Rock Identifier
Amazonite (Microcline (KAlSi3O8) with Pb impurities) — mineral
mineral

Amazonite

Microcline (KAlSi3O8) with Pb impurities

Hardness: 6-6.5 Mohs scale; Color: light green to turquoise; Luster: Vitreous; Crystal Structure: Triclinic; Cleavage: Perfect in two directions; Specific Gravity: 2.56-2.58

Hardness
6-6
Color
light green to turquoise
Luster
Vitreous
Identified More mineral

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Physical properties

Hardness: 6-6.5 Mohs scale; Color: light green to turquoise; Luster: Vitreous; Crystal Structure: Triclinic; Cleavage: Perfect in two directions; Specific Gravity: 2.56-2.58

Formation & geological history

Formed in granitic pegmatites and metamorphic rocks through slow cooling of potassium-rich magma. The green color is caused by trace amounts of lead and water within the feldspar lattice.

Uses & applications

Used primarily as a gemstone for jewelry, cabochons, beads, and as a popular mineral specimen for collectors.

Geological facts

Amazonite is named after the Amazon River, though it is not actually found there. It is sometimes referred to as 'Amazon stone.' It is a variety of Microcline feldspar.

Field identification & locations

Identify by its distinct blue-green color and 'Schiller' effect (shimmery white streaks). Commonly found in Brazil, Russia (Urals), Ethiopia, and Pike's Peak, Colorado, USA.