Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of GeologyLyell, Charles, Sir
Science
Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of Geology
Lyell, Charles, Sir
Geology
But let the configuration of the surface be still farther varied, and
let some large district within or near the tropics, such as Brazil, with
its plains and hills of moderate height, be converted into sea, while
lands of equal elevation and extent rise up in the arctic circle. From
this change there would, in the first place, result a sensible
diminution of temperature near the tropic, for the Brazilian soil would
no longer be heated by the sun; so that the atmosphere would be less
warm, as also the neighboring Atlantic. On the other hand, the whole of
Europe, Northern Asia, and North America, would be chilled by the
enormous quantity of ice and snow, thus generated on the new arctic
continent. If, as we have already seen, there are now some points in the
southern hemisphere where snow is perpetual down to the level of the
sea, in latitudes as low as central England, such might assuredly be the
case throughout a great part of Europe, under the change of
circumstances above supposed: and if at present the extreme range of
drifted icebergs is the Azores, they might easily reach the equator
after the assumed alteration. But to pursue the subject still farther,
let the Himalaya mountains, with the whole of Hindostan, sink down, and
their place be occupied by the Indian Ocean, while an equal extent of
territory and mountains, of the same vast height, rise up between North
Greenland and the Orkney Islands. It seems difficult to exaggerate the
amount to which the climate of the northern hemisphere would then be
cooled.[186]
Public-domain text, read in full here on John Shaqi.
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