88 CONTRIBUTIONS TO PLEISTOCENE GEOLOGY.
STRATIGRAPHY.
APPENDIX.—Corrections to Part I.
We desire to make the following corrections in Section VI.
of the first part of our paper (see Essex Naturalist, Vol. XI.,:
PP- 336—70) :—
(1.) At p. 365, line 37, read "London Bassin movements, as"
instead of "London Basin movements as." See also correction (3).
(2.) At p. 366, par. 3. The argument here as to terraces is
wrongly stated, and the whole case is put too high, but our
meaning will be properly appreciated if this is read in conjunc-
tion with this second part of our paper.
(3.) At p. 369. Final par. of Section VI. We now have
no doubt as to the connection of the anticlinal fold with the
main Wealden and London Basin movements. Our doubts
arose through a difficulty which we had in understanding the
Mardyke evidence. We may as well state here that not only
bad the folding taken place long before Pleistocene times, but
that the top of the anticline had been planed down by some 300
feet prior to High Terrace times.