Radar Structure of Earthquake-Induced, Coastal Landslides in Anchorage, Alaska
Figure 2
Geologic cross sections through the (A) Government Hill and (B) Turnagain Heights landslides were derived from trench exposures and borings shortly after the 1964 earthquake (Hansen, 1965; Seed and Wilson, 1967). Dashed lines approximate the prequake ground surface. Scales are the same in each diagram with no vertical exaggeration.
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