PARTHIA (Illustrated). George Rawlinson

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СКАЧАТЬ about 300 miles, and its average width about 100 or 120. It will have contained an area of about 33,000 square miles, being thus about equal in size to Ireland, Bavaria, or St. Domingo.

      The character of the district has been already stated in general terms; but some further particulars may now be added. It consists, in the first place, of a mountain and a plain region—the mountain region lying towards the north and the plain region towards the south. The mountain region is composed of three main ranges, the Daman-i-Koh, or Hills of the Kurds, upon the north, skirting the great desert of Rharaem, the Alatagh and Meerabee mountains in the centre; and the Jaghetai or Djuvein range, upon the south, which may be regarded as continued in the hills above Tersheez and Khaff. The three ranges are parallel, running east and west, but with an inclination, more or less strong, to the north of west and the south of east. The northern and central ranges are connected by a water-shed, which runs nearly east and west, a little to the south of Kooshan, and separates the head streams of the Ettrek from those of the Meshed river. The central and southern ranges are connected by a more decided, mountain line, a transverse ridge which runs nearly north and south, dividing between the waters that flow westward into the Gurghan, and those which form the river of Nishapur. This conformation of the mountains leaves between the ranges three principal valleys, the valley of Meshed towards the south-east, between the Kurdish range and the Alatagh and Meerabee; that of Miyanabad towards the west, between the Alatagh and the Jaghetai; and that of Nishapur towards the south, between the eastern end of the Jaghetai and the western flank of the Meerabee. As the valleys are three in number, so likewise are the rivers, which are known respectively as the Tejend, or river of Meshed, the river of Nishapur, and the river of Miyanabad.

      The Tejend, which is the principal stream of the three, rises from several sources in the hills south of Kooshan, and flows with a south-easterly course down the valley of Meshed, receiving numerous tributaries from both sides, until it reaches that city, when it bends eastward, and, finding a way through the Kurdish range, joins the course of the Heri-rud, about long. 01° 10’. Here its direction is completely changed. Turning at an angle, which is slightly acute, it proceeds to flow to the west of north, along the northern base of the Kurdish range, from which it receives numerous small streams, till it ends finally in a large swamp or marsh, in lat. 39°, long. 57°, nearly. The entire length of the stream, including only main windings, is about 475 miles. In its later course, however, it is often almost dry, the greater portion of the water being consumed in irrigation in the neighborhood of Meshed.

      The river of Nishapur is formed by numerous small streams, which descend from the mountains that on three sides inclose that city. Its water is at times wholly consumed in the cultivation of the plain; but the natural course may be traced, running in a southerly and south-westerly direction, until it debouches from the hills in the vicinity of Tersheez. The Miyanabad stream is believed to be a tributary of the Gurghan. It rises from several sources in the transverse range joining the Alatagh to the Jaghetai, the streams from which all flow westward in narrow valleys, uniting about long. 57° 35’. The course of the river from this point to Piperne has not been traced, but it is believed to run in a general westerly direction along the southern base of the Alatagh, and to form a junction with the Gurghan a little below the ruins of the same name. Its length to this point is probably about 200 miles.

      The elevation of the mountain chains is not great. No very remarkable peaks occur in them; and it may be doubted whether they anywhere attain a height of above 6000 feet. They are for the most part barren and rugged, very scantily supplied with timber, and only in places capable of furnishing a tolerable pasturage to flocks and herds. The valleys, on the other hand, are rich and fertile in the extreme; that of Meshed, which extends a distance of above a hundred miles from north-west to south-east, and is from twenty to thirty miles broad, has almost everywhere a good and deep soil, is abundantly supplied with water, and yields a plentiful return even to the simplest and most primitive cultivation. The plain about Nishapur, which is in length from eighty to ninety miles, and in width from forty to sixty, boasts a still greater fertility.

      The flat country along the southern base of the mountains, which ancient writers regard as Parthia, par excellence, is A strip of territory about 300 miles long, varying in width ac cording to the labor and the skill applied by its inhabitants to the perfecting of a system of irrigation. At present the kanats, or underground water-courses, are seldom carried to a distance of more than a mile or two from the foot of the hills; but it is thought that anciently the cultivation was extended considerably further. Ruined cities dispersed throughout the tract sufficiently indicate its capabilities, and in a few places where much attention is paid to agriculture the results are such as to imply that the soil is more than ordinarily productive. The salt desert lies, however, in most places within ten or fifteen miles of the hills; and beyond this distance it is obviously impossible that the “Atak” or “Skirt” should at any time have been inhabited.

      It is evident that the entire tract above described must have been at all times a valuable and much coveted region. Compared with the arid and inhospitable deserts which adjoin it upon the north and south, Khorasan, the ancient Parthia and Hyrcania, is a terrestrial Paradise. Parthia, though scantily wooded, still produces in places the pine, the walnut, the sycamore, the ash, the poplar, the willow, the vine, the mulberry, the apricot, and numerous other fruit trees. Saffron, asafoetida, and the gum ammoniac plant, are indigenous in parts of it. Much of the soil is suited for the cultivation of wheat, barley, and cotton. The ordinary return upon wheat and barley is reckoned at ten for one. Game abounds in the mountains, and fish in the underground water-courses. Among the mineral treasures of the region may be enumerated copper, lead, iron, salt, and one of the most exquisite of gems, the turquoise. This gem does not appear to be mentioned by ancient writers; but it is so easily obtainable that we can scarcely suppose it was not known from very ancient times.

      The severity of the climate of Parthia is strongly stated by Justin. According to modern travellers, the winters, though protracted, are not very inclement, the thermometer rarely sinking below ten or eleven degrees of Fahrenheit during the nights, and during the daytime rising, even in December and January, to 40° or 50°. The cold weather, however, which commences about October, continues till nearly the end of March, when storms of sleet and hail are common. Much snow falls in the earlier portion of the winter, and the valleys are scarcely clear of it till March. On the mountains it remains much longer, and forms the chief source of supply to the rivers during the spring and the early summer time. In summer the heat is considerable, more especially in the region known as the “Atak;” and here, too, the unwholesome wind, which blows from the southern desert, is felt from, time to time as a terrible scourge. But in the upland country the heat is at no time very intense, and the natives boast that they are not compelled by it to sleep on their house-tops during more than one month in the year.

      The countries by which Parthia Proper was bounded were the following: Chorasmia, Margiana, Aria, Sarangia, Sagartia, and Hyrcania.

      Chorasmia lay upon the north, consisting of the low tract between the most northerly of the Parthian mountain chains and the old course of the Oxus. This region, which is for the most part an arid and inhospitable desert, can at no time have maintained more than a sparse and scanty population. The Turkoman tribes which at the present day roam over the waste, feeding their flocks and herds alternately on the banks of the Oxus and the Tejend, or finding a bare subsistence for them about the ponds and pools left by the winter rains, represent, it is probable, with sufficient faithfulness, the ancient inhabitants, who, whatever their race, must always have been nomads, and can never have exceeded a few hundred thousands. On this side Parthia must always have been tolerably safe from attacks, unless the Cis-Oxianian tribes were reinforced, as they sometimes were, by hordes from beyond the river.

      On the north-east was Margiana, sometimes regarded as a country by itself, sometimes reckoned a mere district of Bactria. This was the tract of fertile land upon the Murg-ab, or ancient Margus river, which is known among moderns as the district of Merv. The Murg-ab is a stream flowing from the range of the Paropamisus, in a direction which is a little east of north; it debouches from the mountains in about lat. СКАЧАТЬ