can accomplish, are too well marked in the histories of other countries for us to hesitate in ascribing to them the power of overthrowing, under similar turbulent conditions, even so substantial an obstruction as the forest must have been; but a careful study of the locality and of the several sudden incursions of the tide which have occurred during recent years, leads to the belief that the sea was the chief destructive agent, and that the gale which hurled the raging volumes of water over the low-lying lands at the south of Blackpool, and the then level wooded tract beyond, assisted only in the ruinous work. In support of such a hypothesis may be instanced the flood of 1833, when a tide, only estimated to rise to a height of sixteen feet, but greatly swollen by a furious storm from the south-west, burst over at that spot, swept away several dwelling-houses in its course, battered down the hedges, and laid waste the fields far into the surrounding country. Had this inundation occurred during the high spring tides, it is impossible to say to what extent its ravages might have been carried, but the incident as it stands, being within the recollection of many still living, and by no means a solitary example of the usual direction taken by the storm-driven waves, furnishes an apt illustration of the most natural way in which the downfall of the forest may have been accomplished. The Rev. W. Thornber, who has bestowed much time and labour on the subject, says:—“There are some facts that will go far to prove that these forests, once standing on Marton Moss, were overthrown by an inundation of the sea, viz., every tree on the Moss, as well as the Hawes, lies in a south-eastern direction from the shore; and the bank, which appears to have been the extent of this irruption, commencing at the Royal Hotel, runs exactly in the same direction. The shells, similar to those collected on the shore, intermixed with wrack of the sea, which are found in abundance under the peat, also corroborate this supposition. Moreover the tide is constantly depositing a marine silt similar to that which lies beneath the peat, and in some instances upon it.”