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epidote    
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  • 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”
  • Epidote: Mineral information, data and localities.
    Epidote mineral data, information about Epidote, its properties and worldwide locations
  • Epidote Crystal Guide 2026: Meaning, Twinning, Value Healing
    Epidote is a calcium aluminum iron sorosilicate mineral belonging to the epidote-supergroup family, crystallizing in the monoclinic system and most commonly forming elongated prismatic crystals
  • Epidote: Meaning, Properties, and Uses - Wisdom Of The Spirit
    Epidote is a silicate mineral that forms in metamorphic and igneous rocks Its name comes from the Greek word epidosis, meaning “increase” or “addition,” referring to its elongated crystal structure
  • Epidote | Definition, Formula, Uses, Facts | Britannica
    Epidote, any of a group of colorless to green or yellow-green silicate minerals
  • What Is Epidote? Its Properties, Formation, and Uses
    Epidote is a common rock-forming mineral that is widely recognized for its characteristic green coloration, often exhibiting a distinctive pistachio shade This mineral is an abundant silicate of secondary origin, meaning it forms after the host rock has already crystallized
  • Epidote Mineral Data
    Regular - Flat surfaces (not cleavage) fractured in a regular pattern Fibrous - Crystals made up of fibers Massive - Uniformly indistinguishable crystals forming large masses Prismatic - Crystals Shaped like Slender Prisms (e g tourmaline) Non-fluorescent
  • Epidote - Sandatlas
    Epidote is a very common hydrothermal alteration mineral This alteration process, if it happens with feldspars, is known as epidotization Saussuritization is a hydrothermal alteration of plagioclase feldspar which yields epidote It is usually found in mafic igneous rocks





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