mineral

Beryl (likely Pink/Morganite variety)

Beryllium aluminum silicate (Be3Al2Si6O18)

AI-generated identification · may be incorrect

Hardness: 7.5 to 8.0 on Mohs scale; Color: Pale pink, peach, or light orange; Luster: Vitreous (glass-like); Crystal structure: Hexagonal/Prismatic; Cleavage: Imperfect; Specific Gravity: 2.63–2.91

Hardness: 7
Color: Pale pink, peach, or light orange
Luster: Vitreous (glass-like)

Identified June 28, 2026More mineral →

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Physical properties

Hardness: 7.5 to 8.0 on Mohs scale; Color: Pale pink, peach, or light orange; Luster: Vitreous (glass-like); Crystal structure: Hexagonal/Prismatic; Cleavage: Imperfect; Specific Gravity: 2.63–2.91

Formation & geological history

Formed in granitic pegmatites or hydrothermal veins rich in beryllium. These crystals typically grow in late-stage crystallization environments where rare elements concentrate.

Uses & applications

Gemstones for jewelry, industrial source of beryllium (though usually from common beryl), and a popular collector's mineral.

Geological facts

The pink variety 'Morganite' was named after financier J.P. Morgan. While the user's coordinates (Brampton, Ontario area) are largely sedimentary (Ordovician shales/limestones), this specimen likely originated from the nearby Grenville Province of the Canadian Shield, known for pegmatites.

Field identification & locations

Identify by its hexagonal prismatic crystal habit, high hardness (will scratch glass easily), and characteristic pale color. It is often found associated with quartz, feldspar, and mica in igneous host rocks.