Ground-water-level fluctuations in Wasatch Front landslides and adjacent slopes, northern Utah (OFR-448) Paleogeography The Basin is bounded by

The Basin is bounded by the Uncompahgre Uplift to the east and north

To improve the understanding of landslides and their distribution throughout Utah

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The steeply west-dipping Wasatch fault zone trends slightly east of north through the quadrangle and separates Juab Valley on the west from the Wasatch Mountains on the east

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Ground-water-level fluctuations in Wasatch Front landslides and adjacent slopes, northern Utah (OFR-448) Paleogeography The Basin is bounded byBy: F. X. Ashland, R. E. Giraud, and G. N. McDonald We monitored ground water levels in and adjacent to five Wasatch Front landslides to document seasonal and intermediate term ground water level fluctuations that can be used to estimate design ground water levels in landslide and slope stability analyses. Our data span a relative drought period (1999 2003), but locally document the effects of wetter than normal precipitation on ground water levels in