The Rare Earths: Their Occurrence, Chemistry, and TechnologyLevy, Stanley Isaac
Science
The Rare Earths: Their Occurrence, Chemistry, and Technology
Levy, Stanley Isaac
Rare earths
In composition identical with Johnstrupite (_q.v._).
Isomeric with Johnstrupite (_q.v._).
G = 2·93-3·03. H = 4. Reddish brown; translucent.
Langesund Fiord, Norway.
_Muromontite._
A variety of Allanite (_q.v._), rich in yttria earths and Be, but poor
in Al and ceria earths. Cer = 9·1; Yttr = 37·1%.
_See_ Allanite.
G = 4·263. H = 7. Black to greenish black.
Mauersberg, Erzgebirge, Saxony.
~Naegite.~
A silicate of Zr, ZrSiO₄, with E, Th, U, Cb, etc. ZrO₂ = 55·2; Yttr =
9·12; ThO₂ = 5·01%.
Tetragonal; in globular aggregates.
Gr = 4·091. H = 7¹⁄₂. Dark green or brown; dull.
Gravel-tin of Japan.
Narsarsukite.
Na₆FeTi₂Si₁₂O₃₂F. TiO₂ = 14%.
Tetragonal. Habit tabular.
Gr = 2·75. H = 7-7¹⁄₂. Yellow to reddish-brown; pleochroic.
Plain of Narsarsuk, Greenland.
Neptunite.
(K,Na)₂(Fe,Mg,Ca,)₂(Ti,Si)₄O₁₂. TiO₂ = 18%.
Monoclinic. Habit prismatic.
G = 3·23. H = 5¹⁄₂. Black, red in flakes. Translucent to opaque.
Narsarsuk, Greenland.
_Nivenite._
A variety of Cleveite (_q.v._), readily soluble in dilute acids.
Cubic; crystallisation indistinct.
G = 8·01. H = 5¹⁄₂. Velvet black; opaque.
Bluffton, Llano Co., Texas.
_Nohlite._
A variety of Samarskite (_q.v._) containing water (→ 4·6%).
Massive, without cleavage.
G = 5·04. H = 4¹⁄₂-5. Brownish black; opaque.
Nohl, near Kongelf, Sweden.
_Oerstedite._
A variety of Zircon (_q.v._), poor in SiO₂. ZrO₂ = 69%.
Tetragonal; angles exactly those of Zircon.
G = 3·629. H = 5¹⁄₂. Reddish-brown; adamantine lustre.
Arendal, Norway.
~Orangite.~
ThSiO₄, usually with Fe, Ca, H₂O in traces. ThO₂ = 71·2-73·8%.
Tetragonal. Habit prismatic.
G = 5·19-5·40. H = 4¹⁄₂-5. Orange yellow; lustrous.
_See under_ Thorite.
~Parisite.~
E₂CaF₂(CO₃)₃. Cer = 50·8-64·4; Yttr = 0-2·5%.
Hexagonal. Habit pyramidal.
G = 4·36. H = 4¹⁄₂. Yellow to red; transparent.
Muso Valley, Columbia; Montana, U.S.A.; Greenland; Norway; the Urals,
etc.
Perovskite.
CaTiO₃, with traces of Fe´´. TiO₂ = 58·9%.
Pseudo-cubic? Optically biaxial.
G = 4·017. H = 5¹⁄₂. Yellow; transparent to opaque.
The Urals; Switzerland; Tyrol, etc.
_Pilbarite._
PbO,UO₃,ThO₂,2SiO₂,2H₂0 + 2aq. ThO₂ = 31·3%. Cer and Yttr--traces.
Amorphous.
G = 4·4-4·7. H = 2¹⁄₂-3. Bright yellow; opaque.
Pilbara goldfields, West Australia.
_Pitchblende._
A mixture of oxides, chiefly UO₂ and UO₃, but without E₂O₃ or ThO₂.
Amorphous.
G = 5-6·5. H = 3-4. Black; resinous lustre.
Bohemia; Cornwall; Carolina; Norway, etc.
_Plumboniobite._
A variety of Samarskite (_q.v._) containing Pb; R´´₂Cb₂O₇,
R´´´₄(Cb₂O₇)₃, where R´´ = Fe, Pb, Ca, UO, R´´´ = E, Al. Yttr = 14·3%.
Massive, isotropic.
G = 4·80-4·81. H = 5-5¹⁄₂. Dark brown to black.
Morogoro, Uluguru Mountains, German E. Africa.
~Polycrase.~
A titano-columbate of E and U; Yttr = 19·5-32·5; TiO₂ = 25-33%. Cer
and ThO₂ traces. Isomorphous with Euxenite.
Public-domain text, read in full here on John Shaqi.
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