Rock Identifier
Likely milky quartz (Quartz (silicon dioxide, SiO₂), possibly quartz-rich rock or calcite) — mineral
mineral

Likely milky quartz

Quartz (silicon dioxide, SiO₂), possibly quartz-rich rock or calcite

AI-generated identification · may be incorrect

White, opaque to translucent, glassy-to-dull luster with irregular fracture; quartz hardness is 7, no cleavage, and specific gravity about 2.65. The granular, crumbly appearance could also indicate calcite, which is softer (Mohs 3) and effervesces in dilute acid.

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Physical properties

White, opaque to translucent, glassy-to-dull luster with irregular fracture; quartz hardness is 7, no cleavage, and specific gravity about 2.65. The granular, crumbly appearance could also indicate calcite, which is softer (Mohs 3) and effervesces in dilute acid.

Formation & geological history

Quartz commonly crystallizes from silica-rich hydrothermal fluids or forms in igneous and metamorphic rocks; specimens may be Precambrian to recent. Exact identification and age cannot be determined from the photograph alone.

Uses & applications

Common quartz is used in glass, ceramics, abrasives, engineered stone, and electronics; attractive pieces may be collected but this specimen appears low grade.

Geological facts

Quartz is one of Earth’s most abundant minerals and has a distinctive six-sided crystal system when well formed.

Field identification & locations

Look for glassy surfaces and inability to scratch with a steel knife for quartz; a vinegar or dilute hydrochloric-acid fizz suggests calcite instead. Common worldwide, especially in veins and granitic or metamorphic terrains.