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Gerstleyite

A valid IMA mineral species - grandfathered
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About GerstleyiteHide

09750580017271923528502.jpg
James M. Gerstley
Formula:
Na2(Sb,As)8S13 · 2H2O
Colour:
Cinnabar red, darkening on exposure
Lustre:
Sub-Adamantine
Hardness:
Specific Gravity:
3.62
Crystal System:
Monoclinic
Name:
Named in honor of James Mack Gerstley (11 November 1907, London, England - 2 June 2007, San Francisco, California, USA), president of the Pacific Coast Borax Company (later the United States Borax & Chemical Corporation) from 1933-1961. He was inducted into the US National Mining Hall of Fame in 2003.
Homeotypic with gerstleyite and gillulyite.

Occurs as red spherules with fibrous to platy structure up to 2.5 cm in clay with borates. This was the first known sodium sulfosalt.


Unique IdentifiersHide

Mindat ID:
1684
Long-form identifier:
mindat:1:1:1684:7

IMA Classification of GerstleyiteHide

Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Na2(Sb,As)8S13·2H2O
First published:
1956

Classification of GerstleyiteHide

2.HE.05

2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
H : Sulfosalts of SnS archetype
E : With alkalies, H2O
3.8.8.1

3 : SULFOSALTS
8 : 1 < ø < 2
5.0.1

5 : Sulphosalts - Sulpharsenites and Sulphobismuthites (those containing Sn, Ge,or V are in Section 6)
0 : Sulpharsenites etc. of the alkali metals

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

Physical Properties of GerstleyiteHide

Sub-Adamantine
Transparency:
Translucent
Colour:
Cinnabar red, darkening on exposure
Streak:
Bright cinnabar red
Hardness:
2½ on Mohs scale
Hardness Data:
Measured
Tenacity:
Brittle
Cleavage:
Perfect
Perfect on {010} and {100}; poor on {001}.
Fracture:
None observed
Density:
3.62 g/cm3 (Measured)    3.723 g/cm3 (Calculated)

Optical Data of GerstleyiteHide

Type:
Biaxial
Dispersion:
r < v extreme
Pleochroism:
Weak
Comments:
X = salmon red, Y = Z = deep blood red.
Comments:
Refractive indices > 2.0

Chemistry of GerstleyiteHide

Mindat Formula:
Na2(Sb,As)8S13 · 2H2O
Element Weights:
Element% weight
Sb66.132 %
S28.300 %
Na3.122 %
O2.173 %
H0.274 %

Calculated from ideal end-member formula.
Common Impurities:
Li

Crystallography of GerstleyiteHide

Crystal System:
Monoclinic
Class (H-M):
m - Domatic
Space Group:
Bm
Setting:
Cm
Cell Parameters:
a = 9.911(8) Å, b = 23.05(2) Å, c = 7.097(8) Å
β = 127.85(7)°
Ratio:
a:b:c = 0.43 : 1 : 0.308
Unit Cell V:
1,280.21 ų (Calculated from Unit Cell)
Z:
2
Morphology:
Fibrous and platy

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0012197GerstleyiteNakai I, Appleman D E (1981) The crystal structure of gerstleyite Na2(Sb,As)8S13*2H2O: the first sulfosalt mineral of sodium Chemistry Letters 1981 1327-13301981Baker mine, Kern County, Boron, California, USA0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
11.85 Å(100)
3.05 Å(90)
5.64 Å(70)
4.03 Å(70)
2.81 Å(50)
2.739 Å(40)
1.934 Å(40)
Comments:
From type material at Baker Mine, Kern Co., Ca., USA

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
High-? alteration and/or metamorphism
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])
Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere<0.6
53 : Other minerals with taphonomic origins<0.4
Geological Setting:
As above

Type Occurrence of GerstleyiteHide

General Appearance of Type Material:
Cinnabar-red platy-fibrous spherules, up to 2.5 cm, with a crudely radial fibrous structure, in clay. Also occurs as fine-granular aggregates and as groups of small, thick plates with rough surfaces. The individual crystals of the aggregates are warped an
Place of Conservation of Type Material:
Harvard University, Cambridge, Massachusetts, USA, 111307.
National Museum of Natural History, Washington, D.C., USA, 106916.
Geological Setting of Type Material:
Low temperature borate evaporite.
Associated Minerals at Type Locality:

Other Language Names for GerstleyiteHide

Common AssociatesHide

Associations Based on Photo Data:
8 photos of Gerstleyite associated with KerniteNa2[B4O6(OH)2] · 3H2O
7 photos of Gerstleyite associated with ProbertiteNaCa[B5O7(OH)4] · 3H2O
4 photos of Gerstleyite associated with PararealgarAs4S4
1 photo of Gerstleyite associated with 'Clay'

Related Minerals - Strunz-mindat GroupingHide

2.HE.10Ambrinoite[K,(NH4)]2(As,Sb)6(Sb,As)2S13 · H2OTric. 1 : P1

Other InformationHide

Notes:
Fuses at 2.

Completely soluble in dilute alkalies, and is decomposed by dilute HCl with the evolution of H2S and the separation of a yellow residue.
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Industrial Uses:
none

Internet Links for GerstleyiteHide

References for GerstleyiteHide

Localities for GerstleyiteHide

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.
USA
 
  • California
    • Kern County
www.mineralsocal.org (1999)
U.S. Borax
Frondel et al. (1956) +1 other reference
Frondel et al. (1956)
          • West Baker
collected by Rock Currier
 
and/or  
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