On Some New Facts in Relation to the Section of the Cliff at Mundesley, Norfolk*

page 69 note * Phil. Mag. for May, 1840, p. 353.

page 70 note * It is probable that this bed of Freshwater clay, before the building cf the sea-wall might, without a clear erposure of the cliff, have had the appearance of being prolonged from b—being on the same level, and much like in mineral character. The bed of gravel (b4), which necessarily cuts off all communication with the beds beneath, clearly isolating and separating the upper Freshwater beds (b), from the lower one (h).

page 71 note * I am happy to say that the fossils, both of the Forest bed and of the Fresh-water beds (b), are now engaging the active attention of a very zealous observer, who will, no doubt, add materially to our present lists.

* Read before the Meeting of the British Association at Oxford, in June, 1860, and published by permission of the Author.