Chemical Formula |
S |
Composition |
Sulfur |
Color |
Bright yellow to yellow-brown |
Streak |
White |
Hardness |
1.5 - 2.5 |
Crystal System |
Orthorhombic |
Crystal Forms |
Steep dipyramidal and tabular crystals are common. May also be bipyramidal with angled centers. Crystals frequently have hollow skeletons or hoppered growths. Curved and rounded distorted crystals are also common. Small grains, wheat sheaves, and encrustings occur. Massive, earthyspecimens are prevalent, and may have bubbly holes throughout. Also occurs as rounded, waterwornmasses. |
Transparency |
Transparent to opaque |
Specific Gravity |
2.0 - 2.1 |
Luster |
Adamantine on clean, clear crystal surfaces; otherwise resinous or dull |
Cleavage |
3,2 |
Fracture |
Conchoidal |
Tenacity |
Brittle |
Other ID Marks |
1) Cracks when exposed to heat |
Complex Tests |
Melts at only 226° F (108° C) and gives off a blue flame with fumes that smell like rotten eggs |
In Group |
Native Elements; Non-Metallic Elements |
Striking Features |
Color, softness, very low density, and habit of cracking when exposed to heat. |
Environment |
In sedimentary environments in evaporite and salt dome deposits, where it often is a product of breakdown of sulfates caused by cetain bacteria. In volcanic deposits in hot springs and fumaroles as a product of sublimation. Also occurs in igneous basalt rocks of recent volcanic activity. |
Rock Type |
Igneous, Sedimentary |
Popularity (1-4) |
1 |
Prevalence (1-3) |
1 |
Demand (1-3) |
1 |
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