Rock Identifier
Greenstone (Metabaltic/Greenschist) (Chlorite schist / Meta-basalt) — metamorphic
metamorphic

Greenstone (Metabaltic/Greenschist)

Chlorite schist / Meta-basalt

Hardness (Mohs): 3.5 - 4.5. Color: Dark green, grayish-green, mottled with earthy brown oxidation. Luster: Dull to sub-vitreous. Crystal structure: Microcrystalline to foliated. Cleavage: Poorly developed schistosity. Specific Gravity: 2.8 - 3.0.

Luster
Dull to sub-vitreous
Identified More metamorphic

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Physical properties

Hardness (Mohs): 3.5 - 4.5. Color: Dark green, grayish-green, mottled with earthy brown oxidation. Luster: Dull to sub-vitreous. Crystal structure: Microcrystalline to foliated. Cleavage: Poorly developed schistosity. Specific Gravity: 2.8 - 3.0.

Formation & geological history

Formed from the low-grade metamorphism of mafic igneous rocks (such as basalt or gabbro) under relatively low temperatures and pressures. This creates greenish minerals like chlorite, epidote, and actinolite.

Uses & applications

Historically used for stone tools (axes) due to its toughness. Today it is used as crushed stone for road construction, riprap for erosion control, and occasionally as architectural building stone.

Geological facts

Ancient civilizations highly valued certain varieties of greenstone for making 'celt' axes. The green color is primarily due to the presence of the mineral chlorite.

Field identification & locations

Identify by its characteristic dull 'sage' or 'forest' green color and fine-grained texture. It will not react with acid and is generally harder than slate but softer than quartzite. Found commonly in ancient mountain belts and shield areas.