Eclectic Magazine of Foreign Literature, Science, and Art, May 1885Various
History
Eclectic Magazine of Foreign Literature, Science, and Art, May 1885
Various
American literature -- Periodicals; Literature -- Periodicals
on this chronological question and condescended to give us a numerical
determination. And here is how Dr. Croll gets at it.
Every now and again, geological evidence goes to show us, a long cold
spell occurs in a northern or southern hemisphere. During these long
cold spells the ice cap at the poles increases largely, till it spreads
over a great part of what are now the temperate regions of the globe,
and makes ice a mere drug in the market as far south as Covent Garden
or the Halles at Paris. During the greatest extension of this ice
sheet in the last glacial epoch, in fact, all England except a small
south-western corner (about Torquay and Bournemouth) was completely
covered by one enormous mass of glaciers, as is still the case with
almost the whole of Greenland. The ice sheet, grinding slowly over the
hills and rocks, smoothed and polished and striated their surfaces
in many places till they resembled the _roches moutonnées_ similarly
ground down in our own day by the moving ice rivers of Chamouni and
Grindelwald. Now, since these great glaciations have occurred at
various intervals in the world’s past history, they must depend upon
some frequently recurring cause. Such a cause, therefore, Dr. Croll
began ingeniously to hunt about for.
He found it at last in the eccentricity of the earth’s orbit. This
world of ours, though usually steady enough in its movements, is at
times decidedly eccentric. Not that I mean to impute to our old and
exceedingly respectable planet any occasional aberrations of intellect,
or still less of morals (such as might be expected from Mars and
Venus); the word is here to be accepted strictly in its scientific or
Pickwickian sense as implying merely an irregularity of movement, a
slight wobbling out of the established path, a deviation from exact
circularity. Owing to a combination of astronomical revolutions, the
precession of the equinoxes and the motion of the aphelion (I am not
going to explain them here; the names alone will be quite sufficient
for most people; they will take the rest on trust)—owing to the
combination of these profoundly interesting causes, I say, there occur
certain periods in the world’s life when for a very long time together
(10,500 years, to be quite precise) the northern hemisphere is warmer
than the southern, or _vice versa_. Now Dr. Croll has calculated that
about 250,000 years ago this eccentricity of the earth’s orbit was
at its highest, so that a cycle of recurring cold and warm epochs in
either hemisphere alternately then set in; and such cold spells it
was that produced the Great Ice Age in Northern Europe. They went on
till about 80,000 years ago, when they stopped short for the present,
leaving the climate of Britain and the neighboring continent with its
existing inconvenient Laodicean temperature. And, as there are good
reasons for believing that my old master and his contemporaries lived
just before the greatest cold of the Glacial Epoch, and that his
Public-domain text, read in full here on John Shaqi.
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