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Quebrada de las Conchas

View in S direction (upstream). The Quebrada de las Conchas is a transverse valley deeply incised into a sequence of uplifted, tilted, and folded sedimentary rocks of Cretaceous age, connecting the Valles Calchaquíes and the Valle de Lerma.
- Keywords
- fluvial erosion, fluvial processes, fluvial sedimentation, hot deserts, mountainscape, sedimentary rocks, tectonics, Zonobiome III
- Created
- Monday 12 February 2018 by Martin Mergili in South America / Argentina (1370 visits)