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The Seven Great Monarchies Of The Ancient Eastern World, Vol 3. (of 7): Media - The History, Geography, And Antiquities Of Chaldaea, - Assyria, Babylon, Media, Persia, Parthia, And Sassanian - or New Persian Empire; With Maps and Illustrations. by George Rawlinson
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foot of the mountain chains, southward to the Indian Ocean, and eastward
to the country of the Afghans. The western mountain-country consists,
as has been already observed, of six or seven parallel ridges, having
a direction nearly from the north-west to the south-east, enclosing
between them, valleys of great fertility, and well watered by a large
number of plentiful and refreshing streams. This district was known to
the ancients as Zagros, while in modern geography it bears the names of
Kurdistan and Luristan. It has always been inhabited by a multitude of
warlike tribes, and has rarely formed for any long period a portion
of any settled monarchy. Full of torrents, of deep ravines, or rocky
summits, abrupt and almost inaccessible; containing but few passes, and
those narrow and easily defensible; secure, moreover, owing to the rigor
of its climate, from hostile invasion during more than half the year;
it has defied all attempts to effect its permanent subjugation, whether
made by Assyrians, Persians, Greeks, Parthians, or Turks, and remains
to this day as independent of the great powers in its neighborhood as it
was when the Assyrian armies first penetrated its recesses. Nature seems
to have constructed it to be a nursery of hardy and vigorous men, a
stumbling-block to conquerors, a thorn in the side of every powerful
empire which arises in this part of the great eastern continent.

The northern mountain country--known to modern geographers as Eiburz--is
a tract of far less importance. It is not composed, like Zagros, of
a number of parallel chains, but consists of a single lofty ridge,
furrowed by ravines and valleys, from which spurs are thrown
out, running in general at right angles to its axis. Its width is
comparatively slight; and instead of giving birth to numerous large
rivers, it forms only a small number of insignificant streams, often dry
in summer, which have short courses, being soon absorbed either by the
Caspian or the Desert. Its most striking feature is the snowy peak of
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