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TAKEN all in all, the countries included with in the Babylonian Empire were dry and hot.

On the south the desert was in close proximity. The seas which washed the borders of the

dominions of Nebuchadnezzar were small, and their influence was little felt at a distance

from the shore. Nor did the mountain ranges included within the Empire reach to such

length and rise to such height as to insure large quantities of rain or diffuse

everlasting freshness. The country was included between the thirtieth and thirty-seventh

parallels of latitude, and was through the larger part of its extent level and sandy.

From all of these circumstances heat predominated. The summers were long and scorching;

the winters, brief and mild. Of course, the high temperatures of Chaldaea, of Idumaea and

Palmyrene were more excessive in degree than in Mesopotamia and the northern provinces. In

all those parts approximate to the Persian Gulf, even in the hilly regions of Susiana, the

heat of midsummer is fearful. Frequently the thermometer at midday reaches 1.07 of

Fahrenheit, and even in the underground apartments, 'which the people construct to protect

themselves, the temperature hardly falls below 100. At night the heat is assuaged, and

the people find rest on the roofs of their houses. In all the low countries and southern

districts winter brings no snow. In December the rainy season sets in, and continues until

March. Sometimes the clouds pour down abundantly, and at intervals there are violent

storms of hail. Such is the general character of the eastern parts of what was the

Babylonian Empire.

In the western provinces, next to the Mediterranean, there was a moister and cooler

climate. In the mountainous districts of Libanus and Antilibanus the winter is

sufficiently rigorous. In the valleys, however, the climate is more mild than in the

corresponding districts of Europe. In some parts, indeed, as in Palestine and along the

Phoenician coast, the winters are scarcely more severe than in Babylonia proper. At the

Dead Sea the thermometer never falls to the freezing point of water, and in the summer

season the heats are intense and oppressive. In general, the temperature of Syria is about

as here described, but in the higher regions tile air has a freer movement, and the

effects of the heat are thereby assuaged.

The one great climatic drawback, however, in the countries once ruled by (he kings of

Babylon, is the fierce 'Sirocco, or hot wind of the desert. This burning blast is always

blown from the heated sands of Arabia. It is, the terror alike of man and beast. Mixed

with a cloud of fine hot sand the blast sweeps Up over the Syrian or Babylonian plains and

blisters what living thing soever it Smites. The sky grows lurid and the air is darkened.

The animals and birds fly to their covert, and man seeks a shelter for protection.

It is not likely that any great changes have occurred in the climatic conditions of the

Babylonian dominions during the twenty-four hundred years that have elapsed since the days

of the great Empire. Perhaps the soil in many parts has suffered some deterioration, but

the same products are undoubtedly yielded to-day as when they were gathered by the

husbandmen for Nebuchadnezzar's army. In one respect the country has suffered much. Many

regions have been stripped of their forests, and by this fatal procedure the natural

tendencies to drought have been aggravated. 'Especially is this true In Syria, the climate

of which has certainly under- gone some change from the denudation of the woodlands; but

the essential identity of products, ancient and modern, precludes