
sedimentary
Ironstone Pebble
Sedimentary ironstone / Hematitic Sandstone
Hardness: 5.5-6.5 on Mohs scale. Color: Brown, reddish-brown, tan, and dark gray. Luster: Dull, earthy to slightly metallic on fresh surfaces. Crystal Structure: Fine-grained aggregate composed mainly of quartz and iron oxides (hematite, goethite). Cleavage: None.
- Hardness
- 5
- Color
- Brown, reddish-brown, tan, and dark gray
- Luster
- Dull, earthy to slightly metallic on fresh surfaces
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Physical properties
Hardness: 5.5-6.5 on Mohs scale. Color: Brown, reddish-brown, tan, and dark gray. Luster: Dull, earthy to slightly metallic on fresh surfaces. Crystal Structure: Fine-grained aggregate composed mainly of quartz and iron oxides (hematite, goethite). Cleavage: None.
Formation & geological history
Formed in sedimentary environments through the deposition of sand grains cemented by precipitating iron oxides from mineral-rich waters. Later weathered and rounded by stream or wave action into a pebble.
Uses & applications
Commonly found in landscaping gravels, stream beds, and gravel deposits. Generally used as construction aggregate or collected as general rock specimens.
Geological facts
Ironstone cobbles and pebbles frequently exhibit a natural brownish-red weather rind due to the oxidation of iron minerals, similar to the rusting of iron metal.
Field identification & locations
Identified by its heavy weight relative to size (high density due to iron content), earthy brown to reddish color, rounded weathered shape, and dull finish. Common along rivers, lakeshores, and glacial drift regions.
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