Rock Identifier
Sandstone (Clastic Sedimentary Rock (composed mostly of quartz and/or feldspar)) — sedimentary
sedimentary

Sandstone

Clastic Sedimentary Rock (composed mostly of quartz and/or feldspar)

Hardness: 6-7 (Mohs); Color: Yellow, tan, or greenish-grey due to glauconite or iron oxidation; Luster: Dull or earthy; Crystal structure: Granular/fragmental; Cleavage: None (breaks across grains); Specific gravity: 2.2–2.8

Hardness
6-7 (Mohs)
Luster
Dull or earthy
Identified More sedimentary

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Physical properties

Hardness: 6-7 (Mohs); Color: Yellow, tan, or greenish-grey due to glauconite or iron oxidation; Luster: Dull or earthy; Crystal structure: Granular/fragmental; Cleavage: None (breaks across grains); Specific gravity: 2.2–2.8

Formation & geological history

Formed from the accumulation and lithification of sand-sized mineral grains or rock fragments. This specimen appears to be from a marine or fluvial environment, showing weathered surfaces where iron oxides create the yellowish hue.

Uses & applications

Commonly used in construction as a building material, paving stones, and in the production of glass (if high silica content). It is also a significant reservoir for groundwater and petroleum.

Geological facts

Sandstone makes up about 20-25% of all sedimentary rocks on Earth. Famous monuments like the Red Fort in India and Petra in Jordan are carved from sandstone.

Field identification & locations

Identify in the field by its gritty 'sandpaper' texture when rubbed. It often shows layering (bedding). This specific sample displays 'liesegang rings' or weathering crusts. Found globally in basins and coastal areas.