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The colour range

No mineral holds more colour

Tourmaline is not one mineral but a family, and its structure will accept almost any element that happens to be in the melt around it. Iron, manganese, chromium, vanadium, copper — each leaves a different colour behind. That is why the merchants of Ceylon gave it a name that simply meant mixed stones: they could not sort it, because it arrived in every colour they knew.

Rubellite

Manganese

Pink to red. The finest hold their colour under artificial light instead of turning brown.

Indicolite

Iron

Blue to violet-blue. Rare in saturated tones; most material leans grey-green.

Verdelite

Iron

The common green. Wide range, from olive to a clean forest tone.

Chrome

Chromium, vanadium

Intense emerald green from East Africa. Rarely above five carats.

Paraíba

Copper, manganese

Electric blue through blue-green to green and yellowish green. A defined colour range, not a single colour — and defined by copper, not by origin.

Watermelon

Zoned Mn and Fe

Pink core, green rim, in one crystal. Cut in slices to show the section.

Canary

Manganese

Vivid yellow from Malawi. A young variety, on the market since the 2000s.

Achroite

Near-free of chromophores

Colourless. Uncommon, and mostly a collector's stone.

Dravite

Magnesium

Brown to warm amber. A separate species, not elbaite.

Schorl

Iron

Black, and by far the most abundant tourmaline on earth. Rarely cut.

Bi-colour

Changing melt chemistry

Two or more colours along the length of one crystal.

Cat's eye

Parallel growth tubes

A single band of light across the dome, from hollow tubes inside the stone.

How to judge it

Four things, in this order

01

Hue

Which colour it is, and what else is mixed into it. Almost every tourmaline carries a secondary hue — a green with yellow in it, a pink leaning orange. Name both.

02

Saturation

How free the colour is of grey. This is what separates a fine stone from a common one, and it is the hardest thing to judge from a photograph.

03

Tone

How light or dark. Most buyers assume darker is better. In tourmaline it usually is not — past a certain tone the stone closes and stops returning light.

04

Behaviour in light

Take the stone out of the shop lights. Fine rubellite holds its red under incandescent light; ordinary material turns brown. Cuprian material keeps glowing in shade.

The neon

Why some tourmaline appears lit from inside

Neon is not a poetic word here. It describes a measurable behaviour: the stone returns a narrow, almost single colour and keeps returning it when the light around it drops. Ordinary saturated tourmaline goes flat and dark in shade. Cuprian material does not.

The cause is copper. Divalent copper, Cu²⁺, absorbs broadly in the red and the near infrared — bands centred around 700 and 900 nanometres — and leaves the blue-green part of the spectrum almost untouched. What reaches the eye is a clean, narrow band with very little of the grey that iron introduces into most other gems. That absence of grey is what reads as glow.

Manganese decides where in the range the stone lands. Trivalent manganese, Mn³⁺, absorbs near 515 nanometres and adds a violet to purple component; with copper it produces the purple material that comes out of the ground. Low-temperature heating converts Mn³⁺ to Mn²⁺, which barely absorbs in the visible range at all: the 515 nanometre band disappears, the copper band stays exactly where it was, and the stone moves to blue or blue-green. This is why nearly all Paraíba on the market has been heated, and why the treatment is accepted — it removes an absorption, it does not add a colour.

A correction the trade keeps getting wrong

Paraíba is not only blue

The definition agreed by the world's major laboratories covers a range, not a colour: blue — electric blue, neon blue, violet blue — bluish green to greenish green, green, and yellowish green, at medium-light to high saturation and tone, coloured mainly by copper and manganese, of whatever geographical origin.

So a mint or neon green cuprian elbaite is a Paraíba tourmaline, fully and correctly named — the great majority of green Paraíba on the market comes from Mozambique. What differs is price, not legitimacy: electric blue is scarcer and trades at a large premium over green, and the market conflates that premium with the definition. They are separate things, and we keep them separate.

Where the name stops

Copper is necessary but not sufficient. The same standard sets two limits that most sellers never mention, and both exist to stop weak material borrowing the name.

Traces are not enough

Tourmaline with only traces of copper, or with colour saturation below the range, is not called Paraíba — even though the chemistry technically shows copper. A pale, washed stone with a copper reading does not qualify.

Too much iron and it is out

Iron-rich copper-bearing tourmaline whose polarised o-ray spectrum shows the 700 nanometre band higher than the 900 nanometre copper band is excluded by name. In plain terms: if iron is doing more of the work than copper, the stone is a tourmaline that happens to contain copper — not a Paraíba. This is the line that separates a genuine cuprian gem from the green material sold at its price.

Reports name the origin as Brazil, Nigeria, Mozambique, other, or undetermined — and the definition itself is origin-blind. Anyone charging a Brazilian premium is charging for the origin line on the report, not for the word Paraíba.