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Quebrada de Las Conchas

WI_ar317n.jpg

View in S direction (upstream). The Quebrada de Las Conchas is deeply incised into a sequence of uplifted, tilted, and folded sedimentary rocks of Cretaceous age, connecting the the tectonic grabens of the Valles Calchaquíes and the Valle de Lerma.

Location
View on OpenStreetMap
Created
on Monday 12 February 2018 by Martin Mergili
Visits and license
7341 visits, CC BY-NC-SA 4.0 DEED license