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
2) Dissolves in warm water
3) May have a greasy feel
4) Gives off a mild, sulfuric odor. Odor becomes strong if heated.
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.