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e Helmend about Ghirisk. This is a varied region, consisting on the north and the north-east of several high mountain chains which ramify from a common centre, having between them large tracts of hills and downs, while towards the south and the south-west the country is comparatively low and flat, descending to the level of the desert about the thirty second parallel. Here the Thamanseans were adjoined upon by the Sarangians, who held the land about the lake in which the Helmend terminates--the Seistan of Modern Persia. Seistan is mainly desert. One third of the surface of the soil is composed of moving sands, and the other two thirds of a compact sand, mixed with a little clay, but very rich in vegetable matter. It is traversed by a number of streams, as the Haroot-rud, the river of Furrah, the river of Khash, the Helmend, and others, and is very productive along their banks, which are fertilized by annual inundations; but the country between the streams is for the most part an arid desert. The Sattagydians and Arachotians divided between them the remainder of Afghanistan, the former probably occupying south-eastern Kabul, from the Ghuzni river and its tributaries to the valley of the Indus, while the latter were located in the modern Candahar, upon the Urghand-ab and Turnuk rivers. The character of these tracts is similar to that of north-western Kabul, but somewhat less rugged and mountainous. Hills and downs alternate with rocky ranges and fairly fertile vales. There is a scantiness of water, but still a certain number of moderate-sized rivers, tolerably well supplied with affluents. The soil, however, is either rocky or sandy; and without a careful system of irrigation great portions of the country remain of necessity barren and unproductive. The south-eastern corner of the plateau, below the countries of the Sarangians and the Arachotians, was occupied by a people, called Paricanians by Herodotus, perhaps identical with the Gedrosians of later writers. This district, the modern Beloochistan, is still very imperfectly known, but appears to be generally mountainous, to have a singularly barren soil, and to be deficient in rivers. The nomadic life is a necessity in the greater part of the region, which is in few places suitable for cultivation, but has good pastures in the mountains or the plains according to the season of the year. The rivers of the country are for the most part mere torrents, which carry a heavy
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