The Gates of India: Being an Historical Narrative

by Sir Thomas Hungerford Holdich

More recently the Ghilzais have left Zamindawar, and the Taimanis have been pressed backward and upward into the central hills by the Afghan Durani clans, who circle round westward, forming a fringe on the foothills between Herat and Kandahar, and who have now completely monopolized Zamindawar. Here, indeed, the truculent Nurzai and Achakzai, and other elements of the Durani section of Afghan ethnography, flourish exceedingly, and it is in this corner of Afghanistan, bordering on the Herat highway to India, that nearly all the fanatics and ghazis of the country are bred. They presented so turbulent and uncompromising a front to strangers in 1882 that there was great difficulty in getting a fair survey of the land of the Chahar Aimak or of Zamindawar.

The mediæval provinces of Ghur and Bamain figure so largely in the records of Arab geography, and appear to have been so fully open to commerce during the centuries succeeding the Arab conquests, that one naturally wonders whether there can have been any remarkable change in the physical configuration of those regions which, in these later days, has rendered them more inaccessible and unapproachable. The Arab accounts of trade routes flit easily from point to point, taking little reckoning of long distances and gigantic ice-bound passes, or the perils of a treacherous climate. An itinerary which deals with stupendous mountains and extreme altitudes has little more of descriptive illustration in these Arab records than such as would apply to camel tracks across the sandy desert or over the flat plain. Nor is the distance which figures as a "day's journey" sensibly changed to suit the route. Forty miles or so across the backbone of the Hindu Kush is written of in much the same terms as if it were forty miles over the plains. Giving the Arab travellers all credit for far greater powers of endurance and determination than we moderns possess, we must still believe that there is a great deal of exaggeration (or forgetfulness) in these heroic records of the past. It is unlikely that the physical conditions of the country have materially changed.

So little has been written of this central region of modern Afghanistan (within which lie the ruins of more than one kingdom), so little has it been traversed by modern explorers, that it may be useful to give some slight general description of the country with which these records deal, including Bamain and Kabul and the mountain system occupied by the Taimani and Hazara tribes as well as the prolific region of Zamindawar with the routes which traverse it.

No part of Afghanistan has been subject to more speculative theories, or requires more practical elucidation, than this mountain region in which so large a share of the drama of Afghan history has been played. Before the days of the Anglo-Russian agreement on the subject of the northern boundaries of Afghanistan nothing was known of its geography, beyond what might be gathered from the doubtful records of Ferrier's journey—and that was very little. The geography of a country shapes its history just as surely in the East as in the West, and we have consequently much new light thrown on the interesting story of the rise and fall of the Ghur dynasties by the fairly comprehensive surveys of the region of their turbulent activities which were carried out in 1882-83.

From these sources we obtain a very fair idea of the general conformation of Central Afghanistan, i.e. that part of Afghanistan which is occupied by the tribes known as the Chahar Aimak, i.e. the Jamshidis, the Hazaras, Firozkohis, and Taimanis. It consists in the first place of a huge irregular tableland—or uplift—which has been deeply scored and eroded by centuries of river action, the rivers radiating from the central mass of the Koh-i-Babar to the west of Kabul and flowing in deep valleys either directly northward towards the Oxus, due west towards Herat (eventually to turn northward), or south-west in irregular but more or less parallel lines to the Helmund lagoons in Seistan.

The Kabul River basin also finds its head near the same group of river sources. The central mountain mass, the Koh-i-Babar, is high, rocky, generally snow-capped and impassable. To the north it sends down long, barren, and comparatively gentle spurs to the main plateau level, which is deeply cut into by the northern system of rivers, including the Murghab and the Balkh Ab. But the strangest feature in this network of hydrography is the long, deep, narrow valley (almost ditch-like in its regularity) which has been eroded by the Hari Rud River as it makes its way due west, cutting off the sources of the northern group from those of the Helmund or south-western group. It is a most remarkable valley, depressed to a depth of 1000 to 2000 feet below the general plateau level, bounded on the north by a comparatively level line of red-faced cliffs, and on the south by another straight flat-backed range called the Band-i-Baian (or farther west, the Sufed Koh), which has been carved into the semblance of a range by the parallel valleys of the Hari Rud on the north and the Tagao Ishlan on the south, which hug the range between them.

No affluents of any consequence join either stream. Either separate or together they make their way with straight determination westward towards Herat. South of this curious ditch rise the many streamlets which work their way, sometimes through comparatively open valleys where the floor level has been raised by the centuries of detritus, sometimes through steep and narrow gorges where the harder rock of the plateau formation presents more difficulties to erosion, into the great Helmund basin. These are affluents of the Adraskand, the Farah Rud, and the Helmund, all of which have the same bourne in the Seistan depression. High up between the Farah Rud and the Helmund affluents isolated rugged peaks and short ranges crease and crumple the surface of the inhospitable land of the Hazaras, who occupy all the highest of the uplands and all the sources of the streams, a hardy, handy race of Mongols, living in wild seclusion, but proving themselves to be one of the most useful communities amongst the many in Afghanistan. We have some of them as sepoys in the Indian Army. Lower down in the same river basins, where the gentle grass-covered valleys sweep up to the crests of the hills, cultivation becomes possible. Here flocks of sheep dot the hill-sides, and the land is open and free; but there are still isolated and detached ribs of rocky eminence rising to 11,000 and 12,000 feet, maintaining the mountainous character of the scenery, and rivers are still locked in the embrace of occasional gorges which admit of no passing by. This is the land of that very ancient people, the Taimanis.

The fierce and lawless Firozkohis live in the Murghab basin on the plateau north of the Hari Rud, the Jamshidis to the west of them in the milder climate of the lower hills, into which the plateau subsides.

Whilst we are chiefly concerned in tracing out the mediæval commercial routes of Afghanistan, we may briefly summarize the events which prove that those traversed between Herat and the central kingdoms were important routes, worn smooth by the feet of armies as well as by the tread of pack-laden khafilas. They are still very rough and they present solid difficulties here and there, but in the main they are passable commercial roads, although little commerce wends its way about them now.

In the Middle Ages the Kingdom of Ghur included the Herat valley as far as Khwaja Chist above Obeh in the valley of the Hari Rud, as well as all the hill country to the south-east. About the earliest mention of Ghur by any traveller is that of Ibn Haukel, who speaks of Jebel al Ghur, and talks of plains, ring-fenced with mountains, fruitful in cattle and crops, and inhabited by infidels (i.e. non-Mussulmans). The later history of Ghur is inextricably intertwined with that of Ghazni.