The Seven Great Monarchies Of The Ancient Eastern World, Vol 5: Persia: The History, Geography, And Antiquities Of Chaldaea, Assyria, Babylon, Media, Persia, Parthia, And Sassanian or New Persian Empire; With Maps and Illustrations.Rawlinson, George
History
The Seven Great Monarchies Of The Ancient Eastern World, Vol 5: Persia: The History, Geography, And Antiquities Of Chaldaea, Assyria, Babylon, Media, Persia, Parthia, And Sassanian or New Persian Empire; With Maps and Illustrations.
Inside the Zagros and Elburz ranges, bounded on the north and west by
those mountain-lines, on the east by the ranges of Suliman and Hala, and
on the south by the coast-chain which runs from Persia Proper nearly
to the Indus, lies a vast tableland, from 3000 to 5000 feet above the
sea-level, known to modern geographers as the Great Plateau of Iran. Its
shape is an irregular rectangle, or trapezium, extending in its greatest
length, which is from west to east, no less than twenty degrees, or
above 1100 miles, while the breadth from north to south varies from
seven degrees, or 480 miles (which is its measure along the line of
Zagros), to ten degrees, or 690 miles, where it abuts upon the Indus
valley. The area of the tract is probably from 500,000 to 600,000 square
miles.
It is calculated that two thirds of this elevated region are absolutely
and entirely desert. The rivers which flow from the mountains
surrounding it are, with a single exception--that of the Etymandrus or
Helmend--insignificant, and their waters almost always lose themselves,
after a course proportioned to their volume, in the sands of the
interior. Only two, the Helmend and the river of Ghuzni, have even the
strength to form lakes; the others are absorbed by irrigation, or sucked
up by the desert. Occasionally a river, rising within the mountains,
forces its way through the barrier, and so contrives to reach the sea.
This is the case, especially, on the south, where the coast chain is
pierced by a number of streams, some of which have their sources at a
considerable distance inland. On the north the Heri-rud, or River of
Herat, makes its escape in a similar way from the plateau, but only to
be absorbed, after passing through two mountain chains, in the sands of
the Kharesm. Thus by far the greater portion of this region is desert
throughout the year, while, as the summer advances, large tracts, which
in the spring were green, are burnt up--the rivers shrink back towards
their sources--the whole plateau becomes dry and parched--and the
traveller wonders that any portion of it should be inhabited.
Public-domain text, read in full here on John Shaqi.
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