Lead chloro-arsenate. The arsenate radical (AsO4) may be partially replaced by a phosphate radical (PO4) or vanadate radical (VO4), and thereby forms a series with Pyromorphite and Vanadinite.
Variable Formula
Pb5([As,P,V]O4)3Cl
Color
Light yellow, lemon-yellow, dark yellow, orange, brown, reddish-brown, and yellow-green. Rarely colorless or white. May also be multicolored orange, yellow, and greenish-yellow.
Streak
White
Hardness
3.5 - 4
Crystal System
Hexagonal
Crystal Forms and Aggregates
Occurs in small, slender, prismatic crystals and in mammilary and botryoidal crusts. A rare habit is large, stubby, hexagonal crystals. Also occurs as wedge-shaped crystals, acicular, radiating, reniform, encrusting, and in curvy and fibrous aggregates. Some larger crystals may be hollowed out on the ends or have a hopper growth pattern.
Transparency
Transparent to translucent
Specific Gravity
7.0 - 7.3
Luster
Resinous to adamantine
Cleavage
Indiscernible
Fracture
Subconchoidal to uneven
Tenacity
Brittle
Complex Tests
1) Dissolves in hydrochloric acid
2) Gives off a strong garlic odor if heated (fumes are poisonous!)
In Group
Phosphates; Arsenates
Striking Features
Color, crystal habits, mineral associates, and mode of occurrence.
Environment
As a secondary mineral in the oxidation zone of lead ore deposits.