The Tourmaline Group
Tourmaline
Classification Scheme
(Species approved by the International Mineralogical Association)
| Chromium-dravite |
NaMg3Cr6(BO3)3Si6O18(OH)3OH |
| Chromo-alumino-povondraite | NaCr3[Al4Mg2](BO3)3Si6O18(OH)3O |
| Dravite |
NaMg3Al6(BO3)3Si6O18(OH)3OH |
| Elbaite |
Na(Li1.5Al1.5)Al6(BO3)3Si6O18(OH)3OH |
| Feruvite | CaFe2+3[Al5Mg](BO3)3Si6O18(OH)3OH |
| Fluor-buergerite | NaFe3+3Al6(BO3)3Si6O18(O)3F |
| Fluor-dravite | NaMg3Al6(BO3)3Si6O18(OH)3F |
| Fluor-elbaite | Na(Li1.5Al1.5)Al6(BO3)3Si6O18(OH)3F |
| Fluor-liddicoatite | Ca(Li2Al)Al6(BO3)3Si6O18(OH)3F |
| Fluor-schorl | NaFe2+3Al6(BO3)3Si6O18(OH)3F |
| Foitite |
[][Fe2+2Al]Al6(BO3)3Si6O18(OH)3OH |
| Luinaite-(OH) | NaFe3+3Al6(BO3)3Si6O18(OH)3(OH) |
| Magnesio-foitite |
[][Mg2Al]Al6(BO3)3Si6O18(OH)4 |
| Olenite |
NaAl3Al6(BO3)3Si6O18(O)3(OH) |
| Oxy-chromium-dravite | NaCr3(Cr4Mg2)(BO3)3Si6O18(OH)3O |
| Oxy-vanadium-dravite | NaV3(V4Mg2)(BO3)3Si6O18(OH)3O |
| Oxy-schorl | Na(Fe2+2Al)Al6(BO3)3Si6O18(OH)3O |
| Povondraite |
NaFe3+3[Fe3+4Mg2](BO3)3Si6O18(OH)3O |
| Rossmanite |
[](LiAl2)Al6(BO3)3Si6O18(OH)4 |
| Schorl |
NaFe2+3Al6(BO3)3Si6O18(OH)4 |
| Tsilaisite | NaMn2+3Al6(BO3)3Si6O18(OH)3OH |
| Uvite |
CaMg3[Al5Mg](BO3)3Si6O18(OH)3OH |
[] in these formulas refers
to a vacant cation site (the X site)
Tourmaline colors
The color of tourmaline
originates from the metal ions (Fe,
Mn, Cr, V, Ti, Cu) in its structure. Colors come both from light
absorption by the individual ions (eg, Fe2+
or Cr3+)
and by light absorbed by interactions between ions (eg, Fe2+-Ti4+,
Mn2+-Ti4+
or Fe2+-Fe3+
intervalence charge transfer [IVCT]).
Blue color is usually caused by
Fe2+
but can also
come from Cu2+
in rare Brazilian elbaites.
[Blue iron-containing elbaite from Pakistan.] [The spectrum of blue copper-containing elbaite from Paraiba State, Brazil.
Green color comes from either Fe2+-Ti4+
IVCT
together with Fe2+,
or from either Cr3+
or V3+
alone, or in combination.
[Uvite from the Mogok region of Myanmar containing mostly V and some Cr]
Amber to orange-brown colors
(often seen in dravites) come
from Fe2+-Ti4+
alone.
[Dravite from Yinietharra, Western Austrailia, dominated by color derived from the Fe2+-Ti4+ interaction.]
Yellow to yellow-brown colors
result from Mn2+-Ti4+
IVCT.
[Elbaite from the Hyakule Mine, Nepal, displaying colors from interactions with titanium with Mn2+-Ti4+
IVCT and Fe2+-Ti4+
IVCT in different zones].
A greenish yellow to yellow color is from
Mn2+ plus Mn2+-Ti4+
IVCT.
[Faceted 'canary tourmaline' from Zambia]. [Mn-elbaite
spectrum].
Pink and red colors are from Mn3+.
The color of
pink manganese-containing tourmalines often is associated with
exposure to ionizing radiation (such as from the decay of 40K,
a common constituent of pegmatites).
Black tourmalines (schorls,
etc.) are dark because of
their high concentrations of iron, manganese and titanium. When
they are ground very thin, they are usually blue or
brownish-green. [60 cm cluster of schorl from the
Czech Republic]. [schorl
spectrum].
Many tourmalines owe their
color to a mixture of metal ions.
The great diversity of color in tourmalines is due the the
variability in which these mixtures occur.
[A slice of tourmaline from the Himalaya Mine, San Diego County, California, showing different colors from different causes]
Images of Tourmaline Slices
For images of colorful
tourmaline slices and more information
about their color go to the section on tourmaline
slices .
Images of representative
tourmaline spectra
Visible Spectra: polarizations:
(a = incident light polarized
perpendicular to c-axis; c = parallel to c-axis)
Blue, green, brown and black
Fe-containing tourmalines
GRR
512 image; Schorl, GRR 512, White Queen
Mine, Pala, California, 0.010 mm thick. Black in mass, blue when very
thin. Contains 13.5% "FeO" and 0.95% "MnO". Data Files: a 0K; c
0K;
GRR
596
image; Elbaite, GRR 596G,
Afghanistan, 0.25 mm thick. Dark green crystal colored by Fe2+
and Ti4+
- Fe2+
interactions. Contains 4.32% "FeO", 1.67% "MnO" and 0.04% "TiO2".
Data Files: a
8K ; c 8K ;
GRR
787
image; Dravite, GRR 787,
Sweeney Canyon, Anza Borrego, California, USA, 0.10 mm thick. The black
crystal that most people would call schorl is green when thin. The
intense absorptions in the perpendicular to c direction at 730 and 1120
nm result from enhancement of Fe2+
bands caused by interactions with Fe3+.
The intense absorption in the same direction near 430 nm is from Fe2+
- Ti4+
intervalence charge transfer. The crystal contains 6.93% "FeO", 0.05%
"MnO" and 0.53% "TiO2".
Data Files: a
0K ; c 0K .
GRR
794
image; Foitite, GRR 794,
Schindler Mine, California, USA, 0.048 mm thick. Black crystal, blue
when thin. Data Files: a 22 K ;
c
22 K .
S3 image,
Dravite, S3, Newry, Maine, USA. Brown to green, complexly
zoned. Spectra from a green zone. Contains Mg1.19
Fe1.16 Ti 0.04. Data files: a
0K ; c 0K .
CIT 12683 image,
Dravite, CIT 12683, Yinnietharra, Australia. Brown crystal, 0.680 mm
thick. The absorption band near 450 nm arising from Fe2+
- Ti4+
intervalence charge transfer is the primary cause of the color of this
crystal. Data files: a
67 K ; c
66 K .
GRR
2098
image; Uvite, GRR 2098, Wata
Poore area, Konar Province, Afghanistan. 3.98 mm thick. Pale brown
crystal. The color is dominated by the Fe2+
- Ti4+
intervalance charge transfer arising from the minor amounts of both Fe
and Ti that are in this crystal. Data Files: a
0K ; c
0K .
S 8 image;
Uvite, S 8, Pierrepont, New York, USA, NMNH 81511, 0.10 mm thick. Black
crystal. Contains 8.23% "FeO" and 0.55% "TiO2".
Data Files: a
0K ; c 0K .
Elbaite;
Usakos, Namibia, blue crystal. 3.641 mm thick. Data Files: a
20K ; c 20K .
Elbaite;
Usakos, Namibia, green crystal, 3.654 mm thick. Data Files: a
20K ; c 20K .
Cu2+
colored tourmalines
R030
image;
Elbaite, São José da Batalha, Paraíba,
Brazil, 0.20 mm thick. Blue crystal colored by Cu2+.
Ref: Rossman et al. (1991) Amer. Mineral 76, 1479-1484. Data Files: a 7K ; c
12K .
Elbaite-MT image;
Elbaite, São José da Batalha, Paraíba,
Brazil, 1.84 mm thick. Pink crystal colored by both manganese and copper. Data Files: a 14K ; c
14K . Contributed data from Michael Taran, Kiev.
Pink and yellow-green Mn-containing tourmalines
GRR
1368
image; dark pink elbaite from
Otjimbinque, Namibia. The color is from Mn3+
and represents one of the deeper colored natural pink tourmalines.
GRR
565 image; light pink elbaite from the
Himalaya Mine, Mesa Grande, California. The color is natural color from
Mn3+.
GRR
565 image; dark pink elbaite from the
Himalaya Mine, Mesa Grande, California. This sample has been irradiated
with 60Co
gamma rays to enhance its color. The color is from Mn3+
and represents a typical treated color for pink tourmalines.
GRR 876
image; heavily irradiated pink
elbaite from the Stewart Mine, Pala, California. Although the sample
has been treated, the color is from Mn3+
and resembles the color of natural pink tourmaline.
GRR
757 image; Yellow-green elbaite, GRR
757, Zambia, 2.00 mm thick, with high Mn2+
content and some Ti4+ that interacts with the Mn2+. Ref: Rossman & Mattson (1986) Amer. Mineral 71,
599-602. Data Files: a
0K ; c 0K ;
Elbaite;
Usakos, Namibia, pale yellow crystal, 5.353 mm thick. Data Files: a
20K ; c 20K .
GRR
1932
image; rossmanite, GRR 1932,
Rozná, Czech Republic, 2.976 mm thick. This is a light pink
crystal of the type specimen. The color comes from the
radiation-induced Mn3+
content. Here is the NIR
OH
region 4K;
of the same crystal. Data Files: a 0K
; c 0K ;