Notwithstanding what has been written upon the so–called “glacial nightmare,” it still remains an undisputed fact that at some far–distant period the whole of Lancashire was sunk beneath a sea, the waters of which carried along with them huge masses of ice, which, in their passage southward, deposited boulders which they had borne in their chill embrace for hundreds of miles. The hills which rose above the sea were covered with perpetual snow, and the valleys between them were filled with glaciers, which in many instances left a terminal moraine.

The 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 which points to the site of an early settlement. The rampart or entrenchment discovered at Hawkeshead Park is of a similar character. At Scrow Moss, near the foot of Coniston Old Man, is another of these enclosures, a drawing of which is given in ArchÆologia (vol. liii., part 2). At Dunnerdale Fell is an enclosure very similar to that found at Heathwaite, though much smaller, the central homestead being formed by a single wall, near to which are several cairns and remains of walls. On Birkrigg Common, at a place called Appleby Slack, is another of these small enclosures, consisting of a single rampart or vallum of earth, enclosing a pear–shaped area, not far from which is a tumulus, and about half a mile to the south–east is a double concentric stone circle. Concerning these various remains in the Furness district, the writer of the exhaustive article in ArchÆologia5 just referred to is of opinion that their elevated position is due to the fact that the lower ground was at that period such a dense mass of scrub and jungle that it was utterly untenable for residential purposes. These various enclosures do not appear to have been forts, as the homesteads themselves were all on the sloping sides of the hills, but were rather the dwelling–places of a very early tribe of settlers, who were living at peace with their neighbours, and had, therefore, no need of a system of defence, such as we find traces of in other parts of the county. The plan of these settlements was simple—the smaller courts were the living apartments, and were no doubt covered with some kind of roof; the larger enclosures were for the cattle, or possibly for the lower orders of the tribes who held the place.

Many tumuli belonging to the early British settlers have been opened, as at Briercliffe, near Burnley, where the covering of earth had been partly wasted away, leaving a rudely–marked circle of stone, near to which in 1885 was found a sun–baked hand–made urn of pre–Roman origin, containing the remains of an adult and a child. At Wavertree, near Liverpool, in 1867, a large tumulus, since called Urn Mound, was opened, and six urns containing partly–calcined human bones were discovered, all of which were early British. Near to these were found a flint arrow–point and several “scrapers.”6

Canoes assigned to this period have not infrequently been dug out of peat which once formed the bottom of lakes, such as Marton Mere, in Poulton–le–Fylde, and at the estuary of the Ribble, near Penwortham. A very remarkable bronze beaded torque of the late Celtic period was found by some workmen in 1832 at Mowroad, in the parish of Rochdale. This ornament had probably been worn round the neck of some person of rank; it weighed one pound five ounces, was made of bronze, and was of superior workmanship and ornamentation.7 The British tribes did not congregate in such numbers as to establish anything like a town, or even a large village, in these Northern parts; but no doubt when the Romans took possession they found here and there clusters of hut dwellings, which the geographer Ptolemy afterwards described as British settlements. One of these was Regodunum, which was somewhere near the mouth of the Ribble, perhaps at Walton–le–Dale. The author just referred to (who lived about A.D. 140) mentions the estuaries on the west coast, three of which, from the latitude and longitude given, clearly refer to Lancashire rivers; they are named as the Estuary Moricambe, the Haven of the Setantii, and the Estuary Belisama. Belisama was the old name for the Mersey; the Haven of the Setantii was at or near the mouth of the Ribble; and the other estuary was at the conflux of the Kent with the waters of Morecambe Bay.8

At Walton–le–Dale and at Lancaster the Romans are believed to have founded their stations on the sites of British settlements, as in both these places have been found celts, arrow–heads, cinerary urns, and other signs of the earlier race.