Rock Identifier
Weathered sandstone or iron-rich sedimentary rock (Quartz-rich sandstone, likely ferruginous sandstone; composition mainly SiO₂ with iron oxides) — sedimentary
sedimentary

Weathered sandstone or iron-rich sedimentary rock

Quartz-rich sandstone, likely ferruginous sandstone; composition mainly SiO₂ with iron oxides

AI-generated identification · may be incorrect

Tan-brown, dull to earthy luster, visibly granular and porous, with rusty iron-oxide staining; individual grains suggest quartz cement. Typical hardness is about 6–7 for quartz grains, but the rock may crumble along weak cemented surfaces; cleavage absent and specific gravity about 2.2–2.6.

Identified More sedimentary
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Physical properties

Tan-brown, dull to earthy luster, visibly granular and porous, with rusty iron-oxide staining; individual grains suggest quartz cement. Typical hardness is about 6–7 for quartz grains, but the rock may crumble along weak cemented surfaces; cleavage absent and specific gravity about 2.2–2.6.

Formation & geological history

Formed when sand accumulated, was compacted, and cemented, then stained or cemented by iron oxides during weathering or groundwater circulation. Its precise geological age cannot be determined from the photograph.

Uses & applications

Common sandstone is used as building stone, paving, aggregate, and occasionally decorative material; this specimen has little commercial or jewelry value unless it has unusual fossils or mineralization.

Geological facts

The orange-brown coloration commonly comes from hematite or goethite coatings between quartz grains. Iron-rich sandstone can weather into porous, irregular fragments like those shown.

Field identification & locations

Look for gritty texture, visible sand grains, layered bedding, and a streak or coating of iron oxide; it should not fizz strongly with dilute hydrochloric acid. Common worldwide, especially in former river, beach, dune, and desert environments.