Rock Identifier
Quartz-veined dark metamorphic rock (Likely quartz-bearing hornfels, amphibolite, or altered basalt; exact identification requires a fresh surface and tests) — metamorphic
metamorphic

Quartz-veined dark metamorphic rock

Likely quartz-bearing hornfels, amphibolite, or altered basalt; exact identification requires a fresh surface and tests

AI-generated identification · may be incorrect

Dark gray, fine- to medium-grained matrix with white to cream, glassy quartz-rich veins or patches; quartz is Mohs 7 with vitreous luster, while the matrix may be harder than steel and lacks obvious cleavage. The cream material could also include calcite or weathered feldspar.

Identified More metamorphic
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Physical properties

Dark gray, fine- to medium-grained matrix with white to cream, glassy quartz-rich veins or patches; quartz is Mohs 7 with vitreous luster, while the matrix may be harder than steel and lacks obvious cleavage. The cream material could also include calcite or weathered feldspar.

Formation & geological history

Probably formed by metamorphism or hydrothermal alteration of a mafic volcanic rock, with later silica-rich fluids filling fractures; age depends on locality and cannot be determined visually.

Uses & applications

Primarily a collecting specimen or field sample; similar tough rocks may be used as crushed aggregate or decorative stone, but this piece has little commercial value.

Geological facts

The irregular white infill suggests mineralized fractures rather than a fossil. Acid testing, streak, and a close examination of crystal grains would distinguish quartz from calcite and refine the rock name.

Field identification & locations

Commonly found in metamorphic belts, volcanic terrains, and hydrothermal zones worldwide. Look for quartz that scratches glass and does not fizz in dilute hydrochloric acid; calcite fizzes and is softer.