Austinite
A variety of Adelite-descloizite Group
What is Austinite?
Austinite is a rare mineral usually translucent or transparent white or green, but colorless when put up against transmitted light. This mineral may be found alongside metal deposits containing arsenic. Austinite should not be confused with Austenite, which is a form of iron.
Market Value Factors
Pricing varies for every rock and mineral, so use these universal factors to gauge Austinite before comparing listings or appraisals.
Size & Weight
Larger, intact specimens usually command higher prices.
Rarity & Demand
Scarce material or popular varieties sell at a premium.
Condition & Finish
Chips, repairs, and heavy wear lower value; clean prep helps.
Treatment & Provenance
Untreated specimens with documented locality are prized.
Austinite Localities Map
See where Austinite is found with a localities map, collecting zones, and geology context. Generate a sample map preview below.
Key Characteristics
Formation of Austinite
Austinite is a rare mineral in the oxidation zone of arsenic bearing base metal deposits, where it is found developed on the colloform (pertaining to the rounded, globular texture of mineral formed by colloidal precipitation) surface of limonite or lining small cavities. It is closely associated with adamite, and appears to be a later mineral. Austinite is associated with adamite, quartz, talmessite and limonite. Its type locality is Gold Hill Mine (Western Utah Mine), Gold Hill, Gold Hill District (Clifton District), Deep Creek Mts, Tooele County, Utah, US United States.
Composition of Austinite
The structure is composed of chains of edge-sharing polyhedra ZnO6, and very distorted Ca(O,OH)8 polyhedra linked through AsO4 into a three-dimensional network. Any crystal which has a mirror plane as one of its symmetry elements has the property that its mirror image (with any plane as the mirror plane) can always be superimposed on the original crystal by translation or rotation or both. If there are no mirror planes as symmetry elements then the mirror image of a crystal cannot be brought into superposition with the original crystal by rotation or translation. This is enantiomorphism, and the mirror images are said to be enantiomorphs of each other. The possibility of enantiomorphic crystals is determined by the crystal symmetry, i.e., by the point group of the crystal species. There are 32 possible point groups, and 22 of these are capable of forming enantiomorphs. The enantiomorphs are designated right or left handed, according to whether they rotate the plane of polarised light to the right or to the left. Sometimes it is clear from the outward form of the crystal whether it is right or left handed, and sometimes optical methods are needed to determine this. The commonest enantiomorphic mineral is quartz, with point group 32; all quartz crystals will be either right or left handed, but it may not be possible to distinguish this from the external form unless some critical crystal faces are present. Austinite has point group 222, with no mirror planes, so austinite is also an enantiomorphic mineral, occurring as both right handed and left handed crystals, with right handed ones more common.
Health & Safety Information
- ⚠️Austinite dust is toxic because it contains heavy metals Arsenic.
- ⚠️Arsenic
- ⚠️It's advisable to handle austinite carefully to avoid generating dust and wash hands thoroughly afterward. When cutting or polishing austinite, wear a dust mask to prevent inhaling heavy metal particles. Store austinite in a sealed container in a well-ventilated area, away from children and pets. For those involved in crystal healing, never put it in your mouth.
Quick Facts
Physical Properties
- Color
- Colorless to pale yellowish white or bright green, colourless
- Hardness (Mohs)
- 4 - 4.5
- Density
- 4.31 g/cm³
- Streak
- White
- Luster
- Greasy, Silky, Sub-vitreous, Sub-adamantine
- Crystal System
- Orthorhombic
Chemical Properties
- Chemical Formula
- CaZn(AsO4)(OH)
- Elements
- As, Ca, H, O, Zn
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Austinite FAQs
How do I identify Austinite?
Austinite can be identified by its hardness of 4 - 4.5 on the Mohs scale, Colorless to pale yellowish white or bright green color, Greasy, Silky, Sub-vitreous, Sub-adamantine luster, Orthorhombic crystal system. Look for these key characteristics when examining specimens.
What color is Austinite?
Austinite typically appears in Colorless to pale yellowish white or bright green, colourless. Color can vary depending on impurities and formation conditions.
How hard is Austinite?
Austinite has a hardness of 4 - 4.5 on the Mohs scale. This gives it moderate hardness.
What is the formation of austinite of Austinite?
Austinite is a rare mineral in the oxidation zone of arsenic bearing base metal deposits, where it is found developed on the colloform (pertaining to the rounded, globular texture of mineral formed by colloidal precipitation) surface of limonite or lining small cavities. It is closely associated with adamite, and appears to be a later mineral. Austinite is associated with adamite, quartz, talmessite and limonite. Its type locality is Gold Hill Mine (Western Utah Mine), Gold Hill, Gold Hill District (Clifton District), Deep Creek Mts, Tooele County, Utah, US United States.
What is the composition of austinite of Austinite?
The structure is composed of chains of edge-sharing polyhedra ZnO6, and very distorted Ca(O,OH)8 polyhedra linked through AsO4 into a three-dimensional network. Any crystal which has a mirror plane as one of its symmetry elements has the property that its mirror image (with any plane as the mirror plane) can always be superimposed on the original crystal by translation or rotation or both. If there are no mirror planes as symmetry elements then the mirror image of a crystal cannot be brought into superposition with the original crystal by rotation or translation. This is enantiomorphism, and the mirror images are said to be enantiomorphs of each other. The possibility of enantiomorphic crystals is determined by the crystal symmetry, i.e., by the point group of the crystal species. There are 32 possible point groups, and 22 of these are capable of forming enantiomorphs. The enantiomorphs are designated right or left handed, according to whether they rotate the plane of polarised light to the right or to the left. Sometimes it is clear from the outward form of the crystal whether it is right or left handed, and sometimes optical methods are needed to determine this. The commonest enantiomorphic mineral is quartz, with point group 32; all quartz crystals will be either right or left handed, but it may not be possible to distinguish this from the external form unless some critical crystal faces are present. Austinite has point group 222, with no mirror planes, so austinite is also an enantiomorphic mineral, occurring as both right handed and left handed crystals, with right handed ones more common.
