2006
DOI: 10.3133/sir20065085
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Geochemical and mineralogical characterization of the abandoned Valzinco (lead-zinc) and Mitchell (gold) mine sites prior to reclamation, Spotsylvania County, Virginia

Abstract: Horizontal coordinate information is referenced to the insert datum name (and abbreviation) here, for instance, "North American Datum of 1983 (NAD 83)" Altitude, as used in this report, refers to distance above the vertical datum.

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Cited by 2 publications
(4 citation statements)
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“…Fluvial tailings were generally < 1 m (3.3 ft) thick. In general, unoxidized tailings were encountered at depths between 20 and 30 cm (7.9 to 11.8 in) (Hammarstrom et al, 2006). The tailings were dominated by quartz, muscovite, chlorite, and pyrite, and lesser amounts of sphalerite, galena, chalcopyrite, magnetite, and albite.…”
Section: Mine-waste Characteristicsmentioning
confidence: 98%
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“…Fluvial tailings were generally < 1 m (3.3 ft) thick. In general, unoxidized tailings were encountered at depths between 20 and 30 cm (7.9 to 11.8 in) (Hammarstrom et al, 2006). The tailings were dominated by quartz, muscovite, chlorite, and pyrite, and lesser amounts of sphalerite, galena, chalcopyrite, magnetite, and albite.…”
Section: Mine-waste Characteristicsmentioning
confidence: 98%
“…The tailings were dominated by quartz, muscovite, chlorite, and pyrite, and lesser amounts of sphalerite, galena, chalcopyrite, magnetite, and albite. Jarosite, gypsum, and secondary efflorescent salts were common in the oxidized upper zones of the tailings material (Hammarstrom et al, 2006;Seal et al, 2008).…”
Section: Mine-waste Characteristicsmentioning
confidence: 99%
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