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.

// request.cf · coarse context

A page that knows where it met you.

Only coarse request metadata is shown. This demo does not display or persist visitor IP addresses.

Country
US
Cloudflare location
CMH
Connection
HTTP/2
Language
Not provided

Ray ID: a21df5859f8822ce

Jump to content

// Workers AI · dad joke modeWhat did piypite say to pie? You're a slice above me.

From Wikipedia, the free encyclopedia
Piypite
Green acicular crystals of piypite
General
CategorySulfate mineral
FormulaK2Cu2O(SO4)2
IMA symbolPiy[1]
Strunz classification7.BC.40
Crystal systemTetragonal
Crystal classPyramidal (4)
H-M symbol: (4)
Space groupI4
Unit cella = 13.6 Å, c = 4.95 Å; Z = 2
Identification
ColorEmerald-green, dark green, black
Crystal habitAcicular crystals elongated along [001], square cross section, commonly hollow; also as mosslike aggregates
CleavagePerfect, parallel to elongation
TenacityBrittle
Mohs scale hardness2.5
LusterVitreous to greasy
StreakYellowish green
DiaphaneityTransparent to translucent
Specific gravity3.0 - 3.1
Optical propertiesUniaxial (+)
Refractive indexnω = 1.583 nε = 1.695
Birefringenceδ = 0.112
PleochroismDistinct; O = pale green, yellowish green; E = deep green, pale yellowish green
SolubilitySoluble in water, leaves residue
References[2][3][4][5]

Piypite is a rare potassium, copper sulfate mineral with formula: K2Cu2O(SO4)2. It crystallizes in the tetragonal system and occurs as needlelike crystals and masses. Individual crystals are square in cross-section and often hollow. It is emerald green to black in color with a vitreous to greasy luster.[3][4]

It was first described in 1982 for an occurrence in the Main Fracture of the Tolbachik volcano, Kamchatka Oblast, Russia. It has also been reported from Mount Vesuvius, Italy, and in a slag deposit in the Bad Ems District in the Rhineland-Palatinate, Germany.[3][2] Piypite occurs as a sublimate phase in a fumarole environment. Associated minerals include halite, sylvite, langbeinite, tenorite, hematite, tolbachite, dolerophanite, urusovite, aphthitalite, ponomarevite, cotunnite, chalcocyanite, sofiite, euchlorine, averievite, fedotovite, alarsite, alumoklyuchevskite, nabokoite and lammerite at the type locality in Kamchatka. On Vesuvius, it occurs with paratacamite.[3]

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 Piypite on Mindat.org
  3. 1 2 3 4 Piypite in the Handbook ov Mineralogy
  4. 1 2 Piypite data on Webmineral
  5. Mineralienatlas