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Formula: Na2Ca2(V10O28).24H2O
Valence: Na2Ca2(V5+10O28).24H2O
Hydrated decavanadate,
pascoite family group
Crystal System: Triclinic
Specific gravity: 2.35 calculated for the empirical formula and 2.352 for the ideal formula
Hardness: 1½
Streak: Yellow
Colour: Yellow-orange to tinted orange-brown
Luminescence: Does not fluoresce in short wave or long wave UV
Environments
Localities
The type locality, the Saint Jude Mine, Slick Rock Mining District, Colorado, USA, is a stope not far from the interconnected West
Sunday and Sunday mines. All three mines are currently inactive and their entrances are sealed. Kokinosite is rare; it
was found growing on a corvusite -
montroseite-bearing sandstone block
and is closely associated with gypsum, huemulite,
metarossite, pascoite,
rossite and wernerbaurite. Other minerals
found in the same area in the St. Jude mine include calciodelrioite,
delrioite, hendersonite,
hughesite, nashite,
powellite, postite and
schindlerite. Other minerals found nearby in adjacent areas of the West Sunday mine
are andersonite, gunterite,
hewettite, munirite,
natrozippeite, pyrite,
rakovanite, sherwoodite and
tyuyamunite.
The Kokinosite forms from the oxidation of montroseite -
corvusite assemblages in a moist environment. Mining operations have exposed unoxidised
and oxidised phases. Under ambient temperatures and generally oxidising near-surface environments, water reacts with
pyrite in the deposit to form aqueous solutions with relatively low pH (acid). The various
secondary vanadate phases that
formed depend upon the ambient conditions and the presence of other cations such as Na1+, Ca2+,
Mg2+ and Al3+.
Kokinosite typically occurs as tablets or blades up to 0.05 mm thick, with stepped faces, and 1 mm
maximum dimension. Crystals sometimes form larger, irregularly stepped crystal masses up to several mm
across. Kokinosite is yellow orange, although it is sometimes tinted orange-brown; the streak is
yellow, typical of decavanadate-bearing minerals. The lustre of
kokinosite is subadamantine, and the mineral is transparent
(CM 52.1.15-25).
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