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| Esperite
was named in 1965 by Paul Brian Moore and Paul H. Ribbe in
honor of Esper Signius
Larsen, Jr. (March 14, 1879 - March 8, 1961), petrologist and Professor of Geology at Harvard
University, Cambridge, Massachusetts, USA.
| Discovered
in 1928;
IMA
status: Valid (IMA approved
1965) |
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Chemistry
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Chemical
Formula: |
PbCa3Zn4(SiO4)4
|
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Lead
Calcium Zinc Silicate |
Molecular
Weight: |
957.33 gm
|
Composition: |
Calcium |
12.56 % |
Ca |
17.57 % |
CaO |
|
Zinc |
27.32 % |
Zn |
34.01 % |
ZnO |
|
Silicon |
11.73 % |
Si |
25.11 % |
SiO2 |
|
Lead |
21.64 % |
Pb |
23.31 % |
PbO |
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Oxygen |
26.74 % |
O |
|
|
|
|
100.00 % |
|
100.00 % |
= TOTAL OXIDE |
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Classification
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Mineral
Classification: |
Silicates
(Germanates)
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Strunz 8th
Ed. ID:
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8/A.03-20
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Nickel-Strunz 10th
Ed. ID:
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9.AB.15
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9 : SILICATES (Germanates)
A : Nesosilicates
B : Nesosilicates without additional anions; cations in [4] and greater coordination
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Related
to: |
Isostructural with:
Beryllonite, Larsenite
|
Varieties: |
None
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Synonyms: |
Calcium-Larsenite, IMA1964-027
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Crystal
Data
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Crystallography:
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Monoclinic
- Prismatic
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Crystal
Habit:
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Granular
aggregates, massive, to 9 cm
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Twinning:
|
None
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Physical
Properties
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|
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Cleavage: |
Distinct
on {010} and {100}; poor on {101}
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Fracture: |
Conchoidal
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Tenacity:
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Brittle
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Moh's
Hardness: |
5.0
- 5.5
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Density:
|
4.28
- 4.42 (g/cm3)
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Luminescence:
|
Fluoresces
bright yellow under
SW UV (Franklin); dull yellow under LW UV; kelly green
cathodoluminescence |
Radioactivity:
|
Not
Radioactive
|
|
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Optical
Properties
|
|
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Color: |
White, off-white,
pale tan;
darkening on exposure to light
|
Transparency: |
Opaque,
transparent in small grains |
Luster: |
Sub-vitreous;
dull to slightly greasy |
Refractive
Index: |
1.762
- 1.774
Biaxial ( - )
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Birefringence: |
0.012
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Dispersion: |
Very Strong |
Pleochroism: |
None
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Occurances
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Geological
Setting: |
Metamorphosed stratiform zinc-iron-manganese orebody.
|
Common
Associations: |
Willemite,
Zincite, Hardystonite, Glaucochroite, Andradite, Franklinite,
Clinohedrite, Leucophoenicite, Larsenite, Copper
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Common
Impurities: |
Fe,
Mn, Mg
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Type
Locality: |
Parker Mine (Parker shaft), Franklin Mine, Franklin, Franklin Mining District, Sussex County, New Jersey, USA
|
Year
Discovered: |
1928
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View
mineral photos: |
Esperite
Mineral Photos and Locations |
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More
Information
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|
Mindat.org
Webmineral.com
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Esperite is
a rare complex calcium lead zinc silicate mineral that was discovered
in 1928 at the Parker shaft of the Franklin Mine, Franklin,
Sussex County, New Jersey, USA. It was originally named
calcium-Larsenite for its calcium content and relationship
to Larsenite (PbZnSiO4). Larsenite was named in 1928 by Charles
Palache, Lawson Henry Bauer and Harry Berman to
honor Esper Signius Larsen, Jr. (1879 - 1961), petrologist and Professor of Geology at Harvard
University, Cambridge, Massachusetts, USA. Calcium-Larsenite was renamed
"Esperite" in 1965 by Paul Brian Moore
and Paul H. Ribbe also in honor of Esper Larsen, Jr.
It was approved by the International Mineralogical Association
(IMA) as
a valid distinct mineral species in 1965.
Esperite
is one of over 350 types of minerals found at
Franklin and Sterling Hill, New Jersey. It is also one
of about 89 fluorescent minerals found there. Esperite has
a white or off-white to pale tan appearance in daylight but is prized
for its brilliant yellow to yellow-green fluorescence
under shortwave (SW) ultraviolet (UV) light (click on
the picture above to see its color under SW-UV light). It is often
found in association with other fluorescent minerals
such as Calcite,
Hardystonite,
Willemite,
Clinohedrite
and non-fluorescent, black Franklinite. Although Esperite is mainly known for
its occurrence at Franklin, it is also found as prismatic
crystals up to 1 mm in length at the El Dragón Mine,
Antonio Quijarro Province, Potosi Department, Bolivia.
These are the only two localities known to contain Esperite.
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