The geology of the Snyderville basin, western Summit County, Utah, and its relation to ground-water conditions (WRB-28) Self Reliance Part 2: Utah

Part 2: Utah

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

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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 Part 2: UtahBy: 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.