Castles and Cave Dwellings of Europe, Sabine Baring-Gould [ebook reader below 3000 TXT] 📗

slope of the hill is parcelled out into small fields or gardens by means of walls of stones laid one on another without mortar, showing that the inhabitants of these caves lived there permanently and cultivated the ground below their dwellings. [Footnote: There are others, Les Grottes de Rajah, in the same mass of rock, with near them an isolated rock carved about and supposed to have been an idol.] More curious still are the Grottoes de Jonas on the Couze, also in Puy de Dome, near Cheix. They are in stages one range above another to the height of from 90 to 120 feet. The face of the mountain is precipitous, and is of a porous tufa full of holes. As many as sixty of these artificial caves remain; but there were at one time many more, that have been destroyed by the fall of the very friable volcanic rock. It is impossible to determine the period at which these caves were excavated; they were probably prehistoric to begin with, but were tenanted during the Middle Ages when--if not later--the tracks leading to them were cut in the tufa and stairs to connect the several stages. Then paths were bordered by walls as a protection, and fragments of the parapet remain. Probably it was during the English occupation of Guienne which extended into Auvergne, that a castle and a chapel were sculptured out of the living rock. At the same time a remarkable spiral staircase was contrived in like manner. Numerous relics of all periods--flint tools, bronze weapons, statuettes, and coins--have been found among the rubbish thrown out from these dens. [Footnote: G. Tournier, _Les Megalithes et les Grottes des environs de S. Nectaire_. Paris, 1910.]

On the Borne, in Haute Loire, dug out of the volcanic rock are several cave-dwellings. The caves at Conteaux are fourteen in number, the largest is divided into three compartments; each is 45 feet deep and 11 feet wide, but the usual dimension is from 28 to 36 feet. In all, the vault is rather over 6 feet high. An opening in the roof of one gave vent to smoke.

The rock of Ceyssac is curious. Formerly a barrier of volcanic tufa stretched across the valley of the Borne; this barrier had been ejected from the volcano of La Denise. The river, arrested in its onward course, was ponded back and formed a lake that overflowed the dam in two places, leaving between them a fang of harder rock. When the water had spilled for a considerable time over the left-hand lip, and had worn this down to a depth of about 70 feet, it all at once abandoned this mode of outlet and concentrated its efforts on the right-hand portion of the dam where it found the tufa less compact. It eventually sawed its way completely through till it reached its present level, leaving the prong of rock in the middle rising precipitously out of the valley with the river gliding peacefully below it, but attached to the mountain side by the neck it had abandoned. The fang was laid hold of, burrowed into, and converted into a village of Troglodytes. In it are cave-dwellings in five superposed storeys, stables with their mangers, with rings for tying up cattle, a vast hall, that is circular, and chambers with lockers and seats graven out of the sides of the walls. There is also a subterranean chapel, with the entrance blocked by a wall that contains an early Romanesque doorway. The Polignacs seized on the spike of rock and built on the summit a castle that could be reached only by a flight of steps cut in the face of the rock. By degrees the inhabitants have migrated from their caves to the neck of land connecting the prong with the hill, and have built themselves houses thereon. They have even abandoned their monolithic church and erected in its place an unsightly modern building.

There are other cave-dwellings in the volcanic rocks of the Cevennes and Auvergne, but the above account must suffice.

I will now say something about the Troglodyte dwellings in the sandstone in Correze, in the neighbourhood of Brive, caves that have been inhabited from the time of the man who was contemporary with the mammoth, to this day. Some have, however, been abandoned comparatively recently.

They do not run deep into the rock; usually they face the south or south-west, and are sometimes in a series at the same level; sometimes they form several storeys, which communicated with each other by ladders that passed through holes cut in the floor of the upper storey, or else by a narrow cornice, wide enough for one to walk on. Sometimes this cornice has been abraded by the weather, and fallen away; in which case these cave-dwellings can be reached only by a ladder. There are caves in which notches cut in the rock show where beams had been inserted, and struts to maintain them, so as to form a wooden balcony for communication between the chambers, or between the dwellings of neighbours.

The doorways into these habitations are usually cut so as to admit a wooden frame to which a door might be attached; and there are deep holes bored in the rock, very much as in our old churches and towers, for the cross-piece of timber that effectually fastened the door.

The grottoes are cut square, the ceilings are always sensibly horizontal, and the walls always vertical. But where a natural hollow has been artificially deepened, there the opening is usually irregular. Moreover, in such case, the gaping mouth of the cave was in part walled up. The traces of the tool employed are everywhere observable, they indicate that the rock was cut by a pick having a triangular point. Small square holes in the sides, and long horizontal grooves indicate the position of shelves. Square hollows of considerable size served as cupboards, and oblong rectangular recesses, 18 inches above the floor, and from 3 feet 9 inches to 4 feet 6 inches high and a foot deep were benches. Bedplaces were also cut in the rock.

There are also indications of a floor having been carried across in some of the loftier caves, and there are openings in the roofs through which ascent was made to the series of chambers on the upper storey. Holes pierced in the ceiling served for the suspension of articles liable to be injured by proximity to a damp rock. A string was attached to the middle of a short stick, that was thrust into the hole. The string was then pulled and it was fast. Another plan was that of boring holes at an angle into the rock at the side. Into these holes rods were thrust and what was required to be kept dry was suspended from them.

Some of the grottoes served at once for man and beast and fowl. Not only are there chambers for the former, but also mangers for cattle, and silos to contain the fodder; and there are nooks for pigeons in an adjoining cave. In many cases there are cisterns; in one is a well. The cisterns had to be filled laboriously. They are provided with bungholes for the purpose of occasional cleaning out. The walls are scored with concave grooves slanting downwards, uniting and leading into small basins. The moisture condensing on the sides trickled into these runnels and supplied the basins with drinking water. The mangers have holes bored in the stone through which passed the halters. There are indications that the cattle were hauled up by means of a windlass.

That these were not places of refuge in times of danger, but were permanent habitations, would appear from the fact that those of Lamouroux contain mural paintings, and that in them, in addition to stables, there is a pigeonry. In one or two instances the piers that support the roof have sculptured capitals, of the twelfth or thirteenth century. In the cave-dwelling still tenanted at Siourat is cut the date, I.D. 1585, surmounted by a cross. [Footnote: Lalande (Ph.), _Les Grottes artificielles des environs de Brive_. In _Memoires de la Soc. de Speliologie_. Paris, 1897.]

I have given the plan of the caves of Lamouroux in my "Deserts of Southern France."

How general rock habitations were at one time in Perigord may be judged by the prevalence of the place-name _Cluseau_, which always meant a cave that was dwelt in, with the opening walled up, window and door inserted; _roffi_ is applied to any ordinary grotto, whether inhabited or not.

It would be quite impossible for me to give a list of the cave- dwellings in France still inhabited, or occupied till comparatively recent times, they are so numerous and are to be found in every department where is the chalk or the limestone, sandstone or volcanic tufa.

They are to be met with not only in those parts of France from which the above specimens have been taken and described, but also in Var, Bouches du Rhone, Aveyron, Gard, Lozere, Cantal, Charente, Vienne, &c.

There is a good deal of sameness in the appearance of those still inhabited--a walled face, a mask, with window and door, and above a chimney of brick rising out of the rock.

In England, Nottingham drew its ancient British name of Tigguocobauc (House of Caves) from its troglodyte habitations; at Mansfield in that county such caves exist, and were associated with a class of inhabitants somewhat nomadic, who obtained their living by making besoms from the heather of the adjoining forest and moorland. They established a colony on the roadside waste, and sank wells in the rock for water. Nottingham enjoyed possibly the largest brewing and malting business in the country, and those trades were nearly wholly carried on in chambers and cellars and kilns cut out of the living rock. Mr. W. Stevenson, author of "Bygone Nottinghamshire," writes to me: "Last week I was with an antiquarian friend exploring an ancient passage in the castle rock, originally made as a sally-port to the castle, but at some later period when bricks came on the scene, converted or enlarged into a set of malt offices with malt kilns complete. Their original use and locality have been lost for a century, and their recovery is just being brought about. Their situation, high over the adjoining meadow, and their presence in the very heart of the rock that rises abrupt to the height of 133 feet is truly romantic. The foot of the range of cliffs, with a south aspect, was a favoured site. Here we find communities of monks dwelling for centuries, hermits spotted about, and a great part of the town-dwellers, tanners, dyers, and other trades where water was largely required. A peculiarity of these houses was their fresh-water supply. The denizens sank holes in their living apartments with steps cut in the rock until they got down to the water level, where they had little pools of fresh water. The system was known as _Scoop- wells_, and must have been very ancient. Those who lived on higher levels burrowed into the sides of sunken roads, and the track-lines of ancient military defences. In deeds of transfer of property it was customary to describe tenements as _below_ or _above_ ground. Old writers have said that they doubted if the erections above ground would fill the space excavated below ground; and to-day, when erecting new buildings, it is necessary to drill down into the rock a yard or more to ascertain that the foundations are not to be laid above the crowns of hidden vaults, chapels, or unknown habitations."

Thoroton, in his history of Nottinghamshire, 1797, gives an illustration of rock-dwellings at Sneynton, adjoining Nottingham, but they have recently been cleared away for railway extension.

The sanitary authorities have done their