Rock Identifier
Porphyritic Basalt (Chinese Writing Stone) (Porphyritic Basalt with Feldspar Phenocrysts) — igneous
igneous

Porphyritic Basalt (Chinese Writing Stone)

Porphyritic Basalt with Feldspar Phenocrysts

Hardness: 6-6.5 (Mohs); Color: Dark grey to black matrix with white or cream-colored crystals; Luster: Dull to sub-vitreous; Crystal Structure: Aphanitic matrix with lath-like phenocrysts; Cleavage: None in rock, perfect in feldspar crystals; Specific Gravity: 2.8-3.0

Hardness
6-6
Luster
Dull to sub-vitreous
Identified More igneous

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Physical properties

Hardness: 6-6.5 (Mohs); Color: Dark grey to black matrix with white or cream-colored crystals; Luster: Dull to sub-vitreous; Crystal Structure: Aphanitic matrix with lath-like phenocrysts; Cleavage: None in rock, perfect in feldspar crystals; Specific Gravity: 2.8-3.0

Formation & geological history

Formed from rapid cooling of volcanic lava that began cooling slowly underground. This two-stage cooling process allows large crystals (phenocrysts) to form before the remaining magma erupts and cools quickly into a fine-grained matrix. Often associated with Mesozoic to Cenozoic volcanic activity.

Uses & applications

Used primarily as decorative stone, lapidary carvings, cabochons for jewelry, and as a unique collector's specimen. In larger quantities, basalt is used as crushed stone in construction.

Geological facts

Commonly known as 'Chinese Writing Stone' because the white feldspar crystals can resemble ancient calligraphy or characters against the dark background. It is chemically very similar to regular basalt but visually distinctive due to its texture.

Field identification & locations

Identify in the field by the 'porphyritic texture'—distinct white 'laths' or rectangular shapes embedded in a very fine-grained, dark, heavy rock. Commonly found in areas with past volcanic activity like California (USA) or British Columbia (Canada).