La Olla, Aliaga Geological Park
by Elena Núñez-Guerrero, University of Salamanca, Salamanca, Spain
The picture shows an anticlinal vertical axis crease in lower Cretaceous materials whose deposits are the consequence of marine transgression which formed a shallow carbonated platform in the Iberian basin, south of the Ebro Massif, where communities of foraminifera, mollusks and echinoderms growed up.
Taken on 20
July
2015
Submitted on 10 Feb 2020
Categories
- Field (2721)
- Geodynamics (353)
- Stratigraphy, Sedimentology and Palaeontology (480)
- Tectonics and Structural Geology (534)
Location
- Europe (3439)
- Southern Europe (1495)
- Spain (721)
- Exact location (-0.7023 W, 40.6735 N)
Tags
geodynamics, field, tectonics, stratigraphy, paleontology
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Camera:
Nikon D70
Licence
Credit: Elena Núñez-Guerrero (distributed via imaggeo.egu.eu)
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