Larger crystals most commonly have the form of a square prism terminated by a low pyramid, the prism angle being nearly a right angle. The crystals are tetragonal in appearance, though actually orthorhombic. There are perfect cleavages parallel to the faces of the prism. The mineral also often occurs in compact fibrous aggregates, the fibers having a divergent or radial arrangement. Natrolite is readily distinguished from other fibrous zeolites by its optical characteristics. Between crossed
nicols the fibers extinguish parallel to their length, and they do not show an optic figure in convergent
polarized light. Natrolite is usually white or colorless, but sometimes reddish or yellowish. The
luster is vitreous, or, in finely fibrous specimens, silky. The
specific gravity of natrolite is 2.2, and its
hardness is 5.5. The mineral is readily fusible, melting in a candle-flame to which it imparts a yellow color owing to the presence of sodium. It is decomposed by
hydrochloric acid with separation of gelatinous
silica. == Environment ==