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<br /> <br />I <br /> <br />002924 <br /> <br />I <br /> <br />The eastern end of the Uinta }~untains extends in an east-west alignment <br />across the southwestern corner of the basin. This area consists of a <br />central platform with broad slopes about 8,000 feet in elevation and <br />bordered by abrupt slopes on the north and south. The most outstanding <br />features of this area are the spectacular canyons cut through the moun- <br />tain range to depths of as much as 3,000 feet by the Green and Yampa <br />rivers. The Green River flows southward through the Loclore Canyon and <br />the Yampa River flows westward through the Bear Canyon to their conflu- <br />ence at Echo Park in Dinosaur N~tional Monument. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />,- <br />I <br /> <br /> <br />. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />-. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Echo Park in Dinosaur ~ational Monument <br /> <br />I <br /> <br />The remainder of the Yampa River Basin, lying within the Wyoming Basin <br />physiographic province, is an area of diverse topography containing <br />broad plains, gently-sloping ridges, and rough badlands interspersed with <br />hogback ridges and low mountains. Most of the area lies between 6,500 <br />and 7,500 feet elevation. Low dunes of sand and silt are locally prom- <br />inent features, especially in alkali areas ~here the scarcity of vegeta- <br />tion permits the soil to drift into low hummocks. <br /> <br />I <br /> <br />I <br /> <br />- 5 - <br /> <br />I <br /> <br />