Caption
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
Mar 27, 2019
Credit line
Photo12/imageBROKER/Ian Murray
Reference
BRK24B29_476
Model release
NA
Property release
NA
License type
Rights managed
Available size
63,3Mb (4,5Mb) / 19,2in x 12,8in / 5760 x 3840 (300dpi)