The story of the universe. Volume 2 (of 4) : $b The earth : land and sea
History
The story of the universe. Volume 2 (of 4) : $b The earth : land and sea
Astronomy; Earth (Planet); Natural history
If we examine a chart of the world in the light which has been thrown
upon this question by all the reliable soundings obtained up to the
present, it will be found that continents and islands which we have
been in the habit of considering as separated from each other by
wide seas and deep straits virtually form part of the same area of
elevation; and, in a similar manner, that certain oceans and seas,
which we are accustomed to distinguish by separate names, form part
of the same area of depression. It will also appear that, with the
exception of the islands scattered over the face of the ocean and of
the Antarctic region, all the dry land at present existing may be
reduced to one large area of elevation gravitating to the North Pole,
as the common centre of the principal land masses; similarly, if we
except the Arctic region and other inland basins, all the oceans and
seas compose a single vast area of depression, with the South Pole
for common centre of the larger accumulations of water on this globe.
The Arctic region forms a distinct area of depression placed in the
centre of the great area of elevation, and the Antarctic region,
according to the evidence we at present possess, is an area of
elevation, surrounded on all sides by the above-described great area
of depression. The numerous small islands that crop up in the middle
of the oceanic basins are generally found associated in groups, and
they belong to areas of elevation at the present time submerged, that
is to say, in the condition in which we know the dry land to have
been at an epoch more or less remote in the history of our planet. In
support of the above generalization, we may point to the following
facts as established by recent soundings. The 100-fathom line, as is
well known, joins the whole of the British Islands, including the
Hebrides, Orkneys, and Shetland Islands, to the continent of Europe.
It forms a broad band connecting the Asiatic and American continents
across Behring Strait. It unites Australia, Papua, and Tasmania in
a single area of elevation, which, together with the intervening
archipelago of Java, Sumatra, Borneo, Celebes, the Moluccas, and the
Philippines, may be looked upon as a prolongation of the continent of
Asia. It joins Ceylon to Hindostan and the Falkland Islands to the
South American continent. The 500-fathom line connects North America,
Greenland, Iceland, the Faroe Islands, and the continent of Europe,
the only unexplored space being Denmark Strait, between Iceland
and Greenland, where the soundings may exceed the above depth. The
1,000-fathom line unites New Zealand with Australia, Madagascar with
Africa, and nearly exhausts the depth of the more or less landlocked
seas which lie between Australia and Asia, Africa and Europe, South
and North America, and of the seas situated within the Arctic and
Antarctic Circles. The Cape de Verde Islands and the Canaries belong
to Africa, Madeira to Europe, and less than 500 fathoms divide Norway
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