Rock Identifier
Banded Jasper (Silicate Mineral (Microcrystalline Quartz / SiO2)) — sedimentary
sedimentary

Banded Jasper

Silicate Mineral (Microcrystalline Quartz / SiO2)

Hardness: 6.5-7 Mohs; Color: Opaque orange, brown, and tan banding; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture)

Hardness
6
Color
Opaque orange, brown, and tan banding
Luster
Waxy to dull
Identified More sedimentary
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Physical properties

Hardness: 6.5-7 Mohs; Color: Opaque orange, brown, and tan banding; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture)

Formation & geological history

Formed primarily through the chemical precipitation of silica in sedimentary environments or as a replacement of organic material; often found in prehistoric iron formations

Uses & applications

Used for lapidary work, jewelry (beads, cabochons), landscaping, and as a popular specimen for rock tumbling and collecting

Geological facts

Jasper is an opaque variety of chalcedony. The banding is caused by variations in iron oxides and clay content during the formation process over millions of years

Field identification & locations

Identify by its opaqueness (it does not transmit light even on thin edges), its characteristic banding, and its ability to scratch glass. Widely found in gravel pits and riverbeds