The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
As in the former case, we need not confine ourselves to any particular
locality in drawing this conclusion. The arguments apply not only to the
rocks underneath Leipzig, but to the rocks over every part of the globe,
whether on continents or islands, or even if forming the base of an
ocean. No one denies that the law of increase in temperature with the
depth must submit to some variation in accordance with local
circumstances. In essential features it may, however, be conceded that
the law is the same over all the earth. If we take 52° to be the
temperature of the level 100 feet down, which limits the seasonal
variations, and if we add that at two miles further down the temperature
is somewhere about 160° more, we come to the conclusion that at a depth
of a little over two miles the temperature of the rocks forming the
earth’s crust is about 212° Fahrenheit. Thus we draw the important
inference that if, the oceans having been removed, we were then to
remove from the earth’s surface a rind two miles thick—a thickness
which, it is to be observed, is only the two-thousandth part of the
earth’s radius—we should transform the earth into a globe which, while
it still retained appreciably the same size, would have such a
temperature that even the coolest spot would be as hot as boiling water.
This is indeed a remarkable result.
And now that we have gone so far, it is impossible for us to resist
making a further attempt to determine what the temperature of the
earth’s crust must be if we could send a thermometer still lower. A hole
one mile deep we have seen; I do not think we can hope to see a hole two
miles deep, but still it may not be absolutely impracticable; but a hole
of three or more miles deep we may safely regard as transcending present
possibilities in engineering enterprise. Are we therefore to be deprived
of all information as to the condition of our earth at depths exceeding
those already considered? Fortunately we can learn something. We are
assisted by certain laws of heat, and, though the evidence on which we
believe those laws is necessarily limited to the experience of Nature as
it comes within our observation, yet it is impossible to refuse assent
to the belief that the same laws will regulate the transmission of heat
in the crust of the earth two miles, three miles, or many miles beneath
our feet.
Public-domain text, read in full here on John Shaqi.
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