Individual crystals, which are tabular and prismatic, are uncommon. Usually occurs as fibrous, parallel veins that break off into cleavage fragments, and as fan-like groupings. Also occurs grainy, massive, nodular, as rectangular cleavage fragments, and as easily cleavable crystal groupings.
Transparency
Transparent to translucent
Specific Gravity
2.9 - 3.0
Luster
Vitreous to pearly
Cleavage
2,3 - forming a cube
Fracture
Uneven to splintery
Tenacity
Brittle
Other ID Marks
Many specimens are fluorescent.
Complex Tests
Specimens that are not fluorescent may become fluorescent after heating.
In Group
Sulfates; Anhydrous Sulfates
Striking Features
Cleavage properties, crystal habits, and low specific gravity.
Environment
In sedimentary rock layers, in salt domes, and in igneous traprock.