Rock Identifier
Black tourmaline (schorl) with host-rock fragments (Schorl, a sodium–iron tourmaline; approximate formula NaFe₃Al₆(BO₃)₃Si₆O₁₈(OH)₄) — mineral
mineral

Black tourmaline (schorl) with host-rock fragments

Schorl, a sodium–iron tourmaline; approximate formula NaFe₃Al₆(BO₃)₃Si₆O₁₈(OH)₄

AI-generated identification · may be incorrect

The black, glassy fragments are consistent with schorl, commonly Mohs 7–7.5, with a trigonal crystal structure and poor cleavage. The gray pieces appear to be associated host rock, but cannot be identified confidently from the image.

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Physical properties

The black, glassy fragments are consistent with schorl, commonly Mohs 7–7.5, with a trigonal crystal structure and poor cleavage. The gray pieces appear to be associated host rock, but cannot be identified confidently from the image.

Formation & geological history

Schorl crystallizes in boron-rich granitic pegmatites and related hydrothermal environments, often alongside quartz and feldspar. Such deposits range from ancient to geologically recent; the specimen’s age and locality cannot be determined visually.

Uses & applications

Tourmaline is used as a gemstone, mineral specimen, and collector material; industrial use is limited. The pictured rough fragments appear mainly suitable for collecting or lapidary sorting.

Geological facts

Schorl is the most common tourmaline species and is typically opaque black. Tourmaline crystals often show strong lengthwise striations and triangular cross-sections.

Field identification & locations

Look for glossy black, elongated, striated crystals; confirm with hardness and crystal form, since other dark minerals can look similar. Tourmaline occurs in pegmatites worldwide, including Brazil, the United States, and Africa.