Rock Identifier
Tumbled magnesite (Magnesite (MgCO₃), likely compact or veined magnesite) — mineral
mineral

Tumbled magnesite

Magnesite (MgCO₃), likely compact or veined magnesite

AI-generated identification · may be incorrect

Typically opaque white to cream with gray-brown veining, waxy to dull luster, and a smooth tumbled surface; Mohs hardness 3.5–4.5, trigonal crystal structure, and perfect rhombohedral cleavage. Specific gravity is about 3.0–3.1.

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Physical properties

Typically opaque white to cream with gray-brown veining, waxy to dull luster, and a smooth tumbled surface; Mohs hardness 3.5–4.5, trigonal crystal structure, and perfect rhombohedral cleavage. Specific gravity is about 3.0–3.1.

Formation & geological history

Forms when magnesium-rich rocks or hydrothermal fluids alter ultramafic rocks and carbonate sediments; deposits range from Precambrian to recent geological ages. The specimen has been shaped and polished by human processing.

Uses & applications

Used as a magnesium ore, refractory material, and industrial carbonate; attractive pieces are sold as inexpensive lapidary material, beads, and carvings.

Geological facts

Magnesite is commonly dyed to imitate turquoise and may be marketed as “white turquoise,” though that trade name is misleading. Brown veining can result from iron oxides or matrix minerals.

Field identification & locations

Identify it by its soft, chalky-to-waxy feel, white color, moderate weight, and strong reaction to dilute hydrochloric acid when powdered or freshly scratched. Common sources include Austria, Brazil, China, Greece, and the United States.