Simpsonite
A variety of Minerals

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
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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

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