Part 40

The excavations conducted by Mr. Jones in 1867 were made by digging several holes about three feet square. In the first two holes nothing was found, but in the third an ox skull, broken bones, portions of pointed implements of bone, and a bronze socketed spear-head were disinterred. The latter, which was only 18 inches below the surface and above the peaty clay, measured 13 inches long and two inches at its widest part. The bones were of _Bos longifrons_, stag, pig, sheep or goat, large dog or wolf, urus (_Bos primigenius_), and hare. These were all in the peaty stratum. Beside, and along with the bones, were found two or three flint flakes, cores, and rude flint implements. There were several pieces of sandstone, burnt, with the mark of fire plainly upon them, and divers calcined flints. Also a fragment of a thin hand-made vessel. Besides the bones were several stags' antlers, one or two of which were gnawed, probably by dogs, and another had marks of some small-toothed animal, such as a rat. Others were cut by human hands. One antler had a hole rudely worked in it at its broadest part. There were also divers horns of the _Bos longifrons_, and, curiously enough, one of the vertebræ of a Saurian. The latter was a short distance off from the chief "find," and it was suggested that it might have been used as a hammer by some of the natives who brought it to the spot.

The portion of the "find" which caused most conjecture was, however, a fabric of stake and wattle. "I found one stake 2½ inches thick, and 2 feet long, lying close over the spot where we found most of the bones, but the fabric to which I now allude occurred some twenty-eight inches below the surface of the deepest part of the _mere_. The soil in the neighbourhood of it had been disturbed, so I took a spud and trowel and worked the thing out with my own hand. It resulted in an oval or egg-shaped structure of wattle, 5 feet 7 inches long, and 3 feet 10 inches wide. There were 14 uprights, varying from 2 to 2¾ inches in thickness, at nearly equal distances apart. Twigs and sticks were worked in these like the side of a very rough basket. At first I thought it might have been a sunken coracle, but on scooping out the clay with which it was filled, I found that the wattle ceased about 14 inches down, and that the uprights were merely stakes, from 21 to 27 inches long, driven originally into the chalk marl. The bottom of this fabric was filled with broken flints which were also found outside the lower part of the uprights and between them. The flints must have been put in, the points and edges of the points of the stakes being so sharp and clean that they could not have been driven through the bed of flints."

"The top of the wattle was on the level of the chalk marl, on which most of the bones, fragments of pottery, etc., were strewn, and which had been covered over to a depth of from 2 to 4½ feet of dark clay. No more stakes were found, but there occurred divers holes in the chalk marl, some of them nearly in line, in which we could not help thinking they might have once stood. Yet we found no remains of wood in these holes." (B. 161, p. 31.)

Professor Boyd Dawkins, under the heading "Habitations in Britain in the Bronze Age," writes as follows:--

"Sometimes, for the sake of protection, houses were built upon piles driven into a morass or bottom of a lake, as for example in Barton Mere, near Bury St. Edmund's, where bronze spear-heads have been discovered, one 13 inches long, among piles and large blocks of stone, as in some of the lakes in Switzerland. Along with them were vast quantities of the broken bones of the stag, roe, wild boar, and hare, to which must also be added the urus, an animal proved to be wild by its large bones, with strongly-marked ridges for the attachment of muscles. The inhabitants also fed upon domestic animals--the horse, short-horned ox, and domestic hog, and in all probability the dog, the bones of the last-named animal being in the same fractured state as those of the rest. Fragments of pottery were also found. The accumulation may be inferred to belong to the late, rather than the early, Bronze Age, from the discovery of a socketed spear-head. This discovery is of considerable zoological value, since it proves that the urus was living in Britain in a wild state as late as the Bronze Age. It must, however, have been very rare, since this is the only case of its occurrence at this period in Britain with which I am acquainted." ("Early Man in Britain," p. 352.)

LAKE-DWELLINGS IN THE FENLAND.

The discovery of so many submarine dwellings in Holland and the adjacent coasts of Germany which I have already described suggests that similar remains might be found in the Fens and other low-lying districts in Britain. The only reference, however, to such dwellings with which I am acquainted is the following short notice by Mr. Skertchly:--

"I detected the remains of one (lake-dwelling) at Crowland in the year 1870, during some excavations. The piles were of sallow planted very closely together, upon these was laid brushwood, and over this a layer of gravel. Immense quantities of bones, chiefly of the Keltic shorthorn, were found, together with a few bone implements, and a curious ornament of jet. Near Ely, stakes have been found in the peat, but they do not seem to belong to a lake-dwelling." ("The Fenland Past and Present," by Miller and Skertchly. 1878.)

PILE-STRUCTURES IN LONDON.

On December 18th, 1866, Col. Lane Fox (now General Fox-Pitt-Rivers) read a paper at the Anthropological Society entitled, "A Description of certain Piles found near London Wall and Southwark, possibly the Remains of Pile-Buildings."

The author commenced by observing that his attention was directed to this locality by a short paragraph in the _Times_ of the 20th October, stating that upwards of twenty cart-loads of bones had been dug out of the excavations which were being made for the foundations of a wool warehouse near London Wall. The excavation commenced at 40 yards south of the street pavement: therefore, in all probability, at about 70 or 80 yards from the site of the old wall. The area then excavated was of an irregular oblong form, 61 yards in length, running north and south, and 23 yards wide.

A section of the soil consisted of--

"1. Gravel similar to Thames ballast at a depth of 17 feet towards the north, inclining to 22 feet towards the south end. "2. Above this, peat of unequal thickness, varying from 7 to 9 feet. "3. Modern remains of London earth composed of the accumulated rubbish of the city."

Between the bottom of the peat and the highest spring tide water-mark, as at present existing, there is a margin of 5 feet; but, of course, this might have been different in Roman times.

Regarding the remains of piles in this locality the author makes the following observations:--

"Upon looking over the ground, my attention was at once attracted by a number of piles, the decayed tops of which appeared above the unexcavated portions of the peat, dotted here and there over the whole of the space cleared. I noted down the positions of all that were above ground at the time; and as the excavations continued during the last two months, I have marked from time to time the positions of all the others as they became exposed to view.

"Commencing on the south, a row of them ran north and south on the west side, to the right of these a curved row, as if forming part of a ring. Higher up and running obliquely across the ground was a row of piles, having a plank about an inch and a half thick and a foot broad placed along the south face, as if binding the piles together. To the left of these another row of piles ran east and west; to the north-east again were several circular clusters of piles; these were not in rings but grouped in clusters, and the piles were from eight to sixteen inches apart. To the left of this another row of piles and a plank two inches thick ran north and south. There were two other rows north of this and several detached piles, but no doubt several towards the north end had been removed before I arrived.

"The piles averaged 6 to 8 inches square; others of smaller size measured 4 inches by 3; and one or two were as much as a foot square. They appeared to be roughly cut, as if with an axe, and pointed square; there was no trace of iron-shoeing on any of them, nor was there any appearance of metal fastenings in its planks; they may have been tied to the piles, but if so, the binding material had decayed.[120] The grain of the wood was still visible in some of them, and they appear to be of oak. The planks averaged from one to two inches thick. The points of the piles were inserted from one to two feet in the gravel, and were, for the most part, well preserved, but all the tops had rotted off at about two feet above the gravel, which I conclude must have been the surface of the ground, or of the water, at the time these structures were in existence."

These relics were exclusively found in the peat or middle stratum (which varied from 7 to 9 feet in thickness), and "interspersed at different levels from top to bottom throughout it."

"Amongst the articles of human workmanship found in the peat the vast majority are undoubtedly of the Roman era. Amongst them are quantities of broken red Samian pottery, mostly plain, but some of it depicting men and animals in relief; one specimen is stamped with the name of Macrinus. All this pottery, in the opinion of Mr. Franks, to whom I showed it, is of foreign manufacture. Other samples are of the kind supposed to have been manufactured in the Upchurch Marshes in Kent, and upon the site of St. Paul's Churchyard. Bronze and copper pins, iron knives, iron and bronze stylus, tweezers, iron shears, a piece of polished metal mirror so bright that you may see your face in it (this Dr. Percy has pronounced to be of iron pyrites, white sulphuret of iron without alloy), an iron double-edged hatchet, an iron implement, apparently for dressing leather, a piece of bronze vessel, and other bronze and iron implements, which, thanks to the preserving properties of the peat, are all in excellent preservation. Amongst these were also a quantity of leather soles of shoes or sandals, some apparently much worn, and others, being thickly studded with hob-nails, may be recognised as the caliga of the Roman legions; also a piece of tile with the letters P. PR. BR. stamped upon it. Specimens of these are on the table. The coins found are those of Nerva, Vespasian, Trajan, Adrian, and Antoninus Pius....

"In addition to the Roman relics above mentioned, others of ruder construction remain to be described. They consist of what, in the absence of any evidence respecting their uses, may be called handles and points of bone. The former are composed of the metacarpal bones of the red-deer and _Bos longifrons_ cut through in the middle, and roughly squared at the small end; the others, which are called by the workmen spear-heads, are pointed at one end and hollowed out at the other, as if to receive a shaft. Both Professor Owen and Mr. Blake concur in thinking these implements may possibly have been formed with flint, but I cannot ascertain that they were found at a lower level than the Roman remains, nor have any flint implements, to my knowledge, been found in the place. With them were also found the two bone skates on the table; they are of the metacarpal bone of a small horse or ass, one of which has been much used on the ice. Exactly similar skates also of the metacarpal of the horse or ass have been found in a tumulus of the Stone Period at Oosterend in Friesland; a drawing of them is given in Lindenschmit's Catalogue of the Museum at Mayence, etc. Others have also been found in Zeeland, at Utrecht, and in Guelderland, and there is a specimen in the Museum at Hanover. Professor Lindenschmit attributes all these to the Stone Period, but the specimens on the table are evidently of the Iron Age, the holes in the back having been formed for the insertion of an iron staple. Similar skates have been found in the Thames, but they have not hitherto been considered to date so early in England as in Roman times."

Throughout the peat were several kitchen-middens. One, deposited a foot and a half above the gravel, is thus described:--"A layer of oyster and mussel shells about a foot thick, with a filtration of carbonate of lime permeating through the moss. In this kitchen-midden, Roman pottery and a Roman caliga were found. Close by, the point of a pile, part of which is exhibited, was found upright in the peat; it had been driven in in such a manner that the point descends to the level of the kitchen-midden and no farther. Now, as a pile, in order to obtain a holding, must have been driven at least two feet in the ground, it is evident the peat must have grown at least one foot above the summit of the kitchen-midden before this pile was driven in."

A second kitchen-midden is noted at a height of 3½ feet above the gravel, "composed of oyster, cockle, and mussel shells, and periwinkles, with Roman pottery and bones of the goat and _Bos longifrons_, etc., split lengthwise as if to extract the marrow, with the skulls broken and the horns cut off. It is about a foot and a half thick in the centre, thinning out towards the ends as a heap of refuse would naturally do, and from 12 to 14 feet long; above this is peat for about a foot or a foot and a half, and above the peat another kitchen-midden of the same kind as the preceding. Lastly, the soles of shoes and Roman pottery of the same kind as that found lower down have been taken out at the very top of the peat."

The distinguished investigator, being anxious to obtain further evidence as to the thickness of the stratum in which the Roman remains were found, states that he determined to watch the workmen for four or five hours together during several successive days, while they dug from top to bottom, commencing with the superficial earth, and passing through the peat to the gravel below. The result was as follows:--"Roman red Samian ware is found as high as 13 feet from the surface, but very rarely, and in small quantities. At 15 feet it is frequently found, and from that depth it increases in quantity till the gravel is reached at 18 to 21 feet. The chief region of Roman remains is within two or three feet of the gravel."

Amongst the animal remains were, according to Professor Owen, those "of the horse or ass, the red deer, the wild boar, the wild goat (_bouquetin_), the dog, the _Bos longifrons_, and the roebuck. The horns of the roebuck, I afterwards ascertained, were all found at a higher level. These, and also the horse and goat, entered the superficial earth, in which glazed pottery was also found; but the remainder, including the red deer, wild boar, and _Bos longifrons_, appeared, so far as my observations enabled me to judge, to be confined to the peat."

Subsequently Mr. Carter Blake identified amongst these osseous remains no less than four different kinds of the genus _Bos_--viz. _primigenius_, _trochoceros_, _longifrons_, and _frontosus_; as also a specimen of the ibex of the Pyrenees.

Some human skulls were found in the lowest formation of the peat, or immediately over the gravel. Along with these skulls only three other human bones were found; but this, according to the author, might not be the result of an oversight, as both the Celts and the Romans were known to have practised decapitation.

The piles at the south end were identified as elm, the remainder were oak (_Quercus robur_).

From the above carefully observed and recorded facts it will be observed that in addition to the primary piles which were inserted into the gravel there were others which did not penetrate so deeply, one having been carefully noted which terminated in the peat a foot and a half above the gravel. Facts precisely similar have been observed in almost all pile-dwellings whether on land or in water, showing that the elevations on which the platforms and huts were reared were successively renewed. Another conclusion which we are entitled to draw from the character of the relics and the conditions in which they were found is that in the low-lying districts of London the system of pile-dwellings was known in Britain in post-Roman times. Nor can it be said that this was a solitary instance, for similar remains were found in New Southwark Street, in regard to which the author writes as follows:--

"The piles are of the same scantling, also of oak, but somewhat longer than those of London Wall; the points are driven into the gravel; the peat is three to four feet thick; large beams of the same size as the piles have been laid across them horizontally, and Roman pottery is found at all depths in the peat. Judging from the extent over which these piles have been discovered, there can be little doubt that in digging for the foundations of the many large warehouses and other buildings that are now being built within this district the remains of early habitations are constantly turning up and are destroyed without receiving attention."

As to the relics from these London pile-dwellings let me finally observe, that, to a certain extent, both in character and surrounding conditions they correspond with those from the Terp mounds in Holland and North Germany, from which it is probable the earliest Anglo-Saxon invaders hailed.

CRANNOG IN LLANGORSE LAKE, NEAR BRECON, SOUTH WALES.

Only one lake-dwelling has hitherto been recorded in Wales, viz. that of Llangorse. The partial exploration to which it has been subjected was undertaken by the Rev. Mr. Dumbleton, and the results are recorded by him in the _Archæologia Cambrensis_ for 1870 and 1872. (B. 173.) The following extracts from these reports clearly show that the island was entirely artificial and constructed after the manner of the Scottish and Irish crannogs. Its structural features were well seen in the surrounding stockades and log-floorings, while the heaps of charcoal, remains of food-refuse, and other indications point to a prolonged period of human occupancy. Mr. Dumbleton states that until about seven years ago, when the lake was artificially lowered a foot and a half, this island was not half its present size. He then advances various evidences to show that formerly the level of the water was still lower, when, therefore, the island would have been larger than now. This opinion may be, and probably is, correct; but we must remember that another factor has to be taken into account when discussing the invariable submergence of these islands, viz. their own pressure on a yielding lake sediment, together with the decay of the brushwood and other organic materials which generally formed their under strata. It is to be regretted that no relics were found on this island, and I cannot help thinking that, in the circumstances, a more careful search would have furnished some scraps of the handiwork of its occupiers. From the description it is clear that metal tools were used in manipulating the woodwork, but otherwise, and in the absence of any historical notice, we have no means of determining either the age of this singular lacustrine abode or the social condition of its inhabitants.

"Immediately beneath the southern spurs of the Black Mountains, and in the hollow of the great geological fracture which parts that chain from the Brecknockshire Beacons, is situated a sheet of water now called the Lake of Llangorse. Its name was formerly Llyn Savathan, or the lake of the sunken land. The area of water was once far more extensive than it is now; and it has subsequently been, as I think, considerably less than at present. A circuit of five miles will now enclose it. The margin is flat and swampy, except on the north-east, where the mountain descends upon the shore-line somewhat abruptly. The depth, though by vulgar report vast and fearful, Leland has rather overstated in assigning to it thirteen fathoms."

"Within a bow-shot of the flat meadows on the north side there is an island that would appear but little above the water, were it not for some small trees and brushwood that have fastened upon it.

"Sailing by the island one day in 1867, I observed that the stones which stand out on the south and east sides were strangely new looking, and most unlike the water-worn, rounded fragments that on the main shore have been exposed to the action of the waves; neither did there seem to be any original rock-basis at all. It was, in fact, nothing less than a huge heap of stones thrown into water two or three feet in depth. Was this the key, I thought, to the old tradition of a city in the lake? In the summer of last year, my brother, then living in the neighbourhood, first discovered a row of piles or slabs; some standing a few inches above water, for the lake was very low. We have together made some investigations during the past month, the results of which I will detail.

"The island, as now above water, measures 90 yards in circumference, its form being that of a square with the corners rounded off. The highest part is nearly in the centre, and is 5 feet above the water-level. The sides most exposed to weather, where also the water is deepest, are composed of stones sloping into the water, and extending to the distance of fifteen yards from the edge. Under the water, however, they are not nearly so thickly strewn as above. It is remarkable that on the leeward or northern side, about one quarter of the island is almost destitute of stone protection with which the greater part is covered. There is simply a surface of vegetable mould, inclined towards the water. Neither in the water, which is there very shallow, are there more than a score of stones to be found on that side. I must now speak of the piles. These are of two sorts, the most obvious being either at the margin or within a few feet of it. Like the stones, they are most numerous where the action of the storm would be most felt, and upon the shallow side they disappear entirely. They have been disposed in segments of circles, the stones being heaped inside them, and thus saved from being torn away by the waves. These piles (or rather slabs) are of cleft oak, and have been pointed, as it seems, by cuts from a metal adze. We have counted about sixty. They have been driven tightly into the shell-marl, to the depth of four feet. There are also other piles, which are round, generally of soft wood, and are found outside the present edge of the island. Several are in water two feet deep, and are driven into the marl only twelve or eighteen inches. These would have been quite powerless to confine the stones, and were evidently for another purpose.... Is it not likely that the island itself was central common ground? and that the habitations were projected from its edge towards the water and were supported by these thick round piles? Something like a ring of these is found near the oak slabs before mentioned; and traces of a second set are at the distance of twelve or fifteen yards, in water about two feet deep. Between the two, small wood is found abundantly, a few inches in the marl. At about ten yards from the shore, and in two feet of water, there appear to be the actual remains of a sunken platform. Three trunks of soft wood lie nearly parallel to one another. A 6 feet stem of oak, which I cannot account for, was with them. The top of this we sawed off, as it exhibits the marks of some heavy cutting instrument where, in modern days, a saw would have been used.