Radar Structure of Earthquake-Induced, Coastal Landslides in Anchorage, Alaska

Figure 8

GPR profile across eastern side of Turnagain Heights landslide. Slide deposits are intensely deformed and lack the
layercake stratigraphy of the original bluff. Depths are based on radar velocity of 0.10 m/ns. ns, nanosecond; sg, sand and gravel.

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