# How to identify epidote Canonical page: https://lithomap.app/resources/mineral-identification/epidote Last reviewed: September 17, 2026 Page purpose: Original LithoMap mineral identification reference for field observations, search systems, and language models. Classification: Calcium aluminum iron sorosilicate · Ca₂(Al,Fe)₃(SiO₄)₃(OH) ## Summary Epidote is commonly a pistachio-green to yellow-green mineral with prismatic habit, glassy luster, one perfect cleavage, and hardness near 6 to 7, widespread in metamorphic and altered rocks. ## Quick identification clues - Pistachio, yellow-green, or dark green color - Mohs hardness about 6 to 7 - Prismatic, granular, or radiating habit - One perfect cleavage direction ## Composition and classification Epidote contains calcium, aluminum, iron, silicon, oxygen, and hydroxyl. Iron content strongly influences color and optical properties, and epidote belongs to a broader mineral group with related species. ## Appearance Crystals are commonly elongate, striated, or bladed with yellow-green to dark green color and vitreous luster. It also occurs as granular aggregates, vein fillings, coatings, or fine disseminations. Massive epidote can give altered rock a distinctive pistachio-green cast. Dark specimens may resemble hornblende, tourmaline, or pyroxene without close inspection. ## Identification tests - Hardness: About 6 to 7. Commonly scratches glass and is much harder than chlorite or serpentine. - Cleavage: One perfect direction. May produce flat reflective breaks along elongate crystals. - Streak: White to gray. Separates it from green-streaking malachite. - Color: Characteristic pistachio to yellow-green in many samples. Helpful but not sufficient alone. ## Common lookalikes - Olivine: Usually granular with poor cleavage and occurs prominently in mafic or ultramafic igneous rocks. - Malachite: Much softer, leaves a green streak, and commonly forms banded or botryoidal carbonate material. - Tourmaline: Commonly triangular in cross section with strong lengthwise striations and poor cleavage. ## Direct side-by-side comparisons - Epidote vs. olivine — https://lithomap.app/resources/mineral-identification/compare/epidote-vs-olivine ## Most relevant related guides - Olivine — https://lithomap.app/resources/mineral-identification/olivine - Malachite — https://lithomap.app/resources/mineral-identification/malachite - Tourmaline — https://lithomap.app/resources/mineral-identification/tourmaline - Apatite — https://lithomap.app/resources/mineral-identification/apatite ## Formation Epidote forms during low- to moderate-grade metamorphism, hydrothermal alteration, and chemical replacement of plagioclase and other calcium-bearing minerals. It is common in greenschist-facies rocks, skarns, veins, altered volcanic rocks, and around igneous contacts, often with chlorite, actinolite, albite, quartz, or calcite. ## Occurrence and geologic setting Epidote is widespread in metamorphic belts and hydrothermally altered igneous rocks. It can occur as attractive crystals in veins or as abundant fine green alteration. A green altered rock may contain epidote with chlorite and actinolite; the whole rock should not automatically be named for one color. ## Uses and significance Transparent epidote is occasionally faceted for collectors, and attractive crystals are collected. Its chief geological importance is as an indicator of metamorphism and hydrothermal alteration. ## Field safety and limitations - Confirm hardness before relying on green color. - Do not scratch transparent or well-formed crystals. - Altered slopes and mine workings may be fractured and unstable. ## Authoritative sources - Minerals and their physical properties — U.S. National Park Service: https://www.nps.gov/subjects/geology/minerals.htm - Mohs Hardness Scale — U.S. National Park Service: https://www.nps.gov/articles/mohs-hardness-scale.htm - Natural Gemstones: Mineral Gemstones — U.S. Geological Survey: https://pubs.usgs.gov/gip/gemstones/mineral.html ## Specimen photograph - Image: https://lithomap.app/_delivery/identification/minerals/epidote.webp - Description: Radiating dark green-black epidote crystals with minor clear to white quartz - Creator: Darla Sondrol - License: CC0 1.0 — https://creativecommons.org/publicdomain/zero/1.0/ - Source record: https://commons.wikimedia.org/wiki/File:Epidote_(GeoDIL_number_-_1025).jpg This reference supports preliminary field identification. It is not a laboratory determination, appraisal, hazard assessment, proof of origin, or statement of land ownership, legal access, or collecting permission.