Rock Identifier
Red Jasper (Silicon Dioxide with Hematite (SiO2 + Fe2O3)) — sedimentary
sedimentary

Red Jasper

Silicon Dioxide with Hematite (SiO2 + Fe2O3)

Hardness: 6.5-7 (Mohs scale); Color: Bricky red to deep brownish-red; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None; Conchoidal fracture; Specific gravity: 2.58-2.91.

Hardness
6
Color
Bricky red to deep brownish-red
Luster
Vitreous to dull
Identified More sedimentary

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Physical properties

Hardness: 6.5-7 (Mohs scale); Color: Bricky red to deep brownish-red; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None; Conchoidal fracture; Specific gravity: 2.58-2.91.

Formation & geological history

Formed through the accumulation of fine silica-rich materials and iron oxides. Usually occurs in hydrothermal veins or as a secondary mineral in volcanic rocks and sedimentary deposits via silica-rich groundwater precipitation.

Uses & applications

Primarily used as a gemstone for jewelry, cabochons, beads, and decorative ornaments. Historically used for seals, talismans, and as a material for knapping tools.

Geological facts

The red color is caused by impurities of iron (hematite). In ancient civilizations, it was known as the 'rain bringer' and was frequently mentioned in various religious texts and mythologies as a stone of protection and strength.

Field identification & locations

Identify by its opaque nature (unlike carnelian which is translucent) and dull waxy to vitreous luster. Commonly found in riverbeds or beaches where silica-rich rocks weather out. Major deposits are in India, Brazil, Madagascar, and the southwestern USA.