CHAPTER XV

L'AIGOUAL

Meteorological station—Battle of the winds—Warnings of

floods—Different aspects of the Aigoual—The Garden of

God—Meyrueis—Bramabiau—Exploration of—Valleraugue—Roman

road—Barre—Limestone cirques—Causse de l'Hospitalet—Florac—Dirty

streets—Mimente—Cassagnas—Fontaine du Pêcher—The

Dourbie—Trèves—Baume de S. Firmin—Prehistoric man—Nant—Source of

the Durzon—Cantobre—S. Veran—Roquesaltes.

The Aigoual is the hinge or knot of the inner range of the Cévennes,

as Mézenc is that of the outer range. On one of its summits sits a

meteorological observatory astride on the ridge of the watershed.

Indeed, so exactly is it so placed, that the rain pouring off the roof

on one side reaches the Mediterranean, whereas that off the other side

goes to replenish the Atlantic.

[Illustration: PEASANT GIRLS OF THE CAUSSES]

The station is admirably calculated for the purpose, as thence can be

watched the atmospheric currents as they sweep from the north or from

the south, and the battle of the winds may be contemplated when the

northern blast rolls back the moisture-laden currents from the south.

This battle of the winds is an interesting phenomenon. Occasionally

it happens that a veil of mist rising from the Mediterranean is

swept forward, obscuring the landscape as it gathers density, and is

propelled by the south-east wind till it reaches the Cévennes. It

gradually becomes thicker and darker, packing in the valleys and then

creeping up the heights. No sooner, however, has it reached the summit

of the chain, than it is caught by the north-west wind and sent back in

flying streamers, like the mare's tails we are accustomed to see in our

skies presaging a change of wind, but with this difference, that these

streamers are viewed from above.

The north wind gathering strength, as though mustering its forces

against the audacious invasion of the southern vapours, rages and

blusters for several days. Meanwhile the south-east wind is still

thrusting forward volumes of vapour and compacting them in the gorges

and valleys, cautiously throwing up a tentacle towards the heights, up

lateral ravines, as though to feel whether the north wind is still on

the alert. Should Boreas slacken his efforts, then the clouds climb

the mountain sides like storming parties and reach the battlements.

But their success is momentary only. The north wind has been dozing,

and awakes to resume the combat. The heavily charged clouds, packed

beyond endurance in the valleys, can make no progress, and the volleys

of ice-cold wind overhead condense the mist and bring about torrential

rains, accompanied by incessant explosions of thunder and lightning.

In a few minutes the granitic or limestone cliffs are seamed with

cascades. The silver thread that meandered through the meadows below is

transformed into a yellow raging torrent, carrying before it masses of

rock torn from the mountain side, trees, the wreckage of enclosures,

houses even with their inhabitants. The rivers hitherto sliding through

rubbly beds, vastly out of proportion to their diminutive size, swell

to the brim and overflow, carrying devastation on every side. As in

the story of Puss in Boots the magician transforms himself into a mouse

at one moment and into an elephant at another, so is it with these

Cevenol rivers—what is a rill to-day is like the Thames to-morrow.

Those in the Observatory on the Aigoual perform a most valuable

service. They can predict the coming of a flood, and they telegraph

to all villages and towns that are menaced, to be on their guard, and

evacuate dwellings on low ground, and remove their cattle to heights.

The inmates of the Observatory have become very weatherwise, and note

many indications of an approaching tempest. One that is infallible in

summer is the conduct of the bees. These shrewd insects, that have

been humming and honey-gathering among the wild thyme, fly to the

Observatory and cling to the panes, darkening them, and remaining

motionless till the atmospheric disturbance is over.

How furious the wind may be, and what a force it exercises on the

Aigoual, may be judged by looking at the refuge of the Touring Club

that is fastened to the rock by chains, like the ropes of a tent.

The Mont Lozère, though higher than the Aigoual, is not so subject to

these veritable tornadoes. There the wind blows almost invariably from

the north. The Cevenol peasant says:

"Se lo nibou bén de l'Oual prén tons bioous et baï o l'oustal.

Se lo nibou bén de Louzero, prén tons bioous et baï o lo rego";

which may be rendered, "If the cloud comes from the Aigoual, take your

oxen and go to the stable. If the cloud comes from the Lozère, take

your oxen and go to the furrow."

The Aigoual is a granitic mass, reaching to 5,140 feet, whereas the Roc

de Malpertus, in the Mont Lozère group, rises to 5,520 feet, but this

latter is far less suitable for meteorologic observation. Around the

Aigoual erosion has formed a labyrinth of gorges and profound valleys,

in the beds of which race torrents impatient to reach lower levels.

From the side of Merueys, the Aigoual does not present by any means

an imposing appearance. It is a domed green mass, on the top of which

gleam white the walls of the Observatory. From the side of La Luzette

it bears some resemblance to a huge antediluvian monster in a crouching

posture with fore paws extended.

On the south side the Aigoual is rugged and abrupt. Its precipices

descend to great depths. The stream of the Claron there in a succession

of falls drops to the depth of 3,000 feet in a very short distance.

The Aigoual has two heads, one of these, La Fayède, looking towards the

sun-bathed basin of the Rhône; the other, that of the Hort Dieu, the

loftiest but the least picturesque. Between these is a coombe, watered

by a thousand springs that ooze from the turf and nourish a rich

vegetation. It is this coombe really which is the Garden of God, as the

natives term it.

On the one side the Aigoual rises out of mulberry and chestnut woods,

torn and precipitous; on the other it is smooth and velvety, wooded

only with distorted beech. It has been ravaged by the merciless axe

of the peasant that has left it bald and desolate. From the summit

a superb view is obtained of the tossed and torn ridges of schist

mountain, some rounded, but furrowed like the face of one very aged,

some starting up into peaks, some stretching out saw-like ridges, some

flat-headed, according to the nature of the rock of which composed. To

the north rises the Tarnon that passes by Florac, below which it enters

the Tarn. A little to the north-east is the Signal de l'Hospitalet,

and beyond Barre des Cévennes. The old Roman road ran over this latter

col to penetrate into the heart of the Cévennes; it kept to the crest,

commanding glorious views.

The Aigoual should be ascended from Meyrueis, a little town half the

population of which is Protestant. Near it, and on the way, is the

Renaissance castle of Roquedols.

Here one passes abruptly from the limestone to the granite, and at once

notes a corresponding difference in the flora. Among the limestone

rocks the pinks show as drops of blood. On the granite are none. The

fields by Roquedols are white with narcissus poeticus, not a flower

of that bulb is in the calcareous fields. The distance from Meyrueis

to the Aigoual is just over nineteen miles, and a carriage should

be taken at least as far as to Camprieu, where Bramabiau demands a

visit. On the top of the Aigoual a dinner and a bed may be obtained

at the Observatory. Bramabiau may also be visited from Le Vigan. The

rivulet of the Bonheur, that descends from the Col de Séyrerède near

the Aigoual, after flowing over granite and schist, encounters a mass

of Dolomitic limestone, through which it has bored a channel for a

distance of 1,200 feet. The tunnel through which it flows is in one

place open to the sky through the falling in of the roof. The name

Bramabiau given to this cavern traversed by a stream is onomatopœic,

and signifies the bellowing of a bull, as the water in time of flood

gives forth angry sounds.

Nothing surprises one more than the apparent inadequacy of the means

to the end attained. The Bonheur is but a small stream, yet the work

it has achieved is tremendous. But it must be borne in mind that where

stands Camprieu was once a lake, the water held back by the barrier of

limestone, and that the accumulated force was brought to bear on the

rock to effect this tunnel of drainage. Moreover, the rock itself was

full of holes like a sponge, with large vaults like huge bubbles in its

interior, so that it was not a solid mass through which the stream had

to bore its way. It was further aided by several springs rising within

the rock, all working in their several courses to effect their escape.

[Illustration: BRAMABIAU]

The exploration of Bramabiau was accomplished in June, 1888, by M.

Martel and his guides. They attempted first to penetrate by the opening

through which the Bonheur leaps into light again, but found that the

gallery consisted of a series of ascents, with cascades and pools;

and although by wading and with ladders they succeeded in reaching

a considerable distance, they could not attain to the point where

the stream begins to dive underground. On the following day these

indefatigable explorers attacked the tunnel from above, where the

Bonheur enters, and were able to descend to the point reached on the

preceding day, and further to pursue their course till they came out

where the stream issues, a distance as the crow flies of a kilometre.

In January, 1888, a man of Camprieu disappeared, and there was reason

to suspect he had committed suicide. As his body could not be found,

it was supposed that he had flung himself down the abyss of the

Bonheur; and, in fact, when M. Martel searched the cavern he found

the body wedged into a spot where, in the cave itself, the stream

disappears underground for a while, to again reappear and continue

its subterranean course. It goes through these vagaries twice, and

perpetrates seven cascades.

"To avoid repetitions," says M. Martel in his account of the

exploration, "I will say no more of the magic of magnesium light

under vaults lofty as Gothic naves; I must only ask of the reader

to figure, if he can in the profound night of these caverns, the

deafening roar of the falling water, the dispersion of the party

groping in all directions for passages, the flicker of the feeble

candles, the distant calls and signals, whistles, and horns, the

cords strained, and the ladders set up against steep walls, our

silhouettes magnified against the walls in shadows, and profiled

against the boiling torrent, all under vaults 150 feet high and at

the extremity of galleries of 300 feet.

"One portion of our course was effected only by a series of

gymnastics, according to the width of the gallery that varied

from three feet to ten feet, according to how far the ledges were

practicable—so we crept along, a few yards above the torrent,

clinging to the rock with our fingers, our breasts against the

wall, or else wading in the water up to our armpits. Often our

candles went out, caused by our rapid movements, or by the rush

of wind that swept through the tunnel; the drip of our soaked

clothes, the difficulty of communication amidst the roar of the

falling water, increased our difficulties tenfold."

Where the Bonheur escapes into daylight there is an immense rift in

the rocks, and out of this the stream leaps in a fall of some dignity.

Up to 1888 it was not thought possible that the Bonheur could be the

stream that issued at Bramabiau, for anything thrown in above never

issued below. But the exploration by M. Martel solved the mystery.

The stream sinks, filters through the rock, leaving above that which

is thrown in, and issues limpid at the cascade that rushes from the

entrance.

The descent of the Aigoual on the side of Valleraugue is by a thousand

steps hewn in granite and schist, and at the bottom of this is the

vegetable garden of the officials of the Observatory.

Valleraugue lies at the bottom of a cirque of mountains at the

confluence of the rivers of the Mallet and the Clareau, and it is after

their marriage that the united streams assume the name of Hérault. The

descent from the Aigoual to Valleraugue occupies two hours, the ascent

by the carriage road takes seven. Valleraugue is a busy factory town;

the population is mainly engaged in silk spinning and weaving. The

place is almost wholly Protestant. This valley of the Hérault as far

as Ganges is one of the most active in silk industry in the Cévennes.

The vegetation is wholly southern; the hillsides disposed in terraces

are planted with vines and mulberries; and ilexes abound, providing

the tanneries with their bark. "This valley," says Ardouin Dumazet,

"is a synthesis of all the somewhat severe graces of the Cevenol

land." The Roman road over l'Hospitalet has been already referred to.

It runs from Avignon to Anduze and then ascends the crest above the

Gardon, and passing under Barre stretches away to Florac. Barre itself

occupies a Gallo-Roman oppidum, of which traces remain, and throughout

the neighbourhood relics of the Roman tenure of the land are found.

After the Col d'Aire de Côte ensues a series of frightful cirques,

whose vertical walls crumble away by degrees under the action of the

weather. The flanks of the mountain are profoundly breached, and form

precipices. The nature of the rock contributes to augment the savagery

of the region. It is composed of schists steeply inclined towards the

north, and penetrated by numerous veins of porphyry that metamorphized

them. Here are needles, here masses of schist support tables of

limestone. A little triangular plateau, a lost islet of the Causse,

succeeds to the schists. This is the Can de l'Hospitalet.

"Here, atmospheric agencies have carved the strangest edifices.

Huge calcareous hats cover and overhang slender schistous

supports, shaped like the tables in a glacier. Many of these

gigantic mushrooms have reeled on their corroded stalks and are

thrown into a sloping position like fallen dolmens. The plateau of

l'Hospitalet is both picturesque and of scientific interest."[12]

Florac hardly comes within the range that I have marked out for

description, and yet some words must be given to it, as it was the

centre of the Cevenol revolt, and was the scene of several conflicts

and of the execution of Camisards.

It is a very dirty place, originally walled; the houses were so crowded

that the streets were contracted to the narrowest possible width. One

has to be careful not to walk down them before eight o'clock in the

morning, as all the slops are thrown from the windows into the street,

and may fall on the head of the incautious passenger; and here no

warning call is given, as in the narrow lanes of old Edinburgh, to put

the man in the street on his guard. What is cast forth remains where it

falls till torrential rains sweep away the accumulated filth of weeks

and even months. In the Languedoc towns that reek with evil odours, in

a country too where the hillsides are redolent with aromatic herbs,

lavender, sage, marjoram, rosemary, beds of violets, thyme in sheets,

one can hardly help repeating the lines of Bishop Heber:

"What though the spicy breezes

Blow sweet o'er Ceylon's isle,

And every prospect pleases,

Yet only man is vile."

But it is not man who is vile, _that_ he is nowhere, it is the refuse

he casts about him that is offensive, and the offensiveness is a

provision of nature to instruct him to remove it beyond the reach of

the nose. But familiarity must breed a liking for these disgusting

odours, or women would not sit on their doorsteps all day working and

chatting, and let their children play about amidst festering garbage.

Florac is, in spite of dragonades and gallows and the stake, almost

entirely Protestant. The large meeting-house contains nothing but

a pulpit and bare benches. The Catholic church is a new and mean

structure, the temple bare as a barn, the church ugly as a modern

French architect can make one.

Florac is near the influx of the Mimente into the Tarnon. The three

valleys of the Mimente, the Tarn, and the Tarnon lead into the

inextricable labyrinth of defiles in which the Camisards were able

to establish their arsenals, hospitals, and storehouses. The Mimente

rises in the mountain of Bougès, whose summit is crowned by the forest

of Altefage, where under three huge beech trees met the murderers of

the Abbé du Chayla. At Cassagnas, a village near the source of the

Mimente, the caverns may be inspected that served the Camisards as

magazines, filled with corn, wine, oil, and above all chestnuts. Roland

had established here a powder factory; the saltpetre was obtained, as

later during the European wars of Bonaparte, from the numerous caverns

that contained the bones of extinct beasts. Drugs were procured for

the wounded from Montpellier, where there were many well-wishers ready

to smuggle them into the mountains. When the water-mills for grinding

the corn were destroyed by the military commander of Languedoc, the

Camisards reverted to the use of querns. In some of the caves whole

flocks and herds were secreted; others were stored with salted meat.

Florac possesses its natural curiosity, the Fontaine du Pêcher, that

discharges the water infiltrated from the plateau of Méjan. It pours

forth in an abundant stream and forms a cascade, but the water is at

once eagerly captured for the purpose of irrigation. During the winter

and after a storm it vomits forth a torrent with a roar like that of a

lion.

After a visit to the summit of the Aigoual it would be well to

descend the Dourbie to Milau, reaching the Dourbie by the ravine of

the Trévesel. The Pas de l'Ase is a profound gorge, 1,200 feet deep,

between fiery-red dolomitic cliffs, in three stages superposed and

separated by slopes of detritus. At midday, when the sun streams down

on these rocks, the effect is dazzling. At Trèves, where are coal

mines, is the cave called the Baume de S. Firmin, and near by the ruins

of a castle.

S. Firmin was the grandson of Tonantius Ferreolus, Prefect of Gaul,

who, as we have seen, was the host of Sidonius Apollinaris. He had a

villa here, Trevido, as the town was then called, and in it he died

in the year 470. Firminus was educated by his uncle Noricus, Bishop

of Uzès, the son of Tonantius, and he in turn became bishop of the

same see, and died at the early age of thirty-seven, in the year 553,

and was succeeded by his nephew, Ferreolus; so that at that time it

is pretty clear bishoprics had become the perquisites of members of

the great families of Gallo-Roman origin. When S. Firmin visited his

grandfather or his father, at Trèves, he was wont to retire to the

cave that bears his name, for reading and devotion. Possibly the

dampness of this grotto may have sowed the seeds of the disorder from

which he died. The cave runs deep into the mountain, and is adorned

with numerous white and graceful stalactites. But it is very damp;

notwithstanding this, prehistoric man occupied it, for in the first two

halls of the grotto have been found old hearths, remains of feasts,

broken and split bones, and fragments of badly burnt pottery.

About ninety feet above the Baume de S. Firmin is another cave

forming a great vault that is filled with water during heavy rains.

Nevertheless man inhabited it at a remote period; for thence also have

been excavated numerous fragments of vessels, which by their paste and

ornamentation show that they belonged to the age of polished stone.

How the men of that period must have suffered from rheumatism! And it

has been noticed that among the bones of prehistoric man, who was a

cave dweller, rheumatic swellings of the joints are common. Usually the

caves in limestone and chalk are tolerably dry. France must have teemed

with peoples at that early period, for not only on the Causse, but

also in the chalk districts of Dordogne and Lot, and in the sandstone

regions of Maine-et-Loire and Vienne, troglodite habitations abound.

After crossing the Col de la Pierre-Plantée, the road winds down into

the valley of the Dourbie, which wriggles along at a great depth below

between rocks of quartz and schist, then passes among chestnut trees,

and reaches S. Jean-du-Bruel, when we are in the valley of the Dourbie.

Here comes in the road from Saudières, where is a station on the line

from Le Vigan to the junction on the main line opposite Roquefort; and

the lower valley of the Dourbie can be visited from Le Vigan by taking

the train to Saudières and a carriage thence to Milau.

Nant, a little town on the left bank of the Dourbie, has a Celtic

name, very descriptive, for Nant signifies a valley or a river bottom.

Nantes in Brittany has the same derivation, as has also Devon in Welsh,

Dyffneint, the county of valleys. So also the Dourbie and the Durzon

proclaim that they were named by Celts, for _dour_ signifies water in

Welsh.

The church of S. Pierre of the twelfth century is all that remains of a

Benedictine abbey; the Romanesque chapel of S. Alban stands on a barren

rock 2,400 feet high. But the great attraction is the source of the

Durzon, as Reclus describes it:—

"A little river issuing from a deep _foux_ some six or seven

kilometres from Nant, near the Mas-de-Pommier, at the bottom of

a cirque where walls, which are those of the Larzac, rise above

the well to the height of 900 feet. There opens a great gulf,

_un dormant qui ne dort pas toujours_. A slight rain on Larzac

agitates it, and it begins to boil languidly in the centre of

the well; but after a long rain, a storm, or the melting of the

snows, the water rises in clashing floods like a cascade turned

upside down; it is no longer a murmuring stream, but a growling

torrent whose voice breaks the austere silence of the cirque."

Still descending the valley, we see perched high up on the right the

curious village of Cantobre, on a point of the Causse Bégon, shaded

by gigantic dolomitic mushrooms, and comprised within the walls of a

ruined castle that was destroyed in 1660, after its owner, Jean de

Fombesse, had been executed as a coiner.

But more curious even than Cantobre is the village of S. Veran,

plastered against the rocks which shoot up into needles. The ravine

opening behind it describes a circus bristling with pinnacles and rocks

scooped out and shaped into the most fantastic forms. The whole is

commanded by an immense wall of limestone on which, and intermingled

with which, are the artificial structures of a castle, the cradle of

the family of Montcalm, whose most illustrious member was the Marquess

who fell on the heights of Abraham, 14th September, 1759, in the

struggle over Quebec, that cost also the life of Wolfe. The inhabitants

of this poor hamlet, in a barren and waste land, are themselves

wretchedly poor. Some one said to one of them: "So, the Montcalms left

this place!" "Aye! and would to God we could leave it too," was the

reply.

Below this is La Roque, whence Roquesaltes may be visited, and the

Rajol, extraordinary groups of rocks little less curious than those

of Montpellier le Vieux, that are also reached from the valley of

the Dourbie. But these I have described elsewhere, and I am not so

garrulous that I care to repeat myself.

FOOTNOTE:

[12] Martel: _Les Cévennes_. Paris, 1891.

A Book of the Cevennes · 第 15 / 17 章