Buffon's Natural History, Volume 02 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Mineral, &c. &cBuffon, Georges Louis Leclerc, comte de
History
Buffon's Natural History, Volume 02 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Mineral, &c. &c
Buffon, Georges Louis Leclerc, comte de
Natural history
The ocean surrounds the earth on all sides, and penetrates into the
interior parts of different countries, often by large openings, and
frequently by small straits; it forms mediterranean seas, some of which
participate of its motions of flux and reflux, and others seem to have
nothing in common with it except the continuity of water. We shall
follow the ocean through all its extent and windings, enumerating at
the same time all the mediterranean seas, and endeavour to distinguish
them from those which should be only called bays, or gulphs, and lakes.
The sea which washes the western coasts of France forms a gulph between
Spain and Britain; this gulph, which mariners call the Bay of Biscay,
is very open, and the point which projects farthest inland is between
Bayonne and St. Sebastian; another great projection is between Rochelle
and Rochefort: this gulph begins at Cape Ortegal, and ends at Brest,
where a strait commences between the south point of Britain and Cape
Lizard. This strait, which at first is very large, forms a small gulph
in Normandy, the most projecting point of which is at Auranche; it
continues pretty broad until it comes to the channel at the foot of
Calais, where it is very narrow; afterwards it grows broader on a
sudden, and ends between the Texel and the coast of England at Norwich;
at the Texel it forms a small mediterranean sea, called _Zuyder-zee_,
and many other great canals, which are not very deep.
After that the ocean forms a great gulph called the German Ocean; it
begins at the northern point of Scotland, runs along the eastern
coast of Scotland and England as far as Norwich, from thence to the
Texel, along the coasts of Holland and Germany, Jutland, Norway, and
above Bergen. This gulph might be taken for a mediterranean sea,
because the Orkney islands partly shut up its opening, and seem
to be directed as if they were a continuation of the mountains of
Norway. It forms a large strait, which begins at the southern point
of Norway, and continues very broad to the Island of Zetland, where
it narrows all at once, and forms between the coasts of Sweden, the
islands of Denmark and Jutland, four small straits; after which it
widens to a small gulph, the most projecting point of which is at
Lubec: from thence it continues pretty broad to the southern extremity
of Sweden, when it grows broader and broader, and forms the Baltic
Sea, which is a mediterranean, extending from south to north near 300
leagues, comprehending the gulph of Bothnia, which is in fact only a
continuation of it. This sea has two more gulphs, that of Livonia,
whose most projecting point is near Mittau and Riga, and that of
Finland, which is an arm of the Baltic, extending between Livonia and
Finland to Petersburgh, and communicating with the lake Ladoga, and
even with the lake Onega, which communicates by the river Onega to the
White Sea. All this extent of water, which forms the Baltic Sea, the
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