Rock Identifier
Orbicular Rhyolite (Rainforest Jasper) (Rhyolite containing Spherulites (SiO2 with impurities)) — igneous
igneous

Orbicular Rhyolite (Rainforest Jasper)

Rhyolite containing Spherulites (SiO2 with impurities)

Hardness: 6.5–7 on Mohs scale; Color: Cream, tan, and green groundmass with dark grey or blue orbicular patches; Luster: Dull to waxy; Texture: Fine-grained with rounded inclusions; Cleavage: None.

Hardness
6
Luster
Dull to waxy
Identified More igneous

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Physical properties

Hardness: 6.5–7 on Mohs scale; Color: Cream, tan, and green groundmass with dark grey or blue orbicular patches; Luster: Dull to waxy; Texture: Fine-grained with rounded inclusions; Cleavage: None.

Formation & geological history

Formed from rapid cooling of silica-rich volcanic lava where bubbles or seeds allow minerals to crystallize in radial, spherical patterns called spherulites. These deposits are typically associated with volcanic activity from the Cenozoic era.

Uses & applications

Primarily used for ornamental purposes, including stone carvings, cabochons for jewelry, and as decorative pocket stones for collectors.

Geological facts

Also known as 'Rainforest Jasper' despite not being a true jasper (which is sedimentary). The circular 'eyes' or 'orbs' are actually clusters of radiating crystal needles, usually quartz or feldspar.

Field identification & locations

Identify by looking for distinct orb-like or circular patterns within a fine-grained volcanic matrix. Commonly found in Western Australia and parts of the United States like Oregon. Collectors should look for high contrast between the orbs and the background rock.