USGS PCMSC

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

Figure 2

Geologic cross sections through the Government Hill and Turnagain Heights landslides.

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.

Back arrowBack to Report

geotech/radaraapg/fig2.html
contact: Robert Kayen
last modified 2018