August 2.—Walking our horses all the way, we reached Adeljivas in four hours, excluding stoppages. The track follows the shore of the lake the whole distance, and you never lose the expanse of waters. In fact, it is the base of the block of limestones on the west of Sipan that you are skirting throughout the ride; although at first, and for some distance, the stratified rocks are superseded by intrusive material of igneous origin. These sombre heights are flanked by low foothills of purple conglomerate, which have been thrown into a succession of shallow folds, with an axis parallel to the shore. But as you approach Adeljivas the igneous rocks give way, and the conglomerate thins out and disappears. The limestone meets the waters, which it tinges with its own white hue. Hardened almost to the state of marble, it is in places full of corals. The scene becomes remarkable in the neighbourhood of the town, where cliffs of this description and of great elevation descend abruptly into the depths above which you ride. Passing through the enclosure of the ruinous walled city, which recalled the Kala or Ottoman fortress at Akhlat, we encamped among the gardens of the more modern quarter. We stripped on a narrow margin of pebble-strewn shore, regretting our purple rocks at Akhlat. The water is shallow for some distance out; but, in spite of the embouchures of the irrigation channels, it was most intensely blue. We swam forth, enjoying the buoyancy of the waves, with the distant barrier of the Kurdish mountains before our eyes. Their bare escarpments towered up to their crown of snow. In the reverse direction the landscape was already flooded with light, and the foliage merged into the general brilliancy of tone. A conspicuous object was the ruinous citadel, proudly placed against the cliffs—the single When we returned there were two wooden couches with leather seats, and a couple of chairs, of similar pattern and equal shabbiness, arrayed upon the sward. These unusual objects had been unearthed for our benefit. They were not long in finding occupants among the personages of importance who were desirous of paying us the honour of a visit. The Commandant of the garrison came, accompanied by his aide-de-camp; they were followed by the burly mufti, and by several notables; last of all came the two Kaimakams. It was a medley of striped military trousers and gold lace, of flowing cloaks and white turbans, of black frock-coats and the tasselled fez. Each had a word to say upon the details of the expedition; each could help if one would only give them time. My great regret was that time failed me to receive their suggestions; there were indeed so many things which must be done. First I had to feed and water my horses, for the forage had not arrived in the early morning. When it came, the several owners were at variance, one with another; and I was obliged to seize it by force. Then there were my people, who would surely go without their breakfast rather than take the trouble to procure victuals. These I had provided with great difficulty overnight; but the cook had experienced trouble with his fire. Such everyday concerns were augmented on this occasion by several affairs of much greater consequence. It was necessary to engage at least ten porters; when these had been got together with infinite difficulty, there was no possibility of arriving at terms and a price. By the time the Kaimakam appeared, the orchard was alive with people, all intent on delaying the conclusion of their several bargains for the mere love of talk. That official was of great assistance, because he fixed the price himself, and ordered each man to conclude his business on those terms. But there was one matter which called for very delicate treatment, and of which the ultimate issue was not so clear. It was most important that our escort, during the journey through the wild districts interposed between Sipan and BingÖl, should be composed of men who might be trusted at least so far as not to involve us in unnecessary brawls. They must obey my orders to the letter; but my authority could only exist by delegation from It was noon by the time these various matters had been decided—not a bad piece of work under the circumstances. There only remained the last and saddest of our duties—to say good-bye to the energetic and admirable official who had accompanied us thus far on our road. What a contrast between this Circassian, lithe of figure and nimble of mind, and his heavy, Two villages had been mentioned as both presenting a good base from which to climb Sipan. One was Norshunjik, and the other Uran Gazi. The first is situated on the south-western side of the mountain, and the second rather more round towards the west. Uran Gazi—a Circassian settlement—was, after some debate, selected, owing chiefly to the reputation and resources of its head men. It may be reached in about two hours from Adeljivas. Riding in a northerly direction, we pursued a winding track which became involved in the recesses of the hills. We must have been close to the break-off of the plateau of limestone on the west of Sipan; but the view towards the east was never open. The limestone was all about us, white and barren as usual, in striking contrast to the verdant scene we had left behind. So high did the escarpments tower, that although we continued to rise at a considerable gradient for a space of about an hour, it was only towards the latter portion of the ascent that we obtained a view of the summit region of the great volcano. But the vista towards the lake was of striking beauty, with the ruinous castle standing up against the blue. Deep below us on our left hand we admired the site of a walled monastery, high-seated in a broad valley. There was more traffic along this track than one might have expected; we kept meeting laden donkeys and a number of wayfarers. The adjacent slopes were, in places, strewn with blocks of lava. When we reached the pass, we were standing on the edge of an undulating plateau, and were still within the zone of the limestones. A slight descent from this point brought us almost immediately to a shallow but very extensive depression. It had, in fact, the appearance of a vast plain, somewhat of an oval, with an axis roughly from east to west. In the latter direction we could see the plain tonguing into the limestones, or, in other words, the almost latitudinal limestone ridges sinking into the plain. But these were dwarfed in the east by the flows of lava from Sipan, of which the huge frame was now fully exposed. In particular a bold stream plunged down from the summit region, ending in dark, precipitous sides. About in the centre of the depression lay a little lake, fringed by marshes, and bordered by a deep belt of what appeared to be a white efflorescence adhering to its shores. It was the Jil GÖl (lake of rushes), once of considerably greater extent. A village, just a speck at the western extremity of the bold ridge of lava, was identified as Uran Gazi. Behind us the limestones stood up like a wall, screening the lake of Van. Except for the marshes, there was not a trace of verdure in a landscape devoid of trees or even of bush. Far and wide, the surface of the plain was broken only by mounds or gullies—the mounds heaped up with blocks of black lava, the gullies doubly darkened by the same material. Indeed the whole depression has been covered with lava, probably to some considerable depth. Its elevation above sea-level is not much less than 7700 feet. In another three-quarters of an hour we reached Uran Gazi, and were received by two Circassian notables, resident in the village, Murad Effendi and Shakir Effendi. I think I have already observed upon the superiority of the Circassian villages to those of their neighbours, Armenians or Kurds. The bread they make is eatable; fair cheese can be obtained; the tenements are much more solidly built. Great stacks of hay had already been collected against the winter. The Circassian skirted coat and the Fig. 187. Village of Uran Gazi with Sipan. Fig. 187. Village of Uran Gazi with Sipan. The position of the village, at the extremity of the bold ridge of lava (Fig. 187), may be taken as representing the furthest westerly extension of the flows of lava from the volcano, as we see it now. The ridge itself has an axis of about west-south-west. At four o’clock we made our way along its southern margin, up the broad valley by which it is separated from similar outliers on the south. The caterjis, with the packs, followed this valley to its head; but our guides, whether from knowledge of the August 4.—The ascent of Sipan offers no difficulties whatever at this season, and is, indeed, a delightful excursion. There is the joy of awaking to a landscape so inspiring—such a wide segment of a circle, almost without limits on the horizon, framed by the heights descending upon either side. From the rocky island of the Kartevin to the western slopes of the Nimrud crater, an immense region is outspread at our feet. Flatness of outline is the almost universal characteristic; and the marble peaks of the Akh Dagh, conspicuous even at this distance, are at once an exception and a solecism. Further west, the view extends to the even ridge of the BingÖl Dagh, flecked about the centre with snow. Nearer masses of imposing aspect are Bilejan and Khamur; an unknown mountain, which, later in our journey, we came to know as Kolibaba, rising with lesser proportions between the two. But the plains outdo the mountains, resembling a wide sea—although surely no sea can be surrounded by such commanding objects. The treeless, yellow surface commences deep below us, and stretches without a break to the Kartevin. Low ridges come edging towards it from the block of limestones, which, in the west, appears to encircle the lake of Nazik, and to divide it from that of Gop. The outline of the block grows in height towards Lake Van. It was two o’clock in the afternoon before we were ready to start upwards, turning our backs upon this scene, and on foot. The ten porters carry our flying tent and our wraps, besides a little tezek fuel for our camp fire, and four long poles for taking Such perhaps is the most concise description of the strange scene about us and at our feet (Fig. 188). My illustration was taken on the following day from the top of the westerly eminence, or western summit of Sipan. Our position now is on the slope of that lofty eminence, on the upper margin of a field of snow, which is not visible in the picture, but which descends to the little lake in the foreground. The lake is known as Kirklar GÖl, or lake of the forty Mussulman saints, and is probably due to the dissolving of the snowy sheets which hem it in on either shore. The slope on the opposite, or southern side of the basin is very steep where it sinks to the pool; and it sometimes happens that the snow falls headlong and in a mass into the blue water. West of the lake, and especially beneath the western summit, the edge of the basin is low; indeed we have entered into the summit region by a natural passage or partial cleft. Fig. 188. Sipan: View from the Western Summit over the Summit Region. Fig. 188. Sipan: View from the Western Summit over the Summit Region. Adhering to the skirts of this western summit, or taking refuge upon the snow from the deep rubble on its uppermost slope, we The ridge upon which we stand narrows and becomes knife-like, as it bends towards the northern extremity of the upstanding mass. It provides the scantiest strip of bare but level rock between sheets of snow on either side. On the north it is a cornice of snow above the plains, thousands of feet down. In that direction there would appear to be a tremendous abyss. Nor is the slope towards the basin of tolerable gradient; it is so steep that it would be difficult to descend to the second of the lakes without making a considerable circuit. Still this ridge appears to offer a convenient site for our encampment, owing to its central position. There are a few piles of rocks, nearly as high as a man, which will prevent us being swept into the depths on either side, in case a storm should arise. The only danger would be a sudden drift of snow. I give orders to erect the tent against one of these little screens; and, accompanied by a Circassian, Oswald and I continue our march towards the lofty platform on the east. Our slender parapet ends in its steep and talus-strewn side, which we commence to scale. We step from block to block, the boulders consisting of a light brown lava, which has broken up with sharp angles. There can be no doubt that this mass is the latest result of eruptive action upon the summit of Sipan. The whole or nearly the whole of the eastern portion of the crater was PLAN OF THE SUMMIT REGION OF SIPAN PLAN OF THE SUMMIT REGION OF SIPAN measured and drawn out by H. F. B. Lynch and F. Oswald in August 1898 Scale 1 Mile = 2 Inches or 1:31.680 Explanation:
Engraved and printed by Wagner & Debes, Leipzig Published by Longmans, Green & Co., London The sun is setting; so the tripod is rapidly erected, and the bearings of the principal mountains registered with the utmost care. Happily the sky is almost free of cloud. Ararat soars into space, a magnificent object, both peaks of the greater mountain, although almost merged by the perspective, being distinguishable by the naked eye. The bold snow bastion on the west is seen to the fullest advantage. But the Little Ararat is almost hidden by nearer outlines; and only the summit of that graceful cone is exposed. If the mountain of the Ark be without equal, or even rival, in a landscape which in all directions is sublime, it possesses at least a neighbour with many attributes in common—the Kuseh Dagh, beyond the plain of Alashkert. That giant overtops the land forms, almost from the very base—a truly inspiring sight. It is so essentially a great mountain, towering up to a symmetrical, but deeply vaulted dome. Night is falling as we descend to our little tent upon the ridge at an elevation of 13,000 feet. But our poor porters and the several zaptiehs who have, quite unnecessarily, scrambled up—how shall we protect them against the rigour of the night? They prefer to remain with us; so we wrap them up in the stout red cloth which we have by us for our measuring poles. They cower over the smouldering fire against the screen. But August 5.—Neither my companion nor myself are able to sleep, although we are quite fresh for our work next day. The same experience befell our party upon Ararat; at these high altitudes one does not seem to require sleep. We are up before the sun; but the light is already sufficient to disclose the great world, silent at our feet. Not a vestige of cloud is clinging to our mountain; and, as the sun rises, all the outlines in the distance are well defined. To Oswald is apportioned the task of taking measurements, and he starts off over the snow-fields with his telemeter and his poles. I mount to the summit of the platform on the east, which is reached at half-past six. There I erect my instruments in the same cairn which we visited yesterday, and which may be called the eastern summit. The pools on the way are thinly crusted with ice. With what joy I look out from the well upon the cairn, and am greeted with the sight of Ararat in all his majesty, without a particle of cloud! Every minute the outline grows in distinctness, and each familiar feature becomes clear. How radiant the fabric looks—such a bright presence in the sky, above the summits of the Ala Dagh! Those mountains pass insensibly into the outlines on the east—the horizontal heights of the Persian tableland. Westwards it is a series of plains. The plain of Patnotz, deep below us, joins the plain of Melazkert; that expanse is continued into the region of Bulanik, threaded by the silver channel of the Murad. Kartevin and Bilejan rise like islands from this sea-like surface, in which are lapped the blue waters of Lakes Nazik and Gop. In the north the undulations of the plateau country are continued up to the barrier of the Mergemir—Kilich-Gedik; but that outline is so low that you almost see the plain beyond it, supporting the base of the Kuseh Dagh. Further west the plains are bounded by much bolder masses—Khamur with BingÖl showing up behind. The peak of PalandÖken is just perceived. But the Nimrud crater is a conspicuous object—not the least remarkable feature in the scene. How vast it all looks!—stray clouds throwing liquid shadows, and earth reflecting the glow of morning in vague, mysterious lights and hues. In the opposite direction the contrast exceeds expectation—for one is standing in the border region on the outskirts of the plateau, and near the serried ranges which confine it on the south. I remain about three hours upon this summit, and then proceed to the highest eminence on the eastern margin of the circular figure, in order to overlook the eastern arm of Lake Van. On my way there a strange incident occurs. My Circassian has told me that there exists a ziaret, or place of pilgrimage, in the vicinity of this cairn. Curious, and half doubtful, I ask him to show me the spot, which he says is close by. What is my amazement when, opening out a slight hollow of the snowy surface, we see before us a group of Mohammedan women, standing upon the ice with bare feet and ankles, and prostrating themselves before a pair of stag’s horns! Indeed the antlers are so thickly covered with little bits of rag that it is impossible to say for certain to what species of animal they belonged. Stranger still is the fact that a band of women—I count twelve—should have risked their lives in this way. Tantum religio!... And yet the Kaimakam of Melazkert is quite unshaken in his belief that only one man, and he in exceptional circumstances, has ever trodden the sacred summit of Sipan! After spending nearly another three hours upon the eastern eminence, during which I draw in the portion of the lake which lies before me, because I recognise several errors in the existing map, I return to our camp upon the ridge. Oswald has just completed his arduous work upon the snow; and the combination of our labours produces the following results, which must be taken as approximate. The long axis of the figure described by the summit region is but little inclined from an east-west line. The centre of the circular mass, to which the eastern summit belongs, is a little north of a line drawn from the western summit in an easterly direction. The ultimate points of this axis are, on the west, the western summit, and on the east, the eminence upon which I last stood. The distance between the two The Circassians and the porters dance with delight when the order is given to take down the tent. They appear to have made up their minds that we shall keep them shivering for another night. All give utterance to devout and repeated Alhamdilallahs, thanks be to God! Our last duty is to scale the western summit, and to become familiar with the scene which it commands. We overlook the small circular lake of the Aiger GÖl, on the southern slopes of Sipan. It perhaps fills the basin of a parasitic crater. The elevation of this peak is about the same as that of the eastern summit, namely 13,700 feet. On our way down we recognise the traces of a bear; and we reach our standing camp without further incident at about five o’clock. It has been a very full and delightful day. Fig. 189. Grave on the Summit of Khamur. Fig. 189. Grave on the Summit of Khamur. Sipan appears to have been built up by successive lava streams, which became more and more viscous, until that finally emitted had no power to flow at all, and merely welled up, forming the circular mass on the east. The lava composing that mass is spongy and glassy, a glassy mica-andesite. The narrow ridge, upon which we camped, and which may represent the northern rim of the old crater, consists of a slabby rhyolite with impure obsidian; it is covered up with cindery slag. The western summit and surrounding rock is made up of a lava somewhat similar to that on Nimrud—a dull impure obsidian with ill-developed spherulites; the flow structure is well marked. Tuffs were nowhere to be seen. But a bastion on the northern side of the mountain was cloaked with grey pumice sand. The ascent of the mountain is described by Brant (J.R.G.S. 1840, vol. x. pp. 409 seq.) and by Tozer (Turkish Armenia, pp. 327 seq.). But they both largely underestimate the height. They appear to have been misled by the fact that the highest points are free from snow in midsummer; but the summit region in general is a mass of snow even at that season. On Ararat such piles of rock, on which the snow has been unable to obtain a footing, are found quite near the summit, which is nearly 17,000 feet high. |