Charnockite is a variety of orthopyroxene-bearing granite that is typically associated with high-grade metamorphic terrains. It is easily identified by its characteristic greenish-gray to brownish hue, often displaying a greasy luster due to the presence of hypersthene. It is historically significant in petrology and widely quarried for use as a high-durability building stone.
Is this charnockite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch charnockite with a known reference. Charnockite sits at Mohs 6-7, softer than the next harder reference, harder than the previous one.
- 2Read the textureLook at a fresh break with a hand lens. Texture: Non-foliated granofels, often banded.
- 3Pick out the mineralsComposition: Orthopyroxene-bearing quartz-feldspar rock with perthitic alkali feldspar and hypersthene. Identify the two or three most abundant grains.
- 4Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 5Match the color rangeCompare against the expected color range: gray, greenish, brown.
Often confused with
Charnockite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside charnockite
Minerals reported to co-occur with charnockite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 6-7
- Density
- 2.6-2.9 g/cm³
- Luster
- Vitreous
- Transparency
- Opaque
- Rarity
- Common
- Uses
- Decorative, Building stone, Collector
- Host rock
- metamorphic complexes
- Texture
- Non-foliated granofels, often banded
- Composition
- Orthopyroxene-bearing quartz-feldspar rock with perthitic alkali feldspar and hypersthene
Where rockhounds find charnockite
Classic worldwide localities
- India
- Antarctica
- Norway
- Sri Lanka
- Canada
Field-hunting tip
Where it forms: metamorphic complexes. If you start seeing quartz, orthoclase, hypersthene in float, you are in the right ground.









