Rock Identifier
Basalt with Quartz Vein (Basalt with silicon dioxide (SiO2) inclusion) — igneous
igneous

Basalt with Quartz Vein

Basalt with silicon dioxide (SiO2) inclusion

Hardness: 6-7 (Mohs); Color: Dark grey to black matrix with a yellowish-white vein; Luster: Dull to sub-vitreous; Structure: Aphanitic (fine-grained matrix) with a hydrothermal vein.

Hardness
6-7 (Mohs)
Color
Dark grey to black matrix with a yellowish-white vein
Luster
Dull to sub-vitreous
Identified More igneous
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Physical properties

Hardness: 6-7 (Mohs); Color: Dark grey to black matrix with a yellowish-white vein; Luster: Dull to sub-vitreous; Structure: Aphanitic (fine-grained matrix) with a hydrothermal vein.

Formation & geological history

The host rock is an igneous volcanic rock formed from rapid cooling of magnesium-rich and iron-rich lava. The vein formed later when hydrothermal fluids rich in silica filled fractures in the basalt, cooling to form quartz or chalcedony.

Uses & applications

Commonly used as river stones for landscaping, decorative gravel, massage stones, or as a collector's specimen for hobbyists.

Geological facts

The single band across the stone is often referred to in folklore as a 'Wishing Stone' - finding a pebble with a continuous white line circling it is said to bring good luck.

Field identification & locations

Identified by the dark, heavy, fine-grained volcanic matrix and the contrasting lighter mineral band. Commonly found on beaches, in riverbeds, or in volcanic terrains worldwide.