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ARGHANDAB

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Originally appearing in Volume V02, Page 475 of the 1911 Encyclopedia Britannica.
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ARGHANDAB , a See also:

river of See also:Afghanistan, about 250 M. in length. It rises in the See also:Hazara See also:country See also:north-See also:west of See also:Ghazni, and flowing See also:south-west falls into the See also:Helmund 20 M. below See also:Girishk. Very little is known about its upper course. It is said to be shallow, and to run nearly dry in height of summer; but when its See also:depth exceeds 3 ft. its See also:great rapidity makes it a serious obstacle to travellers. In its See also:lower course it is much used for See also:irrigation, and the valley is cultivated and populous; yet the See also:water is said to be somewhat brackish. It is doubtful whether the See also:ancient Arachotus is to be identified with the Arghandab or with its See also:chief confluent the Tarnak, which joins it on the See also:left about 3o m. S. W. of See also:Kandahar. The two See also:rivers run nearly parallel, inclosing the backbone of the See also:Ghilzai See also:plateau. The Tarnak is much the shorter (length about 200 m.) and less copious. The ruins at See also:Ulan Robat, supposed to represent the See also:city Arachosia, are in its See also:basin; and the See also:lake known as Ab-i-Istada, themost probable representative of Lake Arachotus, is near the See also:head of the Tarnak, though not communicating with it. The Tarnak is dammed for irrigation at intervals, and in the hot See also:season almost exhausted.

There is a See also:

good See also:deal of cultivation along the river, but few villages. The high road from See also:Kabul to Kandahar passes this way (another See also:reason for supposing the 'Tarnak to be Arachotus), and the See also:people live off the road to avoid the onerous duties of hospitality.

End of Article: ARGHANDAB

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