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Quebrada de Las Conchas |
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View in S direction (upstream). The Quebrada de Las Conchas connects the tectonic grabens of the Valles Calchaquíes and the Valle de Lerma. It is deeply incised into a sequence of uplifted, tilted, and folded sedimentary rocks of Cretaceous age.
- Location
- View on OpenStreetMap
- Created
- on Monday 12 February 2018 by Martin Mergili
- Region
- Keywords
- cloudscape, fluvial erosion, fluvial processes, fluvial sedimentation, geodiversity, hot deserts, mountainscape, sedimentary rocks, tectonics, time series, Zonobiome III
- Visits and license
- 8815 visits, CC BY-NC-SA 4.0 DEED license