Outlines of the Earth's History: A Popular Study in PhysiographyShaler, Nathaniel Southgate
History
Outlines of the Earth's History: A Popular Study in Physiography
Shaler, Nathaniel Southgate
Physical geography
Flowing by the northwesterly coast of South America, the northern
share of the tropical current, being pressed in against the land by
the trade winds, is narrowed, and therefore acquires at once a swifter
flow, the increased speed being due to conditions like those which add
to the velocity of the water flowing through a hose when it comes to
the constriction of the nozzle. Attaining the line of the southeastern
or Lesser Antilles, often known as the Windward Islands, a part of
this current slips through the interspaces between these isles and
enters the Gulf of Mexico. Another portion, failing to find sufficient
room through these passages, skirts the Antilles on their eastern and
northern sides, passes by and among the Bahama Islands, there to
rejoin the part of the stream which entered the Caribbean. This
Caribbean portion of the tide spreads widely in that broad sea, is
constricted again between Cuba and Yucatan, again expands in the Gulf
of Mexico, and is finally poured forth through the Straits of Florida
as a stream having the width of forty or fifty miles, a depth of a
thousand feet or more, and a speed of from three to five miles an
hour, exceeding in its rate of flow the average of the greatest
rivers, and conveying more water than do all the land streams of the
earth. In this part of its course the deep and swift stream from the
Gulf of Mexico, afterward to be named the Gulf Stream, receives the
contribution of slower moving and shallower currents which skirted the
Antilles on their eastern verge. The conjoined waters then move
northward, veering toward the east, at first as a swift river of the
sea having a width of less than a hundred miles and of great depth;
with each step toward the pole this stream widens, diminishing
proportionately in depth; the speed of its current decreases as the
original impetus is lost, and the baffling winds set its surface
waters to and fro in an irregular way. Where it passes Cape Hatteras
it has already lost a large share of its momentum and much of its
heat, and is greatly widened.
Public-domain text, read in full here on John Shaqi.
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