
sedimentary
Jasper (Red/Yellow Jasper Pebble)
Silicon Dioxide (SiO2 with Iron Oxide inclusions)
Hardness: 6.5 to 7 on the Mohs scale. Color: Opaque reddish-brown to orange-yellow. Luster: Waxy to dull (smooth polished pebble surface). Crystal structure: Trigonal (microcrystalline quartz). Cleavage: None, exhibits conchoidal fracture.
- Hardness
- 6
- Color
- Opaque reddish-brown to orange-yellow
- Luster
- Waxy to dull (smooth polished pebble surface)
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Physical properties
Hardness: 6.5 to 7 on the Mohs scale. Color: Opaque reddish-brown to orange-yellow. Luster: Waxy to dull (smooth polished pebble surface). Crystal structure: Trigonal (microcrystalline quartz). Cleavage: None, exhibits conchoidal fracture.
Formation & geological history
Formed through the deposition of silica-rich fluids filling cavities or sedimentary rocks, often enriched with iron oxide impurities during diagenesis or hydrothermal activity.
Uses & applications
Commonly used for lapidary work, decorative rock collections, tumbled stones, jewelry beads, and cabochons.
Geological facts
Jasper is a microcrystalline variety of quartz. Its vibrant earthy red and yellow colors are caused by varying amounts of iron oxides (hematite or goethite) within the silica matrix.
Field identification & locations
Identified in the field by its opacity, hardness (cannot be scratched by a steel knife), and smooth, water-worn rounded pebble shape. Found in riverbeds, gravel deposits, and sedimentary basins worldwide.
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