disappeared--made use of, no doubt, by after-comers for building purposes; as exemplified on Blackstone Edge itself, where the materials of which the wall near the road has been constructed point only too plainly to their source. Complete remains continuous for any considerable distance are found only upon elevated and unfrequented moorlands; where also the substance of the road appears to have been more rigid. The Blackstone Edge road, one of this kind, ascends the hill at a point about two miles beyond Littleborough--an ancient Roman station, here consisting of a strip of pavement exactly sixteen feet wide. It is composed of square blocks of millstone-grit, obtained upon the spot, laid with consummate care, and presenting, wherever the dense growth of whortleberry and other coarse herbage has been cleared away, a surface so fresh and even, that for seventeen centuries to have elapsed since its construction seems incredible. The unique feature of the road consists in the middle being formed of blocks considerably larger than those used at the sides, harder, and altogether of better quality, laid end to end, and having a continuous longitudinal groove, obviously the work of the chisel. This groove, or "trough," evidently extended down the entire roadway where steep, beginning at the top of the hill. Nothing like it, as said above, is found anywhere else in England, for the simple reason, it would appear, that no other British Roman road descends by so steep an incline. For it can hardly be doubted that Dr. March is correct in his conjecture, that it was intended to steady the passage of wagons or other vehicles when heavily laden; brakes adjusted to the wheels retarding their progress as indicated by marks still distinguishable. In some parts there are indications also of lateral trenches cut for the downflow of water, the road itself being kept dry by a slight convexity of surface. Over the crest of the hill the descent is easy, and here the paving seems to have been discontinued. The Robin Hood rocks close by present remarkably fine examples of typical millstone-grit. Rising to the height of fifty feet and fantastically "weathered," on the summits there are basin-like cavities, popularly attributed, like so many other things they had no hand in, to the Druids; but palpably referable to a far less mythical agency--the quiet action, during thousands of years, of the rain and the atmosphere. VIII THE SEASHORE AND THE LAKE DISTRICT