weeksite
Sign in to saveWeeksite 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).
Key facts
- Mineral.name
- Weeksite
- Mineral.image
- Weeksita-RM1439.jpg
- Mineral.category
- Silicate mineral
- Mineral.formula
- K2(UO2)2Si6O15·4(H2O)
- Mineral.IMAsymbol
- Wks
- Mineral.strunz
- 9.AK.30
- Mineral.system
- Orthorhombic
- Mineral.class
- Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m)
- Mineral.symmetry
- Pnnb (no. 52)
- Mineral.unit cell
- a = 14.26 Å, b = 35.88 Å c = 14.2 Å; Z = 16
- Mineral.colour
- Yellow
- Mineral.habit
- Occurs as acicular to elongated bladed crystals, flattened on {010}, also as radiating fibrous clusters and spherulites, pseudotetragonal
- Mineral.cleavage
- Distinct prismatic
- Mineral.mohs
- 1–2
- Mineral.lustre
- Waxy to silky
- Mineral.streak
- Yellow
- Mineral.diaphaneity
- Transparent to translucent
- Mineral.gravity
- 4.1
via Wikipedia infobox
Wikidata facts
- Subclass of
- nesosilicates
- Named after
- Alice D. Weeks
- Image
- Weeksite.jpg
Show 8 more facts
- Nickel-Strunz 9th edition (updated 2009)
- 9.AK.30
- Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
- 9.AK.30
- crystal system
- monoclinic crystal system
- Commons category
- Weeksite
- streak color
- yellow
- IMA Mineral Symbol
- Wks
- chemical formula
- K₂(UO₂)₂(Si₅O₁₃) * 4H₂O
- Strunz 8th edition (series ID, updated)
- VIII/A’.15
via Wikidata · CC0
~2 min read
Encyclopedic overview
4 sectionsContents
- Appearance
- Occurrence
- See also
- References
{{infobox mineral | name = Weeksite | boxwidth = | image = Weeksita-RM1439.jpg | alt = | caption = | category = Silicate mineral | formula = K2(UO2)2Si6O15·4(H2O) | IMAsymbol = Wks | molweight = | strunz = 9.AK.30 | dana = | system = Orthorhombic | class = Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) | symmetry = Pnnb (no. 52) | unit cell = a = 14.26 Å, b = 35.88 Å c = 14.2 Å; Z = 16 | color = | colour = Yellow | habit = Occurs as acicular to elongated bladed crystals, flattened on {010}, also as radiating fibrous clusters and spherulites, pseudotetragonal | twinning = | cleavage = Distinct prismatic | fracture = | tenacity = | mohs = 1–2 | lustre = Waxy to silky | streak = Yellow | diaphaneity = Transparent to translucent | gravity = 4.1 | density = | polish = | opticalprop = Biaxial (−) | refractive = nα = 1.596 nβ = 1.603 nγ = 1.606 | birefringence = δ = 0.010 | pleochroism = X = colorless; Y = pale yellow-green; Z = yellow-green | 2V = Measured: 60° | dispersion = | extinction = | length fast/slow = | fluorescence = | absorption = | melt = | fusibility = | diagnostic = | solubility = | impurities = | alteration = | other = 25px Radioactive greater than 70 Bq/g | references = }} 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).
==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).
Excerpted from Wikipedia’s “weeksite” article, available under the CC BY-SA 4.0 licence.