Rock Identifier
Dalmatian jasper (Dalmatian stone; commonly a leucocratic alkali-feldspar-rich igneous rock with arfvedsonite or aegirine inclusions) — igneous
igneous

Dalmatian jasper

Dalmatian stone; commonly a leucocratic alkali-feldspar-rich igneous rock with arfvedsonite or aegirine inclusions

AI-generated identification · may be incorrect

Hardness about 6–7 Mohs; cream to pale gray matrix with distinctive black spots, opaque, matte to mildly vitreous when polished, and granular with no prominent cleavage. The black markings are dark amphibole/pyroxene-group minerals rather than true jasper in many commercial specimens.

Identified More igneous
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Physical properties

Hardness about 6–7 Mohs; cream to pale gray matrix with distinctive black spots, opaque, matte to mildly vitreous when polished, and granular with no prominent cleavage. The black markings are dark amphibole/pyroxene-group minerals rather than true jasper in many commercial specimens.

Formation & geological history

An uncommon alkaline igneous rock formed by crystallization of silica-poor magma, generally associated with volcanic or subvolcanic bodies; its precise geological age varies by locality. Commercial material is especially associated with Mexico.

Uses & applications

Used for tumbled stones, cabochons, beads, carvings, and decorative objects; it has modest jewelry and lapidary value rather than major gemstone value.

Geological facts

Despite the trade name “jasper,” much Dalmatian stone is not technically sedimentary jasper. Its spotted appearance resembles a Dalmatian dog’s coat.

Field identification & locations

Identify it by the cream matrix and irregular, sharply contrasting black inclusions; test cautiously because similar spotted rocks and dyed materials occur. Common sources include Chihuahua, Mexico, with additional look-alikes from other alkaline-rock localities.