Chemical Formula |
Al3(PO4)2(OH)3 · 5(H2O) |
Composition |
Aluminum phosphate, sometimes with some iron and fluorine |
Variable Formula |
(Al,Fe)3(PO4)2(OH,F)3 · 5(H2O) |
Color |
Light to dark green, yellowish-green, yellow, brown, gray. Rarely white or colorless. May exhibit concentric multicolored zoning in radial cross-sections. |
Streak |
White |
Hardness |
3.5 - 4 |
Crystal System |
Orthorhombic |
Crystal Forms |
Single crystals, which are long prismatic and usually striated, are rare. Most often in radial and radiatingaggregates, and in rounded, ball-shaped clusters of spherulitic masses. Also botryoidal, stalactitic, and acicular. |
Transparency |
Transparent to opaque |
Specific Gravity |
2.3 - 2.4 |
Luster |
Vitreous, pearly |
Cleavage |
1,1;2,2 |
Fracture |
Uneven |
Tenacity |
Brittle |
In Group |
Phosphates; True Phosphates |
Striking Features |
Crystal aggregate habits and mode of occurrence. |
Environment |
As a secondary mineral in the oxidation zone of low-grade metamorphic rocks, epithermal veins, and in phosphate-rich sedimentary deposits. |
Rock Type |
Sedimentary, Metamorphic |
Popularity (1-4) |
2 |
Prevalence (1-3) |
2 |
Demand (1-3) |
2 |
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