CHAPTER XII

ASCENT OF ARARAT

Next morning the sun had already risen as I let myself down through

the open casement of the window and dropped into the garden among the

dry brushwood encumbering its sandy floor. Not a soul was stirring,

and not a sound disturbed the composure of an Eastern morning, the

great world fulfilling its task in silence and all nature sedate and

serene. A narrow strip of plantation runs at the back of Aralykh,

on the south, sustained by ducts from the Kara Su or Blackwater,

a stream which leads a portion of the waters of the Araxes into the

cotton fields and marshes which border the right bank. Within this

fringe of slim poplars, and just on its southern verge, there is

a little mound and an open summer-house--as pleasant a place as it

is possible to imagine, but which, perhaps, only differs from other

summer-houses in the remarkable situation which it occupies and in

the wonderful view which it commands. It is placed on the extreme

foot of Ararat, exactly on the line where all inclination ceases and

the floor of the plain begins. It immediately faces the summit of

the larger mountain, bearing about south-west (Frontispiece).

Before you the long outline of the Ararat fabric fills the southern

horizon--the gentle undulations of the north-western slope, as it

gathers from its lengthy train; the bold bastions of the snowfields,

rising to the rounded dome; and, further east, beyond the saddle where

the two mountains commingle, the needle form of the lesser Ararat,

free at this season from snow. Yet, although Aralykh lies at the flank

of Ararat, confronting the side which mounts most directly from the

plain to the roof of snow, the distance from a perpendicular drawn

through the summit is over 16 miles. Throughout that space the fabric

is always rising towards the snow-bank 14,000 feet above our heads,

with a symmetry and, so to speak, with a rhythm of structure which

holds the eye in spell. First, there is a belt of loose sand, about

2 miles in depth, beginning on the margin of marsh and irrigation,

and seen from this garden, which directly adjoins it, like the sea-bed

from a grove on the shore. On the ground of yellow, thus presented,

rests a light tissue of green, consisting of the sparse bushes of

the ever-fresh camelthorn, a plant which strikes down into beds of

moisture, deep-seated beneath the surface of the soil. Although it

is possible, crossing this sand-zone, to detect the growing slope,

yet this feature is scarcely perceptible from Aralykh, whence

its smooth, unbroken surface and cool relief of green suggest the

appearance of an embroidered carpet, spread at the threshold of an

Eastern temple for the services of prayer. Beyond this band or belt

of sandy ground, composed no doubt of a pulverised detritus, which

the piety of Parrot was quick to recognise as a leaving of the flood,

the broad and massive base of Ararat sensibly gathers and inclines,

seared by the sinuous furrows of dry watercourses, and stretching,

uninterrupted by any step or obstacle, hill or terrace or bank, to the

veil of thin mist which hangs at this hour along the higher seams. Not

a patch of verdure, not a streak of brighter colour breaks the long

monotony of ochre in the burnt grass and the bleached stones. All

the subtle sensations with which the living earth surrounds us--wide

as are the tracts of barren desert within the limits of the plain

itself--seem to cease, arrested at the fringe of this plantation,

as on a magician's line. When the vapours obscuring the middle slopes

of the mountain dissolve and disappear, you see the shadowed jaws of

the great chasm--the whole side of the mountain burst asunder from

the cornice of the snow-roof to the base, the base itself depressed

and hollow throughout its width of about 10 miles. No cloud has yet

climbed to the snows of the summit, shining in the brilliant blue.

It was the morning of the 17th of September, a period of the year

when the heats have moderated; when the early air, even in the plain

of the Araxes, has acquired a suggestion of crispness, and the sun

still overpowers the first symptoms of winter chills. [71] The tedious

arrangements of Eastern travel occupied the forenoon; and it had been

arranged that we should dine with our host, the Lieutenant, before

making the final start. Six little hacks, impressed in the district

and sadly wanting in flesh, were loaded with our effects; our party

was mounted on Cossack horses, which, by the extreme courtesy of the

Russian authorities, had been placed at our disposal for a week. We

took leave of our new friend under a strong sentiment of gratitude

and esteem; but a new and pleasurable surprise was awaiting us, as we

passed down the neat square. All the Cossacks at that time quartered

in Aralykh--the greater number were absent on the slopes of the

mountain, serving the usual patrols--had been drawn up in marching

order, awaiting the arrival of their Colonel, who had contrived to

keep the secret by expressing his willingness to accompany us a few

versts of the way. My cousin and I were riding with the Colonel,

and the purpose of these elaborate arrangements was explained to us

with a sly smile; the troop with their Colonel were to escort us on

our first day's journey, and to bivouac at Sardar Bulakh. The order

was given to march in half column. It was perhaps the first time that

an English officer had ridden at the head of these famous troops. We

crossed the last runnel on the southern edge of the plantation and

entered the silent waste.

For awhile we slowly rode through the camelthorn, the deep sand

sinking beneath our horses' feet. It was nearly one o'clock, and the

expanse around us streamed in the full glare of noon. A spell seems

to rest upon the landscape of the mountain, sealing all the springs

of life. Only, among the evergreen shrubs about us, a scattered group

of camels cropped the spinous foliage, little lizards darted, a flock

of sand-grouse took wing. Our course lay slantwise across the base of

Ararat, towards the hill of Takjaltu, a table-topped mass, overgrown

with yellow herbage, which rises in advance of the saddle between the

mountains, and lies just below you as you overlook the landscape from

the valley of Sardar Bulakh. Gullies of chalk and ground strewn with

stones succeed the even surface of the belt of sand, and in turn give

way to the covering of burnt grass which clothes the deep slope of

the great sweeping base, and encircles the fabric with a continuous

stretch of ochre, extending up the higher seams. Mile after mile we

rode at easy paces over the parched turf and the cracking soil. When

we had accomplished a space of about 10 miles, and attained a height

of nearly 6000 feet, the land broke about us into miniature ravines,

deep gullies, strewn with stones and boulders, searing the slope about

the line of the limit where the base may be said to determine and the

higher seams begin. Winding down the sides of these rocky hollows,

one might turn in the saddle at a bend of the track, and observe the

long line of horsemen defiling into the ravine (Fig. 31). I noticed

that by far the greater number among them--if, indeed, one might not

say all--were men in the opening years of manhood--lithe, well-knit

figures, and fair complexions, set round with fair hair. At a nearer

view the feature which most impressed me was the smallness of their

eyes. They wear the long, skirted coat of Circassia, a thin and worn

khaki; the faded pink on the cloth of their shoulder-straps relieves

the dull drab. Their little caps of Circassian pattern fit closely

round their heads. Their horses are clumsy, long-backed creatures,

wanting in all the characteristics of quality; and, as each man

maintains his own animal, few among them are shod. Yet I am assured

that the breed is workmanlike and enduring, and I have known it to

yield most satisfactory progeny when crossed with English racing

blood. As we rounded the heap of grass-grown soil which is known as

Takjaltu, we were joined by a second detachment of Cossacks, coming

from Akhury. Together we climbed up the troughs of the ridges which

sweep fanwise down the mountain side, and emerged on the floor of

the upland valley which leads between the greater and the lesser

Ararat, and crosses the back of the Ararat fabric in a direction

from south-west to north-east. We were here at an elevation of 7500

feet above the sea, or nearly 5000 feet above the plain. Both the

stony troughs and ridges, up which we had just marched, as well

as the comparatively level ground upon which we now stood, were

covered with a scorched but abundant vegetation, which had served the

Kurds during earlier summer as pasture for their flocks, and still

sheltered numerous coveys of plump partridges, in which this part of

the mountain abounds.

At the mouth of this valley, on the gently sloping platform which its

even surface presents, we marked out the spaces of our bivouac, the

pickets for the horses, and the fires. Our men were acquainted with

every cranny; we had halted near the site of their summer encampment,

from which they had only recently descended to their winter quarters

in the plain. As we dismounted we were met by a graceful figure,

clad in a Circassian coat of brown material let in across the breast

with pink silk--a young man of most engaging appearance and manners,

presented to us as the chief of the Kurds on Ararat who own allegiance

to the Tsar. In the high refinement of his features, in the bronzed

complexion and soft brown eyes, the Kurd made a striking contrast

to the Cossacks--a contrast by no means to the advantage of the

Cis-Caucasian race. The young chief is also worthy to be remembered

in respect of the remarkable name which he bears. His Kurdish title

of Shamden Agha has been developed and embroidered into the sonorous

appellation of Hasan Bey Shamshadinoff, under which he is officially

known.

From the edge of the platform upon which we were standing the ground

falls away with some abruptness down to the base below, and lends

to the valley its characteristic appearance of an elevated stage and

natural viewing-place, overtowered by the summit regions of the dome

and the pyramid, and commanding all the landscape of the plain. On the

south-west, as it rises towards the pass between the two mountains--a

pass of 8800 feet, leading into Turkish and into Persian territory,

to Bayazid or Maku--the extent of even ground which composes this

platform cannot much exceed a quarter of a mile. It is choked by the

rocky causeways which, sweeping down the side of Great Ararat, tumble

headlong to the bottom of the fork, and, taking the inclination of

the ever-widening valley, descend on the north-western skirt of the

platform in long, oblique curves of branching troughs and ridges,

falling fanwise over the base. The width of the platform, at the mouth

of the valley, may be about three-quarters of a mile. It is here that

the Kurds of the surrounding region gather, as the shades of night

approach, to water their flocks at the lonely pool which is known as

the sirdar's well. On the summit of the lesser Ararat there is a little

lake, formed of melted snows; the water permeates the mountain, and

feeds the sirdar's pool. Close by, at the foot of the lesser mountain,

is the famous covert of birch--low bushes, the only stretch of wood

upon the fabric, which is entirely devoid of trees. The wood was

soon crackling upon our fires, and the water hissing in the pots;

but the wretched pack-horses, upon which our tents had been loaded,

were lagging several hours behind. We ourselves had reached camp at six

o'clock; it was after nine before our baggage arrived. As we stretched

upon the slope, the keen air of the summit region swept the valley

and chilled us to the skin; the temperature sank to below freezing,

and we had nothing but the things in which we stood. [72] Our friends,

the Cossack officers, were lavish of assistance; they wrapped us in the

hairy coats of the Caucasus, placed vodki and partridges before us, and

ranged us around their hospitable circle, beside the leaping flames.

But the mind was absent from the picturesque bivouac, and the eye

which ranged the deepening shadows was still dazzled by the evening

lights. Mind and sense alike were saturated with the beauty and

the brilliance of the landscape, which, as you rise towards the

edge of the platform after rounding the mass of Takjaltu, opens

to an ever-increasing perspective, with ever-growing clearness of

essential features and mystery gathering upon all lesser forms. The

sun, revolving south of the zenith, lights the mountains on the north

of the plain, and fills all the valley from the slopes of Ararat

with the full flood of his rays--tier after tier of crinkled hummock

ranges, aligned upon the opposite margin of the valley at a distance of

over twenty miles, their summit outline fretted with shapes of cones

and craters, their faces buttressed in sand, bare and devoid of all

vegetation, yet richly clothed in lights and hues of fairyland--ochres

flushed with delicate madder, amethyst, shaded opaline, while the

sparse plantations about the river and the labyrinth of the plain

insensibly transfigure, as you rise above them, into an impalpable

web of grey. In the lap of the landscape lies the river, a thin,

looping thread--flashes of white among the shadows, in the lights a

bright mineral green. Here and there on its banks you descry a naked

mound--conjuring a vision of forgotten civilisations and the buried

hives of man. It is a vast prospect over the world.... Yet vaster far

is the expanse you feel about you beyond the limits of sight. It is

nothing but a segment of that expanse, a brief vista from north to

east between two mountain sides. On the north the slopes of Great

Ararat hide the presence of Alagöz, while behind the needle form of

Little Ararat all the barren chains and lonely valleys of Persia are

outspread.... The evening grows, and the sun's returning arc bends

behind the dome of snow. The light falls between the two mountains, and

connects the Little Ararat in a common harmony with the richening tints

of the plain. There it stands on the further margin of the platform,

the clean, sharp outline of a pyramid, clothed in hues of a tender

yellow, seamed with violet veins. At its feet, where its train sweeps

the floor of the river valley in long and regular folds--far away in

the east, towards the mists of the Caspian--the sandy ground breaks

into a troubled surface, like angry waves set solid under a spell,

and from range to range stretch a chain of low white hummocks, like

islands across a sea. Just there, in the distance, beneath the Little

Ararat, you see a patch of shining white, so vivid that it presents

the appearance of a glacier, set in the burnt waste. It is probably

caused by some chemical efflorescence, resting on the dry bed of a

lake. All the landscape reveals the frenzy of volcanic forces, fixed

for ever in an imperishable mould; the imagination plays with the forms

of distant castles and fortresses of sand. Alone the slopes about you

wear the solid colours, and hold you to the real world--the massive

slopes of Great Ararat, raised high above the world. The wreath of

cloud which veils the summit till the last breath of warm air dies

has floated away in the calm heaven before the western lights have

paled. Behind the lofty piles of rocky causeways, concealing the

higher seams, rises the immediate roof of Ararat foreshortened in

the sky--the short side or gable of the dome, a faultless cone of snow.

When we drew aside the curtain of our tent next morning, full daylight

was streaming over the open upland valley, and the vigorous air had

already lost its edge. [73] The sun had risen high above the Sevan

ranges, and swept the plain below us of the lingering vapours which

at morning cling like shining wool to the floor of the river valley,

or float in rosy feathers against the dawn. The long-backed Cossack

horses had been groomed and watered and picketed in line; the men

were sitting smoking in little groups or were strolling about the

camp in pairs (Fig. 32). A few Kurds, who had come down with milk

and provisions, stood listlessly looking on, the beak nose projecting

from the bony cheeks, the brown chest opening from the many-coloured

tatters draped about the shoulders and waist.

The space of level ground between the two mountains cannot much exceed

three-quarters of a mile. On the east the graceful seams of Little

Ararat rise immediately from the slope upon our right, gathering just

beyond the covert of low birchwood, and converging in the form of a

pyramid towards a summit which has been broken across the point. The

platform of this valley is a base for Little Ararat--the rib on the

flank of the greater mountain from which the smaller proceeds. So

sharp are the lines of the Little Ararat, so clean the upward

slope, that the summit, when seen from this pass or saddle, seems

to rise as high in the heaven above us as the dome of Great Ararat

itself. The burnt grass struggles towards the little birch covert,

but scarcely touches the higher seams. The mountain side is broken

into a loose rubble; deep gullies sear it in perpendicular furrows,

which contribute to the impression of height. The prevailing colour

of the stones is a bleached yellow verging upon a delicate pink; but

these paler strata are divided by veins of bluish andesite pointing

upwards, like spear-heads, from the base (Fig. 33).

Very different, on the side of Great Ararat, are the shapes which

meet the eye. We are facing the south-eastern slope of the mountain,

the slope which follows the direction of its axis, the short side or

gable of the dome. In the descending train of the giant volcano this

valley is but an incidental or lesser feature; yet it marks, and in

a sense determines, an important alteration in the disposition of the

surface forms. It is here that the streams of molten matter descending

the mountain side have been arrested and deflected from their original

direction, to fall over the massive base. The dam or obstacle which

has produced this deviation is the sharp, harmonious figure of the

lesser Ararat, emerging from the sea of piled-up boulders, and cleaving

the chaos of troughs and ridges like the lofty prow of a ship. The

course of these streams of lava is signalised by these causeways of

agglomerate rocks; you may follow from a point of vantage upon the

mountain the numerous branches into which they have divided to several

parent or larger streams. On this side of Ararat they have been turned

in an oblique direction, from south-east towards north-east; they skirt

the western margin of the little valley, curving outwards to the river

and the plain. It is just beneath the first of these walls of loose

boulders that our two little tents are pitched; beyond it you see

another, and yet another still higher, and above them the dome of snow.

The distance from this valley of the summit of Great Ararat, if we

measure upon the survey of the Russian Government along a horizontal

line, is rather over 5 miles. The confused sea of boulders, of which

I have just described the nature, extends, according to my own

measurements, to a height of about 12,000 feet. Above that zone,

so arduous to traverse, lies the summit region of the mountain,

robed in perpetual snow. From whatever point you regard that summit

on this south-eastern side, the appearance of its height falls short

of reality in a most substantial degree. Not only does the curve of

the upward slope lend itself to a most deceitful foreshortening when

you follow it from below, but, indeed, the highest point or crown of

the dome is invisible from this the gable side.

If you strike a direct course from the encampment towards the roof

of snow, and, crossing the grain of successive walls and depressions,

emerge upon some higher ridge, the numerous ramifications of the lava

system may be followed to their source, and are seen to issue from

larger causeways which rise in bold relief from the snows of the summit

region, and open fanwise down the higher slopes (Fig. 34). In shape

these causeways may be said to resemble the sharp side of a wedge; the

massive base from which the bank rises narrows to a pointed spine. As

the eye pursues the circle of the summit where it vanishes towards the

north, these ribs of rock which radiate down the mountain diminish in

volume and relief. Their sharp edges commence to cut the snowy canopy

about 3000 feet below the dome. It is rather on this south-eastern

side of Ararat, the side which follows the direction of the axis of

the fabric--the line upon which the forces have acted by which the

whole fabric has been reared--that a formation so characteristic of the

surface of the summit region at once attains its greatest development,

and is productive of a phenomenon which cannot fail to arrest the

eye. At a height of about 14,000 feet, a causeway of truly gigantic

proportions breaks abruptly from the snow. The head of the ridge is

bold and lofty, and towers high above the snow-slope with steep and

rocky sides. The ridge itself is in form a wedge or triangle, cut

deep down into the side of the mountain, and marked along the spine

by a canal-shaped depression which accentuates the descending curve

(see Fig. 34). The troughs and ridges, which you will now be crossing,

have their origin in this parent ridge; you see it bending outwards,

away from Little Ararat, and dividing into branches and systems

of branches as it reaches the lower slopes. Whether its want of

connection with the roof of Ararat, or the inherent characteristics of

its uppermost end, be sufficient evidence to justify the supposition of

Abich that this ridge at its head marks a separate eruptive centre on

the flank of Ararat, I am not competent adequately to discuss. I can

only observe that it is not difficult to find another explanation. It

is possible that the ridge where it narrows to the summit has been

fractured and swept away. This peak, or sharp end of the causeway,

to whatever causes its origin may be ascribed, is a distinguishing

feature on the slope of Ararat, seen far and wide like a tooth or

hump or shoulder on this the south-eastern side. [74]

Although the most direct way to the summit region leads immediately

across the zone of boulders from the camp by the sirdar's pool,

yet it is not that which most travellers have followed, or which

the natives of the district recommend. This line of approach, which

I followed for some distance a few days after our ascent, is open

to the objection that it is no doubt more difficult to scale the

slope of snow upon this side. The tract of uncovered rocks which

breaks the snow-fields, offering ladders to the roof of the dome,

is situated further to the south-east of the mountain, above the

neck of the valley of the pool. Whether it would not be more easy to

reach these ladders by skirting slantwise from the higher slopes,

is a question which is not in itself unreasonable, and which only

actual experience will decide. It was in this manner, I believe,

that the English traveller, my friend the Rt. Hon. James Bryce, made

an ascent which, as a feat, is, I think, the most remarkable of any

of the recorded climbs. Starting from the pool at one o'clock in the

morning, he reached the summit, alone, at about two in the afternoon,

accomplishing within a space of about six hours the last 5000 feet,

and returning to the point from which he started before sunrise on

the following day. We ourselves were advised to follow up the valley,

keeping the causeways upon our right, and only then, when we should

have reached a point about south-east of the summit, to strike across

the belt of rock.

At twenty minutes before two on the 18th of September our little party

left camp in marching order, all in the pride of health and spirits,

and eager for the attack. Thin wreaths of cloud wrapped the snows of

the summit--the jealous spell which baffles the bold lover even when he

already grasps his prize. We had taken leave of the Cossack officers

and their band of light-hearted men. Our friends were returning to

Akhury and Aralykh, the one body to hunt the Kurds of the frontier,

the other to languish in dull inactivity until their turn should

come round again. Four Cossacks were deputed to remain and guard

our camp; we ourselves had decided to dispense with any escort

and to trust to our Kurdish allies. Of these, ten sturdy fellows

accompanied us as porters to carry our effects, their rifles slung

over their many-coloured tatters beside the burden allotted to each

(Fig. 35). With my cousin and myself were the young Swiss, Rudolph

Taugwalder, a worthy example of his race and profession--the large

limbs, the rosy cheeks, the open mien without guile--and young Ernest

Wesson, fresh from the Polytechnic in London, burning to distinguish

himself. My Armenian dragoman followed as best he was able until

the camp at the snow was reached; his plump little figure was not

well adapted to toil over the giant rocks. Of our number was also

an Armenian from Akhury, who had tendered his services as guide;

he was able to indicate a place for our night's encampment, but he

did not venture upon the slope of snow.

A little stream trickles down the valley, but sinks exhausted at this

season before reaching the sirdar's well. In the early summer it is

of the volume of a torrent, which winds past the encampment, like a

serpent of silver, uttering a dull, rumbling sound. [75] It is fed

by the water from the snow-fields, and there is said to be a spring

which contributes to support it at a height of nearly 11,000 feet. [76]

After half an hour's walk over the stony surface of the platform--the

ragged herbage burnt yellow by the sun--we entered the narrows of

the mountain saddle, and followed the dry bed of this rivulet at the

foot of rocky spurs. The tufts of sappy grass sparsely studded on the

margin of the water-course gave place, as we advanced, to a continuous

carpet of soft and verdant turf; here and there the eye rested on the

deep green of the juniper, or the graceful fretwork of a wild rose tree

quivered in the draught. The warm rays flashed in the thin atmosphere,

and tempered the searching breeze. The spurs on our right descend

from the shoulder of Great Ararat, from the causeway of which it forms

the head, and are seen to diverge into two systems as they enter the

narrow pass. The one group pushes forward to the Little Ararat and

is lost in confused detail; the other and, perhaps, the larger system

bends boldly along the side of the valley, sweeping outwards towards

the base. At three o'clock we reached a large pool of clouded water,

collected on a table surface of burnt grass; close by is an extensive

bed of nettles, and a circle of loose stones. This spot is, no doubt,

the site of a Kurdish encampment, and appeared to have been only

recently abandoned by the shepherds and their flocks. The further we

progressed, the more the prospect opened over the slopes of Ararat;

we were approaching the level of the tops of the ridges which skirt

the valley side. Passing, as we now were, between the two Ararats,

we again remarked that the greater seemed no higher than the lesser,

so completely is the eye deceived. In the hollows of the gully there

were small pools of water, but the stream itself was dry.

By half-past three we had left the gentle water-course, and were

winding inwards, up the slope of Great Ararat, to cross the black and

barren region, the girdle of sharp crags and slippery boulders which

is drawn round the upper seams of the mountain, like a succession of

chevaux de frise. We thought it must have been on some other side

of Ararat that the animals descended from the Ark. For a space of

more than three hours we laboured on over a chaos of rocks, through a

labyrinth of troughs and ridges, picking a path and as often retracing

it, or scrambling up the polished sides of the larger blocks which

arrest the most crafty approach. The Kurds, although sorely taxed

by their burdens, were at an advantage compared to ourselves; they

could slip, like cats, from ledge to ledge in their laced slippers of

hide. In one place we passed a gigantic heap of boulders, towering

several hundred feet above our heads. The rock is throughout of the

same character and colour--an andesitic lava of a dark slaty hue. A

little later we threaded up a ravine or gully, and, after keeping for

awhile to the bottom of the depression, climbed slowly along the back

of the ridge. I noticed that the grain or direction of the formation

lay towards east-south-east. From the head of this ravine we turned

into a second, by a natural gap or pass; loose rocks were piled along

the sides of the hollow, which bristled with fantastic, but unreal,

shapes. Here a seated group of camels seemed to munch in silence

on the line of fading sky, or the knotty forms of lifeless willows

stretched a menace of uplifted arms. In the sheltered laps of this

higher region, as we approached our journey's end, the snow still

lay in ragged patches, which increased in volume and depth.... The

surface cleared, the view opened; we emerged from the troubled sea of

stone. Beyond a lake of snow and a stretch of rubble rose the ghostly

sheet of the summit region, holding the last glimmer of day.

It was seven o'clock, and we had no sooner halted than the biting

frost numbed our limbs. [77] The ground about us was not uneven, but

an endless crop of pebbles filled the plainer spaces between little

capes of embedded rock. At length upon the margin of the snow-lake we

found a tiny tongue of turf-grown soil--just sufficient emplacement

to hold the flying tent which we had brought for the purpose of this

lofty bivouac near the line of continuous snow. We were five to share

the modest area which the sloping canvas enclosed; yet the temperature

in the tent sank below freezing before the night was done. Down the

slope beside us the snow water trickled beneath a thin covering of

ice. The sheep-skin coats which we had brought from Aralykh protected

us from chill, but the hardy Kurds slept in their seamy tatters upon

the naked rocks around. One among them sought protection as the cold

became intenser, and we wrapped him in a warm cape. It was the first

time I had passed the night at so great an elevation--12,194 feet above

the sea--and it is possible that the unwonted rarity of the atmosphere

contributed to keep us awake. But, whether it may have arisen from the

conditions which surrounded us, or from a nervous state of physical

excitement inspired by our enterprise, not one among us, excepting

the dragoman, succeeded in courting sleep. That plump little person

had struggled on bravely to this his furthest goal, and his heavy

breathing fell upon the silence of the calm, transparent night.

The site of our camp below the snow-line marks a new stage, or

structural division, in the fabric of Ararat. Of these divisions,

which differ from one another not only in the characteristics presented

by each among them, but also in the gradient of slope, it is natural

to distinguish three. We are dealing in particular with that section

of the mountain which lies between Aralykh and the summit, and with

the features of the south-eastern side. First, there is the massive

base of the mountain, about 10 miles in depth, extending from the

floor of the river valley to a height of about 6000 feet. At that

point the higher seams commence to gather, and the belt of rock

begins. The arduous tracts which we had just traversed, where large,

loose blocks of hard, black lava are piled up like a beach, compose

the upper portion of this middle region, and may be said to touch the

lower margin of the continuous fields of snow. The line of contact

between the extremities of the one and the other stage partakes of the

nature of a transitional system, a neutral zone on the mountain side,

where the rocky layers of the middle slopes have not yet shelved away,

nor the immediate seams of the summit region settled to their long

climb. In this sense the fields of stone about our encampment, with

their patches of last year's snow, are invested with the attributes

of a natural threshold at the foot of the great dome. The stage which

is highest in the structure of Ararat, the stage which holds the dome,

has its origin in this threshold, or neutral district, at an altitude

which varies between 12,000 and 13,000 feet.

Very different in character and in appearance from the region we were

leaving behind was the slope which faced our encampment, robed in

perpetual snow. You have pursued the ramifications of the lava system

to the side of their parent stems; and in place of blind troughs and

prospectless ledges a noble singleness of feature breaks upon the

extricated view. You command the whole summit structure of Ararat

on the short, or gable side; and the shape which rises from the open

ground about you is that of a massive cone. The regular seams which

mount to the summit stretch continuous to the crown of snow, and are

inclined at an angle which diverges very little from an average of

30°. The gradients from which these higher seams gather--the slopes

about our camp--cannot exceed half that inclination, or an angle of

15°. Such is the outline, so harmonious and simple, which a first

glance reveals.... A more intimate study of the summit region, as it

expands to a closer view, disclosed characteristics which were not

exactly similar to those with which we had already become familiar in

the neighbourhood of Sardar Bulakh. It was there the north-eastern

hemisphere of the mountain--if the term may be applied to the oval

figure which the summit region presents--displayed to the prospect upon

the segment between east and south-east. Our present position lay more

to the southward, between the two hemispheres; we were placed near the

axis of the figure, and the roof, as viewed from our encampment, bore

nearly due north-west. The gigantic causeway which at Sardar Bulakh

was seen descending on our left hand from the distant snows, now rose

on our right, like a rocky headland, confronting a gleaming sea of

ice. But, when the eye pursues the summit circle vanishing towards

the west, you miss the sister forms of lesser causeways, radiating

down the mountain side. It is true that the greater proximity of our

standpoint to the foot of these highest slopes curtailed the segment

of the circle which we are able to command. This circumstance is not

in itself sufficient to explain the change in the physiognomy of the

summit region, as we see it on this side. In place of those bold,

black ribs or ridges, spread fanwise down the incline, furrowing the

snows with their sharp edges, and lined along the troughs of their

contiguous bases with broad streaks of sheltered nevé, it seems as

if the fabric had fallen asunder, the surface slipped away--all the

flank of the mountain depressed and hollow, from our camp to the

roof of the dome. The canopy of snow which encircles the summit--a

broad, inviolate bank, unbroken by any rift or rock projection for

a depth of some 2000 feet--breaks sharply off on the verge of this

depression, and leaves the shallow cavity bare. From the base of the

giant causeway just above us to the gently-pursing outline of the

roof you follow the edge of the great snow-field, bordering a rough

and crumbling region which offers scanty foothold to the snow, where

the hollow slope bristles with pointed boulders, and the bold crags

pierce the ruin around them in upstanding combs or saw-shaped ridges,

holding slantwise to the mountain side. On the west side of this broad

and uncovered depression, near the western extremity of the cone,

a long strip of snow descends from the summit, caught by some trough,

or sheltering fissure, in the rough face of the cliff. Beyond it, just

upon the sky-line, the bare rocks reappear, and climb the slope, like

a natural ladder, to a point where the roof of the dome is lowest and

appears to offer the readiest access to the still invisible crown. [78]

In the attenuated atmosphere surrounding the summit every foot that is

gained tells. An approach which promises to ease the gradient at the

time when it presses most seems to offer advantages which some future

traveller may be encouraged to essay. We ourselves were influenced

in the choice of a principle upon which to base our attack by the

confident counsels of the Armenian, which the local knowledge of

the Kurds confirmed. We were advised to keep to the eastern margin

of the depression, by the edge of the great snow-field. You see the

brown rocks still baffling the snow-drifts near the point where the

deceitful slope appears to end, where on the verge of the roof it

just dips a little, then stands up, like a low white wall, on the

luminous ground of blue.

The troubled sea of boulders flowing towards the Little Ararat, from

which we had just emerged, still hemmed us in from any prospect over

the tracts which lay below. The flush of dawn broke between the two

mountains from a narrow vista of sky. The even surface of the snow

slope loomed white and cold above our heads, while the night still

lingered on the dark stone about us, shadowing the little laps of

ice. Before six o'clock we were afoot and ready; it wanted a few

minutes to the hour as we set out from our camp. To the Swiss was

entrusted the post of leader; behind him followed in varying order

my cousin and Wesson and myself. Slowly we passed from the shore of

the snow-lake to the gathering of the higher seams, harbouring our

strength for the steeper gradients as we made across the beach of

boulders, stepping firmly from block to block.

The broad, white sheet of the summit circle descends to the snow-lakes

of the lower region in a tongue, or gulf of deep nevé; you may

follow on the margin of the great depression the western edge of this

gleaming surface unbroken down the side of the cone. On the east the

black wall of the giant causeway borders the shining slope, invading

the field of perpetual winter to a height of over 14,000 feet. The

width of the snow-field between these limits varies as it descends;

on a level with the shoulder, or head of the causeway, it appeared to

span an interval of nearly 200 yards. [79] The depth of the bed must

be considerable, and, while the surface holds the tread in places,

it as often gives and lets you through. No rock-projection, or gap,

or fissure breaks the slope of the white fairway; but the winds have

raised the crust about the centre into a ribbon of tiny waves. Our

plan was to cross the stony region about us, slanting a little east,

and to mount by the rocks on the western margin of the snow-field,

adhering as closely as might be possible to the side of the snow. It

was in the execution of this plan--so simple in its conception--that

the trained instinct of the Swiss availed. Of those who have attempted

the ascent of Ararat--and their number is not large--so many have

failed to reach the summit that, upon a mountain which makes few,

if any, demands upon the resources of the climber's craft, their

discomfiture must be attributed to other reasons: to the peculiar

nature of the ground traversed, no less than to the inordinate

duration of the effort; to the wearisome recurrence of the same kind

of obstacles, and to the rarity of the air. Now the disposition of

the rocks upon the surface of the depression is by no means the same

as that which we have studied in connection with the seams which lie

below. The path no longer struggles across a troubled sea of ridges,

or strays within the blind recesses of a succession of gigantic waves

of stone. On the other hand, the gradients are as a rule steeper;

and the clearings are covered with a loose rubble, which slips from

under the feet. The boulders are piled one upon another in heaps

as they happened to fall, and the sequence of forms is throughout

arbitrary and subject to no fixed law. In one place it is a tower of

this loose masonry which blocks all further approach; in another a

solid barrier of sharp crags, laced together, which it is necessary

to circumvent. When the limbs have been stiffened and the patience

exhausted by the long and devious escalade, the tax upon the lungs

is at its highest, and the strain upon the heart most severe. Many of

the difficulties which travellers have encountered upon this stage of

the climb may be avoided, or met at a greater advantage, by adhering

to the edge of the snow. But the fulfilment of this purpose is by no

means so easy as might at first sight appear. You are always winding

inwards to avoid the heaps of boulders, or emerging on the backs of

gigantic blocks of lava towards the margin of the shining slope. In

the choice of the most direct path, where many offered, the Swiss was

never at fault; he made up the cone without a moment's hesitation,

like a hound threading a close covert, and seldom if ever foiled.

At twenty minutes to seven, when the summit of Little Ararat was

about on a level with the eye, we paused for awhile and turned

towards the prospect, now opening to a wider range. The day was

clear, and promised warmth; above us the snowy dome of Ararat shone

in a cloudless sky. The landscape on either side of the beautiful

pyramid lay outspread at our feet; from north-east, the hidden

shores of Lake Sevan, to where the invisible seas of Van and Urmi

diffused a soft veil of opaline vapour over the long succession of

lonely ranges in the south-east and south. The wild borderland of

Persia and Turkey here for the first time expands to view. The scene,

however much it may belie the conception at a first and hasty glance,

bears the familiar imprint of the characteristics peculiar to the

great tableland. The mountains reveal their essential nature and

disclose the familiar forms--the surface of the tableland broken

into long furrows, of which the ridges tend to hummock shapes. So

lofty is the stage, so aloof this mighty fabric from all surrounding

forms, the world lies dim and featureless about it like the setting

of a dream. In the foreground are the valleys on the south of Little

Ararat, circling round to the Araxes floor; and, on the north-east,

beside the thread of the looping river, is a little lake, dropped

like a turquoise on the sand where the mountain sweeps the plain.

In the space of another hour we had reached an elevation about equal

to that of the head of the causeway on the opposite side of the snow,

a point which I think we should be justified in fixing at over 14,000

feet. [80] We were now no longer threading along the shore of an inlet;

alone the vague horizon of the summit circle was the limit of the

broad, white sea. But on our left hand the snowless region of rock

and rubble still accompanied our course, and a group of red crags

stood up above our heads, just where the upward slope appeared to end.

Yet another two hours of continuous climbing, and, at about half-past

nine, the loose boulders about us open, and we are approaching the

foot of these crags. The end seems near; but the slope is deceitful,

and when once we have reached the head of the formation the long

white way resumes. But the blue vault about us streams with sunlight;

the snow is melting in the crannies; a genial spirit lightens our toil.

And now, without any sign or warning, the mysterious spell which holds

the mountain begins to throw a web about us, craftily, from below. The

spirits of the air come sailing through the azure with shining gossamer

wings, while the heavier vapours gather around us from dense banks

serried upon the slope beneath us, a thousand feet lower down.

The rocks still climb the increasing gradient, but the snow is

closing in. At eleven we halt to copy an inscription, which has

been neatly written in Russian characters on the face of a boulder

stone. It records that on the third day of the eighth month of 1893

the expedition led by the Russian traveller Postukhoff passed the

night in this place. At the foot of the stone lie several objects:

a bottle filled with fluid, an empty tin of biscuits, a tin containing

specimens of rock.

At half-past eleven I take the angle of the snow slope, at this

point 35°. About this time the Swiss thinks it prudent to link us all

together with his rope. The surface of the rocks is still uncovered,

but their bases are embedded in deep snow.

It is now, after six hours' arduous climbing, that the strain of the

effort tells. The lungs are working at the extreme of their capacity,

and the pressure upon the heart is severe. At noon I call a halt, and

release young Wesson from his place in the file of four. His pluck is

still strong, but his look and gait alarm me, and I persuade him to

desist. We leave him to rest in a sheltered place, and there await

our return. From this time on we all three suffer, even the Swiss

himself. My cousin is affected with mountain sickness; as for me, I

find it almost impossible to breathe and climb at the same time. We

make a few steps upwards and then pause breathless, and gasp again

and again. The white slope vanishing above us must end in the crown

of the dome; and the boulders strewn more sparsely before us promise

a fairer way. But the further we go, the goal seems little closer;

and the shallow snow, resting on a crumbling rubble, makes us lose

one step in every three. A strong smell of sulphur permeates the

atmosphere; it proceeds from the sliding surface upon which we are

treading, a detritus of pale sulphurous stones.

At 1.25 we see a plate of white metal, affixed to a cranny in the

rocks. It bears an inscription in Russian character which dates from

1888. I neglect to copy out the unfamiliar letters; but there can be

little doubt that they record the successful ascent of Dr. Markoff,

an ascent which cost him dear.

A few minutes later, at half-past one, the slope at last eases,

the ground flattens, the struggling rocks sink beneath the surface

of a continuous field of snow. At last we stand upon the summit of

Ararat--but the sun no longer pierces the white vapour; a fierce gale

drives across the forbidden region, and whips the eye straining to

distinguish the limits of snow and cloud. Vague forms hurry past on

the wings of the whirlwind; in place of the landscape of the land of

promise we search dense banks of fog.

Disappointed perhaps, but relieved of the gradient, and elated with

the success of our climb, we run in the teeth of the wind across the

platform, our feet scarcely sinking in the storm-swept crust of the

surface, the gently undulating roof of the dome.... Along the edge of

a spacious snow-field which dips towards the centre, and is longest

from north-west to south-east, on the vaulted rim of the saucer which

the surface resembles, four separate elevations may conveniently be

distinguished as the highest points in the irregular oval figure which

the whole platform appears to present. The highest among these rounded

elevations bears north-west from the spot where we first touch the

summit or emerge upon the roof. That spot itself marks another of

these inequalities; the remaining two are situated respectively in

this manner--the one about midway between the two already mentioned,

but nearer to the first and on the north side; the other about south

of the north-western elevation, and this seems the lowest of all. The

difference in height between the north-western elevation and that upon

the south-east is about 200 feet; and the length of the figure between

these points--we paced only a certain portion of the distance--is

about 500 yards. The width of the platform, so far as we could gauge

it, may be some 300 yards. A single object testifies to the efforts

of our fore-runners and to the insatiable enterprise of man--a stout

stake embedded upon the north-western elevation in a little pyramid

of stones. It is here that we take our observations, and make our

longest halt. [81] Before us lies a valley or deep depression, and on

the further side rises the north-western summit, a symmetrical cone of

snow. This summit connects with the bold snow buttresses beyond it,

terraced upon the north-western slope. The distance down and up from

where we stand to that summit may be about 400 yards; but neither

the Swiss nor ourselves consider it higher, and we are prevented

from still further exploring the summit region by the increasing

violence of the gale and by the gathering gloom of cloud. The sides

and floor of the saddle between the two summits are completely covered

with snow, and we see no trace of the lateral fissure which Abich,

no doubt under different circumstances, was able to observe.

We remain forty minutes upon the summit; but the dense veil never lifts

from the platform, nor does the blast cease to pierce us through. No

sooner does an opening in the driving vapours reveal a vista of the

world below than fresh levies fly to the unguarded interval, and

the wild onset resumes. Yet what if the spell had lost its power,

and the mountain and the world lain bare? had the tissue of the air

beamed clear as crystal, and the forms of earth and sea, embroidered

beneath us, shone like the tracery of a shield?

We should have gained a balloon view over Nature. Should we catch her

voice so well?--the ancient voice heard at cool of day in the garden,

or the voice that spoke in accents of thunder to a world condemned

to die. "It repented the Lord that he had made man, and it grieved

him at his heart. The earth was filled with violence: God looked

upon the earth and behold it was corrupt. In the second month, the

seventeenth day of the month, the same day were all the fountains of

the great deep broken up and the windows of heaven were opened. And

the rain was upon the earth forty days and forty nights."

We are standing on the spot where the ark of gopher rested, where first

the patriarch alighted on the face of an earth renewed. Before him

lie the valleys of six hundred years of sorrow; the airiest pinnacle

supports him, a boundless hope fills his eyes. The pulse of life beats

strong and fresh around him; the busy swarms thrill with sweet freedom,

elect of all living things. In the settling exhalations stands the

bow of many colours, eternal token of God's covenant with man.

The peaks which rise on the distant borderland where silence has

first faltered into speech are wrapped about with the wreaths of

fancy, a palpable world of cloud. Do we fix our foot upon these solid

landmarks to wish the vague away, to see the hard summits stark and

naked, and all the floating realm of mystery flown? The truth is firm,

and it is well to touch and feel it and know where the legend begins;

but the legend itself is truth transfigured, as the snow distils into

cloud. The reality of life speaks in every syllable of that solemn,

stately tale--divine hope bursting the bounds of matter to compromise

with despair. And the ancient mountain summons the spirits about him,

and veils a futile frown, as the rising sun illumines the valleys

of Asia and the life of man lies bare. The spectres walk in naked

daylight--Violence and Corruption and Decay. The traveller finds in

majestic Nature consolation for these sordid scenes; while a spirit

seems to whisper in his ears, "Turn from him!--turn from him, that

he may rest till he shall accomplish, as an hireling, his day."

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