PERSIA (Illustrated). George Rawlinson
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turf.” The plains of Khubbes, Merdasht, Ujan, Shiraz, Kazerun, and others, produce abundantly under a very inefficient system of cultivation. Even in the most arid tracts there is generally a time of greenness immediately after the spring rains, when the whole country smiles with verdure.
It has been already remarked that the Empire, which, commencing from Persia Proper, spread itself towards the close of the sixth century before Christ, over the surrounding tracts, included a number of countries not yet described in these volumes, since they formed no part of any of the four Empires which preceded the Persian. To complete, therefore, the geographical survey proper to our subject, it will be necessary to give a sketch of the tracts in question. They will fall naturally into three groups, an eastern, a north-western, and a southwestern—the eastern extending from the skirts of Mount Zagros to the Indian Desert, the north-western from the Caspian to the Propontis, and the south-western from the borders of Palestine to the shores of the Greater Syrtis.
Inside the Zagros and Elburz ranges, bounded on the north and west by those mountain-lines, on the east by the ranges of Suliman and Hala, and on the south by the coast-chain which runs from Persia Proper nearly to the Indus, lies a vast tableland, from 3000 to 5000 feet above the sea-level, known to modern geographers as the Great Plateau of Iran. Its shape is an irregular rectangle, or trapezium, extending in its greatest length, which is from west to east, no less than twenty degrees, or above 1100 miles, while the breadth from north to south varies from seven degrees, or 480 miles (which is its measure along the line of Zagros), to ten degrees, or 690 miles, where it abuts upon the Indus valley. The area of the tract is probably from 500,000 to 600,000 square miles.
It is calculated that two thirds of this elevated region are absolutely and entirely desert. 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. 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 the case, especially, on the south, where the coast chain is pierced by a number of streams, some of which have their sources at a considerable distance inland. On the north the Heri-rud, or River of Herat, makes its escape in a similar way from the plateau, but only to be absorbed, after passing through two mountain chains, in the sands of the Kharesm. Thus by far the greater portion of this region is desert throughout the year, while, as the summer advances, large tracts, which in the spring were green, are burnt up—the rivers shrink back towards their sources—the whole plateau becomes dry and parched—and the traveller wonders that any portion of it should be inhabited.
It must not be supposed that the entire plateau of which we have been speaking is to the eye a single level and unbroken plain. In the western portion of the region the plains are constantly intersected by “brown, irregular, rocky ridges,” rising to no great height, but serving to condense the vapors held in the air, and furnishing thereby springs and wells of inestimable value to the inhabitants. In the southern and eastern districts “immense” ranges of mountains are said to occur; and the south-eastern as well as the north-eastern corners of the plateau are little else than confused masses of giant elevations. Vast flats, however, are found. 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 tract in question, which at the present day is divided between Afghanistan, Beloochistan, and Iran, contained, at the time when the Persian Empire arose, the following nations: the Sagartians, the Cossseans, the Parthians, the Hariva or Arians, the Gandarians, the Sattagydians, the Arachotians, the Thamanseans, the Sarangae, and the Paricanians. The Sagartians and Cossseans dwelt in the western portion of the tract, the latter probably about the Siah-Koh mountains, the former scattered over the whole region from the borders of Persia Proper to the Caspian Gates and the Elburz range. Along its northern edge, east of the Sagartians, were the Parthians, the Arians, and the Gandarians. occurring in that order as we proceed from west to east. The Parthians held the country known now as the Atak or “Skirt,” the flat tract at the southern base of the Elburz from about Shahrud to Khaff, together with a portion of the mountain region adjoining. This is a rich and valuable territory, well watered by a number of small streams, which, issuing from the ravines and valleys of the Elburz, spread fertility around, but lose themselves after a short, course in the Salt Desert. Adjoining the Parthians upon the east were the Haroyu, Hariva, or Arians, an Iranic race of great antiquity, who held the country along the southern skirts of the mountains from the neighborhood of Khaff to the point where the Heri-rud (Arius) issues from the Paropamisan mountains. The character of this country closely resembles that of Parthia, whereof it is a continuation; but the copious stream of the Heri-rud renders it even more productive.
The Gandarians held Kabul, and the mountain tract on both sides of the Kabul river as far as the upper course of the Indus, thus occupying the extreme north-eastern corner of the plateau, the region where its elevation is the greatest. Lofty mountain-ridges, ramifying in various directions but tending generally to run east and west, deep gorges, narrow and tremendous passes, like the Khyber, characterize this district. Its soil is generally rocky and barren; but many of the valleys are fertile, abounding with enchanting scenery and enjoying a delightful climate. More especially is this the case in the neighborhood of the city of Kabul, which is perhaps the Caspatyrus of Herodotus, where Darius built the fleet which descended the Indus.
South of Aria and Gandaria, in the tract between the Great Desert and the Indus valley, the plateau was occupied by four nations—the Thamanseans, the Sarangians, the Sattagydians, and the Arachotians. The Thamanaean country appears to have been that which lies south and south-east of Aria (Herat), reaching from the Haroot-rud or river of Subzawar to the banks of the 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 body of water after rains, but