Rock Identifier
Likely red jasper or iron-rich chert fragments (Microcrystalline quartz (SiO₂), colored by hematite/goethite; exact identification requires testing) — mineral
mineral

Likely red jasper or iron-rich chert fragments

Microcrystalline quartz (SiO₂), colored by hematite/goethite; exact identification requires testing

AI-generated identification · may be incorrect

Opaque reddish-brown, earthy to dull luster, very fine-grained with irregular conchoidal-looking fractures; quartz hardness about 6.5–7 Mohs, no visible cleavage, specific gravity roughly 2.6. The pieces appear naturally broken or possibly tumbled, though the image alone cannot confirm.

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Physical properties

Opaque reddish-brown, earthy to dull luster, very fine-grained with irregular conchoidal-looking fractures; quartz hardness about 6.5–7 Mohs, no visible cleavage, specific gravity roughly 2.6. The pieces appear naturally broken or possibly tumbled, though the image alone cannot confirm.

Formation & geological history

Forms when silica-rich groundwater or sediment is impregnated with iron oxides, commonly in volcanic or sedimentary settings. Formation ages range from Precambrian to recent depending on the deposit.

Uses & applications

Used as lapidary material, cabochons, beads, carvings, and decorative stone; lower-grade material is mainly a collector specimen or craft material.

Geological facts

Red color typically comes from hematite, while yellow-brown zones may reflect goethite or limonite. Similar-looking iron-rich rocks include ferruginous sandstone, brick-red chert, and weathered ironstone.

Field identification & locations

Test for glass scratching and lack of reaction to dilute acid; a streak test may produce a reddish-brown powder. Common sources include India, Brazil, Madagascar, Australia, and the western United States; value depends strongly on pattern, polish, and provenance.