Knoxvillite
A variety of Magnesiocopiapite
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Formula:
MgFe3+4(SO4)6(OH)2 · 20H2O
A chromiferous iron sulphate, not IMA-approved. May be a mixture of magnesiocopiapite and redingtonite, or could be a chromiferous variety of magnesiocopiapite.
Originally reported from Redington Mine, Knoxville, Napa Co., California, USA.
Identity of knoxvillite as magnesiocopiapite stated in Centennial Edition, Mineralogy of California.
Originally reported from Redington Mine, Knoxville, Napa Co., California, USA.
Identity of knoxvillite as magnesiocopiapite stated in Centennial Edition, Mineralogy of California.
Unique Identifiers
Mindat ID:
9302 (as Knoxvillite)
2486 (as Magnesiocopiapite)
2486 (as Magnesiocopiapite)
Long-form identifier:
mindat:1:1:9302:2 (as Knoxvillite)
mindat:1:1:2486:6 (as Magnesiocopiapite)
mindat:1:1:2486:6 (as Magnesiocopiapite)
Chemistry of Knoxvillite
Mindat Formula:
MgFe3+4(SO4)6(OH)2 · 20H2O
Element Weights:
Other Language Names for Knoxvillite
German:Knoxvillit
Spanish:Knoxvillita
Common Associates
Associations Based on Photo Data:
| 2 photos of Knoxvillite associated with Redingtonite | Fe2+Cr3+2(SO4)4 · 22H2O |
| 2 photos of Knoxvillite associated with Botryogen | MgFe3+(SO4)2(OH) · 7H2O |
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 Knoxvillite
mindat.org URL:
https://www.mindat.org/min-9302.html
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References for Knoxvillite
Localities for Knoxvillite
Showing 1 localities.
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).
All localities listed without proper references should be considered as questionable.
USA | |
| Palache et al. (1951) |
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