Rock Identifier
Red jasper pebble (probable) (Jasper; microcrystalline quartz (SiO₂) colored mainly by iron oxides) — metamorphic
metamorphic

Red jasper pebble (probable)

Jasper; microcrystalline quartz (SiO₂) colored mainly by iron oxides

AI-generated identification · may be incorrect

Opaque brick-red to brown, earthy-to-dull waxy luster, massive with no visible crystals or cleavage; Mohs hardness about 6.5–7, specific gravity roughly 2.5–2.7. The rounded shape indicates natural water abrasion or tumbling.

Identified More metamorphic
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Physical properties

Opaque brick-red to brown, earthy-to-dull waxy luster, massive with no visible crystals or cleavage; Mohs hardness about 6.5–7, specific gravity roughly 2.5–2.7. The rounded shape indicates natural water abrasion or tumbling.

Formation & geological history

Jasper forms when silica-rich fluids replace or cement sediments and volcanic material, with hematite/goethite producing the red color; its exact age depends on locality, commonly Precambrian to younger. The image alone cannot establish a precise geological age.

Uses & applications

Used as an ornamental and lapidary stone for cabochons, carvings, beads, bookends, and polished specimens; it has little industrial value.

Geological facts

Jasper is a variety of chalcedony or microcrystalline quartz, though many specimens contain impurities and iron-rich inclusions. Red color generally reflects finely disseminated hematite.

Field identification & locations

Common in volcanic and sedimentary terrains worldwide, including India, Madagascar, Brazil, Australia, and the western United States. Check for hardness against glass, a white streak, lack of cleavage, and red-brown iron-rich patterning; positive identification may require testing.