Excerpt from Underground Water in Sanpete and Central Sevier Valleys, Utah Sevier Plateau forms the greater part of the eastern boundary of Sevier Valley, above which it rises abruptly, and extends from the valley. Of Lost Creek far to the south of the area under consideration. Its culminating point is Monroe Peak, whose elevation is feet. The plateau is underlain by a series of igneous rocks, chiefly Tertiary tuffs and lavas. The East Fork of Sevier River receives a considerable part of the drainage of Sevier Plateau, but Monroe Creek is the only important stream that drains directly from it into the area here considered. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.