
mineral
Limonite with Quartz
FeO(OH)·nH2O (Limonite) with SiO2 (Quartz)
AI-generated identification · may be incorrectHardness: 4-5.5 (Limonite) and 7 (Quartz); Color: Yellowish-brown, ochre, or dark brown; Luster: Earthy to submetallic; Crystal Structure: Amorphous or cryptocrystalline; Cleavage: None; Specific Gravity: 2.7-4.3.
- Hardness
- 4-5
- Color
- Yellowish-brown, ochre, or dark brown
- Luster
- Earthy to submetallic
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Physical properties
Hardness: 4-5.5 (Limonite) and 7 (Quartz); Color: Yellowish-brown, ochre, or dark brown; Luster: Earthy to submetallic; Crystal Structure: Amorphous or cryptocrystalline; Cleavage: None; Specific Gravity: 2.7-4.3.
Formation & geological history
Formed as a secondary mineral through the oxidation and hydration of iron-rich minerals such as pyrite or magnetite. Often found in gossipans (weathered rock covering ore deposits) or bog environments.
Uses & applications
Historically used as a major iron ore and as a source of yellow ochre pigment. Currently mainly of interest to collectors and geological researchers as an indicator of underlying metal deposits.
Geological facts
Limonite is not a single mineral but a mixture of hydrated iron oxide minerals, primarily goethite. It was used by ancient civilizations for cave paintings and pottery dyes dating back thousands of years.
Field identification & locations
Identify by its distinctive yellow-brown streak, earthy appearance, and lack of magnetism compared to magnetite. Commonly found in areas with heavy rain where iron minerals are prone to chemical weathering. Check for nearby quartz veins.
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