Encyclopaedia Britannica, 11th Edition, "Groups, Theory of" to "Gwyniad": Volume 12, Slice 6Various
Science
Encyclopaedia Britannica, 11th Edition, "Groups, Theory of" to "Gwyniad": Volume 12, Slice 6
Various
Encyclopedias and dictionaries
GUIANA (_Guyana_, _Guayana_[1]), the general name given in its widest
acceptation to the part of South America lying to the north-east from 8
deg. 40' N. to 3 deg. 30' S. and from 50 deg. W. to 68 deg. 30' W. Its
greatest length, from Cabo do Norte to the confluence of the Rio Xie and
Rio Negro, is about 1250 m., its greatest breadth, from Barima Point in
the mouth of the Orinoco to the confluence of the Rio Negro and Amazon,
800 m. Its area is roughly 690,000 sq. m. Comprised in this vast
territory are Venezuelan (formerly Spanish) Guiana, lying on both sides
of the Orinoco and extending S. and S.W. to the Rio Negro and Brazilian
settlements; British Guiana, extending from Venezuela to the left bank
of the Corentyn river; Dutch Guiana (or Surinam), from the Corentyn to
the Maroni river; French Guiana (or Cayenne), from the Maroni to the
Oyapock river;[2] Brazilian (formerly Portuguese) Guiana, extending from
the southern boundaries of French, Dutch, British and part of Venezuelan
Guiana, to the Amazon and the Negro. Of these divisions the first and
last are now included in Venezuela and Brazil respectively; British,
Dutch and French Guiana are described in order below, and are alone
considered here.
[Illiustration: Map of Guiana.]
In their physical geography the three Guianas present certain common
characteristics. In each the principal features are the rivers and their
branch streams. In each colony the northern portion consists of a
fluviomarine deposit extending inland and gradually rising to a height
of 10 to 15 ft. above the sea. This alluvial plain varies in width from
50 m. to 18 m. and is traversed by ridges of sand and shells, roughly
parallel to what is now the coast, indicating the trend of former shore
lines. By the draining and diking of these lands the plantations have
been formed along the coast and up the rivers. These low lands are
attached to a somewhat higher plateau, which towards the coast is
traversed by numerous huge sand-dunes and inland by ranges of hills
rising in places to as much as 2000 ft. The greater part of this belt of
country, in which the auriferous districts principally occur, is covered
with a dense growth of jungle and high forest, but savannahs, growing
only a long wiry grass and poor shrubs, intrude here and there, being in
the S.E. much nearer to the coast than in the N.W. The hinterlands
consist of undulating open savannahs rising into hills and mountains,
some grass-covered, some in dense forest.
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