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Only two, the Helmend and the river of Ghuzni, have even the strength to form lakes; the others are absorbed by irrigation, or sucked up by the desert. Occasionally a river, rising within the mountains, forces its way through the barrier, and so contrives to reach the sea.
This is a portion of the high tableland of Iran, the great desert which stretches from the eastern skirts of Zagros to the Hamoon, the Helmend, and the river of Subzawur.
It is formed by the accumulation of the waters brought down by the Helmend, the Haroot-rud, the river of Khash, the Furrah-rud and other streams, which flow from the mountains of Afghanistan, with converging courses to the south-west. It is an extensive basin, composed of two arms, an eastern and a western.
"The Helmend, after passing near Kandahar, flows south-west and west, and enters Sedjestan some four days march from Douchak; making a détour around the mountains, it finally forms a lake. At Peldalek, which we visited, it is about 1200 feet in width, and very deep; the water is very good.
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.
We may conclude from this as probable that he held some Scythic tribes under his sway, probably in Segestan, or Seistan, the country south and east of the Hamoon, or lake in which the Helmend is swallowed up.
The rivers which flow from the mountains surrounding it are, with a single exception that of the Etymandrus or Helmend insignificant, and their waters almost always lose themselves, after a course proportioned to their volume, in the sands of the interior.
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.
In the Great Salt Desert, which extends from Kashan and Koum to the Deriah or "Sea" in which the Helmend terminates, and in the sandy desert of Seistan, which lies east and south-east of that lake, reaching from near Furrah to the Mekran mountains, plains of above a hundred miles in extent appear to occur, sometimes formed of loose sand, which the wind raises into waves like those of the sea, sometimes hard and gravelly, or of baked and indurated clay.
The portions of this district which are inhabited are those upon the river Helmend, whose bed deepens every year. At Elemdar Christie sent for a Hindu, to whom he had an introduction. This man advised him to dismiss his Belutchi attendants and to personate a pilgrim. A few days later he penetrated to Douchak, now known as Jellalabad. He says:
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