Rock Identifier
Polished Jasper / Gneiss (Metamorphic/Siliceous Egg) (Siliceous Gneiss / Banded Metamorphic Rock) — metamorphic
metamorphic

Polished Jasper / Gneiss (Metamorphic/Siliceous Egg)

Siliceous Gneiss / Banded Metamorphic Rock

AI-generated identification · may be incorrect

Hardness 6.5-7 on Mohs scale; vitreous to polished luster; multicolored with bands of dark grey/black, golden-brown, ochre, and green-grey; foliated/banded metamorphic texture composed largely of quartz, feldspar, and amphibole/mica; specific gravity ~2.6-2.8.

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Physical properties

Hardness 6.5-7 on Mohs scale; vitreous to polished luster; multicolored with bands of dark grey/black, golden-brown, ochre, and green-grey; foliated/banded metamorphic texture composed largely of quartz, feldspar, and amphibole/mica; specific gravity ~2.6-2.8.

Formation & geological history

Formed through high-grade regional metamorphism of igneous or sedimentary protoliths subjected to directional tectonic pressures and heat, resulting in mineral segregation into dark and light bands.

Uses & applications

Popular in ornamental carvings, lapidary art, polished decorative eggs, spheres, paperweights, and metaphysical collector items.

Geological facts

Egg-shaped carvings from banded stones date back centuries and are popular in lapidary art to showcase the natural flow of foliated mineral banding around a curved three-dimensional surface.

Field identification & locations

Recognized by its distinct compositional layering (gneissic foliation or banded jasper/flint patterning) visible seamlessly around the polished surface. Frequently carved and produced in regions like Madagascar, India, or Brazil.