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Bostwickite

A valid IMA mineral species
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About BostwickiteHide

00326150017271921783614.jpg
Richard Bostwick
Formula:
CaMn3+6Si3O16 · 7H2O
Colour:
Brownish red
Lustre:
Sub-Vitreous, Greasy, Silky, Sub-Metallic
Hardness:
1
Specific Gravity:
2.93
Crystal System:
Orthorhombic
Name:
Named in 1983 by Pete J. Dunn and Peter B. Leavens in honor of Richard "Dick" Bostwick [January 19, 1943 - ], author, editor, lecturer, a fellow of the International Centre for Diffraction Data (ICDD), and prominent mineral collector, with a particular emphasis concerning fluorescent minerals. He is a past President of the Franklin-Ogdensburg Mineralogical Society, board member of the Franklin Mineral Museum, former hard rock miner in the Sterling Mine, Ogdensberg, New Jersey, USA, and regional Vice President of the Fluorescent Mineral Society. He is a frequent lecturer throughout the U.S.A. Dick is a life member of the National Mining Hall of Fame and Museum, an honorary member of the New York Mineralogical Club, and is in the Fluorescent Mineral Society’s Hall of Fame.
Brownish-red bronzey acicular crystals.


Unique IdentifiersHide

Mindat ID:
731
Long-form identifier:
mindat:1:1:731:9

IMA Classification of BostwickiteHide

Classification of BostwickiteHide

9.HC.10

9 : SILICATES (Germanates)
H : Unclassified silicates
C : With Mn, Fe
78.7.1.1

78 : Unclassified Silicates
7 :
14.18.24

14 : Silicates not Containing Aluminum
18 : Silicates of Mn and Na, K, Mg, Ca or Fe

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
BtwIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Pronunciation of BostwickiteHide

Pronunciation:
PlayRecorded byCountry
Jolyon RalphUnited Kingdom

Physical Properties of BostwickiteHide

Sub-Vitreous, Greasy, Silky, Sub-Metallic
Transparency:
Transparent, Translucent
Comment:
submetallic on prism surfaces.
Colour:
Brownish red
Streak:
White
Hardness:
Tenacity:
Brittle
Cleavage:
None Observed
Fracture:
Irregular/Uneven
Density:
2.93(10) g/cm3 (Measured)    

Optical Data of BostwickiteHide

Type:
Biaxial (-)
RI values:
nα = 1.775 nβ = 1.798 nγ = 1.800
2V:
Measured: 25° , Calculated: 32°
Birefringence:
0.025
Max. Birefringence:
δ = 0.025
Based on recorded range of RI values above.

Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.

Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.

Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
r < v strong
Optical Extinction:
Parallel
Pleochroism:
Strong
Comments:
X = Y = red-brown; Z = yellow-brown.

Chemistry of BostwickiteHide

Mindat Formula:
CaMn3+6Si3O16 · 7H2O
Element Weights:
Element% weight
O44.014 %
Mn39.426 %
Si10.078 %
Ca4.794 %
H1.688 %

Calculated from ideal end-member formula.
O
Mn
Si
Ca
H
Common Impurities:
Al,Fe,As,Mg

Crystallography of BostwickiteHide

Crystal System:
Orthorhombic
Morphology:
acicular in slightly divergent groups
Comment:
Orthorhombic (?). Point Group: n.d; Space Group: n.d.

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
11.30 Å(100)
8.19 Å(10)
6.03 Å(2)
5.57 Å(2)
4.575 Å(5)
3.951 Å(10)
3.826 Å(5)
3.786 Å(5)
3.548 Å(30)
3.238 Å(15)
3.110 Å(2)
2.898 Å(30)
2.718 Å(15)
2.567 Å(40)
2.475 Å(20)
2.442 Å(20)
2.262 Å(25)
2.238 Å(25)
2.094 Å(15)
2.074 Å(10)
1.951 Å(5)
1.863 Å(5)
1.794 Å(15)
1.679 Å(10)
1.634 Å(5)
1.599 Å(10)
1.501 Å(10)
1.470 Å(25)
Comments:
35-616

Geological EnvironmentHide

Type Occurrence of BostwickiteHide

General Appearance of Type Material:
As divergent sprays of bladed crystals, commonly composed of tiny microcrystals, to 250 μm
Place of Conservation of Type Material:
Harvard University, Cambridge, Massachusetts, 125617{125620; National Museum of Natural History, Washington, D.C., USA, C4222.
Geological Setting of Type Material:
Deposited with gray fluorite on fractures in silicate and oxide zinc ore
Associated Minerals at Type Locality:

Synonyms of BostwickiteHide

Other Language Names for BostwickiteHide

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Bostwickite associated with KittatinnyiteCa2Mn2Mn(SiO4)2(OH)4 · 9H2O

Related Minerals - Strunz-mindat GroupingHide

9.HC.05Erlianite(Fe,Mg)4(Fe,V)2Si6O15(OH,O)8Orth.
9.HC.20'Almbosite'Fe2+5Fe3+4V6+4Si3O27
9.HC.25'Aquacreptite (of Shepard)'Mg4Fe2Si6O19 · 8H2O with some Al2O3, or near
9.HC.30'Farallonite'2MgO · W2O5 · SiO2 · nH2O?Mon.
9.HC.35'Hokoite'Mn2+Mn3+2SiO6 · H2O
9.HC.40'Polyhydrite'

Fluorescence of BostwickiteHide

Not fluorescent in UV

Other InformationHide

Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

Internet Links for BostwickiteHide

References for BostwickiteHide

Localities for BostwickiteHide

Showing 1 localities.

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
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Locality ListHide

- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).

All localities listed without proper references should be considered as questionable.
USA (TL)
 
  • New Jersey
    • Sussex County
      • Franklin
        • Franklin Mine
Dunn & Leavens (1983) +2 other references
 
and/or  
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