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)