Rock Identifier
Jasp-Agate (Cryptocrystalline Quartz (SiO2) with Iron Oxide inclusions) — sedimentary
sedimentary

Jasp-Agate

Cryptocrystalline Quartz (SiO2) with Iron Oxide inclusions

Hardness: 6.5-7 (Mohs); Color: Waxy grey-brown chalcedony with bright red jasper patches; Luster: Vitreous to waxy; Structure: Microcrystalline; Cleavage: None (conchoidal fracture).

Hardness
6
Color
Waxy grey-brown chalcedony with bright red jasper patches
Luster
Vitreous to waxy
Identified More sedimentary

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Physical properties

Hardness: 6.5-7 (Mohs); Color: Waxy grey-brown chalcedony with bright red jasper patches; Luster: Vitreous to waxy; Structure: Microcrystalline; Cleavage: None (conchoidal fracture).

Formation & geological history

Formed when silica-rich fluids permeate volcanic or sedimentary rock cavities. The red 'jasper' is caused by iron impurities, while the translucent sections are chalcedony/agate. Often found in volcanic ash beds or gravel deposits.

Uses & applications

Commonly used for lapidary work, cabochons, jewelry, and as decorative pocket stones or healing crystals.

Geological facts

This specimen is a 'bridge' rock, containing both opaque Jasper and translucent Agate. The red color suggests hematite staining within the silica matrix. This material was historically used by indigenous peoples for stone tools due to its controlled fracturing.

Field identification & locations

Identify by looking for translucent edges (agate) mixed with opaque red areas (jasper). It will scratch glass easily. Commonly found in riverbeds or desert washes in the Western United States.