
metamorphic
Dark gray veined metamorphic rock
Likely marble or quartzite; exact identification requires hardness and acid tests
AI-generated identification · may be incorrectDark gray, fine- to medium-grained, subrounded cobble with abundant white mineral veins, probably calcite or quartz. Likely hardness Mohs 3 if marble or 7 if quartzite; nonmetallic luster and massive texture.
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Physical properties
Dark gray, fine- to medium-grained, subrounded cobble with abundant white mineral veins, probably calcite or quartz. Likely hardness Mohs 3 if marble or 7 if quartzite; nonmetallic luster and massive texture.
Formation & geological history
Formed when limestone or quartz-rich sandstone was recrystallized by heat and pressure during regional or contact metamorphism. Its precise geological age and source cannot be determined from the image.
Uses & applications
Common varieties are used as decorative stone, aggregate, paving, and architectural material; attractive pieces may be collected but this specimen appears ordinary.
Geological facts
White cross-cutting veins indicate later mineral-filled fractures. A drop of dilute hydrochloric acid that fizzes suggests calcite-rich marble; scratching glass strongly suggests quartzite.
Field identification & locations
Look for interlocking crystals, absence of bedding, and vein networks. Marble is common in metamorphic belts worldwide; quartzite occurs wherever sandstone has been metamorphosed.
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