Across Coveted Lands Part 58

[Ill.u.s.tration: Rock Pillar between Kirtaka and Saindak.]

The track here (about 13 miles from Kirtaka) turned south-west following the river bed, then due south, where among the mountains we saw a huge pillar of a brilliant yellow colour and over 50 feet high, standing up by the roadside. The ill.u.s.tration gives a fair idea of it. To the south-east in the direction of our track, which for a change was quite tortuous, were mounds of sand and debris. The red rock of the mountains seemed crumbling towards the east, whereas the hills to the west were well rounded and padded with sand and gravel.

We went over a low pa.s.s 3,810 feet, and then along a flat basin with hills to the south-east, and outlets both to the south-east and east. We had descended to 3,680 feet, but had to go up another pa.s.s 4,060 feet, the highest we had so far encountered. Innumerable yellow sand hills were before us to the north-north-east, and here we were on a sort of flat sandy plateau, three-quarters of a mile wide and a mile and a half long.

Ten sharp-pointed peaks could be counted to the south-south-east, high mountains were before us to the south-east, and a long range beyond them east-south-east. Sand dunes, shaped like the back of a whale were to the east, and a remarkable spherical mount south-south-east directly in front of the ten peaks. We arrived at Saindak.

CHAPTER x.x.x

An excursion into Afghanistan--The salt deposits of G.o.d-i-Zirreh--Sand hills--Curious formation of hill range--Barchans and how they are formed--Alexander's march through the country--The water of G.o.dar-i-Chah--Afghans and their looks.

The excursion which I made into Afghan territory to the salt deposit of Gaud- or G.o.d-i-Zirreh, and a lower depression to the east of it, was of great interest to me.

There are a great many theories regarding these former salt lakes, and it is not easy to say which is right and which is wrong. The general belief is that these lakes were formed by the overflow of the Halmund swamp into the Shela (river) which carried sufficient water not only to fill up the G.o.d-i-Zirreh, but to overflow when this was full into the next depression east of the Zirreh.

There is no doubt that to a great extent this was the case, but these lakes were, I think, also fed more directly by several small streams descending from the mountains to the south and west of the Zirreh, which form the watershed--and very probably also from the north by the Halmund River itself. Both lakes were dry and seemed to have been so for some time. The G.o.d-i-Zirreh, forming now a great expanse of solid salt some 26 miles long by 5 or 6 wide, extends in a long oval from west to east. The other lake was somewhat smaller.

To the south of these salt deposits in the zones between them and the present Afghan boundary, and forming the southern fringe of the Afghan desert, the soil is covered with gravel and stones washed down from the mountain sides. Very stony indeed is the desert towards the Malek-Siah end, then further north-east appear brown earth, shale, and sand. To the north of the lakes was a long line of bright yellow sand extending from west to east and broad enough towards the north to reach the bank of the river Halmund. Another s.h.i.+ny patch, which at first, from a distance, I had mistaken for another smaller lake, turned out on examination to be a stretch of polished shale which shone in the sun, and appeared like bluish water.

Stunted tamarisk grows in some parts but not in the immediate neighbourhood of the salt deposits. We have here instead a belt of myriads of small conical sand-hills, also spreading from west to east, quite low to the west and getting higher for several miles towards the east. In the south-west part of the desert, curiously enough, between the zone of conical hills and the salt deposits, and parallel to both, lies a row of semi-spherical sand and salt mounds of a whitish colour.

To the east-south-east of the lakes the sand-hills rise to a great height and eventually form a high ridge, which for some reason or other is cut perpendicularly on its western side, possibly as the result of a volcanic commotion. Of similar origin probably was the gigantic crack caused by an earthquake which we shall examine later on near Nushki. In fact, both the crack at Nushki and the collapse of the west side of this hill range, as well as a great portion of that deep crack in the earth's crest in which the Shela flows, have very likely been formed by the same cause. They are within the same zone of volcanic formation. In the particular case of this hill range in Afghanistan the collapse did not appear to me to be due to the action of water, but to a sudden crumbling which had caused a very sharp vertical cut.

[Ill.u.s.tration: Sand Hills.]

To the north of the salt wastes was another long belt of yellow sand extending for some 40 miles, upon which there was absolutely no vegetation, while intervening between the salt and this sand flat were numerous sand barchans, like horseshoes, with a gradual slope on the windward side (north) and a crescent hollow with a steep but not quite vertical bank on the lee side.

I noticed all over Persia, and in Beluchistan as well as here, that these sand barchans, or barchanes, will only form on level ground--generally on extensive plains. All single sand hills, however, whether barchans, conical, semi-spherical, or of more irregular shapes, are invariably caused by a primary obstacle, however small, arresting the sand.

Various are the theories with regard to the formation of these barchans, and especially with regard to the formation of the hollow on the lee side.

[Ill.u.s.tration]

The explanation from my own observation has--if no other--at least the merit of simplicity. The wind, on meeting the semi-circular back of the barchan, is diverted on the two sides of it; these two currents come into violent collision again on the lee-side, where, the air being more or less still, a considerable portion of the wind is forcibly driven back towards the barchan, corroding its side in a double rotatory way, each such circle having for a diameter the radius of the barchan crescent containing them. In fact in many barchans the sand ripples on the windward slopes cross the direction of the wind at right angles. A line of sand formed in the centre of the barchan crescent in the opposite direction to the wind is often to be seen during wind storms or soon after. I have also seen barchans, the inner crescent of which showed beyond doubt that when there is a prevalent wind from one side only, the above explanation, although less scientifically obscure and elaborate than most, applies, and, I think, it may eventually be found quite the most probable.

The diagram here given will ill.u.s.trate and, I hope, make quite clear the meaning of my words. In the centre of the crescent can be noticed the action of the parting wind currents.

[Ill.u.s.tration: A Caravan of Donkeys in Afghanistan.]

North of Kirtaka was a very pointed high conical hill, and not far from it a small replica of Fujisan in j.a.pan, so much were the lines like those of the j.a.panese mountain. A great many of the drain channels from the mountains to the south extended very far into the desert and some as far as the G.o.d-i-Zirreh.

It is also very probable that in the days when Sistan was a most populous region, with uninterrupted towns and villages along and near the Halmund, numerous ca.n.a.ls may have intersected the Zirreh region and rendered it a very fertile plain. History would indeed point forcibly towards such a hypothesis. Ample proof that the plain was inhabited still remains in the ruins of G.o.dar-i-Chah, situated at the western limit of the Zirreh salt deposits, Chah-i-Mardan, where a ruined fort and a Ziarat are said to exist, Gumbaz-i-Chah, and others. All these places are now deserted and are being fast buried by the sand. They are mostly along the Shela (river) banks, and the natives of Sistan say that they have heard from their ancestors that when the Shela did flow freely its water was quite drinkable.

There was a well at G.o.dar-i-Chah--hence its name, "the well of G.o.dar"--almost entirely dried up and of water so foul that it was not possible to drink it, and another just as bad was said to exist at Gumbaz.

It would be most interesting if one could get at the actual history of this part of the world and gain an insight into its former prosperity and civilisation. It is quite probable that Alexander, in his progress through Beluchistan and Sistan, must have come through this country. No army--not even with a new Craterus at its head--could, of course, march elephants, camels and horses through that country to-day, and this has led some critics to doubt that Alexander could have done so, or to believe that, if he did so, he must have been deceived by his guides who tried to bring him as far as possible from water. But those critics forget that in Alexander's days this portion of country was extremely civilised, fertile, and supplied with plenty of water--or else how can we account for the innumerable ruins we find there, and for the many ca.n.a.ls for irrigation?

Sir Charles McGregor, Goldsmid, Bellew, Major MacMahon, Napier, and one or two others who have visited the country north of the Zirreh, can fully testify to the amazing remains of former prosperity in Sistan and south-west Afghanistan.

Sir Charles McGregor gives an amusing receipt for those who wish to know what the water at G.o.dar-i-Chah is like without having the trouble of going there. "Take the first nasty-looking water you can find. Mix salt with it until it tastes as nasty as it looks, then impregnate it with gas from a London street lamp, and add a little bilge-water, shake vigorously and it is ready for use." Major McMahon also testifies to the accuracy of the above receipt, but, he adds, "it was not nearly so bad as much we found elsewhere."

[Ill.u.s.tration: In Afghanistan. Who are you?]

[Ill.u.s.tration: In the Afghan Desert. Afghan Caravan Men.]

The Zirreh seemed just like a great stretch of country under snow, the thick salt sediment was so beautifully white. It formed a deep depression in the centre. The second deposits to the east of the Zirreh were of a similar shape, with salt extremely thick, but not quite so extensive as in the Zirreh. Near the edge of both dry lakes there was absolutely no vegetation, but most beautifully coloured stones could be found, such as red and brown jasper and agatescent quartz, chalcedony, white and brown limestone.

As I was returning towards the Beluchistan boundary among the sand hills I came upon about a dozen Afghans, who looked as suspiciously at me as I did at them. At first I thought they were soldiers, and as I did not much care to be caught by them and have my goods confiscated--no Englishmen being allowed in their territory--I requested them to stop some way off and explain what they wanted, while I was snapshotting them. They had a great big white fluffy dog with them who seemed very anxious to have a go at the Sahib. One man was asked to come forward alone, which he did with his turban right over his eyes, while the others formed a line behind and appeared most puzzled as to what was going to happen. He said they were glad to see me in their country and that they were "good people,"

and would not injure nor trouble me in any way; so I gave them a small present, which seemed to please them much, and they became quite friendly. They seemed to have some coa.r.s.e humour about them and were rather boisterous. Their faces, however, did not quite appeal to me.

The Afghan invariably has a slippery, treacherous look about his countenance which he cannot disguise, and which, personally, I do not much admire. He seldom looks at one straight in the face, can be very sullen when he is not boisterous, and I should think would easily seek cause of offence and pick a quarrel with any one weaker than himself in order to have a fight. These fellows were, for instance, most unlike the gentlemanly Beluch. They shouted at the top of their voices when they spoke, and were uncouth in speech and manner. I was rather glad when they departed.

Further on I came upon more people and animals, but they, too, were quite peaceful.

Having accomplished my object I again crossed over into Beluchistan.

CHAPTER x.x.xI

Saindak--Beluch prisoners--Thana and Bungalow--Beluch bread--The Saindak mountain and its mineral resources--The Daftan volcano--_Surmah_ and lead--Mukak and its strong man--A sick camel--Gypsum--_Regheth_--Where the track will deviate in future--Difficulty in obtaining drinkable water--Wells made attractive--Sahib chah--A well ventilated rest-house.

Saindak had an imposing _thana_, the elaborate gateway of which was decorated with heads of wild sheep and _dumbahs_. There were nine rooms--some boasting of wooden doors--at the end of the large court, but all were occupied by the seven _sawars_, the postal _moonshee_, the three _ka.s.sildars_ and the _havildar_, one _duffadar_, and one _jemadar_.

[Ill.u.s.tration: The Thana and New Bungalow at Saindak. (Saindak Mt. in background.)]

On my arrival they proceeded to clear one of the chambers for me, and to my astonishment out of it came four wretched men chained together by the hands and feet and in a pitiable condition. Not that their countenances, when one examined their faces, called for much pity. More palpably criminal types could be found nowhere, but somehow or other to see these poor devils stumbling along, with the iron rings round their bruised and sore ankles showing through the torn rags which covered their skeleton legs, and the agonized expressions on their worn, repulsively cruel faces, was not an edifying sight. They had been brought down here to work and, for prisoners, were treated considerately enough, I suppose. But they seemed very ill and suffering. Two were robbers, the other two--father and son--had murdered a man and stolen 400 sheep. They were condemned to captivity for life.

I declined to put up in that room, especially when I happened to peep in and was nearly choked by the foul odour that emanated from inside, and preferred--although it was very cold--to inhabit the unroofed new two-roomed bungalow in course of construction, which I found really very comfortable.

As can be seen by the photograph the thana and bungalow of Saindak are built on rather an attractive site under the shelter of the Saindak Mountain. Whenever I see a mountain I cannot resist the temptation to go up it, and now, after all the thousands of miles of flat country I had traversed, I felt this desire more strongly than ever. The ascent of the mountain presented no difficulty except that its rocky sides were somewhat steep. I resolved to go up early the next morning before making a start with my camels.

In the meantime during the evening I was instructed by Mahommed Hussein, my camel man, in the Beluch fas.h.i.+on of making bread--really a most ingenious device. A stone of moderate size, say 4 inches in diameter and as round as can be found, is made red hot on the fire, and upon it a coating of paste--flour, water, and salt--is deposited evenly so as to make an envelope of paste one inch thick all over. Three, four, five, or as many of these b.a.l.l.s as required being made, they are placed in a circle near a blazing fire, so that the outside may get baked as well as the inside. When ready for consumption the b.a.l.l.s are split open and the stones removed. The bread is really most excellent and resembles a biscuit.

[Ill.u.s.tration: Beluch Prisoners at Saindak.]

At Saindak (alt.i.tude 3,810 feet) there are a number of wells, mostly very salt, but one has quite fair water, only slightly brackish. The water, however, had a peculiar taste of its own, as if it had gone through lead deposits, and, on mentioning this to some Beluch they told me that lead was, in fact, found on the mountains just above this camp. Having drunk two gla.s.ses of this water I was taken with bad internal pains, but I must in fairness own that I do not know whether to attribute this entirely to the water or to indiscreet consumption of an irresistible, extra rich plum-cake which the wonderful Sadek now produced, much to my surprise and delight, from among my provisions.

Travellers, however, would do well to bring their own supply of water from Kirtaka, if they are coming from Robat, or from Mukak, if travelling from Quetta.

The ascent to the summit of the Saindak mountain well repays the traveller for the exertion of getting there, and that not only on account of its geological formation. Looking over the lower mountains one obtained a magnificent view of the Afghan desert as far as the eye could see, to the north-west and north-east, while to the west lay a mountain ma.s.s, the Mirjawa mountains, and innumerable sand hills. To the south-south-west towered above everything the double-humped active volcano of Kuh-i-Daftan, with its snow-capped crater. It was smoking, notwithstanding the ridiculous theory entertained by some F.R.G.S. that volcanoes cannot exist so far south in the Northern Hemisphere! We saw this volcano for several days and it threw up considerable volumes of smoke. At night it occasionally had quite a glow above its crater.

The volcano, I need not say, is in Persian territory, and is some 60 miles distant, as the crow flies, from Saindak, although in the clear atmosphere it does not appear more than a few miles off. It is a most impressive mountain.

Parallel ridges of sand hills, facing east, were to be seen to the south-west of the Saindak mountain, and then a wide flat plain, beyond which four successive mountain ranges, formed a powerful barrier. To the south-east also were high mountains.