Political and commercial geology and the world's mineral resources
Science
Political and commercial geology and the world's mineral resources
Geology, Economic; Mines and mineral resources
At Cooglegong, in _Western Australia_, the uranium mineral fergusonite
and to a less extent the uranium mineral euxenite occur in the surface
detrital material of the region. At Wodgina the minerals mackintoshite,
thorogummite and pilbarite, all hydrous silicates of uranium, thorium
and lead, occur in an albite pegmatite dike. No important quantities of
these Western Australia ores have yet been produced.
=India and Africa.=--Radium and uranium minerals have been reported in
_India_ and _German East Africa_, but no important quantities have yet
been produced.
PROSPECT OF FUTURE DISCOVERIES OF RADIUM AND URANIUM ORES
The prospect for increased discoveries of radium and uranium minerals
at the present time seems best in the carnotite regions of Colorado and
Utah. The workable deposits seem to be more or less superficial, and
perhaps no large quantity of ore may be found in any one spot, yet the
great extent of the region in which the formations carrying carnotite
occur, will supply an immense aggregate amount of ore.
Increased discoveries of uraninite, pitchblende and other uranium
minerals in Europe seem possible, even though that continent has
already been well explored for them. Moreover, new discoveries of
different radium and uranium minerals may very likely be made in
still other parts of the United States than those mentioned, and in
less explored parts of the world, especially certain regions of South
America, Australia, Asia and Africa. Many of these minerals, especially
pitchblende, have no very distinctive features when first observed, and
might readily be overlooked many times before their true nature was
discovered. Hence the possibilities of future discoveries.
CHAPTER XII
ZIRCONIUM
BY H. C. MORRIS
USES OF ZIRCONIUM
As early as 1830 an attempt was made to use zirconia buttons, heated
to incandescence, for lighting the streets of Paris. In 1885 an
incandescent gas mantle of zirconium oxide was patented, but was
replaced in a few years by thorium. About 1900 zirconia was used in the
Nernst glower, and it has also been used in place of lime and magnesia
as the incandescing material in the Drummond light. It is also said to
be used in the Bleriot light, and its use in flares has been suggested.
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