
mineral
Limonite and Goethite
Limonite (hydrated iron(III) oxide-hydroxide) and Goethite (α-FeO(OH))
AI-generated identification · may be incorrectHardness: 4.0 - 5.5; Color: Dark brown to yellow-brown, often with rust-like staining; Luster: Dull, earthy to submetallic; Crystal Structure: Amorphous (limonite) or Orthorhombic (goethite); Specific Gravity: 2.7 - 4.3.
- Hardness
- 4
- Color
- Dark brown to yellow-brown, often with rust-like staining
- Luster
- Dull, earthy to submetallic
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Physical properties
Hardness: 4.0 - 5.5; Color: Dark brown to yellow-brown, often with rust-like staining; Luster: Dull, earthy to submetallic; Crystal Structure: Amorphous (limonite) or Orthorhombic (goethite); Specific Gravity: 2.7 - 4.3.
Formation & geological history
Primary formation through the weathering of iron-rich sulfide minerals (like pyrite) or secondary deposition in sedimentary environments, often forming bog iron or gossans.
Uses & applications
Historically used as an important iron ore; currently used primarily as an ocher pigment for coloring paints, cement, and ceramics. Low industrial value in small quantities.
Geological facts
Limonite was once the primary source of 'yellow ocher' used by early humans for cave paintings. It often forms a 'gossan' or 'iron hat' over deeper metal deposits, serving as a signpost for miners.
Field identification & locations
Identify by its brownish-yellow streak (unlike hematite's red streak). It is often found in wet, oxygen-rich environments where iron minerals oxidize. Collectors look for botryoidal shapes which are more aesthetically pleasing.
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