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Mendipite

A valid IMA mineral species - grandfathered
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About MendipiteHide

Formula:
Pb3Cl2O2
Colour:
Colourless, white, grey, often tinged yellow, blue, red; nearly colourless in transmitted light
Lustre:
Adamantine, Resinous, Silky, Pearly
Hardness:
2½ - 3
Specific Gravity:
7.24
Crystal System:
Orthorhombic
Name:
After the type locality at the Mendip Hills, Somerset, England, UK.
Chemically similar to damaraite. Compare UM1990-25-O:ClPbS.


Unique IdentifiersHide

Mindat ID:
2641
Long-form identifier:
mindat:1:1:2641:9

Similar NamesHide

MendigiteA valid IMA mineral speciesMn2Mn2MnCa(Si3O9)2

IMA Classification of MendipiteHide

Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Pb2+3O2Cl2

Classification of MendipiteHide

3.DC.70

3 : HALIDES
D : Oxyhalides, hydroxyhalides and related double halides
C : With Pb (As,Sb,Bi), without Cu
10.3.1.1

10 : OXYHALIDES AND HYDROXYHALIDES
3 : A3(O,OH)2Xq
8.8.5

8 : Halides - Fluorides, Chlorides, Bromides and Iodides; also Fluoborates and Fluosilicates
8 : Halides of Pb

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

Physical Properties of MendipiteHide

Adamantine, Resinous, Silky, Pearly
Transparency:
Transparent, Translucent
Colour:
Colourless, white, grey, often tinged yellow, blue, red; nearly colourless in transmitted light
Streak:
White
Hardness:
2½ - 3 on Mohs scale
Cleavage:
Perfect
On {110} perfect; {100} and {010} less perfect.
Fracture:
Irregular/Uneven, Conchoidal
Density:
7.24 g/cm3 (Measured)    7.22 g/cm3 (Calculated)

Optical Data of MendipiteHide

Type:
Biaxial (+/-)
RI values:
nα = 2.24 nβ = 2.27 nγ = 2.31
2V:
Measured: 90° , Calculated: 84°
Max. Birefringence:
δ = 0.070
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:
relatively strong
Optical Extinction:
Parallel. X = a; Y = b; Z = c.

Chemistry of MendipiteHide

Mindat Formula:
Pb3Cl2O2
Element Weights:
Element% weight
Pb85.797 %
Cl9.787 %
O4.417 %

Calculated from ideal end-member formula.
Pb
Cl
O

Crystallography of MendipiteHide

Crystal System:
Orthorhombic
Class (H-M):
222 - Disphenoidal
Space Group:
P212121
Cell Parameters:
a = 9.52 Å, b = 11.87 Å, c = 5.87 Å
Ratio:
a:b:c = 0.802 : 1 : 0.495
Unit Cell V:
663.32 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Fibrous or columnar masses, often radiated.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0006898MendipiteKrivovichev S V, Burns P C (2001) Crystal chemistry of lead oxide chlorides. I. Crystal structures of synthetic mendipite, Pb3O2Cl2, and synthetic damaraite, Pb3O2(OH)Cl European Journal of Mineralogy 13 801-80920010293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Loading XRD data...
Data Set:
Data courtesy of RRUFF project at University of Arizona, used with permission.
Powder Diffraction Data:
d-spacingIntensity
7.40 Å(60)
3.78 Å(60)
3.51 Å(70)
3.08 Å(60)
3.04 Å(80)
2.78 Å(100)
2.64 Å(90)
Comments:
Låangban, Sweden.

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
47g : [Halogen-bearing surface weathering minerals]
47h : [Near-surface oxidized, dehydrated minerals]
Stage 10b: Anthropogenic minerals<10 Ka
56 : Slag and smelter minerals (see also #51 and #55)

Type Occurrence of MendipiteHide

General Appearance of Type Material:
Radiating masses of pale straw-yellow prismatic crystals and cleavages.
Associated Minerals at Type Locality:

Synonyms of MendipiteHide

Other Language Names for MendipiteHide