The Economic Aspect of GeologyLeith, C. K. (Charles Kenneth)
Science
The Economic Aspect of Geology
Leith, C. K. (Charles Kenneth)
Geology, Economic
Throughout the history of the iron and steel business there has been a
marked tendency for the iron ore to move to regions of coal production
rather than for the coal to move to the iron ore regions. The coal or
energy factor seems ultimately to control. This is due in considerable
part to the fact that coal furnishes the basis of a great variety of
industries for which iron ore is only one of the feeders, and which are
so interrelated that it is not always easy to move the iron and steel
industry to a spot near the sources of iron ore where iron and steel
alone could be produced.
In regard to iron ore supplies of proper grade and quantity, the United
States is more nearly self-sufficing than any of its competitors. It
imports minor amounts of ore from Cuba and Canada, and even from Chile
and Sweden, to border points, in the main merely because these imported
ores can compete on a price basis with the domestic ores. The entire
exclusion of these ores, however, would make comparatively little
difference in the total volume of our iron and steel industry; though it
would probably make some difference in distribution, to the disadvantage
of plants along the coast. There is only one kind of iron ore in which
the United States has anything approaching deficiency, and that is ore
extremely low in phosphorus, adapted to making the so-called
low-phosphorus pig which is needed for certain special steels. Ordnance
requirements during the war put a premium on these steels. While some of
these extremely low-phosphorus ores are mined in the United States,
additional quantities have been required from Spain and Canada and to a
lesser extent from North Africa and Sweden. Also the Spanish pyrite,
imported ordinarily for its sulphur content, on roasting leaves a
residue of iron oxide extremely low in phosphorus which is similarly
used. The elimination of pyrite imports from Spain during the war,
therefore, was a considerable contributing factor to the stringency in
low-phosphorus iron ores. War experience showed that the United States
was dependent on foreign sources for 40 per cent or upwards of its needs
in this regard. Certain developments in progress, notably the project
for concentration of siliceous eastern Mesabi Range ores, make it likely
that future domestic production will more nearly be able to meet the
requirements.
The equivalent of 15 per cent of the iron ore mined in the United States
is exported as ore to Canadian ports on the Great Lakes and in the form
of crude iron and steel products to many parts of the world. England and
Germany are almost the sole competitors in the export trade.
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