Character of the Rocks near Gardenstone--A Defunct Father-lasher--A Geological Inference--Village of Gardenstone--The drunken Scot--Gardenstone Inn--Lord Gardenstone--A Tempest threatened--The Author's Ghost Story--The Lady in Green--Her Appearance and Tricks--The Rescued Children--The murdered Peddler and his Pack--Where the Green Dress came from--Village of Macduff--Peculiar Appearance of the Beach at the Mouth of the Deveron--Dr. Emslie's Fossils--_Pterichthys quadratus_--Argillaceous Deposit of Blackpots--Pipe-laying in Scotland--Fossils of Blackpots Clay--Mr. Longmuir's Description of them--Blackpots Deposit a Re-formation of a Liasic Patch--Period of its Formation. I lingered on the hill-side considerably longer than I ought; and then, hurrying downwards to the beach, passed eastwards under a range of abrupt, mouldering precipices of red sandstone, to the village. From the lie of the strata, which, instead of inclining coastwise, dip towards the interior of the country, and present in the descent seawards the outcrop of lower and yet lower deposits of the formation, I found it would be in vain to look for the ichthyolite beds along the shore. They may possibly be found, however, though I lacked time to ascertain the fact, along the sides of a deep ravine, which occurs near an old ecclesiastical edifice of gray stone, perched, nest-like, half-way up the bank, on a green hummock that overlooks the sea. The rocks, laid bare by the tide, belong to the bed of coarse-grained red sandstone, varying from eighty to a hundred and fifty feet in thickness, which lies between the lower fish-bed and the great conglomerate, and which, in not a few of its strata, passes itself into a species of conglomerate, different only from that which it overlies, in being more finely comminuted. The continuity of this bed, like that of the deposit on which it rests, is very remarkable. I have found it occurring at many various points, over an area at least ten thousand square miles in extent, and bearing always the same well-marked character of a more thoroughly ground-down conglomerate than the great conglomerate on which it reposes. The underlying bed is composed of broken fragments of the rocks below, crushed, as if by some imperfect rudimentary process, like that which in a mill merely breaks the grain; whereas, in the bed above, a portion of the previously-crushed materials seems to have been subjected to some further attritive process, like that through which, in the mill, the broken grain is ground down into meal or flour.