at New Haven, the Meriden Hills, and the ridge running from Meriden to Mount Tom and Mount Holyoke in Massachusetts are of this character. Claciation. — Connecticut lies within the glaciated region. The great ice sheet mov- ing southward over the hills smoothed them into the rounded forms that are now so common. The materials worn from the hills were spread over the lowlands. In places this material, known as till, was heaped S — S.iti!.Q4.i 20.2J4 Putnam 7,711 6,6(7 Di-rljv ll.2;S S.flo I Roikville 7,726 7.077 H.irtford 138,0,56 gS,oi5 Shelton g.47.=; 4.807 .Mtriden 20,807 27.2U.S St am lord 35.og,0j8 11,851 Water!)nry g ■ . 7 1 .? 73.141 New Britain .Si^.O" 4.3.0 lb \\ illimantic 12,330 1 1.230 New Haven It)2.SI0 IJ3.005 Boroughs Boroughs Bethel ;,2oi ,5.041 Naugatuck I s,osi 12,922 Branford 2, dig 2.560 Soutiiington s 08 s 3.714 Danielson .i.l.iO 2.g34 Stafford .Springs 3,385 3.050 Greenwich S.ijSg ?,806 TorrinRton 20,023 I.';.4S3 Groton 4,2.i(> i,8g5 W'allingfor.l g.04S S,6go Jewett City j.io'J .S.02.3 76 ^ t /-h,-/,.- p,»,,,/^r -^-AiiYl^rli^r^ .E.U:i!/aaiv.>-^y i\ p \ ^\{ /W.Hartlarid ^ / ^\ V Ni- Ir^'i -V . I.P " 0,"''"7''"'?"'*lFa11si Vnlage / /\l5 ,- lO^'^KA - ,''' n \\ V-* ''^"^''Fi-r-J/ t> r > '^^ +^\V\^^ lf\'\ r /^ '^ E Ml V\i / "^ aVv / \ Wfn^tSd-:./. BARkHAMSiTED /( '-n /A -^r^i' //IfflK /^'^rV^^'MY// /IVS''«"''"/''''I^ S" / ■Tfinuft???" < NEW HMTFORSjjy. , /tantori/ J|7 blo»field . feWinlsSr^i, ; ,„ \av.S»i^^ iasdr'7%': Brook I;. «f,Ellihbtpn- jXuitc Vuitchtleld, Bantarr^^ Vyrnon Cen 'E 5i+( o)nI ernf 'flCaVldri.v/le /^i s S-iVg^to n&s' v*'"p„;:S'r ''^-31!*'' VXH\lf/ /ifS ft y?' r6ETHLEHE> U BW*'^^' ^%//(V V //Iw Qfl!l"' 1 S\ IwATERTOWI. Nfm l«liLf"RD\t^ \JiiJ-T — TT^ni Waterto\ yp BsUit-YJ i\ ^lotchkissviUe estvilliE fH«Mi1:^?^lVvJ iT|' /.' IPIantiivillo' MiiJ ' ' .'.111- - ' * J^ "m-ii^.n ty if* TiliiJ (WOLtoTTl SpUT3lNGT6NX';'»rg5tf,.,J,|t ' / l' \l 0\ t y'cW^ ...RoxbSry V-^';^'?^-; / Soiith bucy ) St U iiii'iyC^t.i^i ^l. ft I "XT Vjpi ^"^^ ' ■ i^eSaijdy Hool Pro^ffiScv kitoaf: . |m,odl#>'\ t:S^I^ WVy-tlS i» // :?// / />>^iDU,RHAM / \,HA^5>bA M ox F O R\D\ StHEi / *^ > 1 . ' <>WAriinBfOT«Durham Ceri-.S ,\BranchvHJfT) \ J \\"-| ^ \_, ^ WNL^''*^ » (Jffilfordjiy ^j i V '7'.!/^"' ' V-"!" <'i'^S'ife''M.ti 1 I _l I WE&T PORT v "fordi ^VAAN Winnll ukl i ffl\vtjtp*l' Lf V\... i.S,S?omr,.^rf«l•NorofX^i-^-- 72 .30 West XVI \/rv tCE 4- 'ij-iLL^ i'r"::r??!!KS jT^btJlin, ( ^ C9>rnft^* Ri» ^ o J r Center' ^■-— V- n ^^ W e-S(X r R E f N v/l C H^^-i* J~^ r ^ Narragansctt \i\ * / pier i^' r ( Gciz-rf/nera Pt. j\ bAROlNERS Sandy Pt., \Clay Hd /new/ BLOCK ISLAND M/ (ToNVwporl Co-.U.!,) ,';f UBIock Oivkvns f>t,\»^^fi^KfSOId Hafhai Pi. , B/i(cA PotA Phyt^icul and rulitical Connecticut AND RHODE Island Sl.iIi: ..f ?l.;tult Milt- ■^^g Harboj CD' '•^it Capitals -'-County Scats Citifs are underlined. Size of type indicates n-IuMvt populatinti i>f ritici. towns :iud boroughs. 100.000 and o;cr Bridg'eport T'Coon to 100. 000 Pawtucket lO.OOfi (u r.o.o^n) New Britain r..000 to Ul.dOO Winkled County Seats with less than fj.OOO popnlation Kniyston Steam Uailioadt; Elettru' KaJlroads. — -^ — -*^' COP'RIGHT.SV AMEBICAN ROOK CO I I svn GEOGRAPHY OF RHODE ISLAND By Robert M. Brown Professor of Geography, Rhode Island Normal School, Providence, Rhode Island HISTORY other settlements were made at Newport and Portsmouth on the island which gives its " To hold forth a lively experiment that name to the state and which is said by one a most flourishing civil state may stand and authority to be named for the island of best be maintained with full liberty in reli- Rhodes and by another to have been named gious concernments." This is the inscription by its discoverer, Rhoode Eylanat, "red written on the Capitol at Providence, and the island." These settlements were later united sense of the motto is expressed frequently in under the name of Rhode Island and Pro\i- the early history of Rhode Island. Previous dence Plantations. to 1636, the area about Narragansett Bay was inhabited solely by Indians and they have left behind them as monuments the many names of the physical features of the state. It is recorded that the explorer Verrazano dis- covered Narragansett Bay in 1524 and that The history of the state centers almost entirely about Narragansett Bay, and it is not strange that very early the colony had a navy of its own. Conscious of the intent of the founders, it resisted any imposition of taxation by the mother country, sinking in Adrian Block, who gave his name to Block 1669 the armed sloop Liberty and in 1772 Island, explored the bay in 1614. The first burning the Gaspee, vessels which had been permanent settlement was not made until sent by England to curb the activities of the 1636, when Roger Williams, driven from Massachusetts becau.se his opinions were in- tolerable to his neighbors, established near the headwaters of the bay a town which he called Providence, " for God's merciful provi- inhabitants; and, in reality, these were the first overt acts of the Revolution. Still jealous of her freedom, the state was the last of the thirteen states to enter the Union ; and the strength and insistence of dence to me in my distress." Soon after, her sons in convention during the early years £ P t, Copyright, 1916, 1921, by American Book Company. x\iii J ©CI.A617G06 GEOGRAPHY' OF RHODE ISLAND 79 of the Republic maintained the integrity of line. Mount Hope, the scene of Indian the state and prevented its partition by Mas- sachusetts and Connecticut. Once firmly es- tablished, ho\ve\er, the growth of the state has gone on with tew mterruptions, hrst as a farming community, then as a commercial district, and now as a manufacturing state. POSITION AND SIZE Position. — The southern shore of Block Island is about 8' north of the 41 ' parallel, and the northeastern corner of the state ex- tends about z' north of the 42" parallel. The southern point of the mainlantl, in the ex- treme southwestern corner, is in the latitude of 41° 6' N. The east-to-west dimension of tends along the western side of Narragansett the state is somewhat less than the distance Bay from Pro\idence to Warwick, from north to south, and it lies wholl\ between The most important part of the coast line wars during colonial da\"s, is a knoll, 200 feet high, situated on an inlet of Narragansett Ba\ neai Bristol. The surface of the state has a rolling character; the plain has been cut and worn by streams, lea\ing rounded hills and between them broad \'alle\ s, while the invasion of the great ice sheet during the glacial period co\ered the state with a layer of glacial drift, m which are many bowlders of great size. In places the glacial drift formed moraimc hills. In addition to the hills of drift, the glacier left much material scattered in plains of faint relief, called sand plains, a good representatne of which ex- the 71"' W. and 72' W. meridians. of Rhode Island is the great indentation, Size. — Rhode Island is the smallest state Narragansett Bay, which extends two thirds of the Union. I rom Providence at the head of the way into the state. The south shore, of the Providence Ri\'er, one may reach facing the Atlantic, is low and slopes gradually Woonsocket on the northern border by train under the water, so that vessels cannot ap- within a half hour. Westerly in the southwt-st proach the land except where a river, as the in one ht)ur and fifteen minutes, and the Pawcatuck, scours a channel across the con- sail down the Bay to Newport consumes tinental shelf. Narragansett Bay was formed but two hours. Delaware, the next state in b\' the sinking of the land, which allowed the size, IS nearh' twice as large, while I exas, the sea to enter the broad vallex' now occupied by largest in the United States, is 213 times the the waters of the ba\ . In this broad valley size of Rhode Island. were numerous hills which were not sub- merged in the subsidence and now extend their RELIEl* AND DRAINAGE ^^^^ above the waters, forming the islands of Relief. — The upland region of southern Rhode Island. New England, an uplifted plain, slopes from Drainage. — The term "river" is applied m the Berkshire Hills in western Massachusetts and Connecticut and from the White Moun- tains of New Hampshire to the sea. Rhode Island's position in the southern margin of this upland, with no point fifty miles from the ocean, gives it a relatively low relief, rhe highest point in the state, Durfee Hill, near the northwestern corner, is 805 feet above rhe level of the sea, and only a small section, in the same general locality, is above ^oo feet ; while a much larger area, adjacent to rhe ocean and bay, is below the 200 foot conrour Rhode Island not only to rivers proper but also to the estuaries or great arms of the bay. Thus the Seekonk River is a narrow parr of the bay extending from Pawtucket to Pro\ i- dence. Providence River is the northern and narrower portion of the bay, and the Warren and Barrington rivers are likewise estuaries. The true rivers of the state flow into Nar- ragansett i5a\', except the Pawcatuck which reaches the sea in the extreme southwest- ern corner of rhe state. I he Blackstone River, rising rwent\ miles to the northwest 8o GEOGRAPHY OF RHODE ISLAND of Woonsocket in Massachusetts, flows into the Seekonk ; the Pawtuxet, rising in the western part of tlie state and flowing through the center, flows into the Providence River; and the Pawcatuck, draining a large part of the southwestern part of the state in its lower reaches, forms the boundary line between Connecticut and Rhode Island. The invasion of the ice during the glacial period brought to the state a great quantity of loose materials, which were deposited unevenly over the area when the ice melted. Many streams were turned from their former courses and found new pathways to the sea. In cutting dovv^n new channels these streams encountered bed rock which halted the erosion at various points, and as the softer materials on the downstream side were removed, falls were formed. Navigation is therefore not possible upon them, but the rivers are valuable as sources of power, especially the Blackstone and the Pawtuxet. Besides turning many streams from their original beds, the deposition of glacial drift over the state blocked the headwaters of the streams and formed many small lakes. Rhode Island is dotted with lakes. Some are now used for water supply and some as camping sites. Many of these lakes were shallow and filled up quickly, forming swamps, which remain as undrained areas that sometime may be reclaimed to yield rich harvests of vegetables and fruits. Climate. — The most important climatic control is latitude, and Rhode Island's posi- tion between the 41st and 42d parallels of north latitude gives to it a high sun and long days in summer with the consequent high temperatures, and a low sun and short days in winter with low temperatures. Prevailing winds and nearness to the sea are two other factors that determine its climate. Rhode Island is located in the westerly wind belt (Sees. 61, 62), and the cyclonic storms (lows) and anti-cyclonic storms (highs) of this belt cause great variations in the seasonal temperatures. The proximity to the sea, although less influential on an east coast than a west coast under westerly winds, gives to the state fewer excesses of heat and cold than are experienced by an inland state. In Providence the average temperature ot July is 73.4° and that of January is 27.2°, making an annual range of 46.2° ; while at Block Island, the average temperature ot July is 68.1°, and that of January is 31.4"^, giving an annual range of but 36.7°. The diflerence between the annual range of these two places illustrates the influence of dis- tance from the sea upon climate. Altitude causes only slight local difterences, as the relief of the state is not great. The growing season (Fig. 71), which is the time between the last killing frost in spring and the first killing frost in autumn, is longer in Rhode Island than in any of the other New England states. This period is shorter in the northern part of the state than in the southern part. The last killing frost sometimes occurs in March, but more frequently it comes in April ; and the first killing frost is frequently as late as November. Especially along the coast ot the state the modif\ing influence of the sea IS felt, and thoiigii the winter days are at times bleak, they are never excessively cold. The influence of the sea in modifying tem- perature, however, is most potently marked in the summer, when the cooling influences of the ocean attract many summer visitors to the state and give a temporary increase to the population. Watch Hill, Narragansett Pier, and Newport stand out preeminently as summer resorts. The rainfall of the state is ample and is the heaviest along the ocean front, where over 45 inches per year is the average amount (Fig. 72). In the northern part of the state the annual rainfall is from 40 to 45 inches ; while the extreme north- western section receives 35 to 40 inches. The rainfall is fairly well distributed through the year, so that the soil is kept moist, and long-continued droughts are not common. GEOGRAPHY' OF RHODE ISl^AND Si INDUSTRIES Agriculture. — Most of the soil in the state is of glacial origin. In the upiaiuis it is of no great thickness, and fre(]uently bare ledges are ex- posed, while o\"er the lowland a greater depth pre\ ails. As there are but small areas of alluvial soil, the greater part of the state has a rather coarse-textured soil. In the uplands the clay, usually in glacial soils, is absent, and the porous and stony char- acter of the soil makes it less valuable than the lowland soil, which contains the clay. According to the soil survey nearly fifty per cent of the state has a light brown sandy loam, the most ot this being too rough and too rock\' for profitable tillage and best suited to forestry or to orcharding. About twenty-one per cent ot the state's area has a mellow brown loam, the most productne soil in the state. About two thirds of the area of the state consists of farm land, but only one fourth of the total area consists of improved farm land. It is estimated that about 400 square miles, or thirty-seven per cent of the state, is covered with trees, but the growth is not vigorous and most of the trees are too small for timber. A few patches of pines exist, and cedars fill many of the southern swamps, but most of the forest area is covered with hardwoods. Hay is the leading crop of Rhotle Island and potatoes are second in importance. Corn is the most important cereal crop. In the vicinity of the large centers market gardens have sprung up and have been uniformly successful. Providence and the towns in its immediate vicinity offer an extensive market for garden products, and in the southern part of the state the summer resorts make a good demand for vegetables and fruits grown in -ife i-,-«;^^P .^jjfesiS A market garden near Providence the ail|acent areas. I he state is considered a natural orchard area, but only small quanti- ties of fruit are raised. 1 he most important farm animals of Rhode Island are horses, dairy cattle, and poultry. The large manufacturing centers and summer resorts furnish ready markets for milk, eggs, and poultry. Mining. — Ihe \alue of minerals exceeds the \'alue of the agricultural output of the state, but does not ecjual in value the fisheries, fhe most famous product is granite, and Rhode Island stands ninth among the states in granite protluction. I his stone is quarried in main' places, but the real center of the in- dustiA is at Westerly in the southwestern part of the state. The WesterK granite has, because of its fine texture and color, found an extensn e m.irket for monumental work. Coal is mined 111 small amounts on Aquidneck Island, but it is of inferior (juality. Fishing. -Narragansett Hay offers a great extent of shallow water which has been used since the foundation of the colony as a fishing ground. Fishing gives occupation to onl\ a very small percentage of the people of the state (one half of one per cent), but the yieUl is worth in money ten times the output of the farms. More than one luilf the \alue 82 GEOGRAPHY' OF RHODE ISLAND of the fisheries comes from shellfish. Rhode points in New England. One line runs from Island clams are widely known and its oysters Providence westward into Connecticut, one are shipped in great quantities. The OAster extends northwestward to Pascoag and into catch is valued at three fourths of a mdlion dollars per year. Scup, squeteague, and lobsters are caught and form twenty-five per cent of the value of all products of this industry. Manufacturing. — Rhode Island is above everything else a manufacturing state, about fifty-five per cent of the working population be- ing engaged in this industry. The leading manufactur- ing industries of Rhode Island, in order of mipor- tance, are manufacturmg of Massachusetts, another runs northwestward to Worces- ter, and another southeast- ward to Fall River and Newport. One of the main railroads of this system connects Providence with Boston and New York. From Providence exten- sive trolley lines parallel the railroads and carry on a hea\'y business in both freight and passenger traffic. Providence is also the center of a coastwise traffic and is connected by boats with New York and Chesa- woolen and worsted goods, cotton manufac- peake Bay. One transatlantic line, the Fabre, turing, dyeing and finishing of textiles, and from southern Europe, stops at Providence, the making of jewelry. To-day Rhode Island and the state has recently erected a new holds first rank among the states in the value state pier in the city in order to extend its of jewelry manufactured. The state ranks facilities and attract trade. The bay during second in worsted goods, third in dyeing and the summer months is filled with many kinds finishing, and fifth in cotton goods. of vessels, and a fleet of steamers plies Most of the raw materials for manufactur- between the large resorts. ing come from afar. Rhode Island has no gold nor silver mines, no cotton fields, and but few flocks of sheep. It does, however. GOVERNMENT AND EDUCATION Government. — The settlement of Rhode Is- contain a densely settled district of skilled land in somewhat isolated towns developed a artisans. The disadvantage of distance from purely democratic form of government in the sources of raw products is compensated by the abun- dance of skilled labor and by the nearness of markets for the finished products (Fig. 80). Transportation. — All the railroads in Rhode Island be- long to the New York, New Haven, and Hartford Railroad system (Page iv). By these lines Providence is connected with other cities and villages of the state and with other GEOGRAPHY OF RHODE ISLAND 83 which every voter could liave a hearing and a direct vote upon every issue. As soon as the town meeting became unwieldy, because of the mcreasmg size of the town, cities organized under representative government. Groujis of towns and cities are jomed as counties tor the holding ot court sessions onlv. The governor of Rhode Island, elected biennially, has less power than is granted governors of other states, inasmuch as the veto power is denied him. The legislature, called the General Assemhlv, is a small bodv ; each town or city has one senator, making thirty-nine, and each has representati\es ac- cording to the population, but the House is limited to a membership of seventy-two. Education. — The public schools of Rhode Island consist of elementary schools, high schools, the Rhode Island State Normal School, and the Rhode Island State College. The state board of education and the com- missioner of public schools have general su- pervision of the schools of the state. Some of the best features of the school system of Rhode Island are: the large number of professionally trained teachers, the length ot the school term, evening schools for those who cannot attend day schools, and the introduction of industrial education, including agricultural education. The Normal School trains teachers for the schools of the state. The State College offers courses in agriculture, engineering, and other applied sciences. Brown University, an endowed institution, is one of the leading universities of the United States. POPULATION AND CITIES Population. — Rhode Island has a popula- tion of 604,397. Although it is the smallest state in the I'nion, there are ten states with a smaller population. If the people were distributed uniformly o-'er the state, each square mile of area would contain 563 persons, and tiiis density of population ex- ceeds that of anv other state of the United States. This high density is the result of the concentration of people in manufacturing centers. The six cities of the state contain 429,175 persons, or over seventy per cent (A the entire population, and the total number of people in villages and cities ot 2500 in- habitants or more constitutes 96.7 per cent ot the population. 1 his percentage ot urban population is not exceeded by any other state of the Union. Two thirds of the population is native and one third is foreign born. The foreign white stock, including foreign born and those having one or both parents of foreign birth, exceeds two thirds ot the total population. Providence, at the head of the Providence River, is the largest city, the capital of the state, and the chief distributing center. It is the second city in size in New England, Distribution of population in Rhode Island 84 GEOGRAPHY OF RHODE ISLAND being exceeded by Boston. Providence is primarily a jewelry center. It is also noted for the manufacture of cotton, worsteds, high-grade tools, engmes, and boders. Be- sides being the center of the industrial life, Providence contains the state Capitol, Brown University, and the State Normal School. Pawtucket, the second city in population, is at the ht;id i)f the Seekonk River, an arm of Narragansett Bay, and along the lower reaches of the Blackstone River. Cotton and worsted goods and machinery are manufactured. Woonsocket, on the Blackstone and bordering Massachusetts, is noted for the manufacture of cotton and rubber goods. Newport, once a famous port and the capital of the state, is noted as a summer resort. The # State Capitol, Providence United States War College and Naval Training Station is located here. Cranston and Central Falls are manufacturing centers. The former is noted for bleaching, dye- ing, and calico printing, and the latter for the manufacture of textiles. Cotton goods are manufactured in Lonsdale, Valley Falls, ManviUe, Warren, Warwick, West Warwick, and Westerly. Chemical products are manufactured at East Providence and fish oil and fertilizers at Tiverton. Bristol, noted for ship building, has sent out many " cup defenders." Kingston, in the southern part of the state, is the seat of Rhode Island State College. Block Is- land, Narragansett Pier, Jamestown, and Watch Hill are famous resorts. Population of Counties, Cities, and Towns op Rhode Island, igjo Bristol County . . Barrington Bristol .... Warren Kent County Coventry . East Greenwich . Warwick . West Warwick . West CIrccnwich . Newport County . Jamestown Little Compton . Middletown . Newport (city) . New Shoreliam . Portsmouth . Tiverton . Providence County Burrillville Central Falls (city) Cranston (city) . The State . . 23.11,5 3.8q7 11,375 7.841 38,269 5.670 3,290 13.481 IS. 461 367 42.893 6.633 1.389 2,094 30.255 1,028 2,590 3.894 475.190 S,6o6 24.179 26,407 Cxmiberland . East Providence . Foster .... Gloucester Johnston . Lincoln North Providence North Smithficld Pawtucket (city). Providence (city) Scituate . Smithfield Woonsocket (city) Washington County Charlestown . Exeter .... Hopkinton Narragansett North Kingston . Richmond South Kingston . Westerly . . 10.077 21,798 0C5 1,389 6,855 0,543 7.647 3.200 64.248 237.595 3.006 3.199 43.496 24.932 759 1,033 . 2,316 993 3.397 I..?OI S.iSr 9.952 604.397 • /%'^:-= /^\ -/f^^v /°-o;-->«®;:-- „,*°-\ •■»• /°% ^^ y,:i^^^^\ / ,M,.-^ ^"^^^'.\ /^^;m^%. Z^^^."^. <>, >= - ■■■■ .- -^ V ■A- ' VS^'r'-'* V ^> -= ^,*"<.nV * V "C*. ° '4?SW'\^ ■<• «? ■i^ o ■'.' ■:■■'■'- * i ■^oV^ V„ ^- .^w/).<- -^^^ :^.um^,. ^:^^ % -"..'A <^ -':..- ,G^ ^5 '„..■' A <^ ■'** -^ ^"^ -^i^ ^^^ "^^^ "^Z «1# o 1 ■^t. ^•^. ^%#'<^ -^ ^ ^^€m^'. >. ^ ..^ ^•'*JS-X , ' .v^- %. ,0' .•■''■, o \ \ r ■'^ ^-0^ ^ c A' -/ . /.- '^, ■ ^ ^ • ■■•■■ -■ u -^ ,V ^ ^ ' ■-'^V ■-■ -J.- ,^\ .>>'C-. ■ .0^- <;•. •^■\ .^ ^ ''■V'' .^'v' V e,^ V- o"^- . i'- ,5 0.. • ^ r- "^^'■' -V- ''^^. r. H ,V' 'J^ '>'> .-J." ^^ ^ ; o. As F-^ - .^0 ,0 ■0' "-^ =i^ ^^\- "^^^ /iSfc "^/ /. 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