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Dominant species
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Scorodite
Scorodite
Chemical
Formula
FeAsO4·2H2O
Species
Phosphates
Crystal
System
Orthorhombic
Mohs
Scale
3-4
Specific
Gravity
3.276
Color
Green, blue-green, grey, grayish-green, blue, yellow-brown, nearly colourless, Purple; colourless to faintly greenish or greenish brown in transmitted light.
Streak
Greenish-White
Luster
Sub-Adamantine, Vitreous, Resinous
Refractive
Index
n = 1.741 - 1.784 n = 1.744 - 1.805 n = 1.768 - 1.820
Diaphaneity
Translucent
Cleavage
Imperfect/FairImperfect on , traces on
Fracture
Sub-Conchoidal
Crystal Habit:Crystals commonly pyramidal (sometimes pseudo-octahedral), tabular , or prismatic. Commonly aggregated into crusts or irregular groups. Also occurs massive, crystalline or porous and sinter-like, earthy.
Geological Setting:In the secondary oxidation zone of iron bearing arsenides, in gossans; also observed in a primary hydrothermal deposit (Saubach).
Scorodite is a common hydrated iron arsenate mineral, with the chemical formula FeAsO4·2H2O. It is found in hydrothermal deposits and as a secondary mineral in gossans worldwide. Scorodite weathers to limonite.

Scorodite was discovered in the Schwarzenberg, Saxony district, Erzgebirge, Saxony, Germany. Named from the Greek Scorodion, "garlicky". When heated it smells of garlic, which gives it the name.