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.
It is evident that an Empire which extended over more than twenty
degrees of latitude, touching on the one hand the tropic of Cancer,
while it reached upon the other to the parallel of Astrakan, and which
at the same time varied in elevation, from 20,000 feet above to 1300
below the sea level, must have comprised within it great differences of
climate, and have boasted an immense variety of productions. No general
description can be applicable to such a stretch of territory; and it
will therefore be necessary to speak of the various parts of the
Empire successively in order to convey to the reader a true idea of
the climatic influences to which it was subject, and the animals,
vegetables, and minerals which it produced.
Commencing with Persia Proper, the original seat and home of the race
with whose history we are specially concerned at present, we may observe
that it was regarded by the ancients as possessing three distinct
climates--one along the shore, dry and scorchingly hot; another in the
mountain region beyond, temperate and delightful; and a third in the
tract further inland, which was thought to be disagreeably cold and
wintry. Moderns, on the contrary, find two climates only in Fars--one
that of the Desbistan or “low country,” extremely hot and dry,
with frequent scorching and oppressive winds from the south and the
south-east; the other, that of the highlands, which is cold in winter,
but in summer pleasant and enjoyable. In the Deshistan snow never falls,
and there is but little rain; heavy dews, however, occur at night, so
that the mornings are often fresh and cool; but the middle of the day
is almost always hot, and from March to November the temperature at noon
ranges from 90° to 100° of Fahrenheit. Occasionally it reaches 125°, and
is then fearfully oppressive. Fierce gusts laden with sand sweep over
the plain, causing vegetation to droop or disappear, and the animal
world to hide itself. Man with difficulty retains life at these trying
times, feeling a languor and a depression of spirits which are barely
supportable.10 All who can do so quit the plains and betake themselves
to the upland region till the great heats are past, and the advance of
autumn brings at any rate cool nights and mornings. The climate of the
uplands is severe in winter. Much snow falls, and the thermometer often
marks from ten to fifteen degrees of frost. From time to time there are
furious gales, and, as the spring advances, a good deal of wet falls;
but the summer and autumn are almost rainless. The heat towards midday
is often considerable, but it is tempered by cool winds, and even at the
worst is not relaxing. The variations of temperature are great in the
twenty-four hours, and the climate is, so far, trying; but, on the
whole, it seems to be neither disagreeable nor unhealthy.
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