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epidote
[ ep-i-doht ]
noun
- a mineral, calcium aluminum iron silicate, Ca 2 (Al, Fe) 3 Si 3 O 12 (OH), occurring in green prismatic crystals.
epidote
/ ˈɛpɪˌdəʊt; ˌɛpɪˈdɒtɪk /
noun
- a green mineral consisting of hydrated calcium iron aluminium silicate in monoclinic crystalline form: common in metamorphic rocks. Formula: Ca 2 (Al,Fe) 3 (SiO 4 ) 3 (OH)
epidote
/ ĕp′ĭ-dōt′ /
- A yellowish-green or blackish-green monoclinic mineral. Epidote occurs as formless grains or as prism-shaped crystals, and is found in limestones that have undergone slight metamorphism or in igneous rocks. Chemical formula: Ca 2 (Al, Fe) 3 (SiO 4 ) 3 OH.
Derived Forms
- epidotic, adjective
Other Words From
- ep·i·dot·ic [ep-i-, dot, -ik], adjective
Word History and Origins
Word History and Origins
Origin of epidote1
Example Sentences
Beneath tents and canopies, on block after block, rested every kind of stone imaginable: the opaque, soapy pastels of angeline; dark, mossy-toned epidote; tourmaline streaked with red and green.
“That’s the iron silicate minerals epidote and chlorite. Those two green minerals are part of the bull’s eye.”
It is usually black in color, opaque, and is related to epidote in form and composition.
The purer beds recrystallize as marbles, but where there has been originally an admixture of sand or clay lime-bearing silicates are formed, such as diopside, epidote, garnet, sphene, vesuvianite, scapolite; with these phlogopite, various felspars, pyrites, quartz and actinolite often occur.
Zoisite, zoi′sīt, n. a mineral closely allied to epidote.
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