
mineral
Botryoidal Hematite (Kidney Ore)
Iron(III) oxide (Fe2O3)
Hardness: 5-6.5 (Mohs scale); Color: Metallic grey to rusty red-brown; Luster: Metallic to submetallic; Crystal Structure: Trigonal (often found in botryoidal or kidney-like masses); Cleavage: None; Specific Gravity: 5.26.
- Hardness
- 5-6
- Color
- Metallic grey to rusty red-brown
- Luster
- Metallic to submetallic
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Physical properties
Hardness: 5-6.5 (Mohs scale); Color: Metallic grey to rusty red-brown; Luster: Metallic to submetallic; Crystal Structure: Trigonal (often found in botryoidal or kidney-like masses); Cleavage: None; Specific Gravity: 5.26.
Formation & geological history
Forms primarily in sedimentary environments through precipitation from iron-rich hydrothermal fluids or the weathering of iron-bearing minerals. Can be found in banded iron formations dating back billions of years.
Uses & applications
Primary ore of iron for steel production. Also used as a pigment (ochre), in jewelry as polished stones or beads, and as a popular mineral specimen for collectors.
Geological facts
The name is derived from the Greek word 'haima' meaning blood, due to the reddish streak it leaves when scratched. This specific bubbly appearance is called 'botryoidal,' which comes from the Greek word for a cluster of grapes.
Field identification & locations
Identified by its distinctive bubble-like texture and its reddish-brown streak. It is denser than most rocks of its size. Commonly found in mining districts of England (Cumbria), Morocco, Brazil, and the USA (Great Lakes region).
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Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
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