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Flood hazards from lakes and failures of dams in Utah (M-111) PECO Magnifier Unconsolidated surficial deposits of Holocene

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Unconsolidated surficial deposits of Holocene to lower Pleistocene

the formation may be somewhat older than the type Judithian because of the close relationship of the fauna to the Aquilan fauna recovered from the underlying Wahweap Formation

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Flood hazards from lakes and failures of dams in Utah (M-111) PECO Magnifier Unconsolidated surficial deposits of HoloceneBy: K. M. Harty and G. E. Christenson Parts of Utah are subject to lake flooding hazards from large fluctuations of lake shorelines and intermittent flooding of dry lakes, mud salt flats, and marshes. The greatest potential for damage from lake flooding is along the Wasatch Front, where much of Utahs population is in close proximity to Great Salt Lake and Utah Lake. Lake flooding hazard elsewhere is more localized and generally confined to the

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