Rock Identifier
Yellow jasper or iron-stained chert (Microcrystalline quartz (SiO₂), commonly colored by goethite/limonite and other iron oxides) — mineral
mineral

Yellow jasper or iron-stained chert

Microcrystalline quartz (SiO₂), commonly colored by goethite/limonite and other iron oxides

AI-generated identification · may be incorrect

Typically Mohs hardness 6.5–7, opaque mustard-yellow to brown, with a waxy to dull luster and no visible cleavage; massive cryptocrystalline quartz, with conchoidal fracture. The rounded, wet surface obscures diagnostic texture, so exact identification is uncertain from the image alone.

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Physical properties

Typically Mohs hardness 6.5–7, opaque mustard-yellow to brown, with a waxy to dull luster and no visible cleavage; massive cryptocrystalline quartz, with conchoidal fracture. The rounded, wet surface obscures diagnostic texture, so exact identification is uncertain from the image alone.

Formation & geological history

Forms when silica-rich groundwater replaces or cements sediment, often incorporating iron oxides; it may occur in sedimentary or volcanic environments, with ages ranging from ancient Precambrian deposits to recent gravels.

Uses & applications

Used as ornamental stone, lapidary material, cabochons, carvings, tumbled stones, and sometimes aggregate; generally not a major industrial gemstone.

Geological facts

Yellow jasper is a variety name rather than a rigorously defined mineral species; color commonly comes from hydrated iron oxides. A glassy edge or conchoidal chip would support jasper/chert identification.

Field identification & locations

Common in river gravels and silica-rich outcrops worldwide, including the western United States, Brazil, India, Madagascar, and Australia. Test hardness against steel or glass, inspect a fresh fracture, and check for quartz-like translucency; avoid destructive testing if valuable.