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Encyclopedia Britannica - Main :: MIC-MOL |
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MICHIGAN, LAKE , the only one of the great lakes of North America wholly within the boundaries of the United States, and the second largest body
touch its S. end. It is 32o m. long, and has an average width of 65 m. The maximum depth recorded by the United States Lake Survey is87o ft.; the mean level of the surface is 5811 ft. above mean sea-level, being the same as that of Lake Huron and 21 ft. below that of Lake Superior. Its area is 22,400 sq. m., and it has a basin 68,100 sq. m. in area.The shores of Lake Michigan are generally low and sandy, and the land slopes gradually to the water. The northern shore of the lake is irregular and more rugged and picturesque than the other shores, the summit of the highest peak being about 1400 ft. above the sea. On the eastern side are numerous sand hills, formed by the wind into innumerable fantastic shapes, sometimes covered with stunted trees and scanty vegetation, but usually bare and rising to heights of from 150 to 250 ft. The south-western shore is generally low, with sand hills covered with shrivelled pines and bur oaks. Along the western shore woods and prairies alternate, interspersed with a few high peaks. The cliffs on the east shore of Green Bay form a bold escarpment, and from this ridge
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The lake is practically tideless, though true tidal pulsations amounting to 3 M. in height are stated to have been observed in Chicago. In the water of the lake there is a general set of current towards the outlet at the strait of Mackinac, following the east shore, with slight circular currents in the main portion of the lake and at the northern end around Beaver island. These currents vary in speed from 4 to 10 M. per day. Surface currents are set up by prevailing winds, which also seriously affect water levels, lowering the water at Chicago and raising it at the strait, or the reverse, so as greatly to inconvenience navigation. The level of the lake is subject to seasonal fluctuations, reaching a maximum in midsummer and a minimum in February, as well as to alternating cycles of years of high and low water. Standard high-water of 1838 was 3.36 ft. above mean level and standard low-water of 1895, 2.82 ft. below that datum, giving an extreme recorded range slightly over 6 ft. The northern portion of the lake only is covered with ice in winter, and ice never reaches as far south as Milwaukee. Milwaukee River remains closed on an average for one hundred daysfrom the beginning of December to the middle of March. The average date of the opening and closing of navigation at the strait of Mackinac, where the ice remains longest, is the 17th of April and the 9th of January respectively.l Regular lines of steamers specially equipped to meet winter conditions, most of them being car ferries, cross the lake and the strait of Mackinac all winter between the various ports. No notable rivers flow into Lake Michigan, the largest being the Big Manistee and Muskegon on the east shore, and on the west shore the Menominee and the Fox, both of which empty into Green Bay, the most important arm of the lake. The numerous harbours are chiefly artificial, usually located at the mouths of streams,- the improvements consisting of two parallel piers extending into the lake and protecting a dredged channel. Sand bars keep filling up the mouths of these channels, necessitating frequent dredging and extension of the breakwaters, work
1 Report of Deep Waterways Commission (1896). Chicago, the principal port on the lake, is at its south-west extremity, and is remarkable for the volume of its trade, the number of vessels arriving and departing exceeding that of any port in the United States, though the tonnage is less than that of New York
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