Edge Rewrite
// HTMLRewriter · presentation

This page was redesigned at the edge.

Cloudflare fetched the original article and streamed it through HTMLRewriter to apply an entirely new visual system without rebuilding the source page.

Jump to content

Tamarugite

From Wikipedia, the free encyclopedia
Tamarugite
General
CategorySulfate mineral
FormulaNaAl(SO4)2 · 6H2O
IMA symbolTmr[1]
Strunz classification7.CC.10
Dana classification29.5.3.1
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
Space groupP21/a (no. 14)
Identification
ColorColorless
Crystal habitPrismatic, tabular
TwinningPolysynthetic
Cleavage{010} perfect
Mohs scale hardness3
LusterVitreous
DiaphaneityTransparent
Specific gravity2.07
Density2.07 (measured)
Optical propertiesBiaxial (+), colorless (transmitted light)
2V angle60° (measured), 48° (calculated)
SolubilitySoluble in water
Other characteristicsSlightly astringent and sweet taste
References[2][3][4]

Tamarugite (NaAl(SO4)2·6H2O) is a colorless monoclinic sulfate mineral.[2][3]

Deposits containing tamarugite are geographically dispersed with occurrences of the mineral on all seven continents (Antarctica, Oceania, North America, South America, Europe, Asia, Africa).[3] The mineral's name comes from the Tamarugal Pampa locality in Chile.[2][3] It is also known as lapparentite.

See also

[edit]

References

[edit]
  1. Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. 1 2 3 Webmineral.com - Tamarugite
  3. 1 2 3 4 Mindat.org - Tamarugite
  4. Mereiter, Kurt (15 October 2013). "Redetermination of tamarugite, NaAl(SO 4 ) 2 ·6H 2 O". Acta Crystallographica Section E. 69 (10): i63–i64. doi:10.1107/S1600536813025154. PMC 3790334. PMID 24098156.

Bibliography

[edit]
  • Palache, P.; Berman H.; Frondel, C. (1960). "Dana's System of Mineralogy, Volume II: Halides, Nitrates, Borates, Carbonates, Sulfates, Phosphates, Arsenates, Tungstates, Molybdates, Etc. (Seventh Edition)" John Wiley and Sons, Inc., New York, pp. 466–468.