Formula: Zn4(SO4)(OH)6.4H2O
Hydrated sulphate, namuwite group
Crystal System: Trigonal
Specific gravity: 2.77 measured, 2.81 calculated
Hardness: 2
Streak: Pale green
Colour: Sea green
Common impurities: Cu
Namuwite is a very rare secondary mineral; it is a post-mining phase,
typically formed through the oxidation of sphalerite-bearing veinstone in mine workings and
within zinc and copper rich mine dumps (MW).
Associated minerals include hydrozincite,
schulenbergite, serpierite,
ktenasite, devilline and
gypsum
(HOM).
Localities
At the Smallcleugh Mine, Nenthead, Alston Moor, Eden, Cumbria, England, UK, pearly sea-green namuwite forms flat,
triangular plates up to 200 microns across. Only rarely do the crystals show development of the full hexagonal plates
seen on the type specimen. The plates are commonly curved, and are typically grouped together as sheaves.
Serpierite is present as turquoise to copper-blue mm-long bundles comprising
wispy or stellate acicular groups. Textural evidence tentatively suggests that
schulenbergite and namuwite at Smallcleugh Mine formed later than
the serpierite and as the former have lower
copper:zinc ratios than
serpierite it appears that within the
supergene assemblage
copper became progressively depleted
(JRS 3.23-24).
At the Frongoch Mine, Devil's Bridge, Ceredigion, Wales, UK, namuwite occurs very rarely as crystal clusters to 0.5 mm on
quartz-galena veinstone. It is clearly post-mining in
origin and late in the paragenesis, typically overgrowing langite,
wroewolfeite, susannite or
hydrocerussite
(MW).
At the type locality, the Aberllyn mine, Betws-y-coed, Gwydyr Forest area, Conwy, Wales, UK, namuwite occurs encrusting
hydrozincite (Dana) on a breccia
composed of slate fragments cemented by sphalerite,
quartz, calcite and
ankerite
(AM 81.238-243, Mindat, MW).
At the Dylife Mine, Penegoes, Powys, Wales, UK, namuwite is associated with
schulenbergite on altered sphalerite
(MW).
At Balmat, St Lawrence county, New York, USA, namuwite is associated with magnetite
(Minrec 41.6.536).
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