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Bannister, F. A. (1932) The distinction of pyrite from marcasite in nodular growths. Mineralogical Magazine and Journal of the Mineralogical Society, 23 (138) 179-187 doi:10.1180/minmag.1932.023.138.04

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Reference TypeJournal (article/letter/editorial)
TitleThe distinction of pyrite from marcasite in nodular growths
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsBannister, F. A.Author
Year1932 (September)Volume23
Page(s)179-187Issue138
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_23/23-138-179.pdf+
DOIdoi:10.1180/minmag.1932.023.138.04
Mindat Ref. ID7144Long-form Identifiermindat:1:5:7144:8
GUID10626aef-5df2-4221-9daa-e8f5fad2a833
Full ReferenceBannister, F. A. (1932) The distinction of pyrite from marcasite in nodular growths. Mineralogical Magazine and Journal of the Mineralogical Society, 23 (138) 179-187 doi:10.1180/minmag.1932.023.138.04
Plain TextBannister, F. A. (1932) The distinction of pyrite from marcasite in nodular growths. Mineralogical Magazine and Journal of the Mineralogical Society, 23 (138) 179-187 doi:10.1180/minmag.1932.023.138.04
In(1932) Mineralogical Magazine Vol. 23 (138) Mineralogical Society
Abstract/NotesA recent account of pseudo-meteorites by Dr. L. J. Spencer includes a description of nodules of pyrite ‘popularly thought to be “thunderbolts”’. Dr. Spencer himself collected in 1931 a large number from the Lower Chalk outcropping on the foreshore below ‘The Warren’ at Folkestone, Kent. Some of these show well-developed octahedra 5 to 10 ram. across on the outer surface, undoubtedly to be referred to pyrite. More commonly the nodules exhibit small distorted octahedra which might easily be mistaken for marcasite. Indeed, in the past, many of these nodules from the Chalk at Folkestone and elsewhere, have been named marcasite, and they were so labelled in the British Museum collection. Dr. Spencer, therefore, suggested that modern methods should be applied to those cases where the crystalline form is distorted or shOt sufficiently developed to serve as a means of distinction between pyrite and marcasite. The methods suggested in his paper are (1) X-rays, (2) polarized light reflected from polished sections of nodules.

Map of Localities

Locality Pages

LocalityCitation Details
Morro Velho mine, Nova Lima, Minas Gerais, Brazil
Folkestone and Hythe District, Kent, England, UK
Mineral Point area, Upper Mississippi Valley Mining District, Iowa County, Wisconsin, USA

Mineral Pages

MineralCitation Details
Marcasite
Pyrite

Mineral Occurrences

LocalityMineral(s)
Newhaven Cliffs (Fort Hill), Newhaven, Lewes, East Sussex, England, UK Pyrite


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