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<br />~~ <br />TOPOGRAPHY <br />16 <br />The Virgin River basin, lying .along the boundary {Grand Wash <br />Cliffs) between the Colorado Plateau and the Great Basin, is a land <br />of contrasting topography (Figure 1). The major structural feature <br />of the basin is the Hurricane fault ~rhich roughly divides the basin. <br />into tiro dissimilar topographic areas separated somewhat by the low- <br />lying St. George basin (Cook ]960). To the east of the St. George <br />basin and the Hurricane fault lie the strikingly colorful mesas and <br />plateaus of the Colorado Plateau region. The topography to the west <br />and north of the St. George basin is characteristic of the Basin and <br />Range province. <br />The Colorado Plateau is typified by strata-that lie more or less <br />horizontal and have been eroded .into plateaus, mesas and deep canyons. <br />The topography is due to differential uplift of segments of the earth's <br />crust along northward-trending faults producing a series of terrace- <br />]ike steps (Cook 1960, Ives 1947) that lead from the Grand Canyon <br />to the high plateaus of Utah 80 km to the north. A number.of faults <br />and monoclines roughly paralleling the Hurricane fault divide each <br />terrace step into a series of plateaus. One of these faults, the <br />Sevier fault, determines the eastern boundary of the Virgin River <br />basin along the East Fork. The regional dip of the plateaus is <br />northeasterly but averages about one degree in 160 km {Gardner 1941). <br />