Rock Identifier
Glauconitic sandstone or altered volcanic rock (Glauconite-bearing quartz-rich rock; composition likely quartz (SiO₂), glauconite, feldspar, and iron oxides) — sedimentary
sedimentary

Glauconitic sandstone or altered volcanic rock

Glauconite-bearing quartz-rich rock; composition likely quartz (SiO₂), glauconite, feldspar, and iron oxides

AI-generated identification · may be incorrect

Hardness approximately 6–7 overall; dark olive-green to brown with rusty orange staining, granular texture, and mostly dull to glassy luster. Quartz grains may show no cleavage; exact identification requires a fresh surface and testing.

Identified More sedimentary
Explore Glauconitic sandstone or altered volcanic rock in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness approximately 6–7 overall; dark olive-green to brown with rusty orange staining, granular texture, and mostly dull to glassy luster. Quartz grains may show no cleavage; exact identification requires a fresh surface and testing.

Formation & geological history

Most consistent with sedimentary sandstone containing glauconite, formed in a shallow marine, low-oxygen environment; glauconite commonly forms during slow deposition over millions of years. The orange areas represent later oxidation of iron.

Uses & applications

Used mainly as a geological or lapidary specimen; glauconitic sandstone has limited construction use, while glauconite is used in soil amendments, water treatment, and potassium fertilizer.

Geological facts

Glauconite is an iron-potassium phyllosilicate responsible for the green color and commonly indicates marine deposition. The image alone cannot reliably distinguish it from chlorite-rich altered volcanic rock.

Field identification & locations

Look for rounded quartz grains, green earthy matrix, rusty weathering, and weakly friable texture; a streak, hardness, acid, and thin-section test would help. Common in marine sedimentary basins worldwide.