How to identify Stilbite
Stilbite-Ca
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Open the appTo correctly identify Stilbite (Stilbite-Ca), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.
Step-by-step identification
- 1
Color
Overall color and any zoning or banding
White, colorless, pink, salmon, yellow, brown, reddish-brown. Often pale.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous to pearly, especially on cleavage surfaces.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Typically forms radiating, sheaf-like, or bow-tie aggregates. Individual crystals are tabular.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Monoclinic, often forming tabular crystals elongated along [100], frequently twinned to produce characteristic sheaf-like or bow-tie aggregates. Also found as divergent, fibrous, or granular masses.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Perfect on {010}, yielding pearly luster on this surface.
- 6
Geological Environment
The rock formation and setting where it occurs
Commonly found in amygdaloidal cavities and veins within basaltic and other mafic volcanic rocks. Also occurs in hydrothermal veins, granites, gneisses, and as a diagenetic mineral in some sedimentary rocks.
Key Facts
- Hardness
- 3.5 - 4 on the Mohs scale
- Specific Gravity
- 2.12 - 2.22 g/cm³
- Crystal System
- Monoclinic
- Color
- White, colorless, pink, salmon, yellow, brown, reddish-brown
- Luster
- Vitreous to pearly
- Transparency
- Transparent to translucent
- Fracture
- Uneven
- Cleavage
- Perfect on {010}
- Composition
- Hydrated calcium sodium aluminum silicate
Physical characteristics
- Crystal Habit: Typically forms tabular crystals, often twinned into characteristic sheaf-like, bow-tie, or fan-shaped aggregates. Also found as divergent, fibrous, or granular masses.
- Cleavage Type: Perfect on {010}
- Fracture Type: Uneven
- Tenacity: Brittle
- Luster Type: Vitreous to pearly
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