How to identify Black Moonstone
Orthoclase Feldspar (variety)
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Open the appTo correctly identify Black Moonstone (Orthoclase Feldspar (variety)), 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
Dark grey, black, brownish-black body color, often with a silvery, bluish, or brownish adularescence (schiller).
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous to pearly on cleavage surfaces.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Typically massive, sometimes in tabular or prismatic crystals. The adularescence is a key textural/optical feature.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Monoclinic system, typically forming tabular or prismatic crystals, though often found in massive or anhedral forms in Black Moonstone varieties. Crystals can be twinned (e.g., Carlsbad, Baveno, Manebach twins).
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Perfect cleavage in two directions, nearly at right angles (90 degrees).
- 6
Geological Environment
The rock formation and setting where it occurs
Found in igneous rocks (e.g., granites, syenites, pegmatites) and some metamorphic rocks (e.g., gneisses). The specific conditions for the formation of the dark inclusions are varied but generally involve the presence of iron-rich fluids or minerals during crystallization or subsequent alteration.
Key Facts
- Hardness
- 6 - 6.5 (Mohs scale)
- Specific Gravity
- 2.56 - 2.59
- Crystal System
- Monoclinic
- Color
- Dark grey, black, brownish-black with adularescence
- Luster
- Vitreous to pearly
- Transparency
- Translucent to opaque
- Fracture
- Uneven to conchoidal
- Cleavage
- Perfect in two directions, nearly at 90 degrees ({001} and {010})
- Composition
- Potassium aluminum silicate (KAlSi3O8) with fine mineral inclusions
Physical characteristics
- Crystal Habit: Typically massive, anhedral grains, or tabular to prismatic crystals; often twinned.
- Cleavage Type: Perfect in two directions, nearly at right angles (90 degrees).
- Fracture Type: Uneven to conchoidal.
- Tenacity: Brittle.
- Luster Type: Vitreous to pearly on cleavage surfaces.
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