* r r p a r v OF TIIE j T h e o 1 ogical Seminary. PRINCETON, N. J. Case Division .*L)_ Qi 5- J. . Shelf C cc'.ior. • H ^3 Q Book / CENTRAL ASIA: FROM THE ARYAN TO THE COSSACK. BY , / JAMES AIUTTON, AUTHOR OF ‘ A HUNDRED YEARS AGO,’ 4 MISSIONARY LIFE IN JT HE SOUTHERN SEAS,’ ETC. ETC. LONDON: TINSLEY BROTHERS, S, CATHERINE STREET, STRAND. 1875. [AU Rights reserved.] JOHN CHILDS AND SON, PRINTERS. CONTENTS. CHAPTER I. GENERAL OUTLINE. The Aralo-Caspian Sea — General Outlines of Central Asia — The Aral Sea — The Ust Urt — The Chink — Historical Allusions — Sir Henry Raw- linson’s Theory — Ancient Course of the Oxus — The Amou of the Pre- sent Day — The Jaxartes, or Syr — The Caspian Sea CHAPTER U. EARLY HISTORY. Early Inhabitants — Scythians — Under Darius and Xerxes — Mount Imaus — Margiana — Bactria — Sogdiana — Alexander’s Campaigns — Sikun- der Zulkarnain — The Greco-Bactrian Kingdom — The Parthians — The Scytho-Chinese Domination — The Sassanides— Ardesheer, Hormuz, Feroze, Kobad, Nousheerwan, Khosroo Purvez, Yezdijerd— Arab Con- quest — Justinian and Dizabulus — Embassy of Zemarchus . . . . 22 — 45 CHAPTER III. Mawaralnahr in the 10th century — Bokhara — Samarkand — Khwarezm — The Ghuz — Ibn Mohaihal’s Travels — The Samanides — The Ghuznee- vides — The Seljook Dynasty — Alp Arslan — Malek Shah — Sanjar — Kingdom of Khwarezm — Conquest of Mawaralnahr by the Moghuls — Jelal-ood-deen . , . . . . . . . . 46 — 66 PAGR 1—21 CHAPTER TV. THE MOGHULS. Origin of the Moghuls — Chinghiz Khan — Conquest of Northern China — Massacre of Tatar Envoys at Otrar — Reduction of Otrar — Defeat and Flight of Mohammed Shah — Capture of Bokhara — Capture of Samar- kand, Termedh, Balkh, Talikhan, Merv, Nishapoor, Herat, and Ur- ghunj — -Death of Chinghiz — His Yasakor Code — Batou Khan’s Irrup- tion into Europe — The Moghul Empire — Papal Missions to the Great Khan — Reply of Kuyouk Khan — Mangou Khan’s Rebuke — Mission of William de Rubruquis — Tatar Customs — The Moghul Court at Kara- koram . . . . . . . . . . , . 67—95 IV CONTENTS. CHAPTER V. THE TATARS. PAGiC King Haiton I. of Armenia — Correspondence between Moghul and Chris- tian Princes — Letters of Edward II. to the King of the Tatars — Let- ter from Prester John to Alexius Comnenus — Various Accounts of Prester John — Nestorius — Revival of Mohammedauism — Birth of Timour — His Early Life and Adventures — Raised to the Throne — His Conquests — Sheeahs and Soonees — The Twelve Imams — Defeat of Bayazid — Return of Timour to Samarkand . . . . 96 — 119 CHAPTER VI. TIMOUE-LUNG. Marriage of Jehangheer — Embassy of Clavijo — Kesh — Festivities at Samarkand — Timour’s Magnificence — Hard Drinking — Dress of the Khanum — Badakhshan — Balas Rubies — Lapis Lazuli — Samarkand — Laws and Regulations — Clavijo’s Journey across the Desert — Death of Timour .. .. .. .. .. 120 — 111 CHAPTER VII. MOHAMMED BABES : ANTHONY JENKINSON. Baber — Ferghana — Baber’s Father and Uncle — Capture of Samarkand — Reverse of Fortune — A Moghul Custom — Baber defeated by Sheibani Beg — The Kafirs, Eimauks, and Hazarelis — Baber recovers Samar- kand — Expelled by the Oozbegs — Conquers Hindostan — The Oozbegs — Ismael the Souffavean — The Sheibanides — Anthony Jenkinson — Urgliunj — Attacked by Robbers — Bokhara — The King — Trade — Re- turn to Moscow . . . . . . . . . . 145 — 16T CHAPTER VIII. SEVENTEENTH CENTURY : NADIR SHAH. Bernier and the Tatar Ambassadors at the Court of Arungzeb — A Tatar Heroine — Route from Kashmeer to Kashgar — Travels of Benedict Goes and other Missionaries — AbouT-Ghazee Khan — Khiva and Bokhara in the Seventeenth Century — Nadir Shah — English Tra- vellers— Trade — Decadence of Persia . . . . . . 168 — 188 CHAPTER IX. THE RIVAL POWERS. Commencement of Anglo-Russian Trade — Queen Elizabeth’s Letter to Shah Tahmasp — Christopher llurrough — Expedition of Prince Beck- ovich — Cherkassky — John Elton — Captain Woodroofe — Jonas Han way — Count Voinovich — Relations of Russia with Khiva — Mouravief’s Mission — General Perofski’s Expedition — Russia and England in Central Asia — Major Abbott’s Mission — His Experiences of Khiva — Undertakes a diplomatic Mission to St Petersburg — His Adventures in the Desert . . . . . . . . . . 189 — 224 CONTENTS. V CHAPTER X. KHIVA. PACE Khiva : Historical Notice — Natural Productions — The Saxaul — Popula- tion— The Capital City — The Khan and his Wives— Executions— Persian Captives — Caravan Routes — Urghunj, Old and New — Ilaznr Asp — Kungrad— Captain Conolly’s Journey from Astrabad to Herat — Maimers and Customs of the Toorkomaus — Merv . . . . 225 — 252 CHAPTER XL BOKHARA. Bokhara — Frontiers — Area — Population — The Oozbegs and their Pecu- liarities — The Tajeeks — Other Races — Russian Slaves — The Kohik, or Zarafshan — Valley of Shuhr-i-Subz — Natural Productions — Manu- factures — Trade — M. de Negri's Mission — Journey from Orenburg to Bokhara — The Khan — System of Administration — Manners and Cus- toms-Revenues — Military Forces . . . . • • 253 — 2S2 CHAPTER XII. BOKHARA — RUSSIANIZED. Bokhara — History — Aspect — The Ark — Public Buildings — Hindoos — Jews — Climate — Russian Slaves — Samarkand — Russian Occupation — Karshee — Khoja-Saleh — Shuhr- Islam — Charjui — Karakul — Shuhr- i-Subz — Hissar — Historical Sketch of Bokhara — Executions of Stod- dart, Conolly, and Wyburd — Nusser Oollah Khan — Mozuffar-ood- deen Khan — Advance of the Russians— Prince Gortchakofs Circular — Battle of Yirdjar — Fall of Khojend — Capture of Samarkand — Mis- sion from Bokhara to St Petersburg — Capture of Kulja — The Rus- sian Frontier Line . . . . . . . . . . 283 — 314 CHAPTER XIII. CHINESE TAT ARY. Floods of Migration from the North-East — Zungaria, or Semi-Palatinsk — Fort Vernoe — The Process of Annexation — Internecine Strife be- tween the Bogus and Sara-Bogus Tribes — Habits and Customs of the Kirghiz — Attack upon a Caravan — Issyk-kul — Semirechinsk — The Ili — Almalik — The Trans-Naryn District — Khanat of Khokan — Chief Towns — Ush — Russian Toorkestan — Otrar .. .. 315 — 339 CHAPTER XIV. EASTERN TOORKESTAN. * Little Bucharia ’ — Rivers — Mountains — The Gobi — The Yak — Popula- tion — The Kirghiz — The Tunganis — Houses — Costume,' — Manners — Horses — Ughlak — Coinage — Mr Robert Shaw — Lieutenant Hayward — Sanj u — Karghalik — Posgam — Yarkund — Y anghi ssar — Kashgar — Mohammed Yakoob Beg — Aksu — Ush-Turfan — Kliotan — Mr John- son . . . . . . . . . . . . 340 — 370 VI CONTENTS. CHAPTER XV. THE AMEER OF KASHGAR. PAGE Historical Sketch of Altj'shuhr — Walee Khan Toura — Mohammed Ya- koob Beg — Tungani Rebellion — Heroic Suicide of the Amban — Fall of Kashgar — Yakoob Beg defeats the Tunganis — Receives title of Atalik Ghazee — Treacherous Seizure of Khotan — Reduction of Tash Kurghan — Official Relations with Russia — Mr Forsyth’s first Mission — Baron Von Kaulbars’ Mission — Exports and Imports — Progress of Russian Influence — Aga Mehdie Raphael — Routes to India — Ladakh — Mr Forsyth’s second Mission — Lord Clarendon’s Neutral Zone 371 — 394 CHAPTER XVI. BADAKSHAN. Badakhshan — Historical Sketch — Inhabitants — Hindoo-Koosh — The Ha- zarehs — Sykan — Slaves — Aibek — Khulm, or Tashkurghan — Mazar Balkh — Kunduz — Oozbegs — Khana-a-abad — Talikhau — Fyzabad — Jerm — Manners and Customs — Wakhan — Kooroot — Ish-Kashm — Kundut — Kirghiz Encampment . . . . . . 395 — 417 CHAPTER XVII. PAMEER. Darwaz — Roshan — Shignan — Vardoj Valley — Kafirs or Siahpoosh — Chit- ral — Lieutenant Hayward on the Massacres committed in Yassin by the Dogras — -His Death — Gilgit — Chilas — Baltistan — Pameer — Hiouen Tsang — Marco Polo — Colonel Yule — Ovis Poli — Batu-i-Du- niali — Lake Victoria — Four Confluents of the Oxus, or Arnou — The great Geographical Swindle . . . . . . . . 418 — 441 CHAPTER XVIII. THE KHIVAN EXPEDITION. Colonel Markosof’s Reconnaissance in 1872 — Diplomatic Correspondence — Advance of General Golof’s Corps — A Grand Duke under Felt — Friendliness of the Bokharians — Skirmish with Toorkomans — Re- pulse of the Khivans — Passage of the Amou — Occupation of Hazar- nsp — Fall of Khiva — General Verefkin’s March — Colonel Lomakin’s March — Colonel Markosofs Disaster — Submission of the Khan — Peace — Distribution of Honours — Sir Henry Lawrence on a Russian Invasion of India— Sir Thomas Munro on our Treatment of the Na- tives — Conclusion . . . , . , . . 442 — 472 CHIEF AUTHORITIES CONSULTED FOR THE PURPOSES OF THIS COMPILATION. The Life anti Actions of Alexander the Great. By the Rev. John Williams. 1829. The Histone of Qvintos Curcius. conteyning the Actes of the greate Alexander, trans- lated out of Latino into Englishe, by John Brende. 1553. A History of Greece ; from the earliest period to the close of the generation contem- porary with Alexander the Great. By George Grote. 1862. The History of Herodotus. By the Rev. Geo. Rawlinson, M.A. 1858. Rollin’s Ancient History. Edited by Jas. Bell. 1828. The Geography of Strabo. Translated by H. C. Hamilton and W. Falconer. 1854. A Dictionary of Greek and Roman Geography. Edited by Wm. Smith, L.L.D. 1852. The Oriental Geography of Ebn Ilaukal. an Arabian Traveller of the 10th century. Translated by Sir William Ouseley, Knt., L.L.D. 1800. The Book of Ser Marco Polo, the Venetian. Edited by Col. Hv. Yule, C.B. 1871. Le Livre de Marco Polo. Redige en Franqais par Rustician de Pise. Publie par M. G. Pauthier. 1865. The Travels of Marco Polo. Edited by Hugh Murray, F.R.S.E. 1844. Cathay and the Way Thither. By Col. Hv. Yule, C.B. 1866. The Voyages and Travels of Master Anthony Jenkiuson from Russia to Boghar, or Bokhara, in 1557. Pinkerton’s Collection, vol. ix. 1811. The Voyage of Master Anthony Jcnkinson, made front the citie of Mosco in Russia to the citie of Boghar in Bactria, in the year 1558 ; written by himselfe to the Mer- chants of London of the Muscouie companie. Hakluyt. The Journal of Friar Wm. de Rubruquis, a French man of the order of the minorite friers, unto the East parts of the worlde. An. Dom. 1253. Hakluyt. Memoire sur la Partie Meridionale de l’Asie Centrale. Par N. de Ixhanikof. 1861. A Journey from Bengal to England, by Geo. Foster, in 1783-84. Pinkerton. Journey to the North of India, overland from England, through Russia, Persia, and Afghanistan. By Lieut. Arthur Conolly. 1834. Voyage d’Orenbourg a Boukhara, fait en 1820: redige par M. le Baron G. de Meyendorf, et revu par M. le Chevalier A. Jaubert. 1826. An Account of the Kingdom of Caubul and its dependencies in Persia, Tartary, and India. By the Hon. Mountstuart Elphinstone. 1839. Ladak, Physical, Statistical, and Historical. By Alex. Cunningham, Major, B.E. 1854. The Ancient Geography of India. By Major-General Alex. Cunningham. 1871. An Historical Account of the British Trade over the Caspian Sea. By Jonas Han- way, Merchant. 1754. Narrative of the Embassy of Ruy Gonzalez de Clavijo to the Court of Timour at Samarcand.. a.t>. 1403-6. Translated by Clements R. Markham, F.R.G. S. 1859. Histoire Genealogique des Tatars, traduite du Manuscript Tartare d’Abulgasi — Bay- adur-Chan. 1726. Visits to High Tartary, Yarkund, and Kashgar. By Robert Shaw, British Com- missioner in Ladak. 1871. Travels in the Himalayan Provinces of Hindustan and the Punjab ; in Ladakh and Cashmere ; in Peshiawur, Kabul, Kunduz, and Bokhara. By 51 r Wm. Moor- Vlll CHIEF AUTHORITIES CONSULTED. croft and Mr George Trebeck, from 1819 to 1825. Edited bv II. II. Wilson, M. A. 1811. Narrative of a Mission to Bokhara in tlxe years 1843-45. By the Rev. Jos. Wolff, D.D. 1852. Caravan Journeys and Wanderings in Persia, Afghanistan, Toorkistan, and Biloueb. By J. P. Ferrier, Adjutant-General of the Persian Army. Translated by Capt. Wm Jesse. 1856. Voyage en Turcomanie et d Khiva, fait en 1819 et 1820; par M. N. Mouraviev. Traduit par M. G. Lecomte de I.aveau. 1823. Narrative of a Journey from Herat to Khiva, Moscow, and St Petcrsburgh. By Major James Abbott. 1856. History of Bokhara. By Arminius Vambery. 1873. A Journey to the Source of the River Oxus. By Capt. John Wood, Indian Navy. With an Essay by Col. Hy. Yule, C.B. 1872. Chronological Retrospect, or Memoirs of the Principal Events of Mohammedan His- tory. By Major D. Price. 1811. The History of Persia, from the most Early Period to the Present Time. By Major- General Sir J. Malcolm, G.C.B. 1829. The Life of Baber, Emperor of Hindostan. Translated by Dr I.eydcn and W. Ers- kine. 1844. Bernier’s Voyage to the East Indies. Pinkerton, vol. viii. Memoires sur les Contrces Occidentales, traduits du Sanscrit on Chinois en Tan 648, par Hiouen Tsang, et du Chinois en Franqais par M. Stanislas Julien. 1858. 'The Russians in Central Asia. Translated from the Russian by John and Robert Michell. 1865. Bokhara: its Amir and its People. Translated from the Russian of M. N. de Khan- ikof, by the Baron Clement A. de Bode. 1845. Travels into Bokhara, &c. By Lieut. A. Burnes, F. R. S. 1834. Travels in Central Asia. By A. Vambery. 1864. Sketches of Central Asia. By A. Vambery. 1868. The Delta and Mouths of the Amu Daria or Oxus. By Admiral A. Boutakof of the Russian .Navy. Translated by Jno. Michell. Roy. Geog. Soc. Journ. xxxvii. First Ascent of the Tian Shan or Celestial Mountains, and Visit to the Upper Course of the Jaxartes or Syr Daria, in 1857. By P. P. Semenof. Translated by John Michell. Roy. Geog. Soc. Journ. xxxi. W. II. Johnson’s Report on his Journey to Ilchi, capital of Kliotan in Chinese Tar- tary. Roy. Geog. Soc. Journ. xxxvii. The Jaxartes or Syr Daria; from Russian Sources. By Robt. Michell, F.R.G.S. Roy. Geog. Soc. Journ. xxxviii. A New General Collection of Voyages and Travels. Printed for Thos. Astley. 1747. Journey from Leh to Yarkand and Kashgar, and Exploration of the Sources of the Yarkand River. By G. W. Hayward. Roy. Geog. Soc. Journ. xl. Timour’s Memoirs. Translated by Capt. C. Stewart. An Expedition to the Trans-Naryn Country in 1867. By Baron P. R. Osten Sacken. Translated by E. Delmar Morgan, F.R.G.S. Roy. Geog. Soc. Journ. xl. Gibbon’s Decline and Fall of the Roman Empire. Layard’s Nineveh. Edinburgh and Quarterly Reviews. Odean Highways, &c. &c. &c. CENTRAL ASIA: FROM TIIE ABYAN TO THE COSSACK. CHAPTER I. GENERAL OUTLINE. THE ARALO-CASPIAN SEA — GENERAL OUTLINES OF CENTRAL ASIA — THE ARAL SEA — THE UST URT — THE CHINK — HISTORICAL ALLUSIONS — SIR HENRY RAWLIXSON’S THEORY — ANCIENT COURSE OF THE ONUS — THE AJIOU OF THE PRESENT DAY — THE JAXARTES, OR SYR— THE CASPIAN SEA. According to the late Sir Roderick Murchison, — no mean authority on questions relating to geognosy, — at a time long antecedent to the creation of man, the vast region, familiarly known to the present generation as Central Asia, was covered by a sea that washed the foot of a mountain range, which, at a later period, constituted the boundary lines of Afghanistan and the Chinese Empire. This pre-historic sea was spread over an area computed at 8000 square marine leagues, and extended from the Hindoo Koosh to the European shores of the Black Sea and the Sea of Asof. To this huge depression on the sur- face of the globe Sir Roderick proposed — in compliment to Hum- boldt the originator of the theory — to give the name of the Aralo-Caspian Sea, whose denizens appear to have had a purely local range, and to have been clearly distinguishable from the molluscs and other marine animals inhabiting the outer ocean. l 2 CENTRAL ASIA. At some unknown point in the latest tertiary era the barren plateau between the Caspian and the Aral Seas is believed to have been thrown up by subterranean agencies, followed, at a greater or less interval, by the upheaval of the much fabled range of the Caucasus, the Kaf of Eastern romance and the abode of that marvellous bird the Simurgh, the foe of the Deevs and the friend of man. As no traces, however, have been discovered of the junction of the Euxine with the Caspian, this theory must, to a certain extent, be regarded as rather speculative than scientific, though good grounds may exist for ascribing to volcanic phenomena the separation of the Caspian and the Aral Seas, and the upheaval of the dry lands recently comprising the Khanats of Khwarezm or Khiva, and Bokhara. It is certain that the fossiliferous limestone forming the basis of the steppes contains the identical molluscs, — the cockle, the mussel, and the spirorbis — which, according to General Abbott, still exist in the waters of those two inland seas. Nor is it less indisputable that the surface of the Aral is upwards of a hun- dred feet higher than that of the Caspian, the elevation of the rugged intervening plateau, known as the Ust Urt, averaging GOO feet above the level of the ocean. For our present purpose it may suffice to define Central Asia as the much varied region bounded on the west by the Caspian ; on the south-west by the Persian Province of Khoras- san ; on the south by Afghanistan, Kashmeer, and Little Tibet ; on the east by the Chinese Empire ; on the north by the river Irtish ; and on the north-west by the Ural river. The general aspect of this immense tract is fairly, if roughly, described by a writer in Pinkerton’s Collection : ‘ Between Great Tartary on the north, and Tibet, India, and Persia on the south, there runs a long tract of land, extending from the Great Kobi, or desert on the north-west part of China, westward as far as the Caspian Sea. This country is situated in a sandy desert with which it is GENERAL OUTLINE. 3 surrounded ; or, rather, is itself a vast sandy desert, interspersed with mountains and fruitful plains, well inhabited, and watered with rivers. Nature seems to have divided this region into three large parts, by the names of the countries of Karesm, Great Bucharia, and Little Bucharia.’ Towards the north-west, enclosed between barren rocks and arid steppes, the basin of the Aral Sea — the Blue Sea of the Russians — occupies a space 3G0 miles in length from north to south, by 240 miles in extreme breadth from east to west : equivalent to an area of 86,400 square miles. On the east and north this expanse of brackish water is surrounded by clay plains ridged by hillocks of loose drifting sand, while on the west it is divided from the Caspian by the Ust Urt, a rocky, unculturable waste, 240 miles in length by 160 miles in breadth, and rising almost precipitously from the sea, but sloping gradu- ally to the westward. It is, in fact, a continuation of the great steppe possessed by the Kirghiz Kuzzaks, and more particularly belongs to the Lesser Horde. At its south-eastern extremity it terminates abruptly in a bold escarpment some 500 feet in height, at the foot of which a level plain spreads out to an enormous distance. From this point the high land turns sharply to the west-north-west, and the angle thus formed is called by the Kirghiz, The Chink. The southern portion of the sea is extremely shallow, and swarms with small islands, whose inhabitants live chiefly upon fish, and are described as skilful boatmen venturing upon the use of sails, while the Kirghiz are content to ply the oar. The Aibugir Lake, or Gulf, at the south-western extremity of the Aral, was overgrown with canes when visited by M. Kiihlewein in 1858, although it received the Laudan, an important branch of the Amou. This gulf is stated to be eighty miles long by twenty miles broad, and appears to have been dried up at the time of the late Russian expedition, through the diversion of 4 CENTRAL ASIA. the Laudan by the Khivese for purposes of irrigation. It is only near the mouth of the Amou that the water of the Aral is drinkable, being elsewhere exceedingly brackish. Carp and a small sturgeon are caught in considerable quantities. To the Arab geographers the Aral was only known as the Sea of Khwarezm, by which name and that of the Sea of Urghunj it is still called by the people of the Khanat. Accord- ing to Generals Mouravief and Romanof, Aral Denghiz, the Kirghiz appellation, signifies the Sea of Islands, while others maintain that its proper signification is the Sea of Eagles. It was first surveyed by Admiral Alexis Boutakof, by whom also the first steamship that ever churned these waters was launched and navigated. Moved more by an abstract love of science than by patriotic considerations, the Royal Geographical Society, in 1867, presented their Founder’s Medal to that gallant officer, whose extension of geographical knowledge has been since otherwise appreciated and utilized by his own government. Although on a level with the Euxine, the Aral, as already remarked, is more than one hundred feet above the surface of the Caspian, and the Toorkomans maintain that at Kara Goombuz the waters from the one sea may be heard flowing to the other, under-ground. If it be true that such sounds are at times audible, they arc probably caused by subterranean drainage from the Amou, some portion of whose waters may follow under- ground their old course towards the Caspian. The loorkomans who dwell on the shores of the Kara Bhugaz Bay account for the remarkable current into that gulf, by the theory that the overflow of the Caspian thcnco escapes by a covert channel communicating with the Aral, the comparative elevation of the two seas being a point quite beyond their comprehension. As a scientific fact it may be stated that there is no outlet for the redundant waters of cither, and that the adjacent lands arc saved from flooding by evaporation alono. M ere it not for GENERAL OUTLINE. 5 this powerful agent of nature, the depth of the Aral, if General Abbott’s estimate may be credited, would he annually increased twenty-six inches by the influx of the Amou and the Syr, and to at least an equal extent through the snow and rain that fall on its surface or drain into it from the steppes. Although of considerable depth in the centre, the Aral is not above two or three feet deep near the southern and eastern shores, so that its waters become speedily heated under the fierce rays of the sun of Khiva. There is, besides, good reason to believe that the volume of the Amou has sensibly diminished within quite recent times, through the desiccation of many of its affluents. These again have gradually dried up through the decrease of the glaciers in the high mountains, observed by M. Semenof, and through the neglect of their channels due to the diminution of the agricultural population by incessant strife and bloodshed. It is in this manner that eminent geographer accounts for the drying up of the branch of the Amou which formerly turned off to the south-west and fell into the Caspian, for he holds to the opinion that even at that time the main channel of the river proceeded in a northerly direction to the Aral.* * The late Colonel Romanof wlio was on the personal staff of the Grand-Duke Nicholas Constantinovitch during the recent campaign, made some very per- tinent remarks on this subject in one of his interesting letters headed ‘On the way to Khiva ! ’ ‘ The station of Katty Kul,’ he says, ‘ was founded near a sweet-water lake, which is now completely dried up, and the supply of water is obtained from a well eight versts from the station. The transformation of sweet water into salt, and the desiccation of the latter, are very remarkable and constantly re- curring phenomena in all the steppes of Central Asia. Within the memory of many the water in the rivers Irghiz, Turgai, Sarysu, and others was fresh, but now it has a bitter salt taste. The site for the recently-constructed fort of Lower Emba was chosen on Lake Masshe, chiefly because its water was fresh. When the fortress was built the lake became salt, so that now the garrison have to procure their supply of water from wells in which the water is brackish. The gradual, but very perceptible, diminution of the lakes and other water- basins of Central Asia, arising from the excessive dryness of the climate, is 6 CENTRAL ASIA. The historians of Alexander the Great make no mention of the Aral, nor does any allusion to it occur in the pages of any classical writer until early in the second part of the fourth century of the Christian era, when Ammianus Marcellinus speaks of two rivers that rushed down headlong from the mountains, and, descending into the plains, commingled their waters and formed the Oxia Palus. In Dr Smith’s Dictionary of Greek and Roman Geography, however, it is suggested that the Oxia Palus is identical with the Karakul Lake, which is now the termination of the Kohik, or river of Samarkand. Both Herodotus and Strabo appear to have had some knowledge of a series of lagoons watered by the overflowing of the Jaxartes, which was supposed by most early writers to empty itself into the Caspian some 80 parasangs from the mouth of the Oxus. The Aral, when first recognized as something more than a region of pools and swamps, was regarded as the extreme eastern portion of the Caspian, which was thought to communicate, by a long narrow strait, with the Northern Ocean. Sir Henry Rawlinson rejects Humboldt’s theory — adopted by Sir R. Murchison — of the Aralo-Caspian Sea that once filled the entire concavity of Turan, extending to the Black Sea, the Northern Ocean, and the Balkash Lake. Briefly, Sir Henry maintains that from n. c. 600 to a. r>. 500, that is, for a period of 1100 years, both the Oxus and the Jaxartes emptied them- selves into the Caspian, and that the Aral did not then exist as an inland sea. Even so late as a. i>. 570, when Zomarchus, the Byzantine envoy, was returning to the west from the encamp- ment of the Khakhan at the foot of the Ak-tagh, or "White an undoubted fact, and can be proved by the division of the large Lake of Alakul into three smaller basins, the separation of Lake Chelkar-Tenghiz, which reoeives the water of the Irghiz, f. oin the bay of the Aral Sea, Sary- Chcganak, with which it was at one time united, and many other instauccs of a similar kind which have occurred in the steppe.’ GENERAL OUTLINE. 7 Mountains, to the north of Samarkand, the Aral was only entitled to the appellation of a reedy marsh, though some thirty years afterwards the Oxus may have ceased to fill its western branch, and have kept to its direct northern channel. About that time the Sea of Kardar, or south-western portion of the Aibugir Lake, which had hitherto been fed by the Urghunj branch, became dried up, and exposed to view the ruins of a treasure city submerged in a remote age. According to Persian traditions these ruins were successfully excavated and rifled for a period of twelve years, and are placed by General Abbott, under the name of Berrasin Gelmaz, in a small island, though Admiral Boutakof fixes the locality of ‘ Barsa Kilmesh ’ in a salt marsh a little to the west of the Aibugir Lake. For the next 600 years the Aral is described by the Arab geographers in terms that might be applied to it at the present day, though between the ninth and twelfth centuries three suc- cessive capital cities, situated at the apex of the Delta, were destroyed by sudden floods. The course of the river, too, was constantly shifting, according to the greater or smaller quantity of water diverted from the main channel for purposes of irrigation. In a. d. 1221, — Sir Henry continues, — Octai or Okkadai Khan, the son of Chinghiz Khan, when besieging Urghunj, broke down the dam that regulated the flow of the waters, and directed the full force of the stream against the walls of the town, which, being built of clay, were speedily undermined and swept away ; about three years later the Oxus again forced its way to the Caspian, and the desiccation of the Aral commenced at the same time. The elder Poli travelled from the Volga to Bokhara about 1260 a. d., by a route which must have taken them across the Aral, but that sea is not once mentioned by Marco Polo. Again, in 1330, Hamdullah Mustowfi describes the Amou as flowing from Hazarasp, a town about 40 miles south-east of the 8 CENTRAL ASIA. modern town of Khiva, by the Muslim Pass and Kurlawa to Akricheh on the Caspian, near the mouth of the Attrek, — traces of which course were seen by General Abbott in 1840. The same geographer remarks that, owing to the divergence of the Amou in the previous century, the level of the Caspian was sensibly raised, and that the post of Aboskun at the mouth of the Attrek was consequently overwhelmed. During the whole of the 14th century the entire volume of the Amou was poured into the Caspian, while the Jaxartes, or Syr, lost itself in the sands of the desert, but early in the loth century an anonymous writer, whom Sir Henry Kawlinson suspects to have been Shah Kokh’s minister, — and whose manuscript he obtained at Herat, — speaks of the Aral as being dried up, through the drainage into the Caspian of the waters of the Jyhoon and Syhoon, the names given by Mohammedan geographers and historians to the Oxus and Jaxartes. So far back as the middle of the 13th century the Franciscan Friar, 'William de Kubruquis, states that the Jaxartes, after creating numerous swamps, was lost in the desert, and about the 3 r ear 1340 Pegoletti advises travellers bound for Tatary to leave Urghunj to their right, and to strike straight across from Saraichilc on the Yaik, or Ural river, to Otrar on the Jaxartes, a route that would traverse the bed of the Aral : nor does that sea appear in the Catalan map of 1375. In short, the existence of the Aral Sea depends upon its two great tributaries, the Amou and the Syr. When the former is deflected, the bed of the sea contracts, and the Syr, being no longer able to force its way to the receding shores, becomes absorbed in reedy marshes. There can bo no doubt that in ancient times tho main branch of the Oxus disembogued itself into tho Caspian, for both Strabo and Pliny tell us how the merchandise of India was conveyed across the mountains to a stream that flowed into t lie Oxus, how it descended that river to the Ilyrcanian or Caspian GENERAL OUTLINE. 9 Sea, how it was taken across to the mouth of the Cyrus, — now the Kur, — which it ascended until it could be carried across to the Pliasis, — the modern Rion, — down which it dropped till it reached the Euxine, whence it was transported to the various countries of Europe. In those days the Oxus was known as the river that divided Bactria from Sogdiana, and it plays a con- spicuous part in the campaigns of Alexander the Great, whose troops, in pursuit of Bessus, crossed it on inflated skins stuffed with straw. The name is an obvious Greek corruption of Wakhsh, a small state lying between the Karategeen range and the petty principality of Darwaz. By the Mohammedan * invaders it was called simply Al-Nalir, or The River, and the country to the eastward Mawaralnahr — the Maverulnere of the ‘ Arabian Nights/ — signifying Transamnia, corresponding to the modern Transoxiana. Their writers, however, adopting the fable that the Garden of Eden was placed at the head of the Badakhshan valley, and imagining that the sources of the Jaxartes were near those of the Oxus, confounded these rivers with the Mosaic Gihon and Pison, and corrupted those names respectively into Jyhoon and Syhoon. To the Oozbegs the Oxus is known as the Darya-i-Amou, or the River of Amou, while the Khivese, according to General Mouravief, call it the Amin Darya, and the Persians, if Mr Bell be a sufficiently good authority, the Ab-telah, or "Water of Gold, in allusion to its auriferous sands. Ibn Haukal, who wrote in the 10th century, speaks of the J yhoon as flowing into the Sea of Khwarezm — the Aral — which was in no way affected by the rivers it received into its basin, the redundant waters being carried off to the Sea of Khozr by a secret communication. He adds that in the lower, or northern, part of its course it was covered every winter with such thick * Hiouen Tsang gives Potsou as the Chinese equivalent, while in the old Zoroastrian books it appears as the Veh-rood, and in Sanscrit as Yauksou. 10 CENTRAL ASIA. strong ice that loaded carts were driven across from one bank to the other. At the commencement of the 15th century the Portuguese ambassador, Puy Gonzalez de Clavijo, alludes with reverence to the Yiadme, as he calls it, and describes it as one of the rivers that descended from Paradise. It attains, he says, a league in width, and traverses a flat country with great and wonderful force, until, at last, it reaches its goal in the Sea of Baku — one of the many names of the Caspian. Its muddy waters, he continues, are lowest in the winter season, when its sources in the mountains are congealed, hut in April the melt- ing snows begin to fill its broad, deep bed, and for the next four months it is a noble river. In 1558, Anthony Jenkinson, the shrewd and adventurous representative of the London 1 Muscovy Company/ mentions, that on the 5th October he * struck ’ a gulf of the Caspian — though it is far more likely to have been the Aibugir Gulf of the Sea of Aral — where the water was fresh and sweet. ‘ Note/ he continues, * that in times past there did fal into this gulf the great river Oxus, which hath his springs in the mountains of Paroponisus in India, and now cometh not so far, but falleth into another river called Ardock, which runneth toward the North, and consumeth himself in the groundc, passing under- grounde above 500 miles, and then issueth out againe, and falleth into lake of Kitkay/ A little further on he attributes the desiccation of the Oxus to the numerous canals of irrigation it had to supply, and complains that ‘ the water that servetk all the countrey is drawen by ditches out of the river Oxus, unto the great destruction of the said river, for which cause it falleth not into the Caspian Sea as it hath done in times past, and in short time all the land is like to be destroied, and to become a wilderness for want of water when the river of Oxus shall fade/ Six or seven weeks later, he says, he crossed the great and rapid river Ardock, a branch of the Oxus, running 1000 miles to the GENERAL OUTLINE. 11 northward, — for half of that distance passing under-ground, then issuing from beneath the earth’s surface and terminating in ‘ the Lake of Kitay.’ It is not a little singular that Jenkinson should make no allusion to the Aral as the recipient of the river he calls the Ardock, which could be no other than the main channel of the Oxus, and which some later writers designate as the Khesel or Kizil, that is, the Red River. In Pinkerton’s Collection the Khesel is said to take its rise in the mountains to the north- east of Sogdiana, and to fall into the Aral 50 or GO miles after receiving the Amou. The writer has here evidently confounded the source of the Amou with that of the S} r r, but he goes on to explain how the Khesel, which formerly fell into the Caspian at St Peter’s Bay, was in 1719 diverted from that channel by the Tatars, in the hope of destroying by thirst the expedition commanded by the gallant but ill-fated Prince Beckovitch. The Dutch Orientalist Bentinck, in his notes to the ‘ Ilistoire Genealogique des Tatares ’ — published in 1720 — describes the Oxus as bifurcating about 40 leagues from its embouchure ; the left arm turning off to the Caspian, while the right arm, which 80 years previously flowed under the walls of IJrghunj, then fell into the Kizil, to the ruin of that once flourishing city, and so passed on to the Aral. Jenkinson’s confusion is no doubt attributable to his own ignorance of Persian and Toorkee, and consequent dependence on the intelligence and good faith of his interpreter. That the Oxus did at one time, perhaps at several times, empty itself into the Caspian is a fact that cannot be disputed. The unfortunate Conolly proceeded for some distance up the deserted bed, whose width he estimated at 2000 paces, and General, then Captain Mouravief, met with verdure, reeds, and pools, along the deep broad channel excavated by the mighty river, which seems to have finally divided into two branches 12 CENTRAL ASIA. inclosing the present peninsula of Dardji. According to the latter writer the Syr formerly effected a junction with the Amou, but an earthquake, which is said by the Khivese to have happened in the 14th century, separated the two rivers and gave them each the course they now hold. This earthquake is a very questionable event, though it is mentioned also by Baron Meyendorf as an item of Khivese faith, hut he adds that others assert that the south-western channel was dammed up in 1670 to check the ravages of the Kuzzaks. About the middle of the 18th century Captain TVbodroofe, while engaged in surveying the Caspian, under Captain Elton’s orders, by desire of Nadir Shah, was informed that ‘ it is now a hundred years since the Oxus emptied itself into the upper end of this (Balkan) Bay/ and he adds that, the river drj’ing up in many places through the intense summer heat, the Toorkomans had imagined that by closing the mouth they would retain the water in the channel. The result, however, proved contrary to their expectations, for the river, having no longer any current to clear away the sand that was continually being blown into it, became choked and gradually silted up altogether. This version is adopted also by M. Khanikof, who mentions, in addition, the construction of a second dam to the eastward of Kunya or Kdhne UTgliunj, which effectually turned the Amou to the north. General Abbott’s theory is probably as near the truth as need be desired. The natural course of the Oxus, he says, would be to the Aral, but at some remote period it must have encountered an obstacle that deflected its waters through the easier country lying to the westward. At the same time it never ceased battering the barrier which opposed its proper course, until at length a breach was effected, when it rushed straight onwards to the Aral. General Abbott is further ot opinion that many centuries ago the Syr and the Amou met a GENERAL OUTLINE. 13 little to the north of Urghunj, and that while a small portion of the out-pourings of the former river found its way to the Aral swamp, the main volume rolled on with its sister stream to the Caspian. By degrees, however, the Syr worked out a straight channel for itself to the north-west, while the Amou, relieved from the shock that sent it off to the south-west, also excavated a way to the northward, and thus in the end both rivers separately disembogued themselves into the Aral, as in ancient times they had conjointly deposited their waters in the bed of the Caspian. The old channel of the Amou is still the natural drain of the Kara-koum desert, so that, as already observed, it may not be impossible that the sound of subter- ranean waters may be heal’d at Kara Goombuz. The Oxus, or the Amou, takes its rise in the Pameer Steppe, the loftiest table-land in the world, and known to the people of Central Asia as the Bam-i-Dunya, or the flat, or terraced, roof of the world. The northern branch, issuing from Lake Sir-i- Kul, has been generally accepted as the father of the stream, though the southern branch issuing from the Pameer Kul appears to be somewhat the longer of the two. The northern branch passes by the specific name of the Panja, and on quitting the lake is barely ankle deep, though 15 feet wide, and running at the rate of 3| miles per hour over a smooth bed. It tends at first in a south-west direction as far as Hissar, where it effects a junction with the Bara Sarhad, the southern branch that flows from the Pameer Kul. From this point it pursues a westerly course to Ishkashm, where it turns suddenly to the north, inclosing in the angle thus formed the once celebrated ruby mines of Badakhshan. Bending north- west-by-north, and then towards the south, it forms nearly a semi-circle, receiving three affluents — the Shakh-dara, the Bartang, and the Surk-ab, or Red River — until it reaches the point where it is joined by the Kokcha, nearly due west from the mouth of the Shakh- 14 CENTRAL ASIA. dara. It then proceeds to the westward to the ferry of Khoja Saleh, where it turns to the north-west-by-west to about the 40th degree of latitude, after which it flows nearly due north and falls into the Sea of Aral through many mouths. The entire length of this historic river may be roughly com- puted at 1200 miles. From the head of the Delta, which is about 50 miles from its embouchure, the Amou is navigable to Kunduz, a distance of 750 miles. According to Sir Alexander Burnes, the channel is straight and singularly devoid of rocks, rapids, and whirlpools, and rarely impeded even by sand-banks. The depth varies from 6 to 20 feet, with an average current of 3 j miles an hour. It is, however, subject to floods from melting snows, when the water becomes of a reddish hue and is laden with silt, that is finally deposited in the Aral. Above the junction of the Kokcha, and below the town of Khiva, the Amou is frozen every year, and in severe winters even while traversing the desert. The fertilizing influence of this noble stream does not at present extend further than a mile from its banks, until it reaches the Khanat of Khiva, after which a somewhat broader belt is brought under cultivation. In 1832 there were not above 200 boats throughout the entire course of the river from Kunduz to the sea. These boats are described as measuring 50 feet in length with a beam of 18 feet, and capable of a burden of 20 tons or of conveying 150 troops or passengers. They are the same at both ends,, flat-bottomed, about four feet deep, and drawing only twelve inches of water. Their construction is extremely rude. They are built of squared logs of a dwarf jungle-tree, fastened together with iron clamps. Though clumsy, they are strong and durable, and both Tirnour and Nadir Shah succeeded in making with them bridges, over which their vast hosts passed in safety. ‘ The Oxus/ observes Sir Alexander Burnes, ‘ presents many GENERAL OUTLINE. 15 fair prospects, since it holds the most direct course, and con- * nects, with the exception of a narrow desert, the nations of Europe with the remoter regions of Central Asia.’ These lines were written in the pre-railway era, and in any case evince more enthusiasm than foresight. From Badakhshanto Pitniak, a border town of Kliwarezm, — a distance of 540 miles, — there is not a single place of aDy importance within sight of the river. The settled population shuns the sultry valley, and it is only at ferries and the intersections of caravan routes that even villages are to be met with. * AVhen we also consider,’ remarks M. Yeniukof, * that the shores of the Sea of Aral are so barren as to have defied all the attempts hitherto made of founding even a small settlement on them; that the Aral itself is separated from Russia by intervening steppes 530 miles broad; and lastly, seeing the utter impossibility of modifying the character of the Nomad marauders, we shall be justified in asserting that even in the remote future the Oxus can only be a secondary channel for the advance of industry and civilization.’ It is not improbable indeed that the Amou will lose much of its importance now that Central Asia has practically passed into the hands of Russia. So far as the trade with India is concerned, a long overland route can never hope to vie with the direct communication between Bombay and Odessa opened up through the Suez Canal, while the Afghan market is rather of political than commercial significance. Russian enterprise is far more likely to find for itself a profitable field in the com- mand it has acquired of the old caravan route from the Caspian Sea to China, and it is only in the event of an actual collision between the British Government and that of St Petersburg that the valley of the Oxus may be expected again to be in men’s mouths familiar as a household word. Eor some centuries past it has ceased to be an object of interest to any European public, but for all that, to quote Mr Matthew Arnold, 16 CENTRAL ASIA. *. . The majestic river floated on, Out of the mist and hum of the low land, Into the frosty starlight, and there moved. Rejoicing, through the hush’d Chorasmian waste. Under the solitary moon : he flow’d Right for the Polar Star, past Orgunje, Brimming, and bright, and large : there sands begin To hem his watery march, and dam his streams. And split his currents ; that for many a league The shorn and parcell’d Oxus strains along Through beds of sand and matted rushy isles — Oxus, forgetting the bright speed he had In his high mountain cradle in Pamere, A foil’d circuitous wanderer : till at last, The long’d-for dash of waves is heard, and wide His luminous home of waters opens, bright And tranquil, from whose floor the new-bathed stars Emerge, and shine upon the Aral Sea.’ The ‘ dash of waters ’ must he taken as a poetical licence, for the Aral at the mouth of the Amou is but a shallow, isle- bespangled mere. According to Admiral Boutakof, who care- fully surveyed the Oxus Delta as well as the Sea of Aral, the river first bifurcates between Kipchak and Khoja-ili, and shortly afterwards divides into several branches, or rather into a net- work of lagoons. * The centre part of this portion of the basin forms a sort of depression into which the waters of all the branches, excepting the westernmost, empty themselves in a scries of lakes, overgrown more or less with reeds ; out of these they again flow off in separate channels, discharging themselves into the Sea of Aral.’ The Delta lies between the two main branches, the Laudan to the westward, and the Kuvan Jarma to the eastward, other- wise called Kuk or Blue River, and lower down the Yangy-Su, or New River. The Laudan where it creeps into the Aibugir Lake is not above 18 inches deep, flowing with a feeble current through a thick growth of reeds, and with so firm a bottom GENERAL OUTLINE. 17 that a caravan of 1500 camels has walked across without diffi- culty. To check the inroads of the Yomut or Yamood Toorko- mans, the Khivese erected a fort near Bent, and constructed a dam across the upper portion of the stream, which has been more than once destroyed by their implacable tormentors. The extreme eastern branch, again, fills the lakes Dankara and Tampvne-Ayage and then, as the Yangy-su, flows into the Tushe-bas bight of the Aral, opposite Ermolof Island. The Yangy-su is pronounced by the Kirghiz as Jangy-su, and is consequently sometimes confounded with the Jan-i-Darya, a branch of the Syr that loses itself in the sands. In 1848-19, this was the principal outlet of the Amou, so that the water at Ermolof Island, more than nine miles distant, was quite fresh, whereas ten years later the water close in shore had become uu- drinkably salt owing to the drying up of the Yangy-su. Of the intermediate streams the most important are the Ulkun Darya and the Taldyk, but even these are not three feet deep in July, and are of course still shallower before the melting of the snows at the end of March. The frequent changes in the course of these various branches were exemplified by the sub- merged fields and artificial watercourses which Admiral Bouta- kof observed over the side of his boat, while traversing several small lakes. For at least 50 miles from its mouth the Amou is wholly unfit for navigation, but by closing some of the minor channels the Russians expect to deepen the Ulkun Darya suffi- ciently to keep open a constant communication with the town of Kungrad. Though in every other respect inferior to the Amou, the Syr Darya — the Syhoon of the Arab geographers — is likely to exercise a more direct influence in civilizing Central Asia after the Russian standard. In classical times this river was known as the Jaxartes, mistaken, in wilfulness or ignorance, by Alex- ander’s flatterers for the Tanais or Don. Pliny declares that ■i 18 CENTRAL ASIA. its Scythian name was the Silis, while in Bell’s Notes to Rollin’s Ancient History it is asserted that Jaxartes is a corrup- tion of Ik Sert, or the Great Paver, and that the Sarts were the people who originally dwelt on the banks of the Sort, and were identical with the Abii — from ah, a river, — who sent envoys to Alexander the Great on his reaching the Jaxartes. These Abii are, of course, not to be confounded with Homer’s Thracian Abii, who lived upon mares’ milk and were famed for their love of justice. The Chinese equivalent seems to have been Ye, while the modern appellation signifies the Yellow River. The town of Cyreschata, or Cyropolis, was constructed by Cyrus the Great on the left bank of the Jaxartes, which formed the northern boundary of his empire. Imprudently crossing the river and invading the country of the Massagetac, he lost his army and his life at the hands of their warlike Queen, Toinyris. The same great monarch is said to have built six other cities along the course of the Jaxartes, all of which were destroyod by Alexander, who founded in their place Alexandreia Ultima, probably near the site of the modern Khojend. Ancient writers, as already remarked, made the Jaxartes fall into the Caspian, which it may possibly have done after uniting its waters with those of the Oxus. Strabo, however, deflects one embouchure to a point about 80 parasangs distant from that of the Oxus, and sends all the other channels to the Northern Ocean. The Syr Darya properly begins at the confluence of the Naryn and the Gulishan not far from the town of Namangan. The former rises ont he southern face of the Kirghiz Ala-tagh, and, winding through six degrees of longitude, rushes impetu- ously through the Ferghana valley, swollen by many tributaries. The Gulishan, again, issues from the Chatyr Ivul, and is inferior to the Naryn both in length and in volume. Their united streams, under the name of the Syr Darya, flow a little to the GENERAL OUTLINE. 19 soutli of west until reaching Koshtecrmen below Khojend, where they turn off suddenly to the northward as far as llazret. From this point to Yany Kurgan the Syr runs in a north- westerly direction, and thence holds on to the westward until it discharges itself’ into the Aral near the north-eastern extremity of that sea. During the latter part of its course the Syr Darya receives no tributaries, and its volume is sensibly diminished in crossing the desert. Its total length from the source of the Naryn is estimated at 1200 miles. Below Baildyr Tungai, which is 538 miles above Fort Perofski, the Syr is a noble river, from 300 to 800 yards in width and varying in depth from 18 to 30 feet. It flows between steep clay banks which are often flooded at certain seasons of the year, while its current is computed at from 3 to 4 jennies per hour, according to the period of the day, — for it runs with the gi-eatest strength between ten and eleven in the morning, when it decreases in velocity till two in the afternoon, about which time it recovers its former force and rapidity. The steamers which descend at the rate of six to ten miles in the hour are content to mount the stream at one-third of that speed. At no great distance from its mouth the Syr spreads out into a marshy brackish delta, not above four feet deep in mid- channel and diminishing to a width of 360 feet in the main stx-eam. On both sides a vast plain of grass, or rushes, stretches out far and wide. In 1863 Admiral Boutakof ascended the river as high as Baildyr Tungai, and two years later steamers ascended even to Kamangan. That gallant Admiral is said to have surveyed and mapped the Syr for one thousand miles from its embouchure. According to Captain Meyer the course of the river is persistently shifting more and more to the northward, owing to the slow but continuous rising of the land to the south. 20 CENTRAL ASIA. Throughout the steppe beds of ancient rivers may be traced, while semi-fossilized oceanic molluscs occur in masses, showing that the Aral itself has largely receded from its former limits. Sometimes it happens that a tribe dams up a channel to injure an unfriendly neighbour or rival, and straightway all cultiva- tion ceases, and fields and meadows become an arid waste. Not many years since the main channel of the Syr was the Kuvan Darya, which now stops short in a marshy lake near Khoja Niaz, a hundred miles from the Aral. The present main stream is excessively tortuoxxs between Fort Perofski and Fort 2, and the water has sunk so low that it is navigable for rather less than three months in the year, for vessels drawing three feet of water. It has already been mentioned that the earlier Greek writers regarded the Caspian Sea as a Gulf of the Northern Ocean. Ptolemy, however, observes : ‘ The Ilyrcanian Sea, called also the Caspian, is everywhere shut in by the land, so as to be just the converse of an island encompassed by the water.’ By Ibn Haukal it is named the Sea of Khozr, while to the Muscovites it was originally known as the Sea of Kwalis, that being the name they applied to the tribes dwelling near its shores. In the 14th and 15th centuries it was called the Sea of Baku, from the chief port on the western coast, while Abu’l-Ghazee Khan alludes to it in the 17th century by its Persian appellation of the Sea of Kulsura. It was first navigated by Patroclus, the Admiral of Seleucus and Autiochus. The historical associ- ations connected with this sea will, however, be described in a subsequent chapter. The water appeared to General Abbott as being ver}’ salt, but not bitter, and as clear as crystal. The sea lies in a basin of fossiliferous limestone, the eastern shores being low and swampy, but at the north-eastern extremity precipitous cliffs rise almost out of the water to the height of 700 feet. There GENERAL OUTLINE. (V I are no tides, but, as Jonas Ilanway remarks, ‘a prodigious current and confused sea ’ often result from a sudden change of the wind after it has been blowing for some time from the northward. The Caspian Sea is about 640 miles in length from north to south, and from 100 to 200 miles broad. In the centre it is deep, but shallow at the sides, and, although it receives the waters of eighty-four streams in addition to the stupendous discharge of the Volga, it has no outlet, and preserves its level solely by evaporation. Conjointly with the Aral, it drains an area 2000 miles in length from the sources of the Volga to those of the Syr, and 1800 miles in breadth from the head- streams of the Koanna in North Hussia, to those of the Sefid Rood in Koordistan. The smaller rivers, the lakes, the mountains, and the deserts of Central Asia, will each be described in connection with the countries or provinces to which they respectively belong. 22 CENTRAL ASIA. CHAPTER II. EARLY HISTORY. EARLY INHABITANTS— SCYTHIANS — UNDER DARIUS AND XERXF.S — MOUNT IMAUS — MARGIANA — BACTRIA — SOGDIANA — ALEXANDER'S CAMPAIGNS — SIKUNDER ZULKARNAIN — THE GRECO-BACTRIAN KINGDOM — THE PAR- TIIIANS — THE SCYTHO-CHINESE DOMINATION — THE SASSANIDES — ARDE- SHEER, HORMUZ, FEROZE, KOBAD, NOUSHEERWAN, KHOSROO PURVEZ, YEZDIJERD — ARAB CONQUEST — JUSTINIAN AND DIZABULCS — EMBASSY OF ZEMARCHUS. In Canon Rawlinson’s edition of Herodotus, excellent reasons are given for regarding Armenia as the cradle of the Aryan race. At some very remote period three kindred streams of migration are supposed to have issued, perhaps contemporaneously, from their common source, and to have flowed, one to the northward across the Caucasus, a second in a westerly direction across Asia Minor into Europe, while the third turned to the south-east and stopped only at the Indus. After a time this last-mentioned branch became straitened for space, and, in the 15th century be- fore the Christian era, divided into two floods of emigration and conquest, the one gradually spreading over Hindostan, and driv- ing the Turanian aborigines into the mountains, while the other crossed the Hindoo Koosh and subjected or expelled the Scythian or Turanian races known as Sogdians, Bactrians, Arians (of Herat), Ilyrcanians, Arachosians, and people of Ilagiana and Media Atropatcne, the Modem Azerbijan : here, too, the ab- original inhabitants fleeing into the mountains and deserts. Turanian dialects prevailed from the Caucasus to the Indian Ocean, from the Mediterranean to the Ganges, and perhaps EARLY HISTORY. 23 throughout the whole of Asia. Even now they are spoken ‘ by all the various races which wander over the vast steppes of Northern Asia ancl Eastern Europe ; by the hill tribes of India, and by many nat ions of the Eastern Archipelago.’ This Turanian or Scythic element was still strong in the time of ITerodotus. To that stock belonged the Sacse, the Parthians, the Asiatic Ethiopians, the Colchians, the Sapeiri, the Tibareni, and the Mosclii. Closely allied, too, were the Armenians, the Cappado- cians, the Susianians, and the Chaldmans of Babylon. The race, however, is now extinct. ‘In vain we look for their descendants at the present day. * * The Seyths have disappeared from the earth. Like the American Aztecs, whom tliej r resembled in some degree, they have been swept away by the current of immigra- tion, and, except in the mounds which cover their land, and in the pages of the historian or the ethnologist, not a trace remains to tell of their past existence,’ — though some writers have too hastily confounded the Scythians with the Mongolians, attribut- ing a like origin to both. The empire of Darius Ilystaspes — the Gushtasp of Firdousi — was divided into 20 satrapies, of which the Fifteenth com- prised the Sacac and the Caspians, whose joint tribute amounted to 250 talents per annum, while to the Sixteenth belonged the Parthians, the Chorasmians, the Sogdians, and the Herat Arians, whose annual tribute was 300 talents. The army of Xerxes — • the Isfundear of Firdousi — was largely recruited from the war- like peoples of Central Asia. ‘ The Bactrians went to the war wearing a head-dress very like the Median, but armed with bows of cane, after the custom of their country, and with short spears. The Sac®, or Seyths, were clad in trousers, and had on their heads tall stiff caps rising to a point. They bore the bow of their country and the dagger ; besides which they carried the battle-axe, or sagaris. They were, in truth, Amyrgian Scythians (from the confines of India), but the Persians call 24 CENTRAL ASIA. them Sacte since that is the name they give to all the Scythians. The Bactrians and the Sacae had for leader Ilystaspcs, the son of Darius and of Atossa, the daughter of Cyrus. The Arians (of Herat) carried Median hows, but in other respects were equipped like the Bactrians. The Parthians and Chorasmians, with the Sogdians, the Gandarians, and the Dadica?, had the Bactrian equipment in all respects. The Caspians were clad in cloaks of skin, and carried the cane bow of their country, and the scymitar.’ The Bactrians and the Caspians furnished also horsemen, armed like the foot-soldiers. From Canon Rawlinson’s foot-notes we learn that the Ilyr- canians, an Arian race, probably inhabited the lovely and well- wooded valley of Astrabad, watered by the river now known as the Gurgan. The Caspian, as mentioned in the preceding chapter, was called the Ilyrcanian Sea by the historians of Alexander, and in the Zendavesta this district appears under the name of Vehrkana, the Urkanieh of the 13th century. The Parthians dwelt between the Hyrcanians and the Sarangians, along the southern flank of the Elburz mountains, now called Atak, or ‘ The Skirt.’ The country is at present almost a desert, but covered with extensive ruins, attesting its ancient cultivation. The Parthians were of Scythian origin, and escaped destruction by the Aryans no doubt through the natural diffi- culties of their position. The Chorasmians, again, were an Aryan people, inhabiting the oasis of Khwarezm, or Khiva, — the Khairizas of the Zendavesta. In Alexander’s time they seem to have been independent, and to have been governed by a native ruler, named by the Greeks Pharasmenes, who dis- patched a friendly embassy to the ‘ Macedonian madman.’ The Sogdians also came from the Aryan stock. Their country, the Cugdha of the Zendavesta and known to Mohammedan writers as tho Yale of Soghd, extended from the Jaxartcs to the Oxus, and southward to Bactria. Their capital city Murueanda will EARLY HISTORY. hereafter be mentioned in connection with Alexander. The Apeun of ITerodotus occupied the rich valley of the Ileri- Rood, which is designated Ilariva in the inscriptions of Darius. In the Greek legends of the Assyrian era, no nation is more favourably distinguished than that of the Bactrians, whose apocryphal king Oxyartes is described as valiantly holding his own against Kinus, though finally compelled to yield to the superior arms and fortune of Semiramis. It is certain that the Ar}-ans settled in this province at a very early period, and it is not impossible that Bactra may have been the capital of Persia at a time anterior to the reign of Kei Khosroo, or Cyrus the Great, who experienced considerable difficulty in reducing the Bactrians beneath his sway. In the Hindoo legends of the 3rd and 4th centuries before the Christian era, they appear as the Bahlikas, afterwards easily corrupted into Balkh, the modern representative of Bactra. A less easy task is it to place the Sacac of Herodotus, unless they lined the banks of the old channel of the Oxus. They have certainly nothing in common with the Sacia of Ptolemy, which rather corresponds with the provinces of Kashgar and Yarkund. Of Turanian origin, they were famous for their valour, and in Alexander’s time fought as allies under the banner of Darius. A century later the Sacae, in conjunction with kindred tribes of Tatars, overthrew the short-lived Greco- Bactrian kingdom, and occupied the entire region between the Aral and the Indus. They even crossed that river, but sus- tained a signal repulse about b. c. 56. They were subsequently conquered by the Parthians, and finally absorbed by the Sas- sanides. Of the Caspians it may suffice to say that they were the ancient inhabitants of the provinces now known as Ghilan and Mazanderan ; while the Dadicae, it is suggested, may have been the ancestors of the Tats or Tajeeks, and may have 2G CENTRAL ASIA. emigrated across the Hindoo Koosh from their early settle- ments beside the Gandarians. The ancients, it may be briefly added, divided central and eastern Asia into Scythia-extra-Imaum and Scythia-intra- Imaum, the latter comprising Khiva, Bokhara, Khokan, Eastern Toorkestan, and Badakhshan. Their idea of Mount Imaus, however, was as imaginative as Baron Humboldt’s description of the Bolor range, which is supposed to have been identical with the former. The name is clearly derived from the Sanscrit Himavat, — Lafine ‘ hiems ’ — which is still preserved in the modern Himalaya. The Bolor mountains, as designed by Humboldt and Carl Ritter, would form the meridianal axis of Central Asia, and from their point of view is correctly enough described in Dr Wm Smith’s Dictionary of Greek and Roman Geography, where the Bolor range, — assumed to be the ancient Imaus, — is pronounced to be ‘ one link of a long series of ele- vated ranges running, as it were, from south to north, which, with axes parallel to each other, but alternating in their locali- ties, extend from Cape Comorin to the Icy Sea, between the G4th and 75th degrees of longitude, keeping a mean direction of S.S.E. and N.N.TV.’ Since Humboldt’s theory was first propounded, it has been ascertained that his Bolor Dagh is not a chain of mountains, but an extremely elevated plateau, fully 16,000 feet above the level of the sea, intersected by ridges running from east to west, with open stony plains between, broken by gorges and fissures in which both wood and water are found. Mount Imaus was, however, a westerly prolongation of the Hindoo Koosh, or, rather, of the Himalaya. In the latter half of the 4th century before the Christian era Central Asia, as known to the Greeks, was divided into the three provinces of Margiana, Bactria, and Sogdiana. The first corresponds with Khorassan and the south-eastern portion of the Khanat of Khiva ; the second with Badakhshan ; and tho EARLY HISTORY. third with the Khanat of Bokhara eastward of the Amou. The fertility of Margiana has been the subject of warm eulogies, Strabo affirming that it was no uncommon thing to meet with a vine, whose stock could hardly bo clasped by two men with outstretched arms, while clusters of grapes might be gathered two cubits in length. The chief town, since famous as Mcrv or Merou, was called Alexandreia after its great founder, but falling into decay was rebuilt by Ant ioch us Soter, and named after its resforer. It stood upon the banks of the Margus, — ‘the Epardus of Arrian, and now the Murghab, — and was finally destroyed towards the close of the last century by Shah Moorad Keg, Khan of Bokhara.* Bactria, or Bactriana — the Ninth Satrapy under Carius Ilystaspes — was a rich and populous district, bounded on the south by the ruropamisus range, on the east by the Pameer Steppe, on the north by the Oxus, and on the west by a desert separating it from the fertile province of Margiana. The Paropamisus mountains, called by Ptolemy the Paropanisus, were unknown to the Greeks previous to the Asiatic conquests of Alexander the Great, and were then supposed to be a con- tinuation of the Taurus or the Caucasus. They appear to cor- respond with the modern Hazaret branch of the Himalayas and extend for 400 miles from the site of Herat to the eastward, and are inferior in elevation to the chain that takes its name from its highest peak, the Hindoo Koosh, being covered with snow for no more than four months in the year. They are, in * The natural beauties of this once charming district, the scene of Moore’s ‘Veiled Prophet of Khorasan,’ have been fitly celebrated by that poet : — ‘ In that delightful Province of the Sun, The first of Persian lands be shines upon. Where all the loveliest children of his beam, Plow’rets and fruits, blush over every stream. And, fairest of all streams, the Murga roves Among Merou’s bright palaces and groves.’ 23 CENTRAL ASIA. truth, not so much a chain as a confused mass of barren and rugged mountains 200 miles across from north to south at the base line. The Paropamisan Alexandreia stood at the southern foot of the Bamian Pass, and was intended to secure an un- molested passage into Bactria. In addition to its northern boundarj’, the Oxus, this district was fertilized by five tribu- taries of that noble river, and by the Bactrus, now the Dahash, descending from the Paropamisus and passing under the walls of Bactra — the Zariaspa of Strabo and Pliny — but better known by its modern appellation of Balkh.* The country generally is so graphically described by Quintus Curtius that no apology need be offered for transcribing John Brende’s quaint transla- tion of the passage : — ‘ The nature of the soyle of whiche countrey is divers and of sundrye kindes. Some place is plentifull of woode and vines, and aboundaunte of pleasaunte fruite, the grounde fatte, well watei'ed, and full of springes. Those partes which be most temperate are sowed with corne, and the rest be reserved for fedyng of beastes. But the greater part of the countrey is couered ouer with baraine sandes and withered up for want of moisture, nourishing neither man, nor bringinge forth fruite. But with certaiue wiudes that come from the sea of Ponte (the Caspian), the sand in the plaiues is blowen together in heapes, which seme a farre of like great hilles, wherby the accustomed wayes be damned, so that no signe of them can appcre. Ther- fore such as do passe those plaiues use to observe the starves in the night as thei do that sayle the seas, and by the course of them direct their journey. The nightcs for the more parte be brighter than the daycs, whcrfore in the daye time the countrey is wild and unpassible, when they can neither finde any tracte * Bactria is said to be a corruption of Bukhtiar, an old Persian word signi- fying ‘ The East,’ just as the meaning of Kborassau is ‘The Region of the Sun.’ EARLY HISTORY. 29 nor wave to go in, nor niarke or eigne wherby to passe, the starres beying hidden by the rniste. If the same winde chaunce to come durying the time that men be passying, it overwhelm- eth them with sande. Where the countrey is temperate, it bringeth forth great plenty both of men and horse, so that the Bactrians may make 30,000 horsemen.’ Sir Alexander Burnes bears testimony to the perfect fidelity of this picture even at the present day, especially as regards the desert to the north-west and the mode of travelling therein. In addition to Bactra or Zariaspa, mention is made of a town called Darapsa, Adraspa, or Drapsaca, the first place taken by Alexander after crossing the mountains. ‘ The Bactrians,’ says Archdeacon Williams, ‘ held a middle place between the Persians and Scythians, partaking more of the polished man- ners of the former than of the rudeness of the latter.’ They were, nevertheless, accused of throwing out the bodies of their dying relatives into the streets to be devoured by dogs, thence called ‘entombers,’ or ‘ buriers of the dead’ — a practice that was abolished by Alexander. Professor Wilson, however, was disposed to trace this legend to the Zoroastrian custom of ex- posing dead bodies in the Towers of Silence, to the ordinary process of decomposition accelerated by the foul birds of prey. In Grecian dramatic poetry this region was the scene of the wanderings of Bacchus. The pages of historic romance tell how Ninus sat down before Bactra with an immense army, and only succeeded when reinforced by Semiramis. In the reign of Sardanapalus the Bactrians broke out into a formidable revolt, but in that of Arbaces they largely contributed to the reduction of Nineveh. Against the great Cyrus they waged equal war, until his union with the daughter of Astyages, when they freely tendered their submission. In the army of Xerxes, as we have seen, they were arrayed beside the Sacae and the Caspii, and are represented as wearing a sort of Median head- 30 CENTRAL ASIA. dress, and as being armed with bows and arrows, and short spears. Their cavalry were at all times highly esteemed, and honourably distinguished themselves in the last days of the Persian Empire. The Sogdiani, like the Bactrians, were accused of handing over to canine ‘ entombers ’ the mortal remains of their friends and kinsfolk, and probably under the same circumstances. Their country extended from the Oxus to the Jaxartes, which divided them from the Massagetae, who occupied the vast steppe extending to the Altai Mountains. Their most valued river was that called by the Greeks Polytimetus, the ‘ Very Precious ’ or ‘ Much Honoured,’ now known as the Zarafshan, or ‘ gold- scattering ’ river of Samarkand, which flows past Bokhara, and is finally lost in the Denghiz or Karakul Lake, to the S. S. E. of the latter city. In those days this productive region ap- pears to have been overgrown with forests abounding in wild beasts and in game of all kinds. At Bazaria, for instance — perhaps the modern Bokhara — we read of a royal park, or ‘ paradise,’ that had not been disturbed for four generations, in which 4000 animals were slain by Alexander and his officers. Here, it is said, Alexander overcame a lion in single fight, extorting from the Spartan envoy, who witnessed the rash deed, the hearty exclamation : ‘ Bravo, Alexander ! well hast thou won the prize of royalty from the king of the woods.’ The principal city was Maracanda, though the names of several other towns are preserved, such as Cj’ropolis, Ghaza, Marginiu, Nautaka (near Karshi), Alexandria Ultima (near Khojend), and Oxiana. In Maracanda, however, stood the palace of the Sogdian ruler, and it was here that Alexander murdered his own foster-brother, Clitus. The loca deserta Sogdianorum seem to have been no less terrible than those of the Bactriani, judging from the experiences of the flying column commanded b}’ Alex- ander in person. John Brcnde shall again be our interpreter : — EARLY HISTORY. 31 1 In the wante of water (that hath bene declared before) desperation moved them to thirst before they had desire to drinke. For by the space of 1111 C furlonges they founde no water at all. The vapoure of the Sunne, beynge in the somner season, did so burne the sande that when it began to waxe bote it starrhed all thinges as it had bene with a continuall fire. And then the lyght somewhat obscured by a mist that rose out of the arth by the immoderate heate, caused the playnes to liaue appearaunce of a maine Sea. Their iourney in the nyght seamed tollerable, because their bodyes were somewhat refresh- ed with the dewe and the coolde of the mornynge. But when the daye came and the heate rose, then the drought driying up all ye natural humoures, both their moutlies and their bowels were enflamed for heate. Then their hartes failed and their bodies fainted, beynge in case that thei could neither stand styl, nor passe forwardes. A few that were taught by suche as knew the countrey, had gotten water whiche refreshed them some- what, but as the heate encreased, so their desire grewe againe to drinke.’ After subduing Seistan and Afghanistan without much difficulty except such as arose fi’om the severity of the climate, Alexander appears to have crossed over into Bactria by the Khawak Pass, at an altitude of 13,200 feet above the sea, towards the close of the winter 330 — 329 b. c. The passage over the mountains occupied the best part of a fortnight, nor was it until the fifteenth day that his starved and exhausted army came in sight of Adraspa. Bactria was speedily over- run, but terrible sufferings were endured in traversing the burn- ing and waterless desert that approaches almost to the very bank of the Oxus. As all the boats within a considerable dis- tance had been destroyed by Bessus, the river was crossed by means of inflated skins, and shortly afterwards the murderer of Darius was overtaken and captured by Ptolemy. Stript naked, 32 CENTRAL ASIA. loaded with chains, and his neck encircled by an iron collar, the traitor was placed in a conspicuous position, and exposed to the scorn and derision of the entire army as it defiled past him. lie was then scourged and sent to Bactria, whence he was sub- sequently conveyed into Persia and delivered into the hands of the mother of Darius. By her orders, according to Plutarch, four trees were bent down by main force, to each of which he was attached by a limb. Suddenly the trees were released, and springing back to their natural positions tore the wretched man into shapeless fragments.* From the Oxus Alexander marched straight on to Mara- canda, or near the site of the modern Samarkand. No very serious resistance was offered by the Sogdians, though the Macedonian detachments were much harassed by desultory attacks. The most difficult operations were the reduction of Cyropolis on the Jaxartes, and the storming of an almost in- accessible rock where Alexander himself was severely wounded by an arrow. Within the space of three weeks the town of Alexandreia Ultima was built at no great distance from Kho- jend, to mark the limit of the Macedonian conquests in that direction.' The Jaxartes also was crossed, and an idle victory gained over the nomad Scythians, in which bootless expedition his soldiers suffered greatly from thirst, and the king himself was attacked with illness. A Macedonian brigade having in the mean while been cut to pieces in Sogdiana by Spitamenes, Alexander overran the fertile valley of the Polytimetus — the Kohik, or Zarafshan, of later times — and put to the sword all who came within reach of his vengeance. lie then re-crossed the Oxus and wintered at Zariaspa, another name for Bactra or Balkh. The submission of the Sogdians, however, proved to be * 15y other writers, however, Bessus is said to have been nailed to a cross and pierced with arrows, at Ecbatana. EARLY HISTORY. 33 merely nominal, for no sooner had he quitted their territory than they broke out into open revolt. The greater part of the following year — b. c. 328 — was consequently spent in repeating the work of the preceding one, and it was now that occurred the slaughter of the wild animals in the Royal Chace of Bazaria. This year, too, was marked by that horrible debauch at Mara- canda, at which Alexander slew with his own hand his foster- brother Clitus, who had saved his life at the Battle of the Granicus by cutting off 'with one sweep of his sword the up- raised arm of Spithridates. During the early part of the winter of 328 b. c. the Macedonian army rested from its labours at Hautaka. The next feat of arms, in the spring of b. c. 327, was the reduction of the well-nigh impregnable fort which Archdeacon Will iams places in Bactria, while Bishop Thirlwall alights upon it in Sogdiana, and whose chief peril to the con- queror lay in the beauty of Roxana, daughter of the Bactrian chief Oxyartes, ‘ said to have been, with the exception of the wife of Darius, the loveliest woman seen by the Macedonians during their Asiatic expedition.’ The spring was spent chiefly at Bactria, where Alexander united himself in marriage to Roxana, greatly to the disgust of his Greek soldiery. The intoxicating influences of love, wine, and success without a check, here impelled the king to excesses bordering upon madness. Callisthenes, the nephew of Aristotle, a somewhat impracticable republican — or ‘ philosopher,’ as he would have preferred to be called — having ostentatiously re- fused to adopt the Persian mode of prostration, inevitably in- curred the displeasure of Alexander, too little used to opposition to make allowances for the feelings of others. About the same time Hermolaus, one of the royal pages, presumed to transfix with a javelin a wild boar that had turned upon the king, and for his officious loyalty was deprived of his horse and scourged. Thirsting for revenge, Hermolaus conspired with some of his 3 34 CENTRAL ASIA. brother pages, all of them youths of the best families of Greece, to slay Alexander when he retired to rest. The king, however, escaped that danger by sitting up all night carousing, and on the morrow one of the conspirators, as usual in such cases, be- trayed his accomplices. Hermolaus and his friends were put to the torture, but nobly refused to implicate others in their guilt, and were stoned to death. As the intimate friend of Hermo- laus, Callisthenes also was subjected to torture, and afterwards hanged, though no proof had been obtained of his complicity. In the summer of 327 b. c. Alexander again crossed the mountains, taking with him 30,000 recruits from Bactria and Sogdiana, and marched to the conquest of the Punjab, leaving Amyntas at Bactra with a reserve of 10,000 foot, and 3,500 horse. In Sogdiana he had built eight towns, each of which was a fortified post, but his power over that province was con- fined to the immediate vicinity of those garrisons. The moral effects of his conquests, however, were more extensive and durable, and have been thus succinctty summed up : — ‘ Those nations had not been civilized, had they not been vanquished by Alexander. He taught marriage to the Hyrcanians, and agriculture to the Arachosii ; he instructed the Sogdians to maintain, and not to kill, their parents ; the Persians to respect, and not to marry, their mothers ; the Scythians to bury, and not to cat, their dead.’ The name of the great Sikunder is still revered in the dis- tant East, and the chiefs of the petty principalities