Part 16

[Illustration: Fig. 444.—Valley of the Lark, or of the Little Ouse. 1∕2]

Some implements have also been found at a lower level in the gravel on the slope of the hill towards the Fens, and close to the main street of Lakenheath; amongst them one of ovate form most skilfully chipped into shape.

* * * * *

The curious implement shown in Fig. 444, which was presented |568| to me by Canon Greenwell, F.R.S., was procured from a Lakenheath workman, but it is not certain whether it was found in the gravel near that place, or in one of the pits near Brandon. It differs from all other implements that I have seen from the River-drift, in having an oblique hatchet-like edge at the end, so that the side-view somewhat resembles that of the iron _Francisca_, of Saxon times. A considerable portion of the original crust of the flint remains at the butt-end. Until other specimens of the same form are discovered, it is hardly safe to regard this as furnishing an example of a new type of implement; yet its symmetry and character seem to prove that it was designedly chipped into this form, to fulfil some special purpose.

* * * * *

It will be best to postpone any remarks as to the probable connection of the beds near Lakenheath with the ancient course of the Lark and Little Ouse, until I come to consider the geological aspects of the whole case.

It was from a place called Botany Bay, near Brandon, that Mr. S. B. J. Skertchly, F.G.S., of the Geological Survey, first obtained evidence on which he founded the existence of the beds that he termed Brandon Beds, which though containing palæolithic implements he regarded as occurring below the Chalky Boulder-clay, and as, therefore, of Interglacial date. The evidence that the implement-bearing beds are, at all events in the Eastern Counties, later than the Boulder Clay is now beyond all cavil, and, so far as I could judge, the supposed Boulder Clay lying above the implement bed at Botany Bay was not in its original position, but was either _remanié_ or had slipped down from a higher level. It is, however, but fair to state that the Rev. O. Fisher,[2537] F.G.S., has accepted Mr. Skertchly’s views, at all events with regard to some of the localities, as to there having been three successive Palæolithic Periods in Britain, each preceded and succeeded by a Glacial Period.[2538] I can only say that I am not prepared to accept such a view.

I must now proceed to describe another of the River-drift deposits in the more immediate neighbourhood of the Little Ouse, and lower down its course, at Shrub Hill, in the parish of Feltwell, Norfolk.

This too has been described by Mr. Flower in the paper to which I have already so frequently referred. It has also been described by Mr. H. Trigg,[2539] to whom flakes from this deposit were |569| brought, so early as 1865. It caps a low-lying hill in the middle of the Fens, about 8 miles nearly due W. of Brandon, and 1 mile N. of the present course of the Little Ouse, and just to the N. of Fodder Fen Drove on the old Ordnance Map. Mr. Flower states that the gravel here is about 12 feet in thickness, but that at the surface it is only 6 feet above the river. Of course, however, the thickness varies, being often less than 8 feet; and I am inclined to think that the elevation above the river is somewhat underestimated. The gravel consists mainly of subangular flints, mixed with some rolled chalk, a considerable number of quartzite pebbles, and rolled fragments of other old rocks, derived from the Glacial Beds higher up the river. It is in a very sandy matrix, more or less ochreous at different spots. In places, the sand predominates.

The Drift-beds rest upon the Gault clay, and not, as in most of the cases already described, upon the Chalk. The implements found here occur usually towards the base of the gravel, and as a rule are rolled and waterworn. They have been found in considerable numbers, and of various types, including many flakes. It will be remembered that a barbed arrow-head and a partially polished stone celt were also found here; from which it seems probable that in Neolithic times, Shrub Hill formed a habitable spot in the midst of the Fens, or possibly of the watery waste since choked up by vegetation. Teeth of _Elephas primigenius_,[2540] and fragments of the horns of deer, and teeth of some ruminant—probably deer also—and of a small horse, have been found at Shrub Hill in the gravel, but I have searched in vain for testaceous remains.

* * * * *

Among the implements found at Shrub Hill is one which is probably the largest of its class as yet discovered in England or France, and which was presented by the late Mr. Flower to the Christy Collection. It is fully 11 1∕2 inches long and 5 1∕4 inches broad near the base. Its greatest thickness is 3 inches. One face is much more highly ridged than the other, and it has been boldly chipped with large facets. In general form it resembles Fig. 445 from the same locality, but is somewhat thicker and more elongated in its proportions, and is, as nearly as may be, six times the length of the figure. It weighs 5 lbs. 7 oz.

An interesting account of large and heavy examples of palæolithic implements has been compiled by Mr. Worthington Smith.[2541] The heaviest is one formed of quartzite in the Central Museum at Madras. It is 9 3∕4 inches long and 5 3∕4 wide with a weight of 6 1∕4 lbs.

The small specimen here shown as Fig. 445 was found in 1866, and is less waterworn than is usual with Shrub-Hill implements, though its |570| surface is beautifully sand-polished. It is of dark brown flint, in places mottled with a fine amber colour. It shows a part of the original crust of the flint at its base.

[Illustration: Fig. 445.—Shrub Hill, Feltwell. 1∕2]

[Illustration: Fig. 446.—Shrub Hill, Feltwell. 1∕2]

The same is the case with the implement shown in Fig. 446, which also is in my own collection. It is a specimen of a thin broad type |571| occasionally met with. Towards the point the edge bears all the appearance of having been worn away by use as a scraping tool.

[Illustration: Fig. 447.—Shrub Hill, Feltwell. 1∕2]

Another implement of somewhat the same character, but thicker at the butt, and having the sides rather straighter, so as to be more acutely pointed, is shown in Fig. 447. The angles are much waterworn, and the greater part of the base shows the natural crust of the flint.

The only other specimen which I have thought it worth while to engrave from this locality (Fig. 448), shows a considerably smaller example of the crescent-like implements, such as that already figured from Santon Downham. It is, however, of coarser workmanship, and not so broad in proportion to its length.

[Illustration: Fig. 448.—Shrub Hill, Feltwell. 1∕2]

Most of the forms which are found higher up the valley of the Little Ouse occur also at Shrub Hill, and include some of the flattened oval type. But as a rule, the general _facies_ of the implements is more like that of |572| Redhill and Bromehill than that of either Santon Downham or of Gravel Hill, Brandon.

The Little Ouse joins the main river about 4 miles N.W. of Shrub Hill; and 5 miles N. of the junction the Ouse receives another affluent—the Wissey or Stoke River, draining 243 square miles—along the course of which, however, no palæolithic implements have as yet been found. The same is the case with the valley of the Nar or Setchy, a river which joins the Ouse just above King’s Lynn, a few miles before it discharges into the Wash, and which drains an area of 131 square miles.

Along a great portion of its lower course the Ouse runs through a Fen country, where, of course, no gravel is to be seen; but at Ash Wicken and Leziate, a few miles E. of King’s Lynn, and at South Wootton, about 2 miles to its N., the late Rev. John Gunn, F.G.S., found Drift-beds of apparently fluviatile character. In the gravels in a side valley leading into the marshes, near the School at South Wootton, Mr. W. H. Houghton, having been set upon the search for flint instruments by Mr. Gunn, found, in 1884, a tongue-shaped specimen, 5 1∕4 inches long, in form much like that from Shrub Hill (Fig. 447), but having the whole surface worked, and having the flatter face slightly concave longitudinally. It is stained all over of an ochreous colour, and shows signs of use near the point, a part of which has been broken off. The angles, though not sharp, are not waterworn. The late Mr. James Wyatt, F.G.S., of Bedford, also found, in the year 1870, in gravel in a pit near Lynn—the base of which is seldom reached on account of its lying below the level of the water—an oval flint implement, well formed and deeply stained, and another of rude workmanship.

Many miles to the east, but still in Norfolk, there is seen in the cliff at West Runton,[2542] near Cromer, what appears to be the channel of an old river, filled up with gravelly deposits. In these, at a depth of 12 feet from the surface, and above a black freshwater bed, Mr. A. C. Savin, of Cromer, in 1878, found _in situ_ a fine well-wrought ovate implement of flint 4 3∕4 inches long. A few years later I found on the sea-shore below, a large ochreous flake, apparently palæolithic, which I gave to Mr. Savin.

About 3 miles S.W. of Runton, near Gallows or Gibbet Corner, in Aylmerton parish, Mr. F. C. J. Spurrell found, in 1882, an ochreous implement from the gravels capping the hill, not far from Sherringham Heath. At East Runton,[2543] in the pre-glacial “Forest Bed,” Mr. W. J. Lewis Abbott thinks that he has found worked flints. I fail, however, to see any distinct marks of human workmanship upon his specimens.

With these discoveries in Norfolk and those near the mouth of the river, my account of the basin of the Ouse ceases, but before proceeding southwards I must record some others of the same kind.

Yorkshire lies far away from the usual scenes of palæolithic discoveries, but I have seen a pointed implement (3 3∕4 inches), in form like Fig. 419, that was found on the surface at Huntow, near Bridlington. There is no record of its having been associated with any remains of the Quaternary fauna.

In the first edition of this book I recorded my finding an implement in form like Fig. 434, on a heap of stones near King’s Langley, within |573| a short distance of the railway. As the staining and incrustation upon it were unlike those on the stones of the local gravel, and corresponded with those on the flints in the ballast of the railway, I was inclined to refer the implement to that source, and to believe that it had been brought from Oundle with the gravel, at that time used for ballast. A visit to the pit proved unfruitful, but I suggested that in all probability a prolonged search might result in adding the valley of the Nene to those in which palæolithic implements have been found. My suggestion has now been justified. In 1882 Mr. T. George, F.G.S., found in a ballast pit at Elton, about 5 miles N. of Oundle, an ochreous pointed implement, in colour and appearance identical with mine from Langley, and kindly added it to my collection.

At Overton Longville, or Little Orton, two miles S.W. of Peterborough, a spot visited by Sir Joseph Prestwich and myself in search of palæolithic implements about 1861, some were found a few years ago by the late Dowager Marchioness of Huntly.[2544]

* * * * *

The next valley to be considered is that of the Waveney, a river which, after a circuitous course of 53 miles, joins the Yare a few miles S.W. of Yarmouth, and passes through Breydon Water to the sea. It takes its rise, as has already been stated, at Lopham Ford, close by the source of the Little Ouse.

Up to the present time there is but one locality known in its valley, where palæolithic flint implements have been found; but this is of peculiar interest, on account of the discoveries having been observed and recorded before the close of the last century, and, therefore, at a time when speculations as to the great antiquity of the human race can hardly be said to have commenced. And yet Mr. John Frere, F.R.S.,[2545] in the concise and able account which he gives of the discovery, shows himself to have been so much struck by the situation in which the implements were found as to be tempted to refer them “to a very remote period, indeed, even beyond that of the present world.” Mr. Frere states that the implements or weapons, as he terms them, lay in great numbers at the depth of about 12 feet, in a stratified soil, which was dug into for the purpose of raising clay for bricks; and he gives a section of the strata. He states that shells, which he erroneously regarded as marine, occurred in sand at a depth of 9 feet, together with bones of great size, and that below this, in a gravelly soil, the flints were found. His account is illustrated by excellent engravings of two of the implements, which I was enabled to reproduce in illustration of my first Essay on Flint Implements from the Drift, in 1859, and which have since been copied, on a smaller |574| scale in Lubbock’s “Prehistoric Times.”[2546] Mr. Frere presented some specimens of the Hoxne implements to the Society of Antiquaries, which are still preserved in their museum; and it was my seeing these, on my return from Amiens and Abbeville, in 1859, that again directed attention to this most interesting discovery.

Sir Joseph Prestwich, F.R.S., in his admirable Papers on Flint Implements and their containing Beds, published in the _Philosophical Transactions_[2547] for 1860 and 1864, has given full details of the contour of the surrounding country, and of the section at that time exposed in the brick-field visited by Mr. Frere more than sixty years before, which is still in operation. It is situated to the S.W. of the village of Hoxne, in Suffolk, and close to Fairstead Farm; Hoxne itself being about 4 miles to the east and slightly to the south of the market town of Diss, which is on the other, or Norfolk, side of the Waveney.

The Drift deposits rest in a kind of trough, in the Boulder Clay[2548] which caps all the neighbouring hills, and forms a sort of table-land through which the small valleys are cut. The top of the freshwater beds reaches within 6 or 8 feet of the summit of the hill of which they form an unbroken and uniform part. Their upper surface is about 40 feet above the neighbouring Goldstream, from which they are not more than 200 yards distant, and 50 feet above the Waveney, of which the Goldstream is a tributary, and which flows within about a mile of the spot. The present configuration of the surface is totally unconnected with these beds of Drift, and must have been produced after they were deposited.

* * * * *

The part of the pit which was being worked in 1859 exhibited the following section:—

1. Surface soil, with a few flints 2 feet.

2. Brick-earth, consisting of a light-brown sandy clay, divided by an irregular layer of carbonaceous clay 12 feet.

3. Yellow sub-angular gravel 6 in. to 1 foot.

4. Grey clay, in places peaty, and containing bones, wood, and freshwater and land shells 2 to 4 feet.

5. Sub-angular flint gravel 2 feet.

6. Blue clay, containing freshwater shells 10 feet.

7. Peaty clay, with much woody matter 6 feet.

8. Hard clay 1 foot.

The thickness of these lower beds was ascertained by Sir Joseph |575| Prestwich and myself by boring, as the pit was not worked below the bed of clay, No. 4. In another part of the pit we had a trench dug, which exhibited the following section:-

1. Ochreous sand and gravel, passing down into white sand 4 ft. 9 in.

2. Seams of white and ochreous gravel 1 ft. 8 in.

3. Light grey sandy clay 0 ft. 8 in.

4. Coarse yellow gravel 1 ft. 0 in.

5. Grey and brown clay, with abundance of _Bythinia_ 2 ft. 4 in.

6. Boulder Clay 1 ft. 0 in.

In the gravel thrown out from Bed No. 4, I found an implement in form like Fig. 433, but which had lost its point through having been struck by the pick of the workman.

[Illustration: Fig. 449.—Hoxne. 1∕2]

The mammalian remains, which had then recently been found in this pit, consisted of those of deer, horse, and elephant. The shells comprised _Cyclas_, _Pisidium_, _Unio_, _Bythinia_, _Helix_, _Limnæa_, _Planorbis_, _Succinea_, and _Valvata_. Among the remains of trees, those of oak, yew, and fir had been recognized.

Implements[2549] still continue to be found from time to time in this pit. Several of those found long since are also extant, in addition to those already mentioned. One of pointed form was in the Meyrick[2550] Collection of Armour, and is stated to have been found 12 feet below the surface of the ground, and to have once been in the Leverian Museum. |576| I have another of much the same character, which was sold by auction in London as an ancient British spear-head, but which I at once recognized as Palæolithic, and after purchasing it, found my opinion confirmed by the word _Hoxne_ being written on its base.

In the account given by Mr. Frere, it is stated that the implements had been found in such quantities that they had been thrown into the ruts of the adjoining road, and it therefore appeared probable that in the disturbed upper soil of the worked-out parts of the pit, some implements still existed. I accordingly made search for them, and succeeded in discovering, besides several flakes—one of which is 5 inches long and 2 inches broad—three implements, of which one is engraved in Fig. 449. It will be observed that a flat place has been left on one of the side edges of this instrument, probably to allow of its being held comfortably in the hand, so as to serve for a rude kind of knife.

Two remarkably fine specimens—one of them much like that from Reculver, Fig. 459, and the other somewhat more irregular in form but also round-pointed—were likewise found in the disturbed soil by Mr. Charles M. Doughty, of Caius College, Cambridge, and are now in the Woodwardian Museum. There are other specimens in the Christy Collection. A pointed implement from this place has been figured by Prestwich.[2551]

[Illustration: Fig. 450.—Hoxne.]

Another of these very acutely pointed implements is shown in Fig. 450, the original of which is in my own collection. It presents the peculiarity, which is by no means uncommon in ovate implements, of having the side edges not in one plane but forming a sort of ogee curve like that of Fig. 434. In this instance, the blade is twisted to such an extent that a line, drawn through the two edges near the point, is at an angle of at least 45° to a line through the edges at the broadest part of the implement. I think, however, that this twisting of the edges was not in this case intended to serve any particular purpose, but was rather the accidental result of the method pursued in chipping the flint into its present form. Curiously enough, one of the specimens presented by Mr. Frere[2552] to the Society of Antiquaries exhibits the same peculiarity, and, indeed, so closely resembles mine, that they might have been both made by the same hand. An essay on the Hoxne deposits by the late Mr. Thomas Belt, F.G.S., will be found in the _Quarterly Journal of Science_.[2553] |577|

* * * * *

I have left my original account of this locality almost unaltered, but the whole circumstances of the deposit have now been most thoroughly and satisfactorily investigated. In 1888 Mr. Clement Reid, F.G.S., and Mr. H. N. Ridley, F.L.S., communicated a paper to the British Association,[2554] calling attention to the presence of fossil Arctic plants in the lacustrine deposits at Hoxne. This was followed, in 1895, by some further[2555] notes on the deposits by the same authors, with the result that a small committee, of which I was chairman, was appointed by the Association,[2556] “to ascertain by excavations at Hoxne, the relation of the Palæolithic deposits to the Boulder Clay, and to the deposits with Arctic and Temperate plants.” A sum of money, subsequently supplemented by a grant from the Royal Society, enabled Mr. Clement Reid, Messrs. E. P. and H. N. Ridley, to carry out the necessary borings and excavations, while Miss Morse aided in washing out specimens, and Mr. Mitten in determining the species of the mosses. I cannot here enter into the details of the case, but must refer the reader to the “Report of the Committee”[2557] for them. The general results of the examination are as follows.

The deposits lie in a valley excavated in the Chalky Boulder Clay of the district, through which a stream ran, probably connected with the valley of the Waveney. By subsidence the channel of the stream was converted into the bed of a freshwater lake which gradually silted up, and its site became covered with a dense thicket of alders. From some cause or other, lacustrine conditions reappeared and 20 feet more of freshwater strata were deposited, but the climate had become Arctic or sub-Arctic. Then followed floods which deposited the implement-bearing beds, and finally the strata became sandy. During the formation and the silting up of the channel, the climatic conditions seem to have changed at least twice, having been at one time mild and then again Arctic. To use the words of the report: “The Palæolithic deposits at Hoxne are therefore not only later than the latest Boulder Clay of East Anglia, but are separated from it by two climatic waves, with corresponding changes of the flora. Such sweeping changes cannot have been local. They must have affected wide areas.”

Subsequently, however, to the Palæolithic beds being deposited, all traces of the shores of the old lake have disappeared, and but for artificial excavations the surface of the ground would give no indication either of a stream or lake having existed at the spot. |578|

Though terraces of gravel are found at various places along the course of the Waveney, and apparently of the same age as those of the Little Ouse valley, yet up to the present time no discoveries of implements in them have been recorded, although it seems improbable that it is at Hoxne alone that implements exist.

In the gravels of the valleys of the Gipping, and other small streams between the Waveney and the Stour, no works of man have as yet been discovered; but in a pit worked for ballast, near Melford Junction, on the Great Eastern Railway, and at no great distance from the Stour, the late Mr. Henry Trigg discovered one or two implements of flint, and a portion of a tooth of _Elephas primigenius_. Some worked flints have also been found in the gravel at Sudbury, Suffolk, and some palæolithic implements in the valley of the Stour, north of Colchester. In the cliff at Stutton, opposite Manningtree, is a freshwater deposit containing many shells of _Corbicula fluminalis_. Numbers of these washed out from the cliff are lying on the shore, and among them I found, in 1883, a broad flake about 3 inches long, which has all the appearance of being palæolithic. At Lexden Park,[2558] near Colchester, Mr. Edward Laver has found a small ovate implement with a cutting edge all round, ogival in character. Some other specimens have been discovered to the north of Colchester. On the banks of the Ter, a tributary of the Chelmer, Mr. J. French[2559] has found two palæolithic implements near Felstead; and in 1883, at North End Place, 1 1∕2 miles south of Felstead, the Rev. A. L. Rowe, F.G.S., picked up a rudely chipped heavy oval implement of quartzite (6 inches) which he has kindly added to my collection.

The valleys of the small rivers between the Stour and the Thames, the Colne, the Blackwater, and the Crouch, have up to the present time produced no relics of human workmanship, though I have seen a rudely worked flint, apparently from gravel, which was found on the sea-shore by Mr. W. Whitaker, F.R.S., a little to the north of the mouth of the Colne.

Before proceeding to discuss the discoveries that have been made within the basin of the Thames and in the Southern counties, I must call attention to one that was made in 1890 in the Midland Counties, not far from Birmingham.

The old gravels of the river Rea at Saltley, Warwickshire, have for a long time been subjected to a careful examination by Mr. Joseph Landon, F.G.S., of Saltley College, in the hope of |579| finding in them some relics of human workmanship; and his search has been rewarded by the discovery of the undoubted palæolithic implement, which through his kindness I am able to exhibit in Fig. 450A. It is 4 inches in length and has been formed from a brown quartzite pebble which, by dexterous chipping, has been brought into a nearly symmetrical form with a sharp point and edge. It much resembles one from the Robin Hood Cave, Creswell Crags, Fig. 413A.

[Illustration: Fig. 450A.—Saltley. 1∕2]

The valley of the river Rea runs at Saltley in a more or less N.N.E. direction, and is about a mile in width. Several stretches of gravel are found at different heights on both sides of the valley, but especially on the southern side. The highest and oldest gravels on this side are exposed in a clay-pit just in front of Saltley College, and are about 3 feet in thickness. They consist in the main of small quartzite pebbles in a light-brown sandy matrix, though some large pebbles and a few broken foreign flints also occur, and below the sandy beds is a layer, 3 or 4 feet thick, of Glacial clay and sand, with pebbles and boulders (Arenig felsite, &c.), and below this again come the Keuper marls, which are used for brick-making. The level of the top of the gravels is 395 feet above Ordnance Datum and that of the river is about |580| 315 feet, so that the valley must have been excavated to the depth of at least 80 feet since the gravels were deposited.

The implement was found at the base of the sandy gravel at a distance of about 60 yards from the front of Saltley College. In the same beds and in a small area, some 10 yards square, were found a number of fractured quartzite pebbles, which though not presenting such distinct signs of design may possibly owe their forms to human workmanship. Some of the chipped pieces of quartzite in the caves of Creswell Crags are rude in the extreme. The discovery of this well-fashioned specimen suggests some interesting considerations.

It has been held that the absence of palæolithic implements in Britain north of an imaginary line drawn from about the mouth of the Severn to the Wash, is due to glacial conditions having prevailed in the north-west part of England and in Scotland at the time when the makers of these early tools or weapons occupied the southern and eastern parts of this country, which, however, in those days was not an island but was still connected with the Continent.

The question now arises whether the assumed absence of palæolithic implements over this area may not be due to their not having as yet been found, and not to their non-existence.

It must be remembered:—

1st. That flint is extremely scarce over a great part of the area, and therefore that any implements would almost of necessity have to be formed from some other material, such as quartzite or one of the older rocks.

2nd. That in the case of implements made of such materials, the evidences of human workmanship are not so conspicuous or so easily recognized as on those formed of flint.

3rd. That owing to the nature of the rocks over which the ancient rivers flowed, the alluvial deposits within the area in question are of quite a different character from those formed in districts where flint abounds.

4th. That such alluvial deposits are not so constantly being excavated for economic purposes, and consequently not so open to examination as ordinary flint gravels, and that implements made from such materials as quartzite being probably more difficult to make, they would be fewer in number over a given area and also more highly treasured.

Even in the case of cave-deposits we have seen how, in those of |581| Creswell Crags, a locality which lies within the presumed non-implementiferous district, all the larger implements were made from quartzite, some of the tools being so rude that human workmanship can hardly be recognized upon them. I therefore venture to think that if competent observers like Mr. Landon will devote their attention to the ancient gravel-like alluvial deposits of our northern rivers, and seek for implements not formed of flint but of quartzite or some other of the older rocks, their search will be rewarded. In some of the Welsh caves the implements were for the most part made of felstone and chert.

The finding in the neighbourhood of Bridlington of a flint implement of a distinctly palæolithic type, seems to afford corroborative evidence in favour of extending the area of such discoveries, though it must be admitted that so far as at present known it was not lying in association with any remains of the pleistocene fauna.

It may be incidentally mentioned that palæolithic implements of quartzite, and even of Tertiary sandstones, occur though rarely in districts in which flint abounds. Possibly it was found that this material was tougher and less brittle than flint, and therefore better adapted for certain uses when the sharpness of the edge was not of primary importance. Most of the implements from India are formed of a quartzite which is more easily chipped into form than that of our English pebbles.

I now come to the important district drained by the Thames and its affluents, which comprises an area of upwards of 5,000 square miles. The number of localities within this area, where discoveries have been made in the ancient River-drift, has greatly increased since 1872, and at some of them palæolithic implements have been found in abundance.

[Illustration: Fig. 451.—Gray’s Inn Lane. 1∕1]

The Thames valley may moreover lay claim to the first recorded discovery of any flint implement in the Quaternary gravels, whether in this or any other country. An implement is preserved in the British Museum to which my attention was first directed by Sir A. Wollaston Franks, and which is thus described in the Sloane Catalogue:—“No. 246. A British weapon found, with elephant’s tooth, opposite to black Mary’s, near Grayes Inn Lane. _Conyers._ It is a large black flint shaped into the figure of a spear’s point. K.” This K. signifies that it formed a portion of Kemp’s collection. It appears to have been found at the close of the seventeenth century, and a rude engraving of it illustrates a letter on the antiquities of London, by Mr. Bagford, dated in 1715, and printed |583| in Hearne’s edition of Leland’s “Collectanea.”[2560] From his account it would seem that a skeleton of an elephant was found not far from Battlebridge by Mr. Conyers, and that near the place where it was found, “a British weapon made of a flint lance, like unto the head of a spear, was dug up.”

A full-sized engraving of this implement illustrated my first notice of these discoveries, in the _Archæologia_,[2561] and is here reproduced as Fig. 451. As will be seen, it is remarkably similar in form to that from Santon Downham, Fig. 433, though rather larger in size. During some excavations in Gray’s Inn Lane[2562] in 1883 and 1884, several palæolithic implements of different forms were found; but none I think so fine as that described by Leland. One found in Clerkenwell Road in 1883 by Mr. G. F. Lawrence,[2563] was, however, slightly larger. Another implement was found in Drury Lane,[2564] and others from Jermyn Street and Prince’s Street, Oxford Street, are in the Museum of Economic Geology.

Before describing the recent discoveries which have been made higher up the valleys of the Thames and its affluents, it will be well to discuss the various localities in the immediate neighbourhood of London, so as not to disturb the sequence of the Figures which is necessarily that of my first edition. It will be needless to do this at any great length, as the principal investigator of the gravels around London, to whom indeed the greater part of the discoveries are due—Mr. Worthington G. Smith—has given full particulars in his excellent book, “Man, the Primeval Savage.”[2565]

[Illustration: Fig. 452.—Hackney Down. 1∕2]

* * * * *

In the British Museum is an oval implement, formerly in the collection of the late Rev. Dr. Sparrow Simpson, F.S.A., shown in |584| Fig. 452, and found by Mr. G. H. Gaviller in gravel dug at Hackney Down, to the north-east of London, and not far from Shacklewell. It is of ochreous flint, slightly rolled, and in form remarkably like that from Bournemouth, Fig. 476. Though the exact place whence it came is unknown, there can be no doubt of its belonging to the Hackney Down gravels, which may be regarded as identical in age and character with those of Shacklewell, which have been described by Sir Joseph Prestwich.[2566] The surface of the ground at Hackney Down[2567] is 70 feet above Ordnance Datum, and in 1866 a shaft was there sunk through gravel and sand, to a depth of 22 feet. In the sandy beds at the base Mr. G. J. Smith[2568] discovered numerous land and freshwater shells, and among them the _Hydrobia marginata_—already mentioned as having been found in the Bedford Drift, and as being no longer an inhabitant of Britain—and the _Corbicula fluminalis_, which has already been cited as occurring near Cambridge, and of which more will be said immediately. The Shacklewell gravel mainly consists of subangular broken flints, some large flints but little worn, Lower Tertiary pebbles, a few quartz and sandstone pebbles, and some rolled blocks of hard Tertiary sandstone. In the pit described by Sir Joseph Prestwich there is, at a depth of about 8 feet, a bed of sandy clay intercalated in the gravel, and containing mammalian remains, numerous land and freshwater shells, and remains of oak, elm, alder, and hazel. The group of shells procured here resembles that of the Salisbury Drift, of which mention will be made hereafter.

Since 1854, when his paper was read, numerous specimens of the _Corbicula fluminalis_, or, as it was formerly called, the _Cyrena consobrina_, have been found here by Sir Joseph Prestwich, Sir Charles Lyell,[2569] and others, including myself. This shell, of a mollusc no longer living in Europe, though still found in the Nile and in several Asiatic rivers, has also been found in the Drift deposits of the Somme at Menchecourt, near Abbeville, associated with flint implements; and is likewise to be met with in the drift deposits of the Thames at Gray’s Thurrock, Ilford, Erith, and Crayford, in several of which implements have now been found. The beds at these places have by some geologists been regarded as belonging to an older and Pre-glacial period; but the discovery of an implement at Hackney Down raises a presumption that the gravel there is, like other flint implement-bearing gravels, Post-glacial; and the discovery of an implement in beds of fluviatile origin at a still higher level than those of Hackney Down corroborates this view, as the lower bed is probably the more modern.

The fluviatile beds in question were exposed in two brick-pits at Highbury New Park, near Stoke Newington, and attention was first called to them in August, 1868,[2570] by the late Mr. Alfred Tylor, F.G.S. The surface of the ground at the more eastern of these two pits is, according to Mr. Tylor, 102 feet above Ordnance Datum; and 22 feet below the surface there is a bed of clay 2 feet thick, full of land and freshwater shells, accompanied by much wood. There are |585| also shells in the lower part of the reddish loam or brick-earth immediately above the clay. The shells are said to consist of _Helix_, _Zua_, _Clausilia_, _Succinea_, _Carychium_, _Limnæa_, _Planorbis_, _Valvata_, _Pisidium_, and _Cyclas_; to which Mr. J. Wood Mason, F.G.S.,[2571] added _Achatina_, _Bythinia_, _Pupa_, and _Velletia_.

On reading the account of this discovery, I was at once impressed with the possibility of the occurrence of palæolithic implements in the deposit; and accordingly in September, 1868, I visited the pit with the view of searching for them, taking with me my youngest son, Norman, who had a quick eye, and an almost instinctive power of recognizing a worked flint. Our search was soon rewarded, for immediately on descending into the lower part of the pit, where the shell-bearing beds were exposed, my son picked up the remarkably well-formed implement shown in Fig. 453. It was not _in situ_, but was lying in the bottom of the pit; and judging from the staining upon a portion of its surface, it appears to have been derived from the brick-earth, rather than from the more shelly beds below.

[Illustration: Fig. 453.—Highbury New Park. 1∕2]

It is well adapted for being held in the hand as a sort of knife or chopper, having a thick rounded back formed of the natural crust of the nodule of flint from which it was formed. One face of it has been the result of a single blow, and its surface is that of a portion of a what irregular cone, at the apex of which the blow was struck, by |586| which it was produced. The other face, as will be seen by the figure, has been fashioned by first roughly chipping the implement to a curved edge, by blows administered on the flatter face, and then neatly trimming this edge to a regular sweep by secondary chipping. The ends have also been trimmed into shape. At the upper end, as shown in the figure, a small piece has been broken off, but otherwise the edge is uninjured. In character it is identical with the implement from the Santon Downham gravel, Fig. 437, and it closely resembles some of the large trimmed flakes from High Lodge, near Mildenhall, and the “choppers” from the cave of Le Moustier. The surface of the flint is stained ochreous in places, and presents much the same appearance as do some of the implements from the brick-earth at Hoxne.

It was in consequence of my publication of these discoveries that the attention of Mr. Worthington Smith was directed to the gravels of North-Eastern London, among which his labours have been crowned with such marked success. Not only has he found palæolithic implements in the City,[2572] Gray’s Inn Lane, Clerkenwell, London Fields, Dalston, Kingsland, Homerton, Hackney, Lower Clapton, Upper Clapton, Stamford Hill, Mildmay Park, South Hornsey, Abney Park Cemetery, Stoke Newington, and Shacklewell, but he has been able to identify the old surface of the ground, which was occupied by the early men who chipped out the implements. To this old land-surface he has given the name of the “Palæolithic floor,” and he has been able to trace its existence over a considerable area of ground on the western as well as the eastern side of the river Lea.[2573] It consists of a stratum of five or six inches of subangular ochreous gravel, in some places, however, only one or two inches in thickness, or only visible as a tone of colour. On, and imbedded in this floor among rolled and waterworn stones and bones, black, sharp and unabraded implements of flint occur, together with flakes which, in some instances, have been susceptible of being replaced in their original juxtaposition. Below the floor are usually thin beds of sand containing shells of land and freshwater mollusca, and beds of gravel, sometimes as much as 12 feet thick, containing palæolithic implements more or less abraded. The sand is not always present. Above the floor are usually contorted loamy beds of “warp and trail,” generally 4 to 6 feet thick, including the superficial humus. These seem to be of subaërial origin and may be due to a lengthened prevalence of a cold and rainy climate. The fauna of the gravels is described as including _Felis spelæa_, _Hyæna_, _Elephas primigenius_, _E. antiquus_, _Rhinoceros megarhinus_, _R. leptorhinus_, and _R. tichorhinus_, _Cervus tarandus_, and _Megaceros hibernicus_. Remains of _Antilope Saïga_ have, I believe, been also found. Among the testaceous remains _Corbicula fluminalis_ and _Hydrobia marginata_ have already been noted.

Another diligent investigator of the gravels of North-East London, who has also treated of the Palæolithic floor, is Mr. J. E. Greenhill.[2574] He has given some interesting sections, showing how the waterworn, abraded implements underlie those of the Palæolithic floor which are quite unworn.[2575] Professor Rupert Jones, F.R.S., has also written on |587| the subject. The best geological account is that given by Mr. W. Whitaker, F.R.S.[2576]

By the kindness of Mr. Worthington Smith most of the important specimens that he has found are now in my collection. I am further indebted to him for the use of the blocks illustrating some of the implements.[2577] Fig. 453A exhibits a finely pointed implement from Lower Clapton. Its surface is lustrous and it shows at its butt part of the original crust of the nodule of flint out of which it was chipped.

[Illustration: Fig. 453A.—Lower Clapton. 1∕2]

The fine ovate implement,[2578] Fig. 453B, came from the 12 feet stratum at Stamford Hill. It is of dark colour, lustrous, and has the angles slightly abraded.

A small example from the Palæolithic floor at Stoke Newington is shown in Fig. 453C.[2579] The edges are still quite sharp, and at one place there appear to be traces of use. A quartzite[2580] implement from the same locality is shown in Fig. 453D.

Implements presumably of Palæolithic Age have been found in the bed of the Thames. One from Battersea is of peculiar form, with a |588| truncated butt, and has been presented to the Christy Collection by Sir A. Wollaston Franks, F.R.S. Another from Hammersmith is in the same collection, having been formerly in that of the late Rev. Dr. Sparrow Simpson, F.S.A. It is 8 1∕4 inches long, and much resembles that from Reculver, Fig. 458, though somewhat longer in its proportions and thicker in the butt. It is much rolled and water-worn, so that it has probably belonged to a bed of gravel at a much higher level than that from which it was dredged up. Another (5 5∕16 inches) from the bed of the Thames at the Chelsea Suspension Bridge was found by Mr. Lambton Young, C.E., in 1854, before general attention had been directed to such relics. Mr. G. F. Lawrence, of Wandsworth, has ovate specimens from the Thames, at Wandsworth, Battersea, Putney, and Richmond, all but the latter much rolled.

[Illustration: Fig. 453B.—Stamford Hill. 1∕2]

[Illustration: Fig. 453C.—Stoke Newington Common. 1∕2]

It will be most convenient to reserve the discoveries in the South of London and in the valley of the |589| Lea for future pages, and to proceed up the Thames valley towards its sources.

* * * * *

Nearly ten miles to the west of London, and on the northern side of the Thames, the careful researches of General Pitt Rivers, F.R.S., have been amply rewarded, he having found several implements of well-marked palæolithic types, and numerous flakes, in the gravels of Ealing Dean and Acton.[2581] He has fully described the localities and given sections of the beds in a communication to the Geological Society.[2582]

[Illustration: Fig. 453D.—Stoke Newington Common. 1∕2]

* * * * *

At the former spot, the surface of the ground is 92 feet above Ordnance Datum, and here several implements have been found. At Acton the surface is from 60 to 80 feet above high-water mark, and here an implement of oval form was found beneath 7 feet of stratified sand and gravel, and resting on the clay beneath; another, of pointed form, was found in the middle of the gravel, about 10 feet from the surface, and beneath beds of sand 8 feet in thickness. Others were found in gravel from the same spot, and from Mill Hill, half-a-mile to the westward, which had been spread on the roads. One of the pointed implements from Ealing Dean is shown in Fig. 454. In form it much resembles that from Reculver, Fig. 458, though smaller in size. Like all the other implements from these two spots, it is stained of the ochreous colour of the gravel, and has had its angles worn away by being rolled in water along with the other constituents of the gravel. The flakes, which are comparatively abundant, are for the most part |590| large and rude, but many appear to have had their edges chipped by use. Some have been wrought into the scraper form. Cores or blocks of flint from which flakes have been struck have also been found.

In May, 1871, an implement, 8 inches long, and of rather less tapering form than that from Ealing, Fig. 454, was found at Acton, beneath 13 feet of sand and gravel, at a spot where the surface is 70 feet above high-water mark. General Pitt Rivers has also seven or eight flakes of flint, one of them 5 1∕2 inches long and 1 inch wide, which were found together, beneath 9 feet of brick-earth and gravel, in excavating for the foundations of a house at Acton. Their edges are sharp and unworn, so that they must have been deposited where they were found, prior to the accumulation of the 9 feet of drifted beds above them. They lay in a bed of ochreous sandy clay, about 1 foot in thickness, which reposed immediately on the blue London Clay.

[Illustration: Fig. 454.—Ealing Dean. 1∕2]

In Acton village, the beds of Drift which constitute the first patch of gravel occurring at so high a level as we go westward from London, and which form a sort of terrace overlooking the broad valley of the Thames, attain a thickness of 18 feet, and consist of layers of sub-angular gravel, mixed with yellow and white sand, very irregularly stratified. The gravel consists principally of flints and Tertiary pebbles, with some of quartz and quartzite. A few mammalian remains, including a tooth of _Elephas primigenius_, have been found in these beds, and south of Ealing Park[2583] land and freshwater shells. At |591| a lower level, and cut off from the upper gravels by an outcrop of London Clay, is a wide terrace of alluvial deposits at an average height of about 20 feet above high-water mark, and a lower terrace still is to be found in the immediate neighbourhood of the river. General Pitt Rivers’s researches in the mid-terrace beds of gravel and brick-earth have not produced any implements of the River-drift types, but he has obtained animal remains which were identified by the late Mr. G. Busk, F.R.S., as those of _Elephas primigenius_, _Rhinoceros hemitæchus_, _Hippopotamus major_, _Bos primigenius_, _Bison priscus_, _Cervus tarandus_, and other species of deer. They occur invariably at the base of the gravel 12 or 13 feet from the surface. The late Mr. Thomas Belt, F.G.S.,[2584] has speculated on the age and character of the Acton deposits.

Mr. J. Allen Brown, F.G.S.,[2585] has diligently continued these researches, and in laminated clay, 200 feet above O.D. at the Mount, Ealing, has found an ochreous flake trimmed at the edge. At Creffield Road, Acton,[2586] Middlesex, he has discovered another “Palæolithic floor,” having found more than 600 flakes and implements in an area of not more than 40 feet square. Besides implements from Acton and Ealing up to 130 feet above O.D. he has described specimens from East Sheen, on the other side of the Thames, and Hanwell,[2587] Iver, Gunnersbury, Kew, Turnham Green, and Dawley, near West Drayton. An ovate implement from Dawley is of felsite. He has also described implements found at Southall[2588] associated with remains of _Elephas primigenius_. A pointed specimen from Southall is made of quartzite. At Hounslow[2589] also implements have been found. It is possible that the gravels at West Drayton belong to the valley of the Colne rather than to that of the Thames, as also those at Hillingdon, where in the Town-pit, 180 feet above O.D., Mr. Brown has found palæolithic implements.

Farther west, at Langley and at Burnham, implements have been found in the gravels. One from Burnham was given to me by Mr. E. Sawyer. He has also found a broad-pointed implement at Cookham, near Maidenhead. They have likewise been discovered at Ruscombe,[2590] Taplow,[2591] Maidenhead, and Marlow. A very broad-pointed implement (5 1∕2 inches) found in high-level gravel at Cookham, Maidenhead, has been shown to me by Mr. E. Sawyer. In my own collection are specimens from the majority of the other localities here enumerated. In form and character they approximate so closely to those from similar deposits elsewhere that it seems needless to figure any of them.

Higher up the river Thames, the next important discoveries to recite are those which have been made in and near Reading by Dr. Joseph Stevens. At Grovelands,[2592] about 80 feet above the level of the |592| river, near the junction of the Kennet and the Thames, the Drift deposits are ferruginous and about 15 feet thick. In them were found a tooth of a mammoth and numerous implements, principally of ovate forms and made of flint, but among them one made of quartzite. At Redlands, at a lower level, about 40 feet above the river, mammoth remains occur, as also at the Kennet Mouth Pit, Newtown, where a kite-shaped implement was found. The geological position and structure of the Redlands beds have been described by Prof. Poulton, F.R.S.[2593] In 1882 I found in the gravel at Pig’s Green, near Reading, the butt-end of a pointed implement, which had been originally about 4 1∕2 inches long and had lost its point before being deposited in the Drift. The gravel was subangular and ochreous, and contained from 15 to 20 per cent. of quartzite pebbles. Flint flakes were fairly abundant, but finished implements, scarce. On the other side of the river, at Caversham, Dr. Stevens has found implements in gravel 120 feet above the level of the Thames. I have myself found an acutely-pointed implement (4 inches) in the same beds.

* * * * *

These Caversham Beds have been well described by Mr. O. A. Shrubsole.[2594] At Toots Farm the implements are usually pointed, as also at Shiplake, at a distance of about three miles and at a slightly lower level. At Henley Road, Caversham, about 59 feet above the Thames, he obtained a flat ovoid implement of flint. A molar of _Elephas primigenius_ was found at this spot. South of the Thames, besides the pits mentioned by Dr. Stevens, Mr. Shrubsole enumerates the following localities: a cutting of the South Western Railway at Earley, one of the Great Western Railway at Sonning, a gravel-pit at Charvil Hill, Sonning, and a brick-yard at Ruscombe, near Twyford. In the last-mentioned place several implements of various types have been found. Some extremely doubtful specimens, probably of purely natural origin, have been found on Finchampstead Ridges,[2595] but in gravel at Wokingham[2596] a large highly finished pointed implement has been obtained by Mr. P. Sale.

Some more or less worked flints from the Reading[2597] gravels have been described and figured by Mr. O. A. Shrubsole, who has assigned uses to what he terms “the less familiar forms of Palæolithic Flint Implements.”

Still higher up the Thames, near Wallingford, there is a considerable spread of gravel, some of it at a distance of two miles or more from the existing streams. In this gravel implements have been found, though up to the present time in no great abundance. I |593| have a fine kite-shaped specimen of the type of Plate I., No. 6 (5 1∕2 inches), that was found at Gould’s Heath, East of Wallingford, and two from Turner’s Court,[2598] rather nearer the town. In all three cases the flint has become more or less whitened. I have another large flat ovate implement more like Plate I., No. 16, that was found at Cholsey, on the other side of the river. It is more lustrous and not so much whitened. Another was found on the surface at Ipsden,[2599] 3 miles S.E. of Wallingford.

In the neighbourhood of Oxford a fair number of palæolithic implements have been found, some of which are in the University Museum. The first of these was a fine specimen with a heavy butt and pointed tip (broken off), procured, in 1874, by Sir Joseph Prestwich from gravel on the left bank of the Cherwell, at Marston Ferry, not more than from 4 to 5 feet from the surface. Another, ovate (3 3∕4 inches), was obtained by the late Professor Rolleston from the foundations of the New Schools in the High Street, in 1878, and two more of ruder workmanship came from the site of the Girls’ High School in the Banbury Road, in 1880. Yet another was found below Oxford by the side of Bagley Wood, opposite Iffley. The principal discoveries have, however, been made at Wolvercote, about 1 1∕2 miles north of Oxford, whence many have been collected by Mr. A. M. Bell,[2600] from whose account of the discoveries I have been quoting. Among the specimens in his and other collections are pointed and ovate implements, a fine example of the shoe-shaped type, like Fig. 429 (8 1∕2 inches), trimmed flakes and a hammer-stone. One of Mr. Bell’s pointed implements has been chipped out of quartzite. The brick-earth and gravel deposits lie in what appears to be an old river-channel, which has been cut into the Oxford clay and the superimposed Northern Drift to a depth of about 17 feet from the surface. It is at the base of this channel that the implements are found. In the sand near the base nine or ten species of land and freshwater shells occur, and in a peaty bed immediately above the sand and gravel the remains of various plants; but both the testaceous and vegetable remains belong to species still found in the neighbourhood. Mammoth, rhinoceros, and hippopotamus as well as _Corbicula fluminalis_ have, however, been found in the Oxford gravels. The beds at Wolvercote above the peat consist of clay and sand deposited evenly in successive layers, but towards the surface they are |594| traversed by an irregular line of “trail,” such as is often seen above palæolithic deposits and for which it is so difficult to account.

Mr. Percy Manning, F.S.A., possesses several palæolithic implements found near Oxford. Among eleven specimens from Wolvercote, mostly tongue-shaped, is one of brown flint 9 1∕2 inches long and 4 1∕2 inches broad, sharply pointed with a truncated butt and the sides curving outwards somewhat like Fig. 475. Another fine implement from the same place has straighter sides and is 6 3∕4 inches long. The others are smaller, but among them is one of pointed form rather rudely chipped from a quartzite pebble.

Mr. Manning has also three implements dredged from a backwater of the Thames between Oxford and North Hinksey, one of them (4 3∕4 inches) like Fig. 422, but more roughly chipped and much waterworn. Another (4 inches) is like Fig. 436, but more pointed. The third (5 1∕8 inches), is a remarkably symmetrical ovate-lanceolate implement, in outline like Plate II., No. 11, made out of a pebble of quartzite, or possibly of chert. This also is waterworn.

At Broadwell, Oxon, on the borders of Gloucestershire, Mr. Manning found an implement (4 1∕4 inches) resembling Fig. 459, apparently from gravel dug upon the spot. The village of Broadwell lies about 3 miles to the north of the Thames.

In my former edition I called attention to the discovery in the valley of the Wey, at Peasemarsh, between Guildford and Godalming, by the late Mr. Whitbourn, F.S.A.,[2601] some sixty years ago, of the implement shown in Fig. 455, which is now in my own collection. It was found embedded in the gravel in a layer of sand about 4 or 5 feet from the surface, in apparently undisturbed ground. Mr. Whitbourn had heard of remains of large animals having been discovered in the same beds, but not in very close proximity to the spot where the implement was found. It is, as will be seen by the figure, of a different shape from the majority of the implements found in the River-drift, being very broad at the base and short in proportion to its width. The flint of which it consists is grey and slightly ochreous. At the base is a considerable portion of the original crust of the flint, which is stained of a dull red. The gravel beds, in which it was found, have been described by Mr. R. A. C. Godwin-Austen, F.R.S.[2602] They rest on Wealden Clay, and in places, on beds of the Lower Greensand. The material principally consists of sub-angular chalk flints, and |595| in it have been found numerous remains of _Elephas primigenius_. In places, the gravel overlies what appears to have been an old land-surface, in the mould of which fragments of branches of trees, and bones of ox and elephant, have been found uninjured and lying together. Mr. Godwin-Austen does not record the discovery of any land or freshwater shells in the gravels, nor on visiting the spot was I able to find any, or any more worked flints. In the Woodwardian Museum, at Cambridge, is an implement of palæolithic type, and of the ovate form, found higher up the valley of the Wey, near Alton, but on the surface, and not in gravel.

[Illustration: Fig. 455.—Peasemarsh, Godalming. 1∕2]

At Farnham, between Alton and Godalming, many palæolithic implements have been secured from the gravels of the valley of the Wey, principally through the intelligent care of Mr. Frank Lasham, of Guildford, and Mr. H. A. Mangles, F.G.S., of Littleworth Cross, Tongham. The former has contributed a paper on “Palæolithic Man” to the Surrey Archæological Society,[2603] and has kindly given me much information on the subject. The beds of gravel are from 10 to 40 feet deep, and lie upon the Lower Greensand. They attain an elevation of 364 feet[2604] above the mean sea-level, or about 150 feet above the present bed of the river, and are principally dug in pits on the southern or right side |596| of the Wey towards Wracklesham, pits which have furnished several hundreds of palæolithic implements of various forms and sizes. The oval and ovate seem to predominate, but there have been found not a few fine pointed implements. Associated with the more sharply preserved specimens, are many of dark ochreous colour, with their angles much abraded, which in all probability have been brought down by the old river from beds higher up its valley. Remains of mammoth occur occasionally in the gravels. Some specimens of the implements are preserved in the Charterhouse School Museum. Mr. Lasham informs me of an implement having been found in gravel at Peperharow, of a part of one near Farley Heath, and of one found at Frimley,[2605] in the valley of the Blackwater.

The discoveries of palæolithic implements in the valley of the Colne near its junction with the Thames, have already been recorded. In the valley of the Misbourne, an affluent of the Colne, an implement was found in 1891 in digging the foundations of the bridge over the Metropolitan Extension Railway, just north of Great Missenden. It is of a thick ovate form, made of grey flint, rather narrower than Pl. II., No. 18, and with small flat surfaces of the original crust of the flint left about the middle of each side. The specimen is in my own collection.

In the valley of the Gade, in Hertfordshire, a few have been found by myself. The first of these was lying on the surface of a ploughed field near Bedmond,[2606] in the parish of Abbot’s Langley, at a spot which, though probably 160 feet above the level of the nearest part of the stream, is towards the bottom of one of the lateral valleys leading into the main valley of the Gade, between Boxmoor and Watford. The implement, which has unfortunately lost its point, is remarkably similar in form and size to that from Gray’s Inn Lane, Fig. 451. The flint of which it is made has become nearly white and porcellanous on both faces, though more so on one than on the other. In places it has been so much altered in structure that it can be cut with a knife. I have noticed this feature in flints which have lain long in pervious red brick-earth, and this leads me to suppose that the implement may have been derived from some beds of that character at the spot where it was found, though on this point I have no direct |597| evidence. In 1892[2607] I found another small implement (4 inches) of rude ovate form, among some stones recently placed in a rut at Bedmond Hill. Here, again, there is no evidence as to the exact geological position. Nor is there with regard to two other implements, both of which I found in 1868, in gravel laid on the towing-path of the Grand Junction Canal, which is there united with the Gade, between Apsley and Nash Mills, about two miles south of Hemel Hempstead. There is, however, no doubt of the gravel in which they lay having been dredged or dug from the bottom of the valley in the immediate neighbourhood. One of them, of grey flint, is a neatly-chipped, flat implement, of ovate outline, about 4 inches long, in form much like Fig. 468, from Lake. The other is imperfect, but appears to have been originally of much the same character, though flatter on one face. It is deeply stained of an ochreous colour, and its angles are considerably waterworn. I have searched in the gravels of the neighbourhood for other specimens, but as yet in vain. I may add that during the formation of this part of the canal, some eighty years ago, an elephant’s tooth was found in the gravel, within about 200 yards of the spot where I discovered one of the implements.

Other specimens are reported to have been found near the head of the tributary valley of the Bulbourne, at Wigginton, near Tring.

At Watford, Herts, on the left bank of the Colne, in gravel near Bushey Park, at a height of about 40 feet above the level of the existing river, Mr. Clouston has found several implements of ochreous flint of various types. He has kindly given me a square-ended flake, much like Fig. 426A, from High Lodge, Mildenhall.

Some of the discoveries made by Mr. Worthington G. Smith were in localities within the valley of the Ver, an affluent of the Colne, rather than in that of the Lea, but inasmuch as many of the beds which contained the implements found by him seem to bear but little relation to existing watersheds, and are at no great distance from the Lea, I shall at once proceed to the discussion of the remarkable series of facts which he has brought to light. All details must, however, be sought for in Mr. W. G. Smith’s own book, “Man, the Primeval Savage.”[2608] |598|

The main source of the Lea is at Leagrave Marsh, about 3 miles N.W. of Luton, and 376 feet above Ordnance datum. On the surface near this place, Mr. Smith[2609] found a flat ovate implement, in form much like those from Warren Hill or that from near Dunstable, Fig. 17. He says that it may be neolithic, but that he has found palæolithic flakes, both ochreous and grey, _in situ_ in gravel at Leagrave. At Houghton Regis,[2610] 1 1∕2 miles north of Dunstable, Mr. Smith found a fragment of an ovate implement on the surface. Another implement, found so long ago as 1830 by Mr. William Gutteridge, at Dallow,[2611] or Dollar farm, 3∕4 of a mile west of Luton, is distinctly palæolithic in form.

The most interesting of Mr. Worthington Smith’s discoveries have, however, been made on or near the summit of a hill, a good 2 miles from the Lea, and somewhat nearer the Ver. At and around the village of Caddington there are several brickfields, some of them no longer worked. The original surface of the ground in some of these is as much as 550[2612] to 595 feet above the Ordnance Datum. The brick-earth is of great thickness, in places fully 50 feet, and overlies the Chalk. The upper portion of the beds is much contorted, and has in it occasional seams of flint gravel or tenacious clay, in which cream-coloured or brownish palæolithic implements occur. In the gravel, brown, ochreous, slightly abraded implements and flakes are found, and at the base in many cases is the old land-surface or “Palæolithic floor” resting on and surmounted by brick-earth. In one pit were three heaps of flints brought by hand in Palæolithic times from flint-bearing beds either above or in the Chalk. On the Palæolithic floor were numerous sharp-edged flakes, which had hardly been moved from the original place at which they were struck off. Mr. Smith has replaced more than 500 flakes either on to other flakes or on to implements and cores from the same floor.

One old land-surface was full of narrow vertical fissures, due perhaps to the heat of a burning summer sun. While they were still open 18 inches of watery brick-earth, perhaps brought down by a heavy storm of rain, filled up the fissures, covered up the old surface and formed a new surface at a higher level. The upper deposits often resemble contorted masses of half-frozen mud and stone pushed over an old water-laid and perhaps frozen surface of brick-earth. Mr. Smith’s view is that Palæolithic |599| man lived here by the side of one or more small freshwater lakes, and manufactured his implements upon the spot which eventually, by successive storms and flooding, became buried beneath accumulations of mud. The neighbouring valley on the west was not at that time excavated to its present depth. He considers that the ochreous implements found at Caddington are of earlier date than those of lighter colour found on the Palæolithic floor, and points out that there is, moreover, a difference in the nature of the tools, inasmuch as some well-formed scrapers occur in the brick-earth of the Palæolithic floor, while they are never found amongst the ochreous tools. The difference seems consistent with the probability that the tools for domestic use would be more abundant on the spot where the men of the period were at home than elsewhere. One of the most interesting features of the case is the number of instances in which Mr. Smith has been able to bring together the fragments of implements broken in Palæolithic times,[2613] and to replace upon them the flakes removed during the process of their manufacture. Of these he has given a long series of illustrations in his book;[2614] those relating to one instance are here by his kindness reproduced as Figs. 455A, B, and C.

[Illustration: Fig. 455A.—Caddington. 1∕2]

[Illustration: Fig. 455B.—Caddington. 1∕2]

In Fig. 455A is shown a finished implement broken in Palæolithic times, both pieces found separately and now conjoined. Fig. 455B shows the other side of the implement, with three of the flakes struck off during its manufacture replaced, and Fig. 455C reproduces the first view, but shows a fourth flake replaced. |600|

A good series of these reconstructed implements is in the British Museum.

Fig. 455D shows an ovate implement from the brown stony clay at Caddington. Fig. 455E represents a scraper, and Fig. 455F a pointed tool from the Palæolithic floor, and an ivory-white sharp-edged implement from the same source is illustrated in Fig. 455G. For all these figures,[2615] I am indebted to Mr. Worthington Smith, as well as for very many acts of kindness.

A paper by Mr. Smith on Neolithic and Palæolithic scrapers, re-placed and re-worked, will be found in the _Essex Naturalist_.[2616]

[Illustration: Fig. 455C.—Caddington. 1∕2]

[Illustration: Fig. 455D.—Caddington. 1∕2]

At Mount Pleasant,[2617] Kensworth, to the west, on the other side of the extension northwards of the valley, and at a height of 760 feet above Ordnance datum, or nearly 200 feet higher than the Caddington deposits, Mr. Worthington Smith has found |601| some ochreous flint flakes, apparently of Palæolithic age, one of them trimmed.

[Illustration: Fig. 455E.—Caddington. 1∕2]

[Illustration: Fig. 455F.—Caddington. 1∕2]

At Harpenden, 8 1∕2 miles from the source of the Lea, and not far from the stream, he has obtained a few ochreous palæolithic flakes. At Wheathampstead, a few miles further down the Lea, he also met with a few ochreous flakes in gravel near the railway station.

[Illustration: Fig. 455G.—Caddington. 1∕2]

[Illustration: Fig. 455H.—Wheathampstead. 1∕2]

In gravel brought from No Man’s Land, a common about a mile south of Wheathampstead, the late Rev. Dr. Griffiths, of Sandridge, found two small ovate implements of whitened flint,[2618] one of which he presented to my collection. Mr. Worthington Smith, on visiting the spot in 1886, discovered a rude implement of nearly the same character _in situ_ in the gravel, and has lent me the block,[2619] Fig. 455H, on which it is represented. He subsequently found an implement with only one edge and the point |602| chipped into shape, also _in situ_. He likewise discovered a third implement and a well-formed scraper in the beds. The gravel at No Man’s Land is in a valley along which in former times the Lea or a branch of its stream may have taken its course. Near Ayot St. Peter[2620] and Welwyn, in the valley of the Maran, Mr. Worthington Smith has found flakes only. I have recorded the finding of an implement at North Mimms,[2621] south of Hatfield.

At and near Hertford and Ware, the Lea receives several other affluents coming from the north. Among these is the Beane, the present source of which is near Stevenage. At Fisher’s Green,[2622] a little to the north of that town, pointed ochreous implements have been found in the brick-earth by Mr. Frank Latchmore and myself. I have also a rough ovate specimen made from a large broad flake, and found in a brick-field south of Stevenage. Further south, in gravels exposed in a cutting of the Great Northern Railway near Knebworth,[2623] some well-formed implements, both pointed and ovate, were found in 1887. I have several specimens, as well as an ovate implement found on the surface in 1890. Still farther south, in a clay-pipe near Welwyn Tunnel, a pointed ochreous implement (4 inches) was obtained in 1896, which Mr. Frank Latchmore has kindly added to my collection.

Palæolithic implements have been found by Mr. Worthington Smith in the gravels of the Lea[2624] and Beane at Hertford and Ware, one of them at Bengeo. They are of pointed forms, fairly well made, and much water-worn. He has recorded other implement-bearing gravels a mile north-west of Ware and at Amwell. General Pitt Rivers has a remarkably fine palæolithic implement, which is said to have been found at Bayford, a mile or so south-west of Hertford.

In the valley of the Stort, which joins the Lea near Hoddesdon, two palæolithic implements have been found by Mr. W. H. Penning, F.G.S., in the neighbourhood of Bishop’s Stortford. Though in both instances lying on the surface, yet the condition of the implements is such that there can be no doubt as to their having been but recently dug out of the soil; the colour of both is a dark brown, ochreous in places, and the general appearance |603| much like that of the implements found in the brick-earth at Hoxne. One of them was found at a short distance from the river, by the side of a ditch cut in a thin deposit of valley brick-earth, about a mile north of Bishop’s Stortford, and probably had been thrown out with the soil from the ditch. It is 5 1∕2 inches long and 3 3∕4 inches broad, and in form it much resembles Fig. 421. The other is of the same character, but is somewhat broader, and is squarer at the base. It was found farther north, on the sandy surface of a ploughed field, close to Pesterford Bridge.

In 1872 Mr. Penning also found, near Stocking Pelham, five miles north of Bishop’s Stortford, an ochreous, somewhat water-worn, oval implement 5 inches in length.

At Flamstead End,[2625] one mile west of Cheshunt, and on the right side of the Lea, Mr. Worthington Smith has obtained several implements in the gravels, some of which he has kindly added to my collection. He has also found specimens at Bush Hill Park and Forty Hill, near Enfield; Rowan Tree Farm, Lower Edmonton, and between Edmonton and Winchmore Hill. For his discoveries on the east or left side of the Lea I must refer the reader to Mr. Smith’s book, “Man, the Primeval Savage.” Suffice it to say that he has found implements in Drift deposits at Plaistow,[2626] Stratford, Leyton, Leytonstone, Wanstead, Walthamstow, Higham Hill, West Ham, Forest Gate, and Upton. In the valley of the Roding he has added Barking, East Ham, and Ilford, and farther east again Rainham, Gray’s Thurrock, Little Thurrock, Tilbury, Mucking, Orsett, and Southend.

Mr. Hazzeldine Warren, of the Cedars, Waltham Cross, has obtained several palæolithic implements from gravels at Bull’s Cross and Bush Hill Park, Enfield, and a few at Hoddesdon. A fine pointed specimen (7 inches) from Bull’s Cross is rather like Fig. 459, but is battered at the butt.

From gravel at Grove Green Lane, Leyton,[2627] some good pointed implements have been obtained by Mr. A. P. Wire. One of them is 6 inches long.

A thin ovate implement made from a piece of tabular flint was found in gravel at Lake’s Farm,[2628] Cannhall Lane, Wanstead.

A sub-triangular implement with a heavy butt was found in gravel of the Roding Valley at St. Swithin’s Farm,[2629] Barking |604| Side, and two others at Wallend, one mile west of Barking town. Mr. G. F. Lawrence found an oval implement _in situ_ at Stratford.[2630] I have a rude specimen found at Shoeburyness by Mr. B. Harrison.

Returning to London we must notice some discoveries on the southern side of the Thames.

In 1872[2631] General Pitt Rivers recorded the finding of a palæolithic implement and a flake in gravel on Battersea Rise, at the junction of Grayshot Road and the Wandsworth Road; and in an excavation for a new house on Battersea Rise,[2632] near Clapham Common, on one of the higher gravel-terraces of the Thames, Mr. Worthington Smith picked up a palæolithic implement in 1882.

Mr. G. F. Lawrence has also found two or three implements in gravel at East and West Hill, Wandsworth, on each side of the Wandle, as well as at Earlsfield. One from the latter place, now broken, must originally have been of very large size. This and another are pointed. He has also found one at Lavender Hill, and a small ovate specimen at Roehampton.

At Lewisham also an implement has been discovered. One of ovate form (4 inches) was found in 1874 in gravel on Wickham Road by Mr. A. L. Lewis, and by him liberally added to my collection.

Further south, in a branch of the valley of the Ravensbourne, on a patch of gravel upwards of 300 feet above Ordnance Datum, Mr. George Clinch,[2633] in 1880, found several ovate palæolithic implements, and in subsequent years many more; in all some fifty[2634] in number.

About four miles farther east, at Green Street Green,[2635] about 250 feet above Ordnance Datum, Mr. H. G. Norman found two palæolithic implements, on the surface of what is now a dry part of the valley of the river Cray, about two miles above its present source. They are both of ovate form, one much like Fig. 420, the other like Fig. 468. Each is about 5 1∕2 inches in length. “The gravel at this spot has afforded remains not only of the mammoth, but also of the musk-ox.” |605|

Mr. de B. Crawshay[2636] has also found about 40 ovoid and pointed palæolithic implements near Green Street Green.

The valley may be traced upwards for nearly five miles, in a south-easterly direction, to Currie Wood, between Knockholt and Shoreham; and on the border of this wood, not far from Currie Farm, I found on the surface of the ground, in 1869, a well-marked flint implement, in character and size closely resembling that from Swalecliffe, Fig. 462, and stained of a rich ochreous colour. In places there are some ferruginous concretions adhering to the surface, and it has all the appearance of having been derived from the gravel which here not unusually forms the superficial deposit. A part of one of the faces has been lost owing to a recent fracture, and it can be seen that the implement has been formed of what is now a light buff, somewhat chalcedonic, flint, similar in character to that of most of the pebbles in the gravel at Well Hill, near Chelsfield, about midway between Currie Wood and Green Street Green. A subsequent search on the spot, in company with Sir John Lubbock, Sir Joseph Prestwich, General Pitt Rivers, and Sir Wollaston Franks, was unproductive of any more specimens. The remarkable feature in the case is the elevation at which this implement was found, the level of the ground being probably 300 feet above the neighbouring valley of the Darent, and upwards of 500 feet above the sea. Regarding the gravel, however, as connected with the valley of the Cray, and not with that of the Darent, its elevation above the head of the valley is but slight. In 1872 I remarked that it was “necessary that further discoveries should be made in this district, before it will be safe to speculate on the origin of these gravels, and their relation to the superficial configuration of the neighbourhood.” Since then, as will be seen in subsequent pages, these discoveries have been made.

Farther down the valley of the Cray than Green Street Green, near Dartford Heath, about half a mile to the south of Crayford Station, Mr. Flaxman C. J. Spurrell, F.G.S., has been so fortunate as to discover, _in situ_, the beautifully symmetrical implement which, through his kindness, I am enabled to engrave as Fig. 456.

* * * * *

It is of dark, brownish grey flint, in places mottled with white. It is worked to an edge all round, but is less sharp towards the base than towards the point. On one side, near the point, the edge |606| has been worn away by use into a curved notch. On the opposite side is a more modern break. It is almost equally convex on the two faces.

Mr. Spurrell informs me that he found this implement lying on its face, at a depth of 8 feet below the surface of the gravel, which is that of the upper level of Dartford Heath, and appears to belong to the valley of the Thames, and not to that of either the Cray or the Dart.

* * * * *

Another implement has been found near the same spot by Mr. C. C. S. Fooks.[2637] A little to the north of Crayford, in the brick-earth below an old cliff of chalk and Thanet sands, Mr. Spurrell has found a number of flakes of flint associated with remains of the Pleistocene fauna. He has, indeed, discovered a “Palæolithic floor” on which the ancient workmen lived while they fashioned their tools. Not many of the larger implements were found, but many of the flakes after having been struck off the nucleus had been trimmed at the butt-end. By patience and skill Mr. Spurrell was able to bring many of the flakes together into their original positions, and thus to reconstitute the blocks of flint from which they had been manufactured.[2638] In one instance he was able to build up around an implement—broken in old times—the various flakes struck off during its manufacture, and thus to reproduce the block of flint originally taken in hand by the workman. Two hammer-stones were present, made from cylindrical nodules of flint.

[Illustration: Fig. 456.—Dartford Heath. 1∕2]

It is to be remembered that in April,[2639] 1872, the Rev. O. Fisher, F.G.S., found a worked flint, or flake, in Slade’s Green Pit, Crayford, beneath a sandy stratum containing among other shells those of _Corbicula fluminalis_. In 1875 a large broad flake (5 1∕2 inches) was picked up by Dr. J. H. Gladstone, F.R.S.,[2640] in a |607| brick-earth pit at Erith. It is figured and described in the _Argonaut_.[2641] Another flake found in 1876 in the same stratum as that in which ten years earlier a skull of a musk ox occurred, has been figured by Professor Boyd Dawkins.[2642]