[How the Club Works] [Memberships - Junior, Deluxe , and Platinum] [FAQ] [Past Minerals] Join the Club - Junior, Deluxe and Platinum Memberships Available High Quality Minerals Sent to Your Home or School Each Month Mineral of the Month Club - An Inexpensive Way to Enjoy Minerals General Crossite InformationNa2(Mg,Fe++)3(Al,Fe+++)2Si8O22(OH)2 |
Molecular Weight = 795.32 gm |
|
Sodium 5.78 % Na 7.79 % Na2O |
|
Magnesium 6.11 % Mg 10.14 % MgO |
|
Aluminum 2.54 % Al 4.81 % Al2O3 |
|
Iron 8.78 % Fe 9.03 % FeO / 2.51 % Fe2O3 |
|
Silicon 28.25 % Si 60.44 % SiO2 |
|
Hydrogen 0.25 % H 2.27 % H2O |
|
Oxygen 48.28 % O |
|
______ ______ |
|
100.00 % 96.98 % = TOTAL OXIDE |
Na2Mg2Fe2+Al0.75Fe3+0.25(Si8O22)(OH)2 |
High pressure, low temperature metamorphic mineral. Discredited by IMA amphibole subcommittee (now glaucophane or ferroglaucophane or magnesioriebeckite or riebeckite). |
Discredited IMA 1997 - Valid Species (Pre-IMA) 1894 |
Berkeley, Conta Costa Co., USA. Link to MinDat.org Location Data. |
Named in 1894 for Charles Whitman Cross, (1854-1949), geologist, United States Geological Survey. |
Discredited |
|
ICSD 27459 |
|
PDF 20-376 |
| | Crossite Image
|
|
|
|
Crossite Crystallographya:b:c =0.5387:1:0.2969 |
a = 9.647, b = 17.905, c = 5.316, Z = 2; beta = 103.6° V = 892.48 Den(Calc)= 2.96 |
Monoclinic - PrismaticH-M Symbol (2/m) Space Group: C 2/m |
By Intensity(I/Io): 8.31(1), 3.08(0.7), 2.71(0.4),2.53(0.2), 3.4(0.2), 4.48(0.2), 4.87(0.2), 8.95(0.1), |
| Physical Properties of Crossite{110} Perfect, {010} Good |
Blue, Gray, Gray blue. |
3.16 |
Transparent to translucent |
Brittle - Uneven - Very brittle fracture producing uneven fragments. |
Tabular - Form dimensions are thin in one direction. |
6 - Orthoclase |
Non-fluorescent. |
Vitreous (Glassy) |
white |
| Optical Properties of CrossiteCI meas= -0.02 (Excellent) - where the CI = (1-KPDmeas/KC) |
CI calc= -0.089 (Poor) - where the CI = (1-KPDcalc/KC) KPDcalc= 0.2214,KPDmeas= 0.2074,KC= 0.2033 Ncalc = 1.6 - 1.64 Biaxial (-), a=1.64-1.659, b=1.645-1.666, g=1.652-1.67, bire=0.0110-0.0120, 2V(Calc)=72-82, 2V(Meas)=12-65. Dispersion very strong, r > v. |
wine yellow, pale yellow, colorless, or pale mauve blue. |
blue, prussian blue, purplish blue, or deep blue. |
grayish violet, violet, blue, or deep mauve blue. |
| Calculated Properties of CrossiteBulk Density (Electron Density)=3.13 gm/cc |
note: Specific Gravity of Crossite =3.16 gm/cc. Fermion Index = 0.02 |
Boson Index = 0.98 PECrossite = 3.98 barns/electron |
U=PECrossite x rElectron Density= 12.48 barns/cc. GRapi = 0 (Gamma Ray American Petroleum Institute Units) |
Crossite is Not Radioactive | Crossite Classification66.01.03c.03 (66)Inosilicate Double-Width Unbranched Chains, W=2 |
|
(66.01)with P=2 amphibole configuration |
|
(66.01.03c)Group 4, the sodic amphiboles |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
09.DE.25 09 - SILICATES (Germanates) |
|
09.D - Inosilicates* Structural terminology according to Liebau (1985) |
|
09.DE -Inosilicates with 2-periodic double chains, Si4O11; amphibole family |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
| Other Crossite InformationNAME( Dana8) PHYS. PROP.(Dana8) OPTIC PROP.(Dana) |
Links to other databases for Crossite : |
1 - Am. Min. Crystal Structure Database 2 - Athena 3 - EUROmin Project 4 - Ecole des Mines de Paris 5 - Google Images 6 - Google Scholar 7 - Handbook of Mineralogy (UofA) 8 - MinDAT 9 - MinMax(Deutsch) 10 - MinMax(English) 11 - Mineralienatlas (Deutsch) 12 - QUT Mineral Atlas 13 - Ruff.Info Search for Crossite using: Visit our Advertisers for Crossite : AA Mineral SpecimensB & L Fine Minerals Crystalarium.com Dan Weinrich Fine Minerals Dan Weinrich Auctions Dakota Matrix Desert Winds Gems and Minerals Excalibur Minerals Exceptional Minerals Fabre Minerals Heliodor John Betts Fine Minerals Mason's Minerals Mineral News Mineral of the Month Club Wrights Rock Shop Translate Crossite Mineral Data : Ask about Crossite here : Print or Cut-and-Paste your Crossite Specimen Label here :
| |
|
| | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||