Simpsonite

A variety of Minerals

Simpsonite specimen - rock identification

What is Simpsonite?

Simpsonite has a general formula of Al4(Ta,Nb)3O13(OH). It occurs as euhedral to subhedral tabular to short and prismatic crystals, commonly in subparallel groups. Under the petrographic microscope it has a very high relief. Discovered in 1938, it was named after Edward Sydney Simpson (1875–1939), government mineralogist and analyst of Western Australia. It is an accessory mineral in some tantalum-rich granite pegmatites. It occurs in association with tantalite, manganotantalite, microlite, tapiolite, beryl, spodumene, montebrasite, pollucite, petalite, eucryptite, tourmaline, muscovite and quartz. It is found in a few locations around the world, notably in the Onca and Paraiba mines of Rio Grande do Norte, Brazil and at Tabba Tabba, Western Australia.

Optical Properties

Refractive Index
1.994-2.040
Birefringence
0.046
Pleochroism
None
Optical Character
Uniaxial negative

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Simpsonite Localities Map

See where Simpsonite is found with a localities map, collecting zones, and geology context. Generate a sample map preview below.

Map preview
North ZoneCentral RidgeSouth Basin

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Quick Facts

Physical Properties

Color
Yellow, light brown, colourless, gray
Hardness (Mohs)
7 - 7.5
Density
6.35 g/cm³
Streak
white

Chemical Properties

Chemical Formula
Al4Ta3O13(OH)
Elements
Al, H, O, Ta

Also Known As

SimpsoniteSimpsonite (of Bowley)
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