As long, thin, prismatic or bladed crystals, usually with a pointed pyramid on top (clinopinacoidal), and very often embedded in a matrix. Fibrous masses, radiating acicular sprays, and interlocking thin prismatic crystals are also common. May also be in reticulated masses and in grainy aggregates embedded in a matrix. Crystals are often striated lengthwise, and doubly terminated crystals are occasionally found.
Transparency
Opaque. Translucent in thin splinters.
Specific Gravity
3.5 - 3.6
Luster
Vitreous
Cleavage
1,2; Prismatic at cleavage angles of 87º and 93º (characteristic of minerals in the pyroxene group).
May also exhibit parting in one direction.
Fracture
Uneven, splintery
Tenacity
Brittle
In Group
Silicates; Inosilicates; Pyroxene Group
Striking Features
Unusually steep crystals and environment
Environment
An important mineral nepheline syenite pegmatites, also in metamorphosed schist and gneiss.