Parachrysotile
A structural variant of Chrysotile
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Hardness:
2½ - 3
Crystal System:
Orthorhombic
Name:
Named in 1956 by Eric James William Whittaker from the Greek παρα "para" = beyond and chrysotile for its relationship to the root name mineral.
Unique Identifiers
Mindat ID:
3083
Long-form identifier:
mindat:1:1:3083:6
GUID
(UUID V4):
(UUID V4):
845f22e2-e74f-477f-afde-4f681b92f38d
IMA Classification of Parachrysotile
Discredited
Classification of Parachrysotile
14.4.7
14 : Silicates not Containing Aluminum
4 : Silicates of Mg
14 : Silicates not Containing Aluminum
4 : Silicates of Mg
Physical Properties of Parachrysotile
Hardness:
2½ - 3 on Mohs scale
Optical Data of Parachrysotile
Type:
Biaxial (-)
RI values:
nα = 1.545 - 1.569 nβ = 1.546 - 1.569 nγ = 1.553 - 1.571
2V:
Measured: 20° to 60°
Max Birefringence:
δ = 0.008
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
and does not take into account mineral colouration.
Surface Relief:
Low
Dispersion:
relatively weak
Crystallography of Parachrysotile
Crystal System:
Orthorhombic
Cell Parameters:
a = 5.3 Å, b = 9.24 Å, c = 14.71 Å
Ratio:
a:b:c = 0.574 : 1 : 1.592
Unit Cell V:
720.38 ų (Calculated from Unit Cell)
Z:
4
Other Language Names for Parachrysotile
German:Parachrysotil
Other Information
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 Parachrysotile
mindat.org URL:
https://www.mindat.org/min-3083.html
Please feel free to link to this page.
Please feel free to link to this page.
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References for Parachrysotile
Localities for Parachrysotile
Locality List
- 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.
All localities listed without proper references should be considered as questionable.
Eswatini | |
| Canadian Mineralogist (1979) |
Germany | |
| Wittern (2001) |
South Africa | |
| Cairncross et al. (1995) |
USA | |
| Castor et al. (2004) |
Zimbabwe | |
| Mineralogical Society of America - ... |