sedimentary

Banded Jasper (Carnelian Jasper)

Silicon Dioxide (SiO2) with Iron Oxide inclusions

AI-generated identification · may be incorrect

Hardness: 6.5-7 on Mohs scale; Color: Reddish-brown with white bands; Luster: Vitreous to waxy; Crystal structure: Trigonal (microcrystalline quartz); Cleavage: None; Specific gravity: 2.58–2.91

Hardness: 6
Color: Reddish-brown with white bands
Luster: Vitreous to waxy

Identified April 18, 2026More sedimentary →

Explore Banded Jasper (Carnelian Jasper) in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

App Store Google Play

Physical properties

Hardness: 6.5-7 on Mohs scale; Color: Reddish-brown with white bands; Luster: Vitreous to waxy; Crystal structure: Trigonal (microcrystalline quartz); Cleavage: None; Specific gravity: 2.58–2.91

Formation & geological history

Formed through the deposition of silica from hydrothermal solutions or in sedimentary environments. The red color comes from iron oxide (hematite) inclusions, while the bands represent distinct periods of mineral deposition over millions of years.

Uses & applications

Commonly used for ornamental carvings, tumble polishing, lapidary art, jewelry, and as a decorative stone in home decor.

Geological facts

Jasper is a variety of chalcedony. The name comes from the Greek word 'iaspis', meaning 'spotted stone'. It was highly prized in the ancient world for its toughness and ability to take a high polish.

Field identification & locations

Identify by its opacity (unlike translucent agate) and its distinct banding. Commonly found in riverbeds or volcanic deposits in regions like Brazil, India, and the USA. Collectors look for sharp contrast in the bands.