The evolution of climateBrooks, C. E. P. (Charles Ernest Pelham)
Science
The evolution of climate
Brooks, C. E. P. (Charles Ernest Pelham)
Climatology; Paleoclimatology
An alternative form put forward by P. Kreichgauer, and recently
brought up again by Wegener, explains the apparent variations in
the position of the pole, not through a motion of the earth’s
axis, but by the assumption that the firm crust has moved over the
earth’s core so that the axis, remaining firm in its position,
passes through different points of the earth’s crust. The cause of
these movements is the centrifugal force of the great masses of the
continents, which are distributed symmetrically about the earth.
Imagine a single large continent resting on a sub-fluid magma in
temperate latitudes. Centrifugal force acting on this continent
tends to drive it towards the equator. There is thus a tendency for
the latitude of Europe to decrease. Similar forces acting through
geological ages have caused the poles and equator to wander at large
over the earth’s surface, and also caused the continents to shift
their positions relatively to one another. According to Wegener, in
the Oligocene there was only a single enormous continent, America
being united to Europe and Africa on the one hand, and through
Antarctica to Australia on the other; while the Deccan stretched
south-westwards nearly to Africa. The poles were in Alaska and north
of the Falkland Islands. The treatment in Kreichgauer’s original book
is speculative and at times fanciful; Wegener’s treatise appears
to demand more respectful attention, but is open to some vital
objections. In the first place, theories of this class demand that
the glaciation occurred in different regions at widely different
times, whereas we shall see in the following pages that the evidence
points very strongly to a double glaciation during the Quaternary
occurring simultaneously over the whole earth. This objection, which
was fatal to Croll’s theory in its original form, is equally fatal
to theories of pole-wandering as an explanation of the Quaternary
Ice Age. Secondly, we know that the last phase of this glaciation,
known as the Wisconsin stage in America and the Wurmian in Europe,
was highly developed only 20,000 years ago, and probably reached its
maximum not more than 30,000 years ago. In the last 5000 years there
has been no appreciable change of latitude, at least in Eurasia; and
it seems impossible for the extensive alterations required in the
geography of the world by Wegener’s theory to have taken place in so
short a time.
Public-domain text, read in full here on John Shaqi.
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