Epidote Schist, from Madoc, Ontario.Greenschists are metamorphic rocks that formed under the lowest temperatures and pressures. The green is due to abundant green chlorite, actinolite and epidote minerals that dominate the rock. | |
Licence : | Droits gérés |
Crédit: | Science Photo Library / Degginger, Phil |
Taille de l’image : | 7776 px × 3066 px |
Model Release : | Non requis |
Property Release : | Non requis |
Restrictions : | - |