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George-ericksenite is a mineral with the chemical formula Na6CaMg(IO3)6(CrO4)2(H2O)12. It is vitreous, pale yellow to bright lemon yellow, brittle, and features a prismatic to acicular crystal habit along [001] and somewhat flattened crystal habit on {110}. It was first encountered in 1984 at the Pinch Mineralogical Museum. One specimen of dietzeite from Oficina Chacabuco, Chile had bright lemon-yellow micronodules on it. These crystals produced an X-ray powder diffraction pattern that did not match any XRD data listed for inorganic compounds. The X-ray diffraction pattern and powder mount were set aside until 1994. By then, the entire mineral collection from the Pinch Mineralogical Museum had been purchased by the Canadian Museum of Nature. The specimen was then retrieved and studied furt

AttributesValues
rdf:type
rdfs:label
  • Georgeericksenita (ca)
  • George-ericksenite (en)
  • George-ericksenita (eu)
  • George-ericksenite (it)
rdfs:comment
  • La georgeericksenita és un mineral de la classe dels òxids. Rep el seu nom en honor de George E. Ericksen (1920-1996), qui va estudiar els dipòsits de nitrats pel Servei Geològic dels Estats Units. Va ser descoberta a l'Oficina Chacabuco ; es tracta de l'únic indret on ha estat trobada aquesta espècie mineral. (ca)
  • George-ericksenita oxido motako minerala da. (eu)
  • La george-ericksenite è un minerale. Il nome è stato modificato da georgeericksenite nel 2008 dall'IMA. (it)
  • George-ericksenite is a mineral with the chemical formula Na6CaMg(IO3)6(CrO4)2(H2O)12. It is vitreous, pale yellow to bright lemon yellow, brittle, and features a prismatic to acicular crystal habit along [001] and somewhat flattened crystal habit on {110}. It was first encountered in 1984 at the Pinch Mineralogical Museum. One specimen of dietzeite from Oficina Chacabuco, Chile had bright lemon-yellow micronodules on it. These crystals produced an X-ray powder diffraction pattern that did not match any XRD data listed for inorganic compounds. The X-ray diffraction pattern and powder mount were set aside until 1994. By then, the entire mineral collection from the Pinch Mineralogical Museum had been purchased by the Canadian Museum of Nature. The specimen was then retrieved and studied furt (en)
foaf:name
  • George-ericksenite (en)
name
  • George-ericksenite (en)
dcterms:subject
Wikipage page ID
Wikipage revision ID
Link from a Wikipage to another Wikipage
sameAs
solubility
  • Extreme in cold water (en)
streak
  • Pale yellow (en)
strunz
tenacity
  • Brittle (en)
twinning
  • None observed megascopically nor during single-crystal study (en)
unit cell
  • a = 23.645 Å (en)
  • b = 10.918 Å (en)
  • c = 15.768 Å (en)
  • β = 114.42°; Z=4 (en)
dbp:wikiPageUsesTemplate
category
class
  • Prismatic (en)
color
  • Pale yellow to bright lemon yellow (en)
density
symmetry
  • C2/c (en)
system
has abstract
  • La georgeericksenita és un mineral de la classe dels òxids. Rep el seu nom en honor de George E. Ericksen (1920-1996), qui va estudiar els dipòsits de nitrats pel Servei Geològic dels Estats Units. Va ser descoberta a l'Oficina Chacabuco ; es tracta de l'únic indret on ha estat trobada aquesta espècie mineral. (ca)
  • George-ericksenite is a mineral with the chemical formula Na6CaMg(IO3)6(CrO4)2(H2O)12. It is vitreous, pale yellow to bright lemon yellow, brittle, and features a prismatic to acicular crystal habit along [001] and somewhat flattened crystal habit on {110}. It was first encountered in 1984 at the Pinch Mineralogical Museum. One specimen of dietzeite from Oficina Chacabuco, Chile had bright lemon-yellow micronodules on it. These crystals produced an X-ray powder diffraction pattern that did not match any XRD data listed for inorganic compounds. The X-ray diffraction pattern and powder mount were set aside until 1994. By then, the entire mineral collection from the Pinch Mineralogical Museum had been purchased by the Canadian Museum of Nature. The specimen was then retrieved and studied further. This study was successful and the new mineral george-ericksenite was discovered. The mineral was named for George E. Ericksen who was a research economic geologist with the U.S. Geological Survey for fifty years. The mineral and name have been approved by Commission on New Minerals and Mineral Names (IMA). The specimen, polished thin section, and the actual crystal used for the structure determination are kept in the Display Series of the National Mineral Collection of Canada at the Canadian Museum of Nature, Ottawa, Ontario. (en)
  • George-ericksenita oxido motako minerala da. (eu)
  • La george-ericksenite è un minerale. Il nome è stato modificato da georgeericksenite nel 2008 dall'IMA. (it)
birefringence
  • δ = 0.057 (en)
cleavage
  • None observed (en)
diaphaneity
  • Transparent to translucent (en)
formula
  • Na6CaMg6212 (en)
fracture
  • Unknown (en)
habit
  • Prismatic to acicular along [001] and somewhat flattened on {110} (en)
IMAsymbol
  • Gek (en)
luster
  • Vitreous (en)
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