EPIDOTE

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.

www.mindat.org
Smorf link

Samples:

n6 epidoto

9B.1 Epidote  
Fine-grain massive epidote. 

#neso soro silicates

n7 epidoto 9b2

9B.2 Epidote 
Greenish mm-sized crystals of epidote with white albite.

#neso soro silicates