
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 incorrectThe 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.
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Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary