Silicon dioxide. Its purple coloring is usually caused by impurities of iron or manganese compounds.
Color
Light to dark purple. Sometimes banded with purple and whitish lines. May also be mixed together with Citrine.
Streak
White
Hardness
7
Crystal System
Hexagonal
Crystal Forms
and Aggregates
Most often as protruding clusters of pyramids on a matrix base. These "pyramids" can be quite large. Also occurs as tall prismatic crystals, as short stubby crystals, in drusy aggregates, massive, in geodes, and as rounded waterworn stones. A very interesting habit is as crystalline crusts inside volcanic pipes. Crystals are usually striated horizontally, and occasionally have a scepter growth.
Transparency
Transparent to translucent
Specific Gravity
2.6 - 2.7
Luster
Vitreous
Cleavage
Indiscernible
Fracture
Conchoidal
Tenacity
Brittle
Other ID Marks
Occasionally fluorescent cream or white in shortwave ultraviolet light.
Complex Tests
Dissolves in hydrofluoric acid.
In Group
Silicates; Tectosilicates; Silica Group
Striking Features
Color, crystal habits, and hardness.
Environment
Occurs in all mineral environments, especially in igneous environments.