Garnet

Nesosilicate, Almandine-Pyrope variety · Semi-Precious Gemstone / Mineral Specimen

Garnet

Crystal System

Cubic (Isometric); typically occurs as dodecahedral or trapezohedral crystals, or in rounded granular masses.

Mineral Group

Silicates (Nesosilicates)

Chemical Formula

Fe3Al2(SiO4)3 to Mg3Al2(SiO4)3

Formation Process

Metamorphic (formed under high pressure and temperature in regional metamorphic rocks like mica schists) or Igneous (in pegmatites).

About This Crystal

A deep reddish-brown to brownish-black specimen with an earthy to sub-vitreous luster. Features a rough, weathered surface with visible internal fractures and a translucent to opaque body.

Physical Characteristics

Color: Dark brownish-red; Streak: White; Cleavage: None; Fracture: Sub-conchoidal to uneven; Specific Gravity: 3.6 - 4.3; Fluorescence: Usually inert.

Optical Properties

Singly refractive; Refractive Index: 1.72 - 1.83; Lacks pleochroism due to cubic structure; may show high dispersion but masked by dark body color.

Hardness & Durability

Origin Region

Found globally; notable sources include India, Madagascar, USA (Idaho, New York), and Sri Lanka. Often found in schist and gneiss.

Hardness & Durability

Mohs Hardness: 6.5 - 7.5; Toughness: Fair to Good; highly stable and durable for jewelry though susceptible to sharp blows.

Care & Maintenance

Clean with warm soapy water and a soft brush; ultrasonic cleaners are usually safe but avoid for stones with visible fractures; avoid extreme temperature changes.

Rarity & Value

Common; value is determined by transparency and color saturation; heavily included or opaque specimens are inexpensive and used primarily for industrial abrasive or study.

Special Characteristics

May exhibit minor magnetism due to high iron content in Almandine varieties; surface often shows 'etched' pits from weathering.

Lore & History

Historically used as a 'warrior's stone' for protection; traditionally associated with the Root Chakra and believed to promote grounding, vitality, and strength.

Identified on 5/29/2026