
mineral
Tumbled black stone, possibly black tourmaline
Uncertain from the photo; possible schorl (NaFe₃Al₆(BO₃)₃Si₆O₁₈(OH)₄)
AI-generated identification · may be incorrectSmall, polished, glossy dark specimen with rounded, irregular shape. If schorl, hardness is 7–7.5 Mohs and crystals are trigonal; the image alone cannot confirm composition or cleavage.
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Physical properties
Small, polished, glossy dark specimen with rounded, irregular shape. If schorl, hardness is 7–7.5 Mohs and crystals are trigonal; the image alone cannot confirm composition or cleavage.
Formation & geological history
If tourmaline, it crystallized in boron-rich pegmatites or metamorphic rocks, commonly during the Precambrian to much younger geologic periods. A polished surface obscures diagnostic natural crystal form.
Uses & applications
Black tourmaline is collected and used in jewelry and decorative objects; it has limited industrial use.
Geological facts
Schorl is the most common tourmaline species and is typically black due to iron. This specimen’s identity cannot be established reliably from appearance alone.
Field identification & locations
Check for elongated striated crystals, hardness, and diagnostic mineral tests; polished shape and luster are not sufficient to distinguish tourmaline from other black minerals. Tourmaline occurs worldwide, including Brazil, Afghanistan, and the United States.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary