mineral

Honey-colored quartz cluster

Quartz, silicon dioxide (SiO₂), likely iron-stained or included quartz

AI-generated identification · may be incorrect

Translucent pale honey to tan crystals with vitreous luster and probable hexagonal prismatic/rhombohedral faces; hardness 7 Mohs, no cleavage, conchoidal fracture, specific gravity about 2.65. The granular, drusy appearance may include microcrystalline quartz or minor carbonate material.

Identified September 2, 2026More mineral →

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Physical properties

Formation & geological history

Likely formed when silica-rich hydrothermal fluids filled a cavity or vug in host rock, allowing quartz crystals to grow inward; the tan color commonly comes from iron-oxide staining or fluid inclusions. Exact geological age and locality cannot be determined from the photograph.

Uses & applications

Used as a decorative and collector specimen; quartz is also important in glass, ceramics, electronics, abrasives, and engineered stone. This piece is primarily ornamental rather than gem quality.

Geological facts

Quartz is one of Earth’s most abundant minerals and forms in igneous, sedimentary, and metamorphic settings. Its apparent honey coloration should not be confused with citrine without testing or locality information.

Field identification & locations

Identify by its glassy luster, hardness, lack of cleavage, and six-sided crystal geometry; it should scratch ordinary glass but not be scratched by a steel knife. Common sources include Brazil, Madagascar, Mexico, Morocco, and the United States.