
mineral
Botryoidal Goethite
Goethite (α-Fe3+O(OH))
AI-generated identification · may be incorrectHardness: 5.0-5.5; Color: Black, brownish-black; Luster: Submetallic, dull, or silky; Crystal structure: Orthorhombic (often botryoidal or acicular); Cleavage: Perfect in one direction; Specific gravity: 3.3-4.3
- Hardness
- 5
- Color
- Black, brownish-black
- Luster
- Submetallic, dull, or silky
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Physical properties
Hardness: 5.0-5.5; Color: Black, brownish-black; Luster: Submetallic, dull, or silky; Crystal structure: Orthorhombic (often botryoidal or acicular); Cleavage: Perfect in one direction; Specific gravity: 3.3-4.3
Formation & geological history
Formed as a secondary mineral in the oxidation zones of iron ore deposits, often as a weathering product of other iron minerals like pyrite or siderite. Found in soil and bog iron ore environments.
Uses & applications
Primary source of iron ore; historically used as a brown ochre pigment; polished specimens are used by collectors and in lapidary work.
Geological facts
Named after the German philosopher and poet Johann Wolfgang von Goethe. It is the main component of iron rust and a common soil constituent ubiquitous across the Earth's crust.
Field identification & locations
Identify by its bubbly (botryoidal) texture, extreme darkness, and characteristic yellowish-brown streak on a porcelain plate. Commonly found in large deposits in the Appalachian Mountains and Michigan in the USA.
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