Rock Identifier
Jasper (Silicon Dioxide (SiO2) with impurities (mostly Iron Oxides)) — sedimentary
sedimentary

Jasper

Silicon Dioxide (SiO2) with impurities (mostly Iron Oxides)

Hardness: 6.5-7 (Mohs scale); Color: Typically red, brown, or yellow; Luster: Dull to vitreous; Crystal Structure: Microcrystalline (Trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.91

Hardness
6
Color
Typically red, brown, or yellow
Luster
Dull to vitreous
Identified More sedimentary

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Physical properties

Hardness: 6.5-7 (Mohs scale); Color: Typically red, brown, or yellow; Luster: Dull to vitreous; Crystal Structure: Microcrystalline (Trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.91

Formation & geological history

Formed through the deposition of silica from volcanic ash or water circulation through sediment during the Proterozoic to Cenozoic eras. The red coloring is caused by iron inclusions (Hematite) oxidizing during the formation process.

Uses & applications

Commonly used in lapidary work for cabochons, beads, and carvings. Historically used for making tools due to its conchoidal fracture, and currently popular for 'healing' stones and jewelry.

Geological facts

Jasper was a favorite gem in the ancient world, mentioned in multiple historical texts including the Bible. It is a variety of chalcedony, which is a cryptocrystalline form of quartz.

Field identification & locations

Identify in the field by its opaque nature (even when held to light), high hardness (cannot be scratched by a steel knife), and smooth, shell-like fracture pattern. Often found in riverbeds or near volcanic deposits.