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Formula: Cu3PbO(AsO3OH)2(OH)2
Anhydrous arsenate
Crystal System: Monoclinic
Specific gravity: 5.5
Hardness: 4½
Streak: Siskin green to apple green
Colour: Green, apple-green, yellow-green
Solubility: Soluble with difficulty in hydrochloric acid
Bayldonite is a relatively rare secondary mineral
occurring in the oxidised zones of copper and lead bearing deposits. Associated minerals include
adamite, anglesite,
azurite, baryte,
beudantite, cerussite,
duftite, keyite,
malachite, mimetite,
olivenite, schultenite and
tsumebite
(Mindat).
Localities
At the Kintore open cut, Broken Hill, New South Wales, Australia, bayldonite most commonly occurs with
mimetite, segnitite -
beudantite, mawbyite and members of
the olivenite - adamite series. It also
occurs with carminite, duftite and
conichalcite, and with late-stage minerals including
brochantite, malachite,
azurite and iodargyrite. In one
unusual assemblage bayldonite crystals were found with pyromorphite and
natrojarosite on gahnite-bearing
quartzite
(AJM 3.1.55).
Bayldonite from the Kintore Open Cut - Image
At the New Cobar deposit, New South Wales, Australia, bayldonite occurs as crystals on
quartz commonly associated with duftite.
Other associated minerals include gartrellite,
segnitite, agardite-(Y) and
azurite; a bayldonite pseudomorph after
mimetite has also been found here
(AJM 11.2.79).
Bayldonite from the New Cobar Mine - Image
At Kayrakty, Kazakhstan, bayldonite occurs in the oxidation zone of a metasomatic
lead-zinc deposit in the upper
layers of baryte lenses of considerable size embedded in
sandstone. Bayldonite is formed by
pseudomorphic substitution of cerussite,
resulting in accumulations in malachite and
azurite. Occasionally bayldonite is found on thick crusts formed in
fractures in the baryte. The bayldonite is usually intergrown with
beudantite, and sometimes has cavities with small crystals of
anglesite and azurite
(AM 66.148–153).
Associated minerals include beudantite,
anglesite, cerussite,
malachite, azurite and
baryte
(HOM).
At Tsumeb, Namibia, bayldonite is associated with mimetite,
olivenite, azurite,
malachite, tsumebite,
cuprian adamite, duftite,
keyite, schultenite and
philipsbornite
(HOM). Bayldonite pseudomorphs after
mimetite have been found here
(KL p199).
Bayldonite from the Tsumeb Mine - Image
At the type locality, Penberthy Croft mine, St Hilary, Cornwall, England, UK, bayldonite is associated with
quartz
(Mindat).
At Brandy Gill mine, Caldbeck, Allerdale, Cumbria, England, UK, bayldonite occurs with
galena on a
quartz matrix
(AESS).
Bayldonite from the Brandy Gill Mine - Image
At the San Rafael mine, Nye county, Nevada, USA, spherules and druses to 1 mm of bayldonite have been found
associated with plumbojarosite and
wulfenite crystals. Rarer single crystals of
chlorargyrite - bromargyrite
and coatings of arseniosiderite also occur in this assemblage
(R&M 85.6.516).
The Activity-pH diagram below was calculated at 298.2 K for the main
Cu2+ and Pb2+ arsenate minerals.
Boundaries are calculated for constant activities (roughly equivalent to concentrations) of Pb2+ and Cl-
ions in solution, over a range of values of pH and of Cu2+ activity. Higher chloride activites make the stability
fields of bayldonite and duftite vanish,
with respect to the encroachment of that of mimetite
(LMW p269).
The arsenate mineral formulae are:
philipsbornite PbAl3(AsO4)(AsO3OH)(OH)6
mimetite Pb5(AsO4)3Cl
duftite PbCu(AsO4)(OH)
bayldonite Cu3PbO(AsO3OH)2(OH)2
olivenite Cu2(AsO4)(OH)
cornwallite Cu5(AsO4)2(OH)4
clinoclase Cu3(AsO4)(OH)3
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