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International research Center for Earth Environment & water
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Reposted by International research Center for Earth Environment & water
It is sourced in deglacial glaciolacustrine sediments along the Takhini River. This more vertical view shows the mobility of the flows and active zones in the head scarp. The left side of the main slide and the entirety of the satellite slide are active. In 2023 it retrogressed 13 m.
June 27, 2025 at 1:02 AM