
mineral
Beryl (var. Aquamarine/Blue Beryl) in Quartz Matrix
Beryllium Aluminum Silicate (Be3Al2Si6O18)
Hardness: 7.5-8.0 (Mohs scale), Color: Pale blue to greenish-blue (aquamarine) surrounded by white quartz and micaceous minerals, Luster: Vitreous (glassy), Crystal Structure: Hexagonal, Cleavage: Imperfect/Pinacoidal.
- Hardness
- 7
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Physical properties
Hardness: 7.5-8.0 (Mohs scale), Color: Pale blue to greenish-blue (aquamarine) surrounded by white quartz and micaceous minerals, Luster: Vitreous (glassy), Crystal Structure: Hexagonal, Cleavage: Imperfect/Pinacoidal.
Formation & geological history
Typically forms in granitic pegmatites or metamorphic hydrothermal veins when beryllium is enriched in the final stages of magma crystallization. Frequently found in Precambrian and Mesozoic deposits.
Uses & applications
Finer specimens are cut into gemstones for jewelry. Raw matrix specimens are prized by mineral collectors and used as a source of Beryllium for aerospace and electronics alloys.
Geological facts
The name 'Aquamarine' is derived from the Latin 'aqua marina', meaning sea water, owing to its distinct color. It is the birthstone for March and is chemically related to Emerald.
Field identification & locations
Identify in the field by looking for hexagonal crystal habits within quartz or feldspar veins. Commonly found in Brazil, Pakistan, and parts of the United States (Colorado, Idaho). Look for the characteristic glassy, blue-tinted transparency in coarse-grained igneous rocks.
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