A Book of the United States: Exhibiting its geography, divisions, constitution, and government ... and presenting a view of the republic generally, and of the individual states; together with a condensed history of the land, from its first discovery to the present time. The biography of about two hundred of the leading men: a description of the principal cities and towns; with statistical tables
History
A Book of the United States: Exhibiting its geography, divisions, constitution, and government ... and presenting a view of the republic generally, and of the individual states; together with a condensed history of the land, from its first discovery to the present time. The biography of about two hundred of the leading men: a description of the principal cities and towns; with statistical tables
United States -- Biography; United States -- Description and travel; United States -- History
The sea exercises an important equalizing influence on the
temperature of the globe. In the tropical regions a large
extent of ocean spreads coolness on every side, and affords a
perpetual succession of refreshing breezes. Islands are always,
comparatively, of more temperate climates than continents, and
those scattered over the expanse of the Pacific may be said to
enjoy almost a perpetual spring. The influence of the winds is
also very important; particularly that of the trade-winds. Blowing
from east to west across the sands of Africa, the latter produce,
on its western coast, a most intense heat, much greater than
is experienced on the eastern. In passing the Atlantic they are
considerably cooled; and though their temperature is again raised
in traversing South America, yet, before reaching the opposite
coast, they meet the tremendous snow-clad Andes, which stop their
progress and diffuse a wide coolness.
Again, the mountain ranges of the earth not only present and
retain on their sides a refreshing coolness, but, by the mighty
rivers to which they give rise, diffuse a great amelioration of
the temperature through extensive regions. They are particularly
of this character, and give rise to the largest rivers in the
torrid and burning zones of the earth. In the temperate climate,
and those approaching to the poles, mountains are of moderate
elevation, are almost always barren, and give rise to few
considerable streams.
It appears probable that the climates of European countries were
more severe in ancient times than they are at present. Cæsar says
that the vine could not be cultivated in Gaul on account of its
winter cold. The reindeer, now found only in the zone of Lapland,
was then an inhabitant of the Pyrenees. The Tiber was frequently
frozen over, and the ground about Rome covered with snow for
several weeks together, which very rarely happens in our time.
The Rhine and the Danube, in the time of Augustus, was generally
frozen over for several months of winter. The barbarians who
overran the Roman empire a few centuries afterwards, transported
their armies and wagons across the ice of these rivers. Though the
fact is well established, the causes of this change of climate do
not seem to be satisfactorily explained.
CHAPTER XV.――MINERALS.
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