mineral

Mixed Mineral Collection (with Quartz, Beryl, and host rock)

Silicon Dioxide (Quartz), Be3Al2Si6O18 (Beryl), and associated Schist/Pegmatite

AI-generated identification · may be incorrect

Variable: Quartz (H: 7.0, vitreous, hexagonal); Emerald/Beryl (H: 7.5-8.0, green, vitreous, hexagonal prisms); Host rock (foliated, dark grey/green, dull to pearly luster).

Identified July 1, 2026More mineral →

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Physical properties

Variable: Quartz (H: 7.0, vitreous, hexagonal); Emerald/Beryl (H: 7.5-8.0, green, vitreous, hexagonal prisms); Host rock (foliated, dark grey/green, dull to pearly luster).

Formation & geological history

Formed in hydrothermal veins and pegmatite deposits where cooling magma or hot mineral-rich fluids interact with metamorphic host rocks, often during Orogenic events (mountain building).

Uses & applications

Primarily used for lapidary work, gemstone collecting, and as scientific specimens. Low-grade Beryl is used for Beryllium ore; Quartz is used in electronics and glass.

Geological facts

The green crystals are likely Emerald (a variety of Beryl) in their raw matrix. North Carolina is a famous US locality where these 'mine-your-own' buckets are commonly sourced.

Field identification & locations

Identify by hexagonal crystal habits, hardness (resistance to scratching steel), and the association of green beryl within dark, micaceous schist or white quartz matrix.