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
Certain high-grade low-phosphorus iron ores which are not present in
the United States in sufficient quantity to supply domestic needs have
been imported in past years from Spain, North Africa, and to a small
extent from Sweden. During the war, when the shortage of shipping
facilities necessitated combing this country for supplies of high-grade
low-phosphorus ores, it was shown that the United States is more or
less dependent upon foreign sources for such ores.
There are a number of mines in the United States, such as the Lyon
Mountain mine in New York, and the Cranberry mine in North Carolina,
which produce limited amounts of high-grade low-phosphorus ore.
Several mines on the Menominee Range, Michigan, produce a very
siliceous low-phosphorus ore that can be used to supplement in part
the high-grade ores. A considerable quantity of low-phosphorus pyrite
residue from sulphuric acid and fertilizer plants is also used for
making low-phosphorus iron. Much of the pyrite yielding this residue is
imported from Spain, some of it is of domestic origin, and some of it
comes from Canada. Altogether, the United States supplies about 60 per
cent. of the material required for the manufacture of its normal output
of low-phosphorus pig iron.
Certain developments in progress make it probable that a greater
percentage of ore used for this purpose can be supplied from domestic
mines. The principal enterprise is one that plans to concentrate the
siliceous magnetite ore of the eastern Mesabi Range. Experiments have
yielded a high-grade product and work on a commercial scale is planned.
The reserves of the ordinary grades of iron ore in the United States
are large, and no shortage of such ore is anticipated for many years.
They are easily capable of taking care of a considerably increased
consumption. The largest reserves are in the Lake Superior district and
in the southeastern states, but large untouched reserves occur in the
western states as well. The iron ores in the Pacific Coast region have
remained undeveloped from the lack of sufficient demand for pig iron
and crude forms of iron and steel on the Pacific Coast. Undoubtedly
this demand will increase in the future, and iron and steel industries
will be established there.
The reserves of ore in the Lake Superior district are large. The grade
of ore mined, however, has been gradually getting lower, and it is
possible that before many years Lake iron ores averaging considerably
below 50 per cent. will have to be utilized. At present the average
grade of the ores mined in the Lake Superior district is about 51 per
cent.
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