A History of Lancashire. Fishwick Henry
direction which these icebergs took was invariably from north–west to south–east, or north–north–west to south–south–east, that being sufficiently indicated by the polished and striated rocks frequently discovered in all parts of the county. A careful investigation of the erratic blocks which have been discovered in one small district alone1 shows nearly 400 of these rocks, some of which have travelled from Scotland, but by far the larger number have come from the Lake District; these are occasionally found in the valleys, but are generally located on the sides and tops of hills at an elevation of from 600 to 1,200 feet above the sea–level. Geology furnishes abundant proofs that at this period the level of the land in what is now known as Lancashire was fifty or sixty feet higher than it is at the present day; this is very apparent along the coast–line, where the remains of submarine forests are frequently met with. It is more than probable that, from the mouth of the Mersey to the estuary of the Dudden, what are now sand banks were in prehistoric times dry land on which grew forests of the oak, the birch, the ash, the yew, and Scotch firs.
All along the coast–line from Liverpool to Preston have been found at low water the roots and trunks of trees.
Near Fleetwood and Blackpool frequent traces of these forests have been met with below the high–tide level, the trunks of the trees all pointing eastward, with their torn–up roots to the west; stumps of Scotch firs were found near Rossall, and near to them the cones which had fallen from their branches; trunks of oak and yew trees were also discovered at Martin Mere (in Poulton).
In these forests the brown bear, the wild boar, roes and stags, the wolf and the reindeer, and a host of other wild animals, would all be discovered by the neolithic man when he first made his appearance in the district.
Whence came this earlier settler? and at what exact period did he come? are questions which modern scientific research has failed to satisfactorily answer.
It has been suggested – and with some show of reason – that the early neolithic man in Lancashire had been driven from the Yorkshire coast by the victorious invader, who came armed with a war–spear and polished stone axe.2 Be this as it may, the evidence of such a race of men having for some time lived in parts of the county is of the most conclusive character. Although odd specimens of flint instruments have been unearthed, in various districts, it is only in the eastern portion of the county that distinct traces of a neolithic floor have been discovered – that is to say that, on removing the top soil, beneath it has been found a surface so profusely sprinkled with flint chippings and implements as to leave no room for doubt but that at some very early period there was settled upon it a race of men whose weapons of offence and defence, as well as the few instruments required for their simple personal wants, were made out of the flints collected from this drift.
This neolithic floor is found on both sides of Blackstone edge, and is generally at least 1,300 feet above the sea–level, but on the Lancashire side its area is not very large, as it does not reach Burnley on the north, nor Bolton on the west. The depth of the soil or peat above this floor varies from one to ten feet. The flints consist of knives, scrapers, arrow–heads, spear–tips, and minute instruments, probably used to bore holes in bone needles; they are none of them polished or ornamented.
In the parish of Rochdale alone there are twenty–five places where these implements have been found; in fact, there is scarcely a hill–top in the district where traces of them have not been unearthed. The great number of chippings met with in small areas of these high lands indicate that these are the sites of the primitive man’s workshop – here he sat and laboriously fashioned the weapon or the instrument which he required. Barbed arrow–heads are extremely rare, but a beautiful specimen was lately found on Trough Edge, a hill near Rochdale.3
These men have left no traces of their dwelling–place, and they do not appear to have made pottery; probably they lived in earth dwellings or caves in the hillsides. The single fact of their inhabiting only the high ground indicates that the fear of an enemy was ever before them, and it may well be that the foe which drove them from Yorkshire may have ultimately expelled them from their hillside settlements.
At some later period the district became inhabited, though probably only sparsely, by Celtic races and people of Celtic extraction; of the latter were the numerous tribes of the Brigantes, one of which was the Setanii or Segantii (the dwellers in the water country), which is said to have been chiefly located between Morecambe Bay and the ridge of hills which divide Lancashire from Yorkshire. Another tribe also located here was the Voluntii.
At this date Lancashire contained many extensive forests, and in every direction were trackless morasses. As these almost savage tribes lived in tents or huts, and spent their time in hunting or fighting, it is not surprising that the traces of their existence are faint and unsatisfactory, and that it is often impossible to decide whether particular remains belong to the early Celtic or the late British. The geographical nomenclature of the county furnishes some examples of Celtic origin, but for the most part it clearly points to a later period. That these Celtic settlers were well spread over the entire district is certain, as traces of them have been discovered in almost every parish.
Stone hammers, stone axes, spear–heads, socketed celts, cinerary urns, and remains of that class, have been unearthed in many places, amongst which are Aldringham, Cartmel, Tatham, Penwortham, Garstang, Preston, Pilling Moss, Silverdale, Kirkham, Bolton, Cuerden, Flixton, Liverpool, Winwick, Lancaster, Manchester, Royton, Rochdale, and Burnley; this list is alone sufficient to demonstrate that the early settlers had penetrated into all parts of the county.4
In the Furness district remains of entrenchments, ramparts, stone rings, and other evidences of these early settlers are abundant; they have been unearthed at Hawkshead, Hall Park, Bleaberry Haws Torver, Holme Bank, Urswick, Heathwaite Fell, Coniston, and other places in the neighbourhood, proving beyond a doubt that here was an extensive British settlement. Beside these there are several cairns, and portions of stone wall attributable to the same period.
One of the most extensive of the latter group is the one at Heathwaite Fell, where on the top of an elevated piece of moorland is a site near half a mile long by 700 yards wide, which has been encompassed by a stone wall originally 2 feet thick. This enclosed space has been subdivided into five or more smaller enclosures by cross walls, and each of these divisions had its own water–supply. The apex of the ground has been cut by a wall, and this encloses the north elevation of the site. About midway along the west side another wall leaves the outer one and crosses the summit, and cuts off the west angle. On the centre of this wall are situated the “homesteads” or headquarters of the settlement. The homesteads are situated upon the south–east slope of the hill, and upon the cross wall dividing off the western ward. They consist of seven walled courts or yards, three smaller chambers, and two very small mural huts and chambers. The walls of these are usually of dry–built masonry, and are in some places 3 feet thick and in others from 6 to 7 feet.
The main entrance to these enclosures is on the south. The mural huts are placed at the north–west angle of the west court and the south–west angle of the south court. The first is the most interesting; it is contained in a small rectangular block of masonry filling up the angle, and the plan of the chamber itself is that of a joiner’s square. There is no trace left of any covering to these huts, but they were probably covered with stone flags or branches of trees. Within and without the enclosures are cairns of all sizes, one of which is known as The Giant’s Grave. It is remarkable that all the settlements in the Furness district are found on the fells, and never in the dales, some of them being 300 feet above the sea–level. Of any actual defensive structure there is no trace. The settlers here evidently buried their dead close to their homes, and from the calcined bones found it is clear that the bodies were burnt.
These earthen burial–mounds are, however, very scarce in the district; rude–stone cists have been unearthed, but no trace of metals or ornamental workmanship except a few pieces of rude pottery.
At Holme Bank, Urswick, the rampart of earthed stones encloses a five–sided figure, within which are traces of cross walls, the general plan of
“Recent Results of the Investigation into Local [Rochdale] Erratic Blocks,” by S. S. Platt.
H. Colley March, F.S.A., “The Early Neolithic Floor of East Lancashire,” p. 7.
Engraved, with other flints, in “History of Rochdale,” p. 4.
A complete list, up to date, will be found in Rev. William Harrison’s “Archæological Survey of Lancashire,” which will appear in the next volume of the Lancashire and Cheshire Antiquarian Society.