are, as has been stated before, eventually lost in a swamp. This is the most watery region I have seen in Persia. Besides the gushing, powerful springs which form vigorous streams at the moment of their exit from the mountain sides, there are many moist, spongy places in the three valleys, regularly boggy, giving out a pleasant squish under a horse's tread, and abounding in plants associated in my ideas with Highland bogs, such as the Drosera rotundifolia, which seems to thrive on a small red fly unknown to me. These waters and swampy places occupy a small area, just within the Outer range, below the southern slopes of the Kuh-i-Rang.
From this place I made an expedition of thirty miles up a very fine valley, much of which is irrigated and cultivated, by an ascent of 2500 feet to the Gal-i-Bard-i-Jamal, a pass 10,500 feet in altitude, with a tremendous descent into an apparent abyss, from whose blue depths rise the imposing mass of the Kuh-i-Shahan, and among other heights Faidun, a striking peak of naked rock, superimposed on a rocky ridge. At this height the air was really cool, and it was an escape from the heat of Dima.
This region seems much disturbed. We heard of bloodshed two days ago, and to-day in the Kharba valley of fighting among the Kuh-i-Shahan mountains with the loss of twelve lives, and horsemen passed us armed with long guns and swords on their way to tribal war. I fear I shall have to return to Isfahan. Things are regarded as looking very precarious farther on, and every movement, retrograde or forward, is beset with difficulties.
LETTER XVII
From Dima we ascended to high tablelands, having the snowy Zard Kuh ever in sight, one nameless peak being at present pure white, and descended into and crossed the Shorab, a fertile valley, on one side of which is the famous cleft called Kar Kanun, an artificial gash across a spur of the Kuh-i-Rang of the same name. After winding among mountains we descended on the Karun, whose waters, clear, rapid, and peacock-green, fertilise a plain of fine flowery turf lying at the base of hills, with another branch of the Karun between them and the Zard Kuh.
It is a lovely plain, bright and smiling, contrasting with the savage magnificence of the Zard Kuh, which comes down upon it with its peaks, chasms, and precipices, and glittering fields of unbroken snow. It was given up to mares and foals, but green platforms high above, and little hollows in the foot-hills were spotted with Ilyat tents, and in the four days which we spent there the camps were never free from Ilyat visitors. The Sahib came in the first evening with one man badly hurt, and another apparently in the first stage of rheumatic fever. A small tent was rigged for this poor fellow, who was in intense pain and quite helpless, with a temperature of 104°, and every joint swollen. The usual remedies had no effect on him. I had had a present of a small quantity of salol, a newish drug, with directions for its use, and his master Hadji undertook to make him take it regularly, and hot tea when he fancied it, and at the end of twenty-two hours he was not only free from fever but from pain, and was able to mount a mule.1
There are two definite objects of interest close to the plain of Chaman Kushan, the reputed source of the Karun and the great artificial cleft of Kar Kanun. I visited the first on a misty day, which exaggerated the height of the mountains, and by filling their chasms with translucent blue atmosphere gave a rare loveliness to the whole, for it must be said that the beauties of Persian scenery are usually staring, hard, and unveiled. The fords of two or three rivers, including the Karun, some steep ascents and descents, a rough ride along a stony slope of the Zard Kuh, and the crossing of a very solid snow-bridge took us to the top of a cliff exactly opposite the powerful springs in which the Karun has its reputed origin.
Over this source towers the mighty range of the Zard Kuh, – a colossal mountain barrier, a mass of yellow and gray limestone, with stupendous snow-filled chasms, huge precipices, and vast snow-fields, treeless and destitute of herbage except where the tulip-studded grass runs up to meet the moisture from the snow-fields. It is the birthplace of innumerable torrents, but one alone finds its way to the sea.
These springs are in a lateral slit in a lofty limestone precipice below a snow-field, at one end of which, as if from a shaft, the most powerful of them wells up, and uniting with the others in a sort of grotto of ferns and mosses pours over a ledge in a sheet of foam, a powerful waterfall, and slides away, a vigorous river of a wonderful blue-green colour, under a snow-bridge, starting full fledged on its course. The surroundings of this spring are wild and magnificent. A few Bakhtiaris crept across the lower part of the face of rock, and perched themselves above it. The roar of the water, now loud, now subdued, made wild music, and the snow-bridges added to the impressiveness of the scene.
Of course the geographical interest of this region is engrossing.2 This remarkable spring, called by the Bakhtiaris Sar-i-Cheshmeh-i-Kurang ("the head source of the Kurang"), and until this journey held to be the real source, is not, however, the actual birthplace of the Karun or Kurang, which was afterwards traced up to its headwaters in the magnificent Kuh-i-Rang.3
A few words on this, the one real river of which Persia can boast, and which seems destined to play an important part in her commercial future, will not be out of place. From its source it is a powerful and important stream, full, deep, and flowing with great velocity for much of its upper course between precipices varying in height from 1000 to 3000 feet. It is a perennial stream, fordable in very few places, and then only in its upper waters. Varying in width usually from fifty to a hundred yards, it is compressed at the Pul-i-Ali-kuh into a breadth of about nine feet.
The steepness and height of its banks make it in general useless for irrigation purposes, but some day it may be turned to account as a great "water power." Its windings, dictated by the singular formation of the mountain ranges (for I reject the idea of it having "carved" its channel), are almost phenomenal. After flowing south-east for a hundred miles from its source, it makes an acute bend, flows for fifty miles to the south-west, and then making another fantastic turn it flows in an exactly opposite direction to that of its earlier course, proceeding north-west to Shuster for a hundred miles.
It is calculated that the distance from the Kuh-i-Rang to Shuster as the crow flies is seventy-five miles, but the distance travelled by the waters of the Karun is 250 miles, with an aggregate fall of 9000 feet.
Besides being fed on its journey through the Bakhtiari country by many mountain-side fountain springs of pure fresh water, as well as by salt streams and springs, it receives various tributaries, among the most important of which are the Ab-i-Bazuft and a stream which, though known locally under various names, may be called from the Chigakhor basin in which it rises the Ab-i-Chigakhor, which makes a course of ninety miles to get over a distance of twenty; the Darkash Warkash flowing in from the Chahar Mahals near Ardal, the Dinarud rising in the fair valley of Gorab, and the Ab-i-Cherri or Duab.
This mountain range, the Zard Kuh, in whose steep side at a height of over 8000 feet the Sar-i-Cheshmeh-i-Kurang wells up so grandly, is rather a series of rock summits and precipices than a range of mountains. In late June its naked shelves and battlements upbore great snow-fields, and its huge rifts or passes – the Gil-i-Shah, nearly 11,700 feet in altitude, and the Pambakal, 11,400 – were full of snow. But even in four days it melted rapidly, and probably by August little remains except a few patches, in the highest and most sunless of the rifts. It is only on the north side that the snow lasts even into July.
The marked features of this range are its narrow wall-like character, its ruggedness on both sides, its absence of any peaks rising very remarkably above the ordinary jagged level of the barrier, its lack of prominent spurs, and its almost complete nakedness. It is grand, but only under rare atmospheric conditions can it be termed beautiful. Its length may be about thirty miles. It runs from north-west to south-east. Some of its highest summits attain an elevation of 13,000 feet. Its name is a corruption of Sard Kuh, "cold mountain."
After
For the benefit of other travellers I add that the dose of
A few geographical paragraphs which follow here and on p. 35 are later additions to the letter.
Although the correct name of this river is undoubtedly Kurang, I have throughout adopted the ordinary spelling
