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Updated: June 23, 2025
This track differs from the Chaldaean lowland, by being at once less flat and more elevated. Geologically it is of secondary formation, while Chaldaea proper is tertiary or post-tertiary. It is fairly watered towards the north, but below the Sinjar is only very scantily supplied.
In the central part of Western Assyria, on either side of the Sinjar range, the climate is decidedly cooler than in the region adjoining Babylonia. In summer, though the heat is great, especially from noon to sunset, yet the nights are rarely oppressive, and the mornings enjoyable.
These Ghuzes waged war with Sinjar in 1153, when he was signally defeated, and eventually made prisoner. It is to this battle that Benjamin must have made reference, when he writes that it took place fifteen years ago. See Dr. A. Müller's Islam, also Dr. In the Middle Ages the island of Kish or Kis was an important station on the trade route from India to Europe.
Success attended both these movements; and, before winter set in, the Romans had made themselves masters of the whole of Upper Mesopotamia, and had even pushed southwards as far as Singara, a town on the skirts of the modern Sinjar mountain-range. Mesopotarnia was at once, like Armenia, "reduced into the form of a Roman province."
In all Northern Mesopotamia, between the hills of the Sinjar and the last slopes of Mount Masius, the Assyrians encountered only nomad tribes whom they could drive when they chose into the Syrian desert. Over all that region the remains of artificial mounds have been found which must at one time have been the sites of palaces and cities.
It is broken into innumerable valleys and ravines, abounding with wild animals, and is scantily wooded with dwarf oak. Streams of water abound in it. South of the Sinjar range, the country resumes the same level appearance which characterizes it between the Sinjar and the Mons Masius.
Below this, a vast slightly undulating plain extends from the northern mountains to the Babylonian alluvium, only interrupted about midway by a range of low limestone hills called the Sinjar, which leaving the Tigris near Mosul runs nearly from east to west across central Mesopotamia, and strikes the Euphrates half-way between Rakkeh and Kerkesiyeh, nearly in long. 40°.
The other spur is thrown out near the western extremity, and runs towards the north-west, parallel to the course of the upper Khabour, which rises from its flank at Ras-el-Ain. The name of Abd-el-aziz is applied to this spur, as well as to the continuation of the Sinjar between Arban and Halebi.
Sapor was thus enabled to choose his position, to establish a fortified camp at a convenient distance from the enemy, and to occupy the hills in its vicinity some portion of the Sinjar range with his archers. It is uncertain whether, in making these dispositions, he was merely providing for his own safety, or whether he was laying a trap into which he hoped to entice the Roman army.
Sheets of water are so rare in this region that the small lake of Khatouniyeh seems to deserve especial description. This lake is situated near the point where the Sinjar changes its character, and from a high rocky range subsides into low broken hills. In the middle of the lake is a hilly peninsula, joined to the mainland by a narrow causeway, and beyond it a small island covered with trees.
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