Rock Identifier
Red Jasper (Silicon dioxide (SiO2) with iron oxide (Fe2O3) inclusions) — sedimentary/mineral
sedimentary/mineral

Red Jasper

Silicon dioxide (SiO2) with iron oxide (Fe2O3) inclusions

Hardness: 6.5-7 (Mohs scale); Color: Brick red to deep maroon; Luster: Dull to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None/Conchoidal fracture; Specific gravity: 2.58-2.91

Hardness
6
Color
Brick red to deep maroon
Luster
Dull to vitreous
Identified More sedimentary/mineral

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Physical properties

Hardness: 6.5-7 (Mohs scale); Color: Brick red to deep maroon; Luster: Dull to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None/Conchoidal fracture; Specific gravity: 2.58-2.91

Formation & geological history

Formed in sedimentary or volcanic environments as silica-rich fluids permeate rock cavities or replace organic material. The red color is derived from iron impurities that oxidized during the lithification process over millions of years.

Uses & applications

Commonly used in jewelry for cabochons, beads, and carvings. Also used as an ornamental stone in home decor and by collectors for its healing folklore and grounding properties.

Geological facts

Red Jasper was widely used in ancient times as a sacred stone; it was known as the 'blood of Mother Earth' in some cultures and was used to make the seal of the 'King of the Gods' in Egypt.

Field identification & locations

Identified in the field by its opaque red color, smooth waxy texture when wet, and extreme hardness (it will scratch glass). Commonly found in riverbeds, deserts, and volcanic regions globally, including South Africa, Brazil, and the USA.