Weeksite

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Weeksite
Weeksita-RM1439.jpg
General
CategorySilicate mineral
Formula
(repeating unit)
K2(UO2)2Si6O15·4(H2O)
Strunz classification9.AK.30
Crystal systemOrthorhombic
Crystal classDipyramidal (mmm)
H-M symbol: (2/m 2/m 2/m)
Space groupPnnb (no. 52)
Unit cella = 14.26 Å, b = 35.88 Å
c = 14.2 Å; Z = 16
Identification
ColourYellow
Crystal habitOccurs as acicular to elongated bladed crystals, flattened on {010}, also as radiating fibrous clusters and spherulites, pseudotetragonal
CleavageDistinct prismatic
Mohs scale hardness1 - 2
LustreWaxy to silky
StreakYellow
DiaphaneityTransparent to translucent
Specific gravity4.1
Optical propertiesBiaxial (-)
Refractive indexnα = 1.596 nβ = 1.603 nγ = 1.606
Birefringenceδ = 0.010
PleochroismX = colorless; Y = pale yellow-green; Z = yellow-green
2V angleMeasured: 60°
Other characteristicsRadioactive.svg Radioactive greater than 70 Bq/g
References[1][2][3]

Weeksite is a naturally occurring uranium silicate mineral with the chemical formula: K2(UO2)2Si6O15•4(H2O), potassium uranyl silicate. Weeksite has a Mohs hardness of 1-2. It was named for USGS mineralogist Alice Mary Dowse Weeks (1909–1988).[2][3]

Appearance[]

Weeksite is visually similar to other uranium minerals such as carnotite and zippeite, both being encrustations that form on other rocks (usually sandstones or limestones).

Occurrence[]

Weeksite was first described in 1960 for an occurrence on Topaz Mountain, Thomas Range, Juab County, Utah.[1]

Weeksite occurs within small "opal" veins within rhyolite and agglomerates, and as encrustations in sandstones and limestones. It occurs associated with opal, chalcedony, calcite, gypsum, fluorite, uraninite, , uranophane, boltwoodite, carnotite and margaritasite.[2]

See also[]

References[]

  1. ^ a b "Weeksite mineral information and data". Mindat.org. 2011-06-19. Retrieved 2012-02-10.
  2. ^ a b c Handbook of Mineralogy
  3. ^ a b Webmineral data for weeksite
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