Légende
Strata of sandstone sedimentary rock in a coastal cliff with layers folded down to form a geological structure called a syncline, near Zambujeiro do Mar, Alentejo Littoral, Portugal, southern Europe. A syncline is a trough or fold of stratified rock in which the strata slope upwards from the axis. Folds typically form during crustal deformation as the result of compression that accompanies orogenic mountain building, Europe
Date
27 mars 2019
Crédit
Photo12/imageBROKER/Ian Murray
Notre référence
BRK24B29_476
Model release
NA
Property release
NA
Licence
Droits gérés
Format disponible
63,3Mo (4,5Mo) / 48,8cm x 32,5cm / 5760 x 3840 (300dpi)