1) Hornblende 2) Mineral from a Russian range 
• (n.) Amphibole resulting from the alternation of pyroxene by paramorphism. It is not uncommon in massive eruptive rocks.
Uralite, so called because it was first observed in the Ural Mountains, is an amphibole resulting from the alternation of pyroxene by paramorphism. It is not uncommon in massive eruptive rocks. Uralite is green in colour.
a fibrous, dark-green hornblende formed by the hydrothermal alteration of pyroxene.