Bellecombe, Châtillon, Aosta Valley, Italy
Ca2(Al2Fe3+)(Si2O7)(SiO4)O(OH)
Crystal System: monoclinic
Colour: yellowish-green, green, brownish-green or black
Habitus: prismatic
Hardness: 6
Fracture: irregular/uneven
Density: 3.43 g/cm3
Origin and geological occurrence: epidote is a mineral (belonging to the epidote supergroup) typical of several facies of regionally metamorphosed rocks and in contact metamorphism (e.g., in marbles). It occurs also in some contaminated felsic magmatic rocks. It can be the product of hydrothermal alteration of plagioclase.
Samples:
9B.1 Epidote #neso soro silicates |
|
9B.2 Epidote #neso soro silicates |