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