
metamorphic
Jasper (likely brecciated or orbicular jasper)
Microcrystalline quartz/chalcedony (SiO₂) with iron-oxide and possibly chlorite or epidote inclusions
AI-generated identification · may be incorrectOpaque, fine-grained, waxy to dull luster; mottled salmon-red, orange, gray-green, and cream colors from iron oxides and alteration minerals. Hardness about 6.5–7 Mohs, no visible cleavage, conchoidal to uneven fracture; exact crystal structure is cryptocrystalline quartz.
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Physical properties
Opaque, fine-grained, waxy to dull luster; mottled salmon-red, orange, gray-green, and cream colors from iron oxides and alteration minerals. Hardness about 6.5–7 Mohs, no visible cleavage, conchoidal to uneven fracture; exact crystal structure is cryptocrystalline quartz.
Formation & geological history
Forms when silica-rich fluids cement or replace volcanic sediments and breccias, with iron-bearing minerals producing the red-orange colors. Commonly associated with altered volcanic rocks; age depends on locality and cannot be determined from the image.
Uses & applications
Used as lapidary rough, cabochons, carvings, beads, and decorative stone; attractive pieces have modest collector value.
Geological facts
The specimen’s irregular color patches and dark green-gray areas are consistent with jasper containing volcanic or alteration-mineral fragments, though a photograph cannot confirm the exact variety.
Field identification & locations
Identify by its opaque appearance, very fine texture, hardness, and inability to scratch with a steel nail easily; common sources include Oregon, Idaho, California, Australia, India, and Madagascar. A streak, hardness, and locality test would improve identification.
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