Rock Identifier
Quartz-rich weathered rock, possibly quartz geode or vuggy quartz vein (Quartz (SiO₂), likely with iron-oxide staining and possible feldspar/calcite matrix) — mineral
mineral

Quartz-rich weathered rock, possibly quartz geode or vuggy quartz vein

Quartz (SiO₂), likely with iron-oxide staining and possible feldspar/calcite matrix

AI-generated identification · may be incorrect

Pale cream to gray, white crystalline surfaces with earthy brown staining; likely vitreous to dull luster and irregular fracture. Quartz has Mohs hardness 7, no cleavage, hexagonal crystal structure, and specific gravity about 2.65; exact properties are uncertain without testing.

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Physical properties

Pale cream to gray, white crystalline surfaces with earthy brown staining; likely vitreous to dull luster and irregular fracture. Quartz has Mohs hardness 7, no cleavage, hexagonal crystal structure, and specific gravity about 2.65; exact properties are uncertain without testing.

Formation & geological history

Likely formed when silica-rich hydrothermal fluids deposited quartz in a cavity or fracture, later weathered near the surface; the specimen’s geological age cannot be determined from the image. Brown coloration commonly comes from limonite or other iron oxides.

Uses & applications

Quartz is used in glass, electronics, abrasives, and engineered stone; attractive crystals are collected or used decoratively. This rough specimen has modest commercial value.

Geological facts

The granular, cavity-filled texture resembles a quartz vein or small geode, but the image does not show diagnostic crystal faces clearly enough for a precise identification.

Field identification & locations

Test with a steel file or knife: quartz should resist scratching; it will scratch ordinary glass. Common sources include hydrothermal veins and weathered granitic or metamorphic terrains worldwide; acid testing can help distinguish calcite matrix.