a few fossils sparingly distributed, five to six feet; (3) Turritella carinifera bed, one foot and a half; (4) fossil bed, characterized by Conus deperditus, and the abundance of Pecten corneus within a few inches of the bottom, one foot and a half.
It is worth noticing that these, like all the Bracklesham beds, roll. In a pit which Mr. Keeping and myself dug we found there had been a regular displacement of the gravel, and that the beds rose at an angle of thirty degrees, whilst the fossil bed was three feet lower on one side than the other of the pit. In another, after cutting through a foot of gravel, in which we found the os inominatum, of probably Bos longifrons,[1] and a bed of sandy clay about two feet in thickness, we came upon a deposit of gravel about four inches thick, lying in the depressions of the stiff brown clay which succeeded, and in which still remained roots and vegetable matter. Thus we can plainly see that, after the clay had been deposited, vegetable, and perhaps animal, life flourished. Then came the gravel, carrying all before it, and in its turn, too, was nearly swept away, and only left here and there in a few scattered patches.
Perhaps, nothing is so startling as this insecurity of life. As was the Past so will be the Future, guided, though, always by that Law, which at every step still rises, moving in no circle, but out of ruin bringing order, and from Death, Life.
The Brook Beds I can best describe for the general reader by an account of a pit which Mr. Keeping and myself made. It was sunk about 20 feet from the King's Gairn Brook, and measured about 6 yards long by 4 broad. We first cut through
- ↑ I say probably, for Professor Owen, who examined the specimen, states that it is of a bovine animal of the size of Bos longifrons, but does not yield characters for an exact specific identification. I may here add that the celt mentioned at p. 207, foot-note, is hardly satisfactory.
