however, is that of a bird perched on the high lighthouse and looking south-west over Hollesley Bay and the adjacent land to the Naze, and it gives a very vivid idea of the struggles of the sluggish Suffolk streams before they reach the sea. "The triangular projection encloses salt marshes, and extends from Aldeburgh to Landguard Point. Successive ridges or waves of shingle are, indeed, a marked characteristic of such headlands. Under ordinary circumstances, and when the shore line is stationary, each succeeding tide obliterates the ridge made by the last; but when the shore is encroaching on the sea, some great storm will throw up the shingle in the form of a ridge, after which another accumulation commences, and eventually forms another ridge. The development of this beach, however, has not been invariably progressive, breaches made by storms having sometimes given a temporary exit for the waters of the Ore and of the Butley River at the Upper Narrows, where the part of the channel to the south would be partially closed. The Ordnance map of 1831 shows separate knolls of shingle for a mile southwards from North Weir Point. The point no longer exists as there shown, the knolls having been united into a continuous bank, as marked on the Geological Survey map, which has been corrected from a later survey." One more short passage is quoted here, as tending to round off the subject under discussion, although, perhaps, it might have been quoted when we were at Yarmouth. Still, the shifting shore did not thrust itself upon our attention then, and now it is pushing itself forward as steadily as North Weir Point has made its progress on the maps. "The sands of Yarmouth, like those of Lowestoft, have, in recent years, been comparatively stationary. The town of Yarmouth stands on a spot of sea-driven sand, thrown up in 1008 A.D."--it is no use therefore to look for Roman remains at Yarmouth itself--"and which crosses the outfalls of the Waveney and the Yare, enclosing a large mere--Breydon Water--the outlet of which, like that of other Suffolk rivers, is being constantly forced southwards by the accumulating sand from the north." All this is due to the steady trend of the beach from the north to the south, tending to form a barrier across all harbours and estuaries, to denude outlying capes, to fill up hollows in the coastline; and less calculable than the influence of the tide is the spasmodic influence of storms. What, then, is the moral? Of a truth there are many morals. He who buys a promontory may become a landless man. His neighbour in a hollow of the coast to the south may find himself endowed with salt marshes, whereon the sheep of his posterity will attain a flavour of supreme excellence. A port may become an inland community. River beds, the boundary of many an inland county and of many an estate out of reach of the sea, because they are accepted as eternal and immutable, are the most