
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 incorrectDark 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.
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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.
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