Canyons of the Colorado by J. W. Powell
page 36 of 264 (13%)
page 36 of 264 (13%)
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the valley stand the Gros Ventre and the Wyoming mountains, low ranges
of peaks, but picturesque in form and forest stretch. Leaving the mountain, the river meanders through the Green River Plains, a cold elevated district much like that of northern Norway, except that the humidity of Norway is replaced by the aridity of Wyoming. South of the plains the Big Sandy joins the Green from the east. South of the Big Sandy a long zone of sand-dunes stretches eastward. The western winds blowing up the valley drift these sands from hill to hill, so that the hills themselves are slowly journeying eastward on the wings of arid gales, and sand tempests may be encountered more terrible than storms of snow or hail. Here the northern boundary of the Plateau Province is found, for mesas and high table-lands are found on either side of the river. On the east side of the Green, mesas and plateaus have irregular escarpments with points extending into the valleys, and between these points canyons come down that head in the highlands. Everywhere the escarpments are fringed with outlying buttes. Many portions of the region are characterized by bad lands. These are hills carved out of sandstone, shales, and easily disintegrated rocks, which present many fantastic forms and are highly colored in a great variety of tint and tone, and everywhere they are naked of vegetation. Now and then low mountains crown the plateaus. Altogether it is a region of desolation. Through the midst of the country, from east to west, flows an intermittent stream known as Bitter Creek. In seasons of rain it carries floods; in seasons of drought it disappears in the sands, and its waters are alkaline and often poisonous. Stretches of bad-land desert are interrupted by other stretches of sage plain, and on the high lands gnarled and picturesque forests of juniper and pinon are found. On the west side of the river the mesas rise by grassy slopes to the westward |
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