Rock Identifier
Jasper in Quartz (River Cobble) (Silicon Dioxide (SiO2) with Ferric Iron inclusions) — sedimentary
sedimentary

Jasper in Quartz (River Cobble)

Silicon Dioxide (SiO2) with Ferric Iron inclusions

Hardness: 6.5-7 (Mohs scale); Color: Cream/gray quartz with reddish-brown jasper patches; Luster: Dull to waxy; Structure: Microcrystalline; Cleavage: None/Conchoidal fracture; Specific gravity: 2.6-2.7

Hardness
6
Color
Cream/gray quartz with reddish-brown jasper patches
Luster
Dull to waxy
Identified More sedimentary

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Physical properties

Hardness: 6.5-7 (Mohs scale); Color: Cream/gray quartz with reddish-brown jasper patches; Luster: Dull to waxy; Structure: Microcrystalline; Cleavage: None/Conchoidal fracture; Specific gravity: 2.6-2.7

Formation & geological history

Formed through the deposition of silica-rich fluids in volcanic or sedimentary voids. This specific specimen is a water-worn river cobble, rounded by alluvial transport over thousands of years.

Uses & applications

Commonly used for lapidary work (tumbling, cabochons), landscaping, and as a educational specimen for beginner collectors.

Geological facts

Jasper gets its red color from iron impurities. When found in riverbeds like this, the smooth exterior is created by 'natural milling' where the rock is polished by sand and water over long distances.

Field identification & locations

Identify by its hardness (it will scratch glass) and the characteristic 'skin' or cortex that forms on river rocks. Look for these in gravel bars or dry creek beds in volcanic regions.