
sedimentary
Ferruginous Sandstone
Clastic Sedimentary Rock (Iron-rich)
Hardness: 6-7 (Mohs scale); Color: Brown, reddish-brown, tan, with earthy gray undertones; Luster: Dull/Earthy; Crystal structure: Clastic (sand-sized grains); Cleavage: None/Conchoidal fractures; Specific gravity: 2.2 - 2.8.
- Hardness
- 6-7 (Mohs scale)
- Color
- Brown, reddish-brown, tan, with earthy gray undertones
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (Mohs scale); Color: Brown, reddish-brown, tan, with earthy gray undertones; Luster: Dull/Earthy; Crystal structure: Clastic (sand-sized grains); Cleavage: None/Conchoidal fractures; Specific gravity: 2.2 - 2.8.
Formation & geological history
Formed through the accumulation and cementation of mineral particles or rock fragments (detritus). The brown-reddish staining indicates the presence of iron oxide (hematite or limonite) that acted as the cementing agent or has weathered over geological time.
Uses & applications
Commonly used in construction as crushed stone or building material. Historically used for architectural facades and walling. Low-quality specimens are mostly significant for landscaping.
Geological facts
Sandstone makes up about 20% to 25% of all sedimentary rocks on Earth. The rusty color often tells a story of ancient oxygen levels in the environment during deposition.
Field identification & locations
Identify in the field by its gritty texture (feels like sandpaper) and distinct layering or bedding planes. It is often found in river beds, deserts, and coastal areas where sediment accumulates.
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