| ⓘAlbite Formula:Na(AlSi3O8) Colour: White References:Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |
ⓘ'Alkali Feldspar'References:Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |
| ✪Anatase Formula:TiO2 Habit: Most commonly as bipyramids to about 2mm. Also as flattened tabular crystals and plates. Small numbers of tiny rosettes ("anatase roses"). Colour: Black, rarely inky blue. Description: First collected by the Nova Scotia Mineral and Gem Society and visitors from Ontario. It is localized to a brecciated rock along the northeastern end of the pit. Not reported from the rest of the mine.Associated with adularia, chlorite, quartz, bertrandite, and other minerals. Rarely found on or included in quartz. Some palm sized pieces contained hundreds of crystals. |
| ⓘAndalusite Formula:Al2(SiO4)O References:Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |
| ⓘ'Apatite' Formula:Ca5(PO4)3(Cl/F/OH) Colour: Cream, green References:Richardson, J. M., Roberts, A. C., Grice, J. D., Ramik, R. A. (1988) Mcauslanite, a supergene hydrated iron aluminum fluorophosphate from the East Kemptville tin mine, Yarmouth County, Nova Scotia.The Canadian Mineralogist, 26 (4) 917-921 Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |
| ⓘArsenopyrite Formula:FeAsS |
| ⓘAzurite Formula:Cu3(CO3)2(OH)2 |
| ⓘBertrandite Formula:Be4(Si2O7)(OH)2 Habit: Butterfly-twins and plates. The edges of the crystals show many complex faces. Colour: White, colorless. Description: These were common in a very localized part of the mine. Associated with anatase on clinochlore. Most formed butterfly twins to 1 cm, but more commonly to 5 mm. |
| ⓘBeryl Formula:Be3Al2(Si6O18) |
| ⓘ'Biotite' Formula:K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 References:Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |
| ⓘBismuthinite Formula:Bi2S3 |
| ⓘBrookite Formula:TiO2 Habit: Bladed crystals with very complex faces around the edges. Striated along their length. Colour: Dark brown. Description: The brookites were found localised to the northeast corner of the quarry. Associated with bertrandite, anatase, and clinochlore. Far less common than anatase. Crystals to 2 mm. |
| ⓘCalcite Formula:CaCO3 |
| ⓘCassiterite Formula:SnO2 Habit: Sometimes twinned. Colour: Dark brown. References:Richardson, J. M., Roberts, A. C., Grice, J. D., Ramik, R. A. (1988) Mcauslanite, a supergene hydrated iron aluminum fluorophosphate from the East Kemptville tin mine, Yarmouth County, Nova Scotia.The Canadian Mineralogist, 26 (4) 917-921 Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |
| ⓘChalcopyrite Formula:CuFeS2 |
| ⓘChildrenite Formula:Fe2+Al(PO4)(OH)2 · H2O Habit: Prismatic, in bowtie shaped sprays. Colour: Brown |
| ⓘ'Childrenite-Eosphorite Series' Habit: Prismatic crystals, sometimes in bowtie sprays. Colour: Brown. References:Richardson, J. M., Roberts, A. C., Grice, J. D., Ramik, R. A. (1988) Mcauslanite, a supergene hydrated iron aluminum fluorophosphate from the East Kemptville tin mine, Yarmouth County, Nova Scotia.The Canadian Mineralogist, 26 (4) 917-921 |
| ⓘ'Columbite-(Fe)-Columbite-(Mn) Series' |
| ⓘCovellite Formula:CuS |
| ⓘDickite Formula:Al2(Si2O5)(OH)4 |
| ⓘDolomite Formula:CaMg(CO3)2 |
| ⓘEpidote Formula:(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
ⓘ'Feldspar Group'References:Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |
| ⓘFluorite Formula:CaF2 Habit: Cubes, generally less than 1cm. Colour: Purple (common), yellow (rare) Fluorescence: None Description: Very common, often covering large surfaces of boulders. Frequently covered in a white clay mineral. Sometimes sprinkled with pyrite. Associated with most other minerals. References:Richardson, J.M., Spooner, E.T., McAuslan, D.A. (1982) The East Kemptville Tin Deposit, Nova Scotia: An example of a large tonnage, low grade, greisen-hosted deposit in the endocontact zone of a granite batholith. Current Research, Part B, Geological Survey of Canada, Paper 82-1B: 27-32. |
| ⓘGalena Formula:PbS Colour: Metallic gray |
| ⓘGypsum Formula:CaSO4 · 2H2O Habit: Elongated blades. Colour: White. Description: Pretty sprays of white, elongated blades. Sprays are less than 1 mm across. Crystals exhibit gypsum's flexibility. Known from a single pocket collected by Terry Collett and Doug Wilson. |
| ⓘHeulandite-Ca Formula:(Ca,Na)5(Si27Al9)O72 · 26H2O |
| ⓘ'Heulandite Subgroup' Formula:(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O Habit: Coffin shaped. Colour: White. Description: Visual and Raman ID of heulandite. They could also be clinoptilolite. Associated with quartz and pyrite. |
| ⓘHisingerite Formula:Fe3+2(Si2O5)(OH)4 · 2H2O Habit: Botryoidal Description: Richardson adds hisingerite to a paragenetic sequence plot, with a question mark behind the name. More recent WDS testing on very good material gives Si and Fe, with a bit of Al as an impurity. The material is red, botryoidal, and resinous, with a conchoidal fracture, all fitting most closely with hisingerite. |
| ⓘKaolinite Formula:Al2(Si2O5)(OH)4 |
| ⓘKellyite Formula:Mn2+2Al(AlSiO5)(OH)4 |
ⓘ'K Feldspar'References:Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |
| ⓘKulanite Formula:Ba(Fe2+,Mn2+,Mg)2(Al,Fe3+)2(PO4)3(OH)3 |
| ⓘMalachite Formula:Cu2(CO3)(OH)2 |
| ⓘMarcasite Formula:FeS2 |
| ✪Mcauslanite (TL) Formula:Fe3Al2(PO4)3(PO3OH)F · 18H2O Type Locality: Habit: Fibers and bladed crystals, sprays to 4mm. Colour: Clear yellowish white. Fluorescence: None Description: 3 institutions have HT (& part of HT) and CT specimens including the GSC in Ottawa which has a matrix specimen, two polished sections, one vial and some small fragments. References:Richardson, J. M., Roberts, A. C., Grice, J. D., Ramik, R. A. (1988) Mcauslanite, a supergene hydrated iron aluminum fluorophosphate from the East Kemptville tin mine, Yarmouth County, Nova Scotia.The Canadian Mineralogist, 26 (4) 917-921 |
| ⓘMolybdenite Formula:MoS2 Habit: Plates. Colour: Metallic gray. References:Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |
| ⓘ'Monazite Group' Formula:REE(PO4) References:Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |
| ⓘMuscovite Formula:KAl2(AlSi3O10)(OH)2 References:Richardson, J. M., Roberts, A. C., Grice, J. D., Ramik, R. A. (1988) Mcauslanite, a supergene hydrated iron aluminum fluorophosphate from the East Kemptville tin mine, Yarmouth County, Nova Scotia.The Canadian Mineralogist, 26 (4) 917-921 Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |
| ⓘMuscovite var. Illite Formula:K0.65Al2.0[Al0.65Si3.35O10](OH)2 References:Richardson, J. M., Roberts, A. C., Grice, J. D., Ramik, R. A. (1988) Mcauslanite, a supergene hydrated iron aluminum fluorophosphate from the East Kemptville tin mine, Yarmouth County, Nova Scotia.The Canadian Mineralogist, 26 (4) 917-921 |
| ⓘMuscovite var. Sericite Formula:KAl2(AlSi3O10)(OH)2 |
| ⓘNative Bismuth Formula:Bi |
| ⓘNative Copper Formula:Cu |
| ⓘOrthoclase Formula:K(AlSi3O8) References:Richardson, J. M., Roberts, A. C., Grice, J. D., Ramik, R. A. (1988) Mcauslanite, a supergene hydrated iron aluminum fluorophosphate from the East Kemptville tin mine, Yarmouth County, Nova Scotia.The Canadian Mineralogist, 26 (4) 917-921 |
| ⓘ'Parisite' Formula:Ca(Ce/La/Nd/REE)2(CO3)3F2 Description:Interesting brown-cream colored prismatic crystals with excellent cleavage are parisite, a cerium carbonate mineral. Actually, recent microprobe tests have shown that the central parts of the crystals are parisite and the rinds are a cerium phosphate. More identification work is being carried out. These crystals are generally about 5 mm or less, but have been found to about 1 cm. Rarely they will have a dusting of extremely tiny pyrites. Note the undulating growth along the prism and the fat midsection of the rear crystal.http://nsminerals.atspace.com/EastKemp.html |
| ⓘPhenakite Formula:Be2SiO4 Habit: Prismatic, with striations along their length. Colour: Colorless Description: Found in a brecciated rock along the northeastern edge of the pit. |
| ⓘPhosphophyllite Formula:Zn2Fe2+(PO4)2 · 4H2O References:Richardson, J. M., Roberts, A. C., Grice, J. D., Ramik, R. A. (1988) Mcauslanite, a supergene hydrated iron aluminum fluorophosphate from the East Kemptville tin mine, Yarmouth County, Nova Scotia.The Canadian Mineralogist, 26 (4) 917-921 |
| ⓘ'Plagioclase' Formula:(Na,Ca)[(Si,Al)AlSi2]O8 References:Richardson, J. M., Roberts, A. C., Grice, J. D., Ramik, R. A. (1988) Mcauslanite, a supergene hydrated iron aluminum fluorophosphate from the East Kemptville tin mine, Yarmouth County, Nova Scotia.The Canadian Mineralogist, 26 (4) 917-921 |
| ⓘPyrite Formula:FeS2 Habit: Cubes, octahedrons, and pyritohedrons. Colour: Brassy metallic Description: Associated with most of the other minerals. References:Richardson, J. M., Roberts, A. C., Grice, J. D., Ramik, R. A. (1988) Mcauslanite, a supergene hydrated iron aluminum fluorophosphate from the East Kemptville tin mine, Yarmouth County, Nova Scotia.The Canadian Mineralogist, 26 (4) 917-921 |
| ⓘPyrrhotite Formula:Fe1-xS |
| ⓘQuartz Formula:SiO2 Habit: Prismatic Colour: White References:Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |
| ⓘRhodochrosite Formula:MnCO3 Habit: Massive Colour: Colorless |
| ⓘRozenite Formula:FeSO4 · 4H2O |
| ⓘSiderite Formula:FeCO3 Habit: A wide variety of shapes. Thin round discs, elongated rhombs with flat terminations, etc. Colour: Tan, light brown, dark brown, reddish-brown. |
| ⓘSphalerite Formula:ZnS Colour: Orange-red, black. |
| ⓘStannite Formula:Cu2FeSnS4 |
| ⓘ'Stilbite Subgroup' Formula:M6-7[Al8-9Si27-28O72] · nH2O Habit: Commonly found as large surfaces of druses of crystals. The endfaces of the stilbite sheaves was a smooth curved surface and highly lustrous. Often sprinkled with tiny pyrite crystals. Colour: Bright orange, brown. |
| ⓘSynchysite-(Ce) Formula:CaCe(CO3)2F |
| ⓘ'Tetrahedrite Subgroup' Formula:Cu6(Cu4C2+2)Sb4S12S |
| ⓘTitanite Formula:CaTi(SiO4)O Habit: Arrowhead shaped. Colour: Tan. Description: From localized northeast zone of the open pit. Found in breccia zone with anatase etc. On clinochlore. |
| ⓘTopaz Formula:Al2(SiO4)(F,OH)2 Colour: Colorless Description: Massive topaz is reported to be very common at the mine and makes up a high percentage of the rock. Euhedral freestanding crystals are very rare though. References:Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |
| ⓘTriplite Formula:Mn2+2(PO4)F Habit: Massive, rare crude crystals. Colour: Vibrant salmon, reddish-pink. Description: From Mandarino et al: Creamy-pink anhedral grains, 3 to 10 mm in diameter. The main associated minerals are apatite, quartz, pyrite, and sphalerite. First locality in Canada for triplite. |
| ⓘUraninite Formula:UO2 References:Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |
| ⓘVivianite Formula:Fe2+Fe2+2(PO4)2 · 8H2O Colour: Gray References:Richardson, J. M., Roberts, A. C., Grice, J. D., Ramik, R. A. (1988) Mcauslanite, a supergene hydrated iron aluminum fluorophosphate from the East Kemptville tin mine, Yarmouth County, Nova Scotia.The Canadian Mineralogist, 26 (4) 917-921 |
ⓘ'White mica'References:Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |
ⓘ'Wolframite Group'References:Richardson, J. M., Roberts, A. C., Grice, J. D., Ramik, R. A. (1988) Mcauslanite, a supergene hydrated iron aluminum fluorophosphate from the East Kemptville tin mine, Yarmouth County, Nova Scotia.The Canadian Mineralogist, 26 (4) 917-921 |
| ⓘZircon Formula:Zr(SiO4) References:Kontak, Daniel J., Ansdell, Kevin, Dostal, Jaroslav, Halter, Werner, Martin, Robert, Williams-Jones, Anthony E. (2001) The nature and origin of pegmatites in a fluorine-rich leucogranite, East Kemptville Tin Deposit, Nova Scotia, Canada.Transactions of the Royal Society of Edinburgh: Earth Sciences, 92 (2) 173-200doi:10.1017/s0263593300000122 |