Epidote - Wikipedia Epidote is an abundant rock-forming mineral, but one of secondary origin It occurs in marble and schistose rocks of metamorphic origin It is also a product of hydrothermal alteration of various minerals (feldspars, micas, pyroxenes, amphiboles, garnets, and others) composing igneous rocks
Epidote: A metamorphic mineral and silicate mineral group. Epidote is the word used for a calcium-iron silicate mineral that forms through regional and contact metamorphism It is also the name of a diverse group of silicate minerals that often contain rare earth elements
Epidote Meanings and Crystal Properties - The Crystal Council Epidote is an aluminum-iron mineral that can be found in either crystal or stone form The stone was first described in 1801 by R J Hauy and was named after the Greek word meaning to “increase” They are commonly found in Norway, U S A, and Brazil, which has been known to have the nicest crystallized forms of Epidote ever seen
Epidote: Mineral information, data and localities. - mindat. org Epidote Group > Epidote Supergroup Name: Named in 1801 by Rene Just Haüy from the Greek επιδοσιζ ("epidosis"), meaning "increase", in allusion to the crystal characteristic of one longer side at the base of the prism
Epidote Group Minerals | Properties, Occurrence, Uses » Gemstone Epidote is a mineral that belongs to the sorosilicate group and is known for its distinct green to yellow-green color It is widely found in metamorphic rocks, igneous rocks, and hydrothermal veins
Epidote: Properties, Occurrence, Uses – Geology In Epidote is a mineral belonging to the sorosilicate group, primarily composed of calcium, aluminum, iron, and silica It typically occurs in metamorphic rocks, where it forms as a result of the alteration of primary minerals under high-pressure and temperature conditions
Epidote | Definition, Formula, Uses, Facts | Britannica epidote, any of a group of colourless to green or yellow-green silicate minerals with the general chemical formula A2B3 (SiO 4) (Si 2 O 7)O (OH), in which A is usually calcium (Ca), though manganese (Mn) or cerium (Ce) is sometimes substituted, and B is generally aluminum (Al), with the main substitution being ferric iron (Fe +3)