ye'elimite
Sign in to saveAlso known as IMA1984-052, Yeelimit
'''Ye'elimite''' is the naturally occurring form of anhydrous calcium sulfoaluminate, . It gets its name from Har Ye'elim in Israel in the Hatrurim Basin west of the Dead Sea where it was first found in nature by Shulamit Gross, an Israeli mineralogist and geologist who studied the Hatrurim Formation.
Key facts
- Mineral.name
- Ye'elimite
- Mineral.image
- Ye'elimite, Hydroxylellestadite, Anhydrite - Ronneburg, Thuringia.jpg
- Mineral.imagesize
- 260px
- Mineral.caption
- Ye'elimite (white) intergrown with Hydroxylellestadite (reddish-brown) in grey Anhydrite from Ronneburg, Thuringia, Germany (Picture size 6 mm)
- Mineral.category
- Sulfate mineral
- Mineral.IMAsymbol
- Ye
- Mineral.strunz
- 7.BC.15
- Mineral.system
- Isometric
- Mineral.class
- Gyroidal (432) H-M symbol: (432)
- Mineral.symmetry
- I4132
- Mineral.unit cell
- a = 18.392 Å; Z = 16
- Mineral.color
- White, gray
via Wikipedia infobox
Wikidata facts
- Subclass of
- sulfate mineral
- Image
- Ye'elimite, Hydroxylellestadite, Anhydrite - Ronneburg, Thuringia.jpg
Show 6 more facts
- crystal system
- cubic crystal system
- Commons category
- Ye'elimite
- Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
- 7.BC.15
- Nickel-Strunz 9th edition (updated 2009)
- 7.BC.15
- IMA Mineral Symbol
- Ye
- chemical formula
- Ca₄Al₆O₁₂(SO₄)
Sources (1)
via Wikidata · CC0
~2 min read
Encyclopedic overview
3 sectionsContents
- Occurrence in cement
- See also
- References
'''Ye'elimite''' is the naturally occurring form of anhydrous calcium sulfoaluminate, . It gets its name from Har Ye'elim in Israel in the Hatrurim Basin west of the Dead Sea where it was first found in nature by Shulamit Gross, an Israeli mineralogist and geologist who studied the Hatrurim Formation.
The mineral is cubic, with 16 formula units per unit cell, and a cell dimension of 1.8392 nm, and is readily detected and quantified in mixtures by powder x-ray diffraction.
Excerpted from Wikipedia’s “ye'elimite” article, available under the CC BY-SA 4.0 licence.