Geology: The Science of the Earth's Crust — John Stuart Mill — John Shaqi
Geology: The Science of the Earth's Crust
John Stuart Mill · en
The conditions under which successive layers of vegetable matter (later
turned into coal) become embedded in the earth's crust have been
outlined in the chapter on the "Evolution of Plants." The most perfect
conditions for prolific plant growth, and accumulation as great beds
in the earth's crust, were during the Pennsylvanian period of the late
Paleozoic era in many parts of the world, but especially in the United
States, China, Great Britain, and Germany. Most of the world's great
supply of coal comes from rocks of Pennsylvanian Age, while next in
importance are Cretaceous rocks, and some comes from strata of other
ages later than the Pennsylvanian, even as late as the Tertiary.
The United States not only has the greatest known coal fields, but
it also produces far more coal than any other country. In 1918 the
production was 678,000,000 tons, the greatest in our history, or
enough, if loaded into cars of forty tons capacity, to fill a train
which would reach around the earth at the equator about six times!
Equally amazing is the fact that this coal was nearly all consumed by
this one nation! In 1919 the production fell to 544,000,000 tons. Is
there real danger that our supply of coal will soon run out? Hardly so
when we consider, first, the fact that probably not more than 1 per
cent of the readily available coal has thus far been removed, and,
second, the high probability that rate of increase in coal production
for the last twenty years will not continue. In fact, during the last
two or three years the production has fallen off considerably. But even
so, coal, which is our greatest natural resource, and which can never
be replaced, should be scientifically conserved. In the case of the
very restricted anthracite coal fields what might be called a crisis
has already been reached, because a very considerable part of the
available supply has been taken out.
Something like 350,000 square miles of the United States are underlain
with one or more beds of workable coal (not including lignite)--in
some areas five to twenty or more beds one above the other. There are
also about 150,000 square miles of country underlain with the more or
less imperfect coal called lignite. It has been estimated that there
are more than a trillion tons of easily accessible coal, and another
trillion tons accessible with some difficulty in the principal coal
fields of the United States.