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Roweite

A valid IMA mineral species - grandfathered
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About RoweiteHide

02549140017271926471730.jpg
George Rowe
Formula:
Ca2Mn2+2B4O7(OH)6
Colour:
Light brown; colourless in transmitted light
Lustre:
Vitreous
Hardness:
4½ - 5
Specific Gravity:
2.935
Crystal System:
Orthorhombic
Name:
Named in 1937 by Harry Berman and Forest A. Gonyer in honor of Mr. George Rowe [1868 Cornwall, England, United Kingdom - 1947 USA], Mine Captain and mineral collector, of Franklin, New Jersey, USA.
Fedorovskite-Roweite Series. The manganese analogue of Fedorovskite.

Only one specimen known is known from the type locality (all additional specimens are "crumbs" from the original single specimen).


Unique IdentifiersHide

Mindat ID:
3466
Long-form identifier:
mindat:1:1:3466:7

Similar NamesHide

LöweiteA valid IMA mineral species - grandfatheredNa12Mg7(SO4)13 · 15H2O
RoméiteA solid-solution series between two end-member minerals
Roseite(Os,Ir)S

IMA Classification of RoweiteHide

Approved, 'Grandfathered' (first described prior to 1959)
First published:
1937

Classification of RoweiteHide

6.DA.25

6 : BORATES
D : Tetraborates
A : Neso-tetraborates
25.4.1.1

25 : ANHYDROUS BORATES CONTAINING HYDROXYL OR HALOGEN
4 : Tetraborates
9.4.1

9 : Borates
4 : Borates of Ca and Mn

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

Physical Properties of RoweiteHide

Vitreous
Transparency:
Transparent
Colour:
Light brown; colourless in transmitted light
Hardness:
4½ - 5 on Mohs scale
Tenacity:
Brittle
Cleavage:
Imperfect/Fair
{100}, fair; on {001}, {021}, poor
Fracture:
Conchoidal
Density:
2.935(5) g/cm3 (Measured)    2.939 g/cm3 (Calculated)

Optical Data of RoweiteHide

Type:
Biaxial (-)
RI values:
nα = 1.631 - 1.648 nβ = 1.640 - 1.660 nγ = 1.641 - 1.663
2V:
Measured: 15° to 28°, Calculated: 44°
Max. Birefringence:
δ = 0.010 - 0.015
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:
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:
weak
Pleochroism:
Weak
Comments:
X = very pale brown to colorless; Y = pale amber; Z = yellowish brown.
Comments:
Orientation: X = c; Y = b; Z = a

Chemistry of RoweiteHide

Mindat Formula:
Ca2Mn2+2B4O7(OH)6
Element Weights:
Element% weight
O46.498 %
Mn24.563 %
Ca17.919 %
B9.667 %
H1.352 %

Calculated from ideal end-member formula.
O
Mn
Ca
B
H

Crystallography of RoweiteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Space Group:
Pbam
Setting:
Pbam
Cell Parameters:
a = 8.28 Å, b = 13.35 Å, c = 9.02 Å
Ratio:
a:b:c = 0.62 : 1 : 0.676
Unit Cell V:
997.05 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Crystals rough, lath-shaped, flattened {010} and elongated [001]. Terminations not measurable.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0000393RoweiteMoore P B, Araki T (1974) Roweite, Ca2Mn2(OH)4[B4O7(OH)2]: Its atomic arrangement American Mineralogist 59 60-6519740293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.974 Å(100)
2.600 Å(72)
2.184 Å(49)
2.128 Å(37)
2.264 Å(32)
1.708 Å(32)
1.641 Å(29)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)
High-? alteration and/or metamorphism
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Type Occurrence of RoweiteHide

General Appearance of Type Material:
Narrow veinlet of almost pure roweite
Place of Conservation of Type Material:
National School of Mines, Paris, France.
Harvard University, Cambridge,Massachusetts, USA, 96252.
National Museum of Natural History (Smithsonian), Washington, D.C., USA, 105493, C6291.
Geological Setting of Type Material:
Hydrothermal veinlets transversing Precambrian metamorphosed Zn-Mn-Fe orebody (Franklin, NJ).
Associated Minerals at Type Locality:

Other Language Names for RoweiteHide

Dutch:Roweiet
German:Roweit
Russian:Ровеит
Spanish:Roweita

Relationship of Roweite to other SpeciesHide

Common AssociatesHide

Associations Based on Photo Data:
62 photos of Roweite associated with OlshanskyiteCa2[B3O3(OH)6](OH) · 3H2O
32 photos of Roweite associated with AndraditeCa3Fe3+2(SiO4)3
14 photos of Roweite associated with MagnetiteFe2+Fe3+2O4
9 photos of Roweite associated with CalciteCaCO3
8 photos of Roweite associated with JohnbaumiteCa5(AsO4)3(OH)
2 photos of Roweite associated with Wurtzite(Zn,Fe)S
1 photo of Roweite associated with BorcariteCa4Mg(B4O6(OH)6)(CO3)2
1 photo of Roweite associated with BultfonteiniteCa2(HSiO4)F · H2O
1 photo of Roweite associated with DatoliteCaB(SiO4)(OH)
1 photo of Roweite associated with TatarinoviteCa3Al(SO4)[B(OH)4](OH)6 · 12H2O

Related Minerals - Strunz-mindat GroupingHide

6.DA.10BoraxNa2(B4O5)(OH)4 · 8H2OMon. 2/m : B2/b
6.DA.15TincalconiteNa2(B4O7) · 5H2OTrig. 32 : R32
6.DA.20HungchaoiteMg(B4O7) · 9H2OTric. 1 : P1
6.DA.25FedorovskiteCa2Mg2B4O7(OH)6Orth. mmm(2/m2/m2/m) : Pbam
6.DA.30HydrochlorboriteCa4B8O15Cl2 · 21H2OMon. 2/m
6.DA.35UralboriteCa2[B3O3(OH)5 · OB(OH)3]Mon. 2/m
6.DA.40NumanoiteCa4Cu(B4O6(OH)6)(CO3)2Mon. 2/m : B2/m
6.DA.40BorcariteCa4Mg(B4O6(OH)6)(CO3)2Mon. 2/m : B2/m
6.DA.60Fontarnauite(Na,K)2(Sr,Ca)(SO4)[B5O8(OH)] · 2H2OMon. 2/m : P21/b

Other InformationHide

Notes:
Perfectly soluble in dilute HCl, solution giving boron reaction with turmeric paper.

Fuses at 1 (candle flame) to a black glass.

Colors the flame faintly green. With boron flux a strong green (boron).

In closed tube turns brown, gives off water and after long heating melts to a glass.
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 RoweiteHide

References for RoweiteHide

Reference List:

Localities for RoweiteHide

Showing 6 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.
China
 
  • Inner Mongolia
    • Chifeng City (Ulanhad League; Chifeng Prefecture)
      • Hexigten Banner (Keshiketeng Co.)
Pristine Minerals +1 other reference
Japan
 
  • Okayama Prefecture
    • Takahashi City
      • Bitchū
        • Fuka
Ando et al. (2015)
Mexico
 
  • San Luis Potosí
    • Charcas Municipality
Christopher Emproto
Chris Emproto (SCXRD,PXRD)
Russia
 
  • Buryatia
    • Yeravninsky District
      • Ozernoe ore cluster
Nikita Chukanov (IR- and EDS-analyses) +2 other references
USA (TL)
 
  • New Jersey
    • Sussex County
      • Franklin
Berman et al. (1937) +2 other references
 
and/or  
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