Dunn, Pete J., Leavens, Peter B. (1983) Bostwickite, a new calcium manganese silicate hydrate from Franklin, New Jersey. Mineralogical Magazine, 47 (344) 387-389 doi:10.1180/minmag.1983.047.344.16

Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | Bostwickite, a new calcium manganese silicate hydrate from Franklin, New Jersey | ||
Journal | Mineralogical Magazine | ISSN | 0026-461X |
Authors | Dunn, Pete J. | Author | |
Leavens, Peter B. | Author | ||
Year | 1983 (September) | Volume | 47 |
Issue | 344 | ||
Publisher | Mineralogical Society | ||
Download URL | https://rruff.info/doclib/MinMag/Volume_47/47-344-387.pdf+ | ||
DOI | doi:10.1180/minmag.1983.047.344.16Search in ResearchGate | ||
Generate Citation Formats | |||
Mindat Ref. ID | 3535 | Long-form Identifier | mindat:1:5:3535:8 |
GUID | 0 | ||
Full Reference | Dunn, Pete J., Leavens, Peter B. (1983) Bostwickite, a new calcium manganese silicate hydrate from Franklin, New Jersey. Mineralogical Magazine, 47 (344) 387-389 doi:10.1180/minmag.1983.047.344.16 | ||
Plain Text | Dunn, Pete J., Leavens, Peter B. (1983) Bostwickite, a new calcium manganese silicate hydrate from Franklin, New Jersey. Mineralogical Magazine, 47 (344) 387-389 doi:10.1180/minmag.1983.047.344.16 | ||
In | (1983, September) Mineralogical Magazine Vol. 47 (344) Mineralogical Society | ||
Abstract/Notes | AbstractBostwickite, CaMn63+Si3O16-7H2O, is a new species from the Franklin Mine, Franklin, New Jersey. Chemical analysis yielded MgO 0.9, CaO 5.1, Mn2O3 56.3, Fe2O3 0.5, Al2O3 1.0, As2O5 1.0, SiO2 20.1, H2O [15.1], sum = 100.0%. This yields (Ca0.76Mg0.19)Σ0.95(Mn5.973+Fe0.053+)Σ6.02(Si2.80Al0.16As0.075+)Σ6.02(Si2.80Al0.16AS5+0.07)Σ3.03O16·7.01H2O, corresponding to the idealized formula. The strongest lines in the X-ray powder diffraction pattern are (d, I): 11.3, 100; 3.548, 30; 2.898, 30; 2.567, 40; 2.262, 25; 2.238, 25; 1.470, 25. Bostwickite is dark red in colour; hardness c. 1 (Mohs'); density (meas.)= 2.93 g/cm3. It occurs in radial aggregates of acicular compound crystals. Optically, bostwickite is biaxial negative with 2Vα = 25deg; α = 1.775, Β = 1.798, γ = 1.800;, dispersion strong, r > v; strongly pleochroic with α = β redbrown, γ = yellow-brown; absorption is α = β = γ. Bostwickite is named in honour of Richard C. Bostwick, collector and compiler of data on the minerals of Franklin and Sterling Hill. |
Map of Localities
Locality Pages
Locality | Citation Details |
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Taylor Mine, Franklin Mine, Franklin, Sussex County, New Jersey, USA |
Mineral Pages
Mineral | Citation Details |
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Bostwickite |
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