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The bare earth model has
also allowed for distinction of other larger scale features on other parts of
the mountain. While the main focus of
studies over the past 100 years has been on the 1903 slide (right) and South
Peak, we are now seeing features with the bare earth model that were not
obvious with the vegetation obscuring the slope. The feature on the left appears to be some
sort of historical movement that may have been rapid and of similar magnitude
to the 1903 slide.
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