Log InRegister
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreOur ScienceMindat Newsletter [Free Download]Contact Us
Donate to MindatSponsor a PageCorporate SponsorshipSponsored Pages
Learning CenterWhat Is a Mineral?The Most Common Minerals on EarthInformation for EducatorsMindat ArticlesMindat Newsletter [Free Download]The ElementsThe Mineral Quiz
Search FormMinerals by PropertiesMinerals by ChemistryMineral Visual ExplorerAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDMinerals by CountryAlphabetical Mineral IndexAlphabetical Locality SearchMineral Association SearchList of CountriesLocalities Near MePhoto SearchSearch ArticlesSearch GlossaryThe Rock H. Currier Digital LibraryMore Search Options
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
MineralsPetrologyFossilsMeteoritesGeologic Time
Mining CompaniesStatisticsMineral MuseumsClubs & OrganizationsMineral Shows & EventsDevice SettingsTime Machine
Read DiscussionsIdentification Request
Photo SearchPhoto GalleriesSearch by ColourPhoto Colour ExplorerNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Metavoltine from
Brigham Quarry, Brigham, Allerdale, Cumbria, England, UK


Locality type:Quarry
Classification
Species:Metavoltine
Formula:K2Na6Fe2+Fe63+O2(SO4)12 · 18H2O
Comments: It occurs as patchy, vivid yellow efflorescent crusts coating areas up to 1.5 m across
of the lowest two sandstone beds exposed in the quarry. Individual crusts, which are up to 10 cm
across and 0.5 mm thick, consist of rounded aggregates up to 1 mm across composed of minute platy crystals. The two sandstone beds are separated by a 25 mm thick dark grey carbonaceous mudstone parting. In places small patches of metavoltine encrust this parting, or are concentrated on the sandstone within 10 cm above or below this level. Oxidation of pyrite within the mudstone parting
together with diffusion of sulphate-rich fluids through the surface layers of the adjacent very
porous sandstone have almost certainly provided the source of the metavoltine.
a
Habit:minute platy crystals
Colour:vivid yellow.
Quality for species:Good crystals or rich for species - important (!)
Abundance at site:Common
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Metavoltine data
Locality Data:Click here to view Brigham Quarry, Brigham, Allerdale, Cumbria, England, UK
Data Identifiers
Mindat Occurrence Record ID:19217
Long-form Identifier:1:3:19217:0
GUID (UUID V4):0
References
 
and/or  
Mindat.orgÂŪ is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization. MindatÂŪ and mindat.orgÂŪ are registered trademarks of the Hudson Institute of Mineralogy.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2026, except where stated. Most political location boundaries are ÂĐ OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph and Ida Chau.
Content on this site may not be used to train, fine-tune, or otherwise develop artificial intelligence or machine learning models without prior written permission - see our Terms & Conditions.
To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: October 22, 2026 04:03:11
Go to top of page