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silicates

Dravite

NaMg3Al6(Si6O18)(BO3)3(OH)3(OH)

Mineral species Low None Drv
Also known as
brown tourmalinechrome dravite
Crystal system
trigonal
Hardness
7–7.5 on the Mohs scale
Lustre
vitreous
Colour
Brown to yellow-brown, occasionally green
Where it forms
In metamorphosed sediments rich in magnesium, and in some limestones.
Chiefly from
Drava valley, Slovenia and AustriaAustraliaBrazilKenya

Why it is that colour

Magnesium, with iron and titanium giving the brown tones.

Safety

Safe to handle.

Where it comes from

Common, of little commercial interest except for the rare chromium-rich green material.

Historical use

Named in 1884 after the Drava river district. Of geological rather than gemmological interest — dravite in a metamorphic rock indicates the sediment it formed from was rich in boron and magnesium, which constrains what it originally was.

Recorded as history and attributed where possible. That a stone was used for something establishes that people used it, not that it worked.

Worth knowing

Dravite completes the trio that makes the group's point. Schorl is the iron tourmaline, elbaite the lithium one, dravite the magnesium one. Same structure, same boron backbone, different metal in one position, and the results range from a black waste mineral to the most expensive coloured gem in the world.

Tourmaline is arguably the best single illustration in mineralogy of how little it takes to change what something is worth, and how little that has to do with what it is.

Identity checked against IMA-CNMNC master list, June 2025.