things at present found. Still, in one way, it is most interesting, as completely disproving the Chroniclers' accounts that, before its afforestation by the Conqueror, the district of the Forest was so fertile. The fact is a sheer impossibility. No wheat could ever be grown on this great bed of chalk-gravel, which is varied only by patches of sand.
But nowhere, perhaps, in the world can we see the stratification of the upper portion of the Middle-Eocene better than at Hordle and Barton, as the sea serves to keep the different strata exposed. The beds dip easterly with a fall of about one in a hundred, though, at the extreme west, at High Cliff, it is much less, and here and there in some few places they lie almost horizontally.[1] At Hordle they seem to have been deposited in a river of a very uniform depth. There is but one single fault in the whole series, just under Mead End, where all the beds have alike suffered. Here and there, however, they are deposited with an undulating line; and here and there, too, a rippled surface occurs, caused by the action of small waves. The river appears to have varied very much in the amount and force of its stream, as some of the beds, where the shells are less frequent, have been deposited very rapidly, whilst others, where the organic remains are more abundant, have been laid on very slowly and in very still water.[2]
It will be impossible to examine all the beds. One or two, however, may be mentioned. And since the beds rise at the east we will begin from Milford. First of all, at Mineway, there
- ↑ In the coast-map at p. 148, the principal beds are marked, so that, I trust, there will be no difficulty in finding them.
- ↑ For the direction of the river from east to west, see a paper "On the Discovery of an Alligator and several New Mammalia in Hordwell Cliff," by Searles Wood, F.G.S.: London Geological Journal, No. 1., pp. 6, 7.
