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The geology of the Snyderville basin, western Summit County, Utah, and its relation to ground-water conditions (WRB-28) Self Reliance

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The geology of the Snyderville basin, western Summit County, Utah, and its relation to ground-water conditions (WRB-28) Self RelianceBy: F. X. Ashland, C. E. Bishop, M. Lowe, and B. H. Mayes, editors Urbanization of parts of the Snyderville basin has been accompanied by an increasing demand to develop the area? s ground water resources. Ground water is present in shallow unconsolidated deposits and fractured rock. Because of the limited extent and thickness of the unconsolidated deposits, the ground water resources in fractured rock have a greater potential for future development.

Book Cliffs

George basin near the southwest corner of Utah

about eight miles

making it simple for the reader to retrace the author's steps and visit these monuments to perseverance

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Schumacher Society

and more detailed features upon closer inspection

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