Rock Identifier
Moonstone (Orthoclase Feldspar (KAlSi3O8)) — Mineral
Mineral

Moonstone

Orthoclase Feldspar (KAlSi3O8)

Hardness: 6-6.5 (Mohs scale), Color: Typically light pink to reddish-orange, but can be white, cream, or greenish. Often shows schiller or adularescence (a milky bluish sheen) due to internal reflections from lamellar twinning and exsolution. Luster: Vitreous to pearly.…

Hardness
6-6
Luster
Vitreous to pearly
Identified More mineral

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Physical properties

Hardness: 6-6.5 (Mohs scale), Color: Typically light pink to reddish-orange, but can be white, cream, or greenish. Often shows schiller or adularescence (a milky bluish sheen) due to internal reflections from lamellar twinning and exsolution. Luster: Vitreous to pearly. Crystal Structure: Monoclinic, part of the feldspar group. Cleavage: Perfect in two directions, intersecting at nearly 90 degrees. Specific Gravity: 2.55-2.58.

Formation & geological history

Moonstone is a variety of the feldspar group mineral orthoclase (KAlSi3O8). It forms in igneous and metamorphic rocks under specific cooling conditions that allow for the exsolution of albite lamellae within the orthoclase structure, creating the adularescence. It is often found in pegmatites and granitic rocks. Its geological age varies depending on the specific formation.

Uses & applications

Primarily used as a gemstone in jewelry, particularly for cabochons due to its unique optical effect (adularescence). It's also collected by mineral enthusiasts.

Geological facts

Moonstone is strongly associated with lunar energy and intuition in many cultures. It is often given as a gift for new beginnings and is considered a traveler's stone. The most prized moonstones show a strong blue adularescence on a colorless, transparent background. Historically, it was used in Roman jewelry and was popular during the Art Nouveau period.

Field identification & locations

To identify moonstone in the field, look for its distinctive adularescence; rotating the stone will reveal a milky or bluish sheen that appears to glide across its surface. Its characteristic pearly or milky luster can also be a good indicator. It's commonly found in Sri Lanka, India, Madagascar, Myanmar, Tanzania, and the United States (especially in New Mexico, Pennsylvania, and Virginia). For collectors, polished cabochons are most common, but rough specimens showing good adularescence are also sought after. Be cautious of imitations like opalite glass or synthetic spinels; true moonstone has a specific gravity and hardness that can distinguish it.