
sedimentary
Siltstone (Yellow/Brown Sandstone or Siltstone)
Siltstone / Fine-grained Sandstone (rich in iron oxides like limonite)
Hardness: 6-7 on the Mohs scale depending on cementation; Color: Mustard brown to yellowish-tan; Luster: Dull, earthy; Crystal Structure: Microcrystalline to fine-grained particulate matrix; Cleavage: None, exhibits blocky to uneven fracture; Specific Gravity: 2.2-2.8.
- Hardness
- 6-7 on the Mohs scale depending on cementation
- Color
- Mustard brown to yellowish-tan
- Luster
- Dull, earthy
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Physical properties
Hardness: 6-7 on the Mohs scale depending on cementation; Color: Mustard brown to yellowish-tan; Luster: Dull, earthy; Crystal Structure: Microcrystalline to fine-grained particulate matrix; Cleavage: None, exhibits blocky to uneven fracture; Specific Gravity: 2.2-2.8.
Formation & geological history
Formed from the compaction and cementation of fine silty and sandy sediments deposited in river, lake, or shallow marine environments. The yellowish-brown coloration comes from iron oxide (limonite) mineral staining during diagenesis.
Uses & applications
Used primarily in building construction, paving stones, landscaping, aggregate materials, and as educational rock specimens.
Geological facts
Yellow siltstones and sandstones often feature detailed bedding structures and can sometimes host microfossils or plant impressions. The iron oxides coating the grains act as both a natural pigment and a cementing agent.
Field identification & locations
Identified in the field by its gritty or slightly powdery texture, earthy brown-yellow uniform color, and fine-grained matrix. Found abundantly in sedimentary basins worldwide.
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