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Many landslides and debris flows have originated from Mount Rainier since the retreat of glaciers from Puget Sound about 10,000
years ago. The recurrent instability is due to several factors--height of the steep-sided volcanic cone, frequent volcanic activity,
continuous weakening of rock by steam and hot, chemical-laden water, and exposure of unstable areas as the mountains glaciers
have receded. the landslide scars and deposits tell a
fascinating story of the changing shape of the volcano.
-- Scott and Vallance, 1993
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