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Quebrada Ishinca | Laguna Milluacocha

WI_pe038_509.jpg

In 1952, almost the entire trough between these moraine ridges was filled by a glacier tongue, with a small proglacial lake at the front. That lake drained suddenly, the flood eroding a deep breach into the terminal moraine. Since then, the lake has redeveloped to a much larger size - however, at a lower level - due to the retreat of the parent glacier.

Location
View on OpenStreetMap
Created
on Monday 16 July 2018 by Martin Mergili
Visits and license
2828 visits, CC BY-NC-SA 4.0 DEED license