Rock Identifier
Sandstone (likely Siltstone or Mudstone variety) (Clastic Sedimentary Rock (primarily SiO2 with iron oxides)) — sedimentary
sedimentary

Sandstone (likely Siltstone or Mudstone variety)

Clastic Sedimentary Rock (primarily SiO2 with iron oxides)

Hardness: 6-7 on Mohs scale (if well-indurated); Color: Reddish-brown, terracotta, or tan; Luster: Dull/Earthy; Crystal structure: Non-crystalline (clastic texture); Cleavage: None (tends to fracture along bedding planes); Specific gravity: 2.2-2.8

Hardness
6-7 on Mohs scale (if well-indurated)
Color
Reddish-brown, terracotta, or tan
Luster
Dull/Earthy
Identified More sedimentary

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Physical properties

Hardness: 6-7 on Mohs scale (if well-indurated); Color: Reddish-brown, terracotta, or tan; Luster: Dull/Earthy; Crystal structure: Non-crystalline (clastic texture); Cleavage: None (tends to fracture along bedding planes); Specific gravity: 2.2-2.8

Formation & geological history

Formed by the accumulation of sand-sized or silt-sized grains often in arid, river, or lake environments. Red coloration indicates the presence of iron oxide (hematite) during lithification under oxidizing conditions. These specimens often date from the Permian or Triassic periods.

Uses & applications

Commonly used as building stone, pavers, and decorative landscaping. Fine-grained varieties are used in ceramics or as sharpeners. Small specimens are prized by collectors for their distinct layering.

Geological facts

The distinct bands visible in the specimen represent different periods of sediment deposition, also known as varves. Many famous landmarks, such as the Grand Canyon or Petra, are carved from similar red sandstone formations.

Field identification & locations

Identify in the field by its gritty texture (feels like sandpaper) and visible horizontal layering (bedding planes). When scratched with a steel nail, it often leaves a light-colored streak. Commonly found in desert regions or ancient riverbeds.