Page:EB1911 - Volume 16.djvu/110

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90
LAKE CHARLES—LAKE DISTRICT


African Lakes

   Length 
in
Miles.
Depth
in
Feet.
Area
in
sq. m.
Volume in
million
cub. ft.
     Max.  Mean.   
 Victoria Nyanza  200 240 .. 26,200 5,800,000 
 Nyasa 350 2580 .. 14,200 396,000,000 
 Tanganyika 420  2100  ..  12,700   283,000,000 


Asiatic Lakes

   Length 
in
Miles.
Depth
in
Feet.
Area
in
sq. m.
Volume in
million
cub. ft.
     Max.  Mean.   
 Aral 265  222 52  24,400 43,600,000 
 Baikal 330   5413 .. 11,580  274,000,000 
 Balkash 323  33 .. 7,000 4,880,000 
 Urmia 80  50 15 1,750 732,000 


American Lakes

   Length 
in
Miles.
Depth
in
Feet.
Area
in
sq. m.
Volume in
million
cub. ft.
     Max.  Mean.   
 Superior 412   1008 475   31,200  413,000,000
 Huron 263  730 250  23,800 166,000,000
 Michigan 335  870 325  22,450 203,000,000
 Erie 240  210 70  9,960 19,500,000
 Ontario 190  738 300  7,240 61,000,000
 Titicaca 120  924 347  3,200 30,900,000


New Zealand Lakes

   Length 
in
Miles.
Depth
in
Feet.
Area
in
 sq. m. 
Volume in
million
cub. ft.
     Max.  Mean.   
 Taupo 25 534 367   238.0  2,435,000
 Wakatipu 49  1242 707  112.3 2,205,000
 Manapouri 19 1458 328  56.0 512,000
 Rotorua 7.5 120 39  31.6 34,000
 Waikarimoana 7.25  846 397  14.7 166,000
 Wairaumoana 5.25  375 175  6.1 30,000
 Rotoiti 10.7   230 69  14.2 27,000

Authorities.—F. A. Forel, “Handbuch der Seenkunde: allgemeine Limnologie,” Bibliothek geogr. Handbücher (Stuttgart, 1901), Le Léman, monographie limnologique (3 vols., Lausanne, 1892–1901); A. Delebecque, Les Lacs français, text and plates (Paris, 1898); H. R. Mill, “Bathymetrical Survey of the English Lakes,” Geogr. Journ. vol. vi. pp. 46 and 135 (1895); Jehu, “Bathymetrical and Geological Study of the Lakes of Snowdonia,” Trans. Roy. Soc. Edin. vol. xl. p. 419 (1902); Sir John Murray and Laurence Pullar, “Bathymetrical Survey of the Freshwater Lochs of Scotland,” Geogr. Journ. (1900 to 1908, re-issued in six volumes, Edinburgh, 1910); W. Halbfass, “Die Morphometrie der europäischen Seen,” Zeitschr. Gesell. Erdkunde Berlin (Jahrg. 1903, p. 592; 1904, p. 204); I. C. Russell, Lakes of North America (Boston and London, 1895); O. Zacharias, “Forschungsberichte aus der biologischen Station zu Plön” (Stuttgart); F. E. Bourcart, Les Lacs alpins suisses: étude chimique et physique (Geneva, 1906); G. P. Magrini, Limnologia (Milan, 1907).  (J. Mu.) 


LAKE CHARLES, a city of Louisiana, U.S.A., capital of Calcasieu Parish, 30 m. from the Gulf of Mexico and about 218 m. (by rail) W. of New Orleans. Pop. (1889) 838, (1890) 3442, (1900) 6680 (2407 negroes); (1910) 11,449. It is served by the Louisiana & Texas (Southern Pacific System), the St Louis, Watkins & Gulf, the Louisiana & Pacific and the Kansas City Southern railways. The city is charmingly situated on the shore of Lake Charles, and on the Calcasieu river, which with some dredging can be made navigable for large vessels for 132 m. from the Gulf. It is a winter resort. Among the principal buildings are a Carnegie library, the city hall, the Government building, the court house, St Patrick’s sanatorium, the masonic temple and the Elks’ club. Lake Charles is in the prairie region of southern Louisiana, to the N. of which, covering a large part of the state, are magnificent forests of long-leaf pine, and lesser lowland growths of oak, ash, magnolia, cypress and other valuable timber. The Watkins railway extending to the N.E. and the Kansas City Southern extending to the N.W. have opened up the very best of the forest. The country to the S. and W. is largely given over to rice culture. Lake Charles is the chief centre of lumber manufacture in the state, and has rice mills, car shops and an important trade in wool. Ten miles W. are sulphur mines (product in 1907 about 362,000 tons), which with those of Sicily produce a large part of the total product of the world. Jennings, about 34 m. to the E., is the centre of oil fields, once very productive but now of diminishing importance. Welsh, 23 m. E., is the centre of a newer field; and others lie to the N. Lake Charles was settled about 1852, largely by people from Iowa and neighbouring states, was incorporated as a town in 1857 under the name of Charleston and again in 1867 under its present name, and was chartered as a city in 1886. The city suffered severely by fire in April 1910.

LAKE CITY, a town and the county-seat of Columbia county, Florida, U.S.A., 59 m. by rail W. by S. of Jacksonville. Pop. (1900) 4013, of whom 2159 were negroes; (1905) 6509; (1910) 5032. Lake City is served by the Atlantic Coast Line, the Seaboard Air Line and the Georgia Southern & Florida railways. There are ten small lakes in the neighbourhood, and the town is a winter and health resort. It is the seat of Columbia College (Baptist, 1907); the Florida Agricultural College was opened here in 1883, became the university of Florida in 1903, and in 1905 was abolished by the Buckman Law. Vegetables and fruits grown for the northern markets, sea-island cotton and tobacco are important products of the surrounding country, and Lake City has some trade in cotton, lumber, phosphates and turpentine. The town was first settled about 1826 as Alligator; it was incorporated in 1854; adopted the present name in 1859; and in 1901, with an enlarged area, was re-incorporated.


LAKE DISTRICT, in England, a district containing all the principal English lakes, and variously termed the Lake Country, Lakeland and “the Lakes.” It falls within the north-western counties of Cumberland, Westmorland and Lancashire (Furness district), about one-half being within the first of these. Although celebrated far outside the confines of Great Britain as a district of remarkable and strongly individual physical beauty, its area is only some 700 sq. m., a circle with radius of 15 m. from the central point covering practically the whole. Within this circle, besides the largest lake, Windermere, is the highest point in England, Scafell Pike; yet Windermere is but 101/2 m. in length, and covers an area of 5.69 sq. m., while Scafell Pike is only 3210 ft. in height. But the lakes show a wonderful variety of character, from open expanse and steep rock-bound shores to picturesque island-groups and soft wooded banks; while the mountains have always a remarkable dignity, less from the profile of their summits than from the bold sweeping lines of their flanks, unbroken by vegetation, and often culminating in sheer cliffs or crags. At their feet, the flat green valley floors of the higher elevations give place in the lower parts to lovely woods. The streams are swift and clear, and numerous small waterfalls are characteristic of the district. To the north, west and south, a flat coastal belt, bordering the Irish Sea, with its inlets Morecambe Bay and Solway Firth, and broadest in the north, marks off the Lake District, while to the east the valleys of the Eden and the Lune divide it from the Pennine mountain system. Geologically, too, it is individual. Its centre is of volcanic rocks, complex in character, while the Coal-measures and New Red Sandstone appear round the edges. The district as a whole is grooved by a main depression, running from north to south along the valleys of St John, Thirlmere, Grasmere and Windermere, surmounting a pass (Dunmail Raise) of only 783 ft.; while a secondary depression, in the same direction, runs along Derwentwater, Borrowdale, Wasdale and Wastwater, but here Sty Head Pass, between Borrowdale and Wasdale, rises to 1600 ft. The centre of the 15-m. radius lies on the lesser heights between Langstrath and Dunmail Raise, which may, however, be the crown of an ancient dome of rocks, “the dissected skeleton of which, worn by the warfare of air and rain