Erosional features in shale, Paria, Utah, USA. Rare events of heavy precipitation have gradually eroded the soft shale strata of the Triassic Chinle formation. Colour differences in the rock strata are due to varying amounts of iron minerals. In the foreground a hoodoo is beginning to form. | |
Licence : | Droits gérés |
Crédit: | Science Photo Library / Alean, Dr. Juerg |
Taille de l’image : | 5760 px × 3840 px |
Model Release : | Non requis |
Property Release : | Non requis |
Restrictions : | - |