WYOMING, a State in the western divisions of the North American Union; bounded by Montana, South Dakota, Nebraska, Colorado, Utah, and Idaho; admitted July 10, 1890; capital Chey enne; counties 14; area, 97,914 square miles; pop. (1890) 60,705; (1900) 92, 531; (1910) 145,965; (1920) 194,402.
surface of the State is very rugged, being diversified by moun tains, valleys, plains, and plateaus, the latter covered with grasses of great nutrition and furnishing admirable pas ture for live stock. The main range of the Rocky Mountains enters the State from the S. terminating in the Wind River Mountains, with an altitude of from 10,000 to 14,000 feet, and snow capped the entire year. The Shoshone Mountains extend N. of the Wind River range. Running S. from the N. bound ary to the center of the State are the Big Horn Mountains. Other notable ranges are the Sweetwater, Rattlesnake, Med icine Bow, and Sierra Madre. The high est peak is Fremont's Peak, in the Wind River range, 13,790 feet. Other high points are Grand Teton Peak, 13,690 feet ; Mount Sheridan, 13,691 feet, and Atlantic Peak, 12,700 feet. The princi pal rivers, are the North Platte, enter ing the State from Colorado; Green river flowing S. E. into Utah; Snake or Sho shone river, rising in Yellowstone Park, flows into Idaho; the Yellowstone; Big Horn; Cheyenne; Belle Fourche; and Powder. None of these streams are navigable in a commercial sense, but they furnish water for the irrigation and development of the surrounding country, and in some instances are used for the transportation of timber. There are several important lakes, including Yellowstone Lake in Yellowstone Park, the N. W. corner of the State; Jackson's; Shoshone; Lewis; Madison; Fremont; Boulder, and Uradisa.
Geology and geolog ical formations of Wyoming cover nearly every age, and though not thoroughly ex plored are known to contain at least the Tertiary, Carboniferous, Cretaceous, Eozoic, Silurian, Triassic, Jurassic, Devo nian, and Volcanic. The mineral produc tions are quite extensive, including cop per, gold and silver, coal, iron, oil, soda, and building stones. The oil belt extends
entirely across the State from S. W. to N. E.
Mineral Production.—The coal produc tion in 1919 was 7,100,000 tons, a de 2rease over the production of 1917 of over 2,000,000 tons. The production of petroleum in 1918 was 12,596,287 barrels, valued at $18,159,778. Iron ore is pro duced in considerable quantities. The production of natural gas in 1918 was 4,338,840 thousand cubic feet, valued at $156,171. A small amount of gold is produced, as well as stone and phosphate rock.
soil of the moun tains and high plateaus is a light sandy loam; darker and richer in the valleys, slightly alkaline, but, under irrigation producing large crops. It is estimated that 10,000,000 acres of the State are suitable for agricultural purposes by irrigation. The acreage, production and value of the principal crops in 1919 was as follows : corn, 48,000 acres, produc tion 768,000 bushels, value $1,267,000; oats, 315,000 acres, production 5,670,000 bushels, value $6,350,000; barley, 35,000 acres, production 525,000 bushels, value $919,000; wheat, 284,000 acres, produc tion 4,008,000 bushels, value $8,497,000; hay, 605,000 acres, production 853,000 tons, value $19,619,000; potatoes, 33,000 acres, production 2,640,000 bushels, value $5,016,000.
were in 1914 337 manufacturing establishments, em ploying 2,989 wage earners. The capital invested was $29,270,000; the amount paid in wages $2,312,000; the value of materials used $5,560,000; and the value of the finished product $11,224,000. The chief manufactures included railroad cars and railroad supplies, lumber and timber products, saddlery and harness. tobacco, boots and shoes, millinery, brooms, flour and grist, lime and cement, and malt.
Oct. 31, 1919, there were reported 43 National banks in oper ation, having $2,350,000 in capital, $1,855,000 in outstanding circulation; and $6,827,000 in United States bonds. There were also 101 State banks, having $2,390,000 capital, and $868,000 surplus.