Rock Identifier
Iron Meteorite (Siderite (Meteoric Iron-Nickel alloy)) — igneous
igneous

Iron Meteorite

Siderite (Meteoric Iron-Nickel alloy)

Hardness: 4-5 (Mohs scale); Color: Dark brown to metallic silver-grey; Luster: Metallic; Crystal structure: Octahedral or Hexahedral; Cleavage: None; Specific Gravity: 7.0 - 8.0 (Extremely heavy/dense)

Hardness
4-5 (Mohs scale)
Color
Dark brown to metallic silver-grey
Luster
Metallic
Identified More igneous

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Physical properties

Hardness: 4-5 (Mohs scale); Color: Dark brown to metallic silver-grey; Luster: Metallic; Crystal structure: Octahedral or Hexahedral; Cleavage: None; Specific Gravity: 7.0 - 8.0 (Extremely heavy/dense)

Formation & geological history

Formed in the molten cores of differentiated asteroids or protoplanets early in the solar system's history (approx. 4.5 billion years ago). They were released into space via massive collisions.

Uses & applications

Primarily for scientific research and private collection. Highly valued by museums and space enthusiasts. Historically used as a source of iron by ancient civilizations.

Geological facts

Many iron meteorites exhibit Widmanstätten patterns—a unique crisscross crystalline structure visible when sliced and etched, which can only form by cooling extremely slowly over millions of years.

Field identification & locations

Identify by high density (very heavy for its size), strong magnetism, and a fusion crust (a dark, thin rind). In the field, look for 'regmaglypts' (thumbprint-like depressions) on the surface.