sedimentary

Likely weathered sandstone or loose sediment

Quartz-rich sandstone, probably disaggregated into sand; exact identification is uncertain from the image

AI-generated identification · may be incorrect

Pale tan, earthy, dull to weakly granular texture with no visible crystals or cleavage; likely Mohs hardness around 6–7 for individual quartz grains, but the loose material has little cohesion. Specific gravity is approximately 2.6 if quartz-rich.

Identified September 1, 2026More sedimentary →

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At a glance

Common name: Likely weathered sandstone or loose sediment
Scientific name: Quartz-rich sandstone, probably disaggregated into sand; exact identification is uncertain from the image
Category: sedimentary
Identified: September 1, 2026
Method: Standard

AI Estimated Value

About $0–$10 for ordinary loose material; attractive documented sandstone specimens may sell for $10–$50.

Not an official valuation

AI estimate for general interest only — not an appraisal. Actual value depends on condition, provenance, and market demand. Verify with a professional before buying, selling, or insuring.

This identification was generated by AI and may contain errors. Verify important details before relying on them — and never use an AI result to judge whether a specimen is safe to handle. Read the full disclaimer

Physical properties

Formation & geological history

Probably deposited sand later cemented into sandstone, then heavily weathered or crushed into loose grains. The geological age and original environment cannot be determined from the photograph.

Uses & applications

Unconsolidated sandstone material may be used as fill, aggregate, abrasives, or landscaping sand; it has essentially no jewelry value.

Geological facts

The apparent fibrous or cracked surface may reflect fine bedding, weathering, or handling rather than crystal structure. It could alternatively be a clay-rich sediment or soil, which would require testing.

Field identification & locations

Common in deserts, river deposits, beaches, and weathered sedimentary outcrops. Check grain size with a hand lens, test for fizz with dilute hydrochloric acid, and assess whether grains scratch glass; a streak, magnet, and acid test help distinguish sandstone from limestone or clay.