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: a431f38abf66cf3a

Jump to content

Aikinite

From Wikipedia, the free encyclopedia
Aikinite
General
CategorySulfide mineral
FormulaPb Cu Bi S3
IMA symbolAik[1]
Strunz classification2.HB.05a
Dana classification3.4.5.1
Crystal systemOrthorhombic
Crystal classDipyramidal (mmm)
H-M symbol: (2/m 2/m 2/m)
Space groupPnma
Unit cella = 11.297, b = 11.654
c = 4.061 [Å], Z = 4
Identification
Formula mass575.92 g/mol
ColorLead gray, grayish black, reddish brown
Crystal habitAcicular, massive
Cleavage{010} indistinct
Mohs scale hardness2–2.5
LusterMetallic
StreakGrayish black
DiaphaneityOpaque
Specific gravity6.1–6.8, Average = 6.44
Other characteristicsNot radioactive
References[2][3]

Aikinite is a sulfide mineral of lead, copper and bismuth with formula Pb Cu Bi S3. It forms black to grey or reddish brown acicular orthorhombic crystals with a Mohs hardness of 2 to 2.5 and a specific gravity of 6.1 to 6.8. It was originally found in 1843 in the Beryozovskoye deposit, Ural Mountains. It is named after Arthur Aikin (1773–1854), an English geologist.

It has been found in Western Tasmania, in mines located near Dundas, Tasmania.

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. ↑ Aikinite. Webmineral
  3. ↑ Aikinite. Mindat.org