The purpose of this study is to evaluate the potential for future movement of the landslides during earthquakes to determine the hazard these features may pose. Goals of the study were to: (1) determine when landslide movement occurred, (2) determine the failure mode (lateral spread versus flow failure), (3) determine if recurrent movement has occurred, (4) correlate, where possible, through radiocarbon dating, the timing of landslide movement(s) with the paleoseismic record from fault studies along the Wasatch Front, and (5) assess the current hazard from liquefaction-induced landslides along the Wasatch Front. Once the study was underway, it became evident that not all 13 landslides were liquefaction induced, or even landslides at all. Thus, an additional goal of the study became determining which of the 13 mapped landslides were liquefaction induced, which were not liquefaction induced, and which were formed by other processes. 40 pages + 16 plates
Therefore, summaries of late Quaternary climatic and lacustral conditions (for example, Madsen and Currey, 1979; Currey and James, 1982; Murchison, 1989; Rhode and Madsen, 1995) provide a useful context within which to reconstruct ...
The problem with landslide risk management is that it is seen as a series of events leading to landslide risk reduction. It includes landslide monitoring, mapping, landslide forecast, engineering, slope strengthening, insurance and others.
Guidelines for Evaluating Landslide Hazards in Utah