Rock Identifier
Banded Sandstone or Quartzite Pebble (SiO2 (dominant) with impurities) — sedimentary or metamorphic
sedimentary or metamorphic

Banded Sandstone or Quartzite Pebble

SiO2 (dominant) with impurities

AI-generated identification · may be incorrect

Hardness: 6-7 (Mohs); Color: Tan, brown, grey bands; Luster: Dull to waxy when wet; Crystal structure: Microcrystalline or granular quartz; Cleavage: None; Specific gravity: ~2.6-2.7

Hardness
6-7 (Mohs)
Color
Tan, brown, grey bands
Luster
Dull to waxy when wet
Identified More sedimentary or metamorphic
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Physical properties

Hardness: 6-7 (Mohs); Color: Tan, brown, grey bands; Luster: Dull to waxy when wet; Crystal structure: Microcrystalline or granular quartz; Cleavage: None; Specific gravity: ~2.6-2.7

Formation & geological history

Formed originally as sedimentary layers of sand, subsequently lithified (sandstone) and potentially metamorphosed into quartzite, then rounded by water action in a river or beach environment.

Uses & applications

Decorative gravel, landscaping, casual collecting

Geological facts

The distinct banding represents different depositional events or mineral impurities (like iron oxides) during the original sediment accumulation.

Field identification & locations

Can be identified by its distinct sedimentary layers and rounded shape resulting from fluvial or coastal tumbling. Common on beaches and riverbeds.