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Investigation of Land Subsidence and Earth Fissures in Cedar Valley, Iron County, Utah (SS-150) Canyonlands National Park The Paradox Basin is a

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The Paradox Basin is a geologic area in southeastern Utah defined by the location of Pennsylvanian salt deposits

water is traveling from the gravel pit towards the region of the principal aquifer of Cache Valley

west-central Utah

Hintze on July 1

Conodont biostratigraphy of Lower Triassic rocks

Investigation of Land Subsidence and Earth Fissures in Cedar Valley, Iron County, Utah (SS-150) Canyonlands National Park The Paradox Basin is aBy: Tyler Knudsen, Paul Inkenbrandt, William Lund, Mike Lowe, and Steve Bowman This 116 page report presents the results of an investigation by the Utah Geological Survey of land subsidence and earth fissures in Cedar Valley, Iron County, Utah. Basin fill sediments of the Cedar Valley Aquifer contain a high percentage of fine grained material susceptible to compaction upon dewatering. Groundwater discharge in excess of recharge (groundwater mining)

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