Epidote
This article is largely based on an article in the out-of-copyright Encyclopædia Britannica Eleventh Edition, which was produced in 1911. (November 2019) |
Epidote | ||
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Specific gravity 3.38–3.49 | | |
Optical properties | Biaxial (-) | |
Refractive index | nα = 1.715–1.751 nβ = 1.725–1.784 nγ = 1.734–1.797 | |
Birefringence | δ = 0.019–0.046 | |
Pleochroism | Strong | |
References | [2][3][4] |
Epidote is a
Description
Well developed crystals of epidote, Ca2Al2(Fe3+;Al)(SiO4)(Si2O7)O(OH),
, is derived from the Greek word "epidosis" (ἐπίδοσις) which means "addition" in allusion to one side of the ideal prism being longer than the other.Epidote is an abundant rock-forming mineral, but one of secondary origin. It occurs in
The perfectly transparent, dark green crystals from the Knappenwand and from Brazil have occasionally been cut as gemstones.[6] The green part of several mixed-rock ornamental stones is composed of epidote. These include Unakite and Australian Dragon Bloodstone.
Related species
Belonging to the same isomorphous group with epidote are the REE-rich allanite (containing primarily lanthanum, cerium, and yttrium), and the manganese-rich piemontite.
Piemontite occurs as small, reddish-black, monoclinic crystals in the manganese mines at San Marcel, near Ivrea in Piedmont, and in crystalline schists at several places in Japan. The purple color of the Egyptian porfido rosso antico is due to the presence of this mineral.[6]
Allanite and
Gallery
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Epidote from Alaska
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Deformed epidote within greenschist rock from Itogon, Philippines
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Sample of dollaseite (dark brown matrix at arrow points) from Sweden
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Well-developed epidote prismatic crystals from Russia
References
- S2CID 235729616.
- ^ Epidote. Handbook of Mineralogy
- ^ Epidote. Mindat
- ^ Epidote. Webmineral
- ^ "About Epidote".
- ^ a b c d e public domain: Spencer, Leonard James (1911). "Epidote". In Chisholm, Hugh (ed.). Encyclopædia Britannica. Vol. 9 (11th ed.). Cambridge University Press. p. 689. One or more of the preceding sentences incorporates text from a publication now in the