General Cuspidine Information Chemical Formula: |
Ca4Si2O7(F,OH)2 |
Composition: |
Molecular Weight = 365.48 gm |
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Calcium 43.86 % Ca 61.37 % CaO |
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Silicon 15.37 % Si 32.88 % SiO2 |
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Hydrogen 0.14 % H 1.23 % H2O |
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Oxygen 32.83 % O |
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Fluorine 7.80 % F 7.80 % F |
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F -3.28 % -O=F2 |
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______ ______ |
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100.00 % 100.00 % = TOTAL OXIDE |
Empirical Formula: |
Ca4Si2O7F1.5(OH)0.5 |
Environment: |
Ejected masses from Mte. Somma, Vesuvius. |
IMA Status: |
Valid Species (Pre-IMA) 1876 |
Locality: |
At Monte Somma and Vesuvius, Campania, and in the Alban Hills, as at Ariccia, Lazio, Italy. Link to MinDat.org Location Data. |
Name Origin: |
From the Greek cuspis, for a spear, the characteristic shape of the twinned crystals. |
Synonym: |
Custerite |
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ICSD 34339 |
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PDF 41-1474 |
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Cuspidine Crystallography Axial Ratios: |
a:b:c =1.034:1:0.7161 |
Cell Dimensions: |
a = 10.93, b = 10.57, c = 7.57, Z = 4; beta = 110.1° V = 821.30 Den(Calc)= 2.96 |
Crystal System: |
Monoclinic - PrismaticH-M Symbol (2/m) Space Group: P 21/c |
X Ray Diffraction: |
By Intensity(I/Io): 3.062(1), 2.943(0.35), 3.259(0.3), |
Crystal Structure:
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Mouse
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| Physical Properties of Cuspidine Cleavage: |
{001} Good, {110} Imperfect |
Color: |
Colorless, Green, White, Light pink. |
Density: |
2.8 - 2.9, Average = 2.84 |
Diaphaneity: |
Transparent |
Fracture: |
Brittle - Generally displayed by glasses and most non-metallic minerals. |
Habit: |
Acicular - Occurs as needle-like crystals. |
Habit: |
Massive - Granular - Common texture observed in granite and other igneous rock. |
Hardness: |
5-6 - Between Apatite and Orthoclase |
Luminescence: |
Non-fluorescent. |
Luster: |
Vitreous (Glassy) |
Magnetism: |
Nonmagnetic |
Streak: |
white |
| Optical Properties of Cuspidine Gladstone-Dale: |
CI meas= -0.019 (Superior) - where the CI = (1-KPDmeas/KC) |
CI calc= 0.019 (Excellent) - where the CI = (1-KPDcalc/KC) KPDcalc= 0.2012,KPDmeas= 0.2089,KC= 0.2051 Ncalc = 1.57 - 1.61 Optical Data: |
Biaxial (+), a=1.586-1.592, b=1.595-1.596, g=1.598-1.606, bire=0.0120-0.0140, 2V(Calc)=58-66, 2V(Meas)=63. Dispersion r > v distinct. |
| Calculated Properties of Cuspidine Electron Density: |
Bulk Density (Electron Density)=2.95 gm/cc |
note: Specific Gravity of Cuspidine =2.96 gm/cc. Fermion Index: |
Fermion Index = 0.0079273277 |
Boson Index = 0.9920726723 Photoelectric: |
PECuspidine = 6.02 barns/electron |
U=PECuspidine x rElectron Density= 17.74 barns/cc. Radioactivity: |
GRapi = 0 (Gamma Ray American Petroleum Institute Units) |
Cuspidine is Not Radioactive | Cuspidine Classification Dana Class: |
56.02.04.03 (56)Sorosilicate Si2O7 Groups and O, OH, F. and H2O |
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(56.02)with cations in [4] and/or >[4] coordination |
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(56.02.04)Cuspidine - Wohlerite group |
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Strunz Class: |
09.BE.17 09 - SILICATES (Germanates) |
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09.B - Sorosilicates |
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09.BE -Si2O7 groups with additional anions; |
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| Other Cuspidine Information References: |
NAME( Ford32) PHYS. PROP.(Enc. of Minerals,2nd ed.,1990) OPTIC PROP.(Heinrich65) |
See Also: |
Links to other databases for Cuspidine : |
1 - Am. Min. Crystal Structure Database 2 - Athena 3 - EUROmin Project 4 - Ecole des Mines de Paris 5 - Franklin Minerals(Dunn) 6 - Franklin Minerals(Palache) 7 - GeoScienceWorld 8 - Google Images 9 - Google Scholar 10 - Handbook of Mineralogy (MinSocAm) 11 - Handbook of Mineralogy (UofA) 12 - MinDAT 13 - Mineralienatlas (Deutsch) 14 - Online Mineral Museum 15 - QUT Mineral Atlas 16 - Ruff.Info 17 - WWW-MINCRYST Search for Cuspidine using: Visit our Advertisers for Cuspidine : A Bijoux Google Search for CuspidineAdam's Minerals Google Search for Cuspidine Cape Minerals Google Search for Cuspidine Dakota Matrix Minerals Google Search for Cuspidine Excalibur Mineral Corp. Google Search for Cuspidine Exceptional Minerals Google Search for Cuspidine John Betts Fine Minerals Search for Cuspidine McDougall Minerals Google Search for Cuspidine Mineral News Website Link Rock and Mineral Shows Google Search for Cuspidine Weinrich Minerals, Inc. Google Search for Cuspidine Ask about Cuspidine here : Print or Cut-and-Paste your Cuspidine Specimen Label here :
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