Observations 3 Part 2

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178

OBSERVATIONS.

OBSERVATIONS. " The Are The The

charms that m i n d delights to trace those that glow in N a t u r e ' s face : only beauties that withstand touch of time's destroving h a n d . " J. W . Douglas (Ent. Mag. 1838, 257V

GEOLOGY.—At a Meeting of the Geological Society on 20 May Mr. J. Selwyn T u r n e r exhibited specimens from temporary exposures around Chelmsford, of Boulder-clay underlying the Glacial-sands and -gravels of the Chelmer Valley (as well as the majority of central Suffolk). Brown Boulder-clay was thus found two-and-a-half miles east of Chelmsford beneath the gravels west of the Sandon Brook, and Chalky Boulder-clay about a mile north of Chelmsford near Broomfield Lodge. Other occurrences had been mapped on the western and southern sides of Danbury Hill and at Widford. T h e deposition of this early Boulder-clay over an area of considerable topographical relief must have produced appreciable modifications of the pre-glacial drainage, and the well-bedded character of much of the succeeding sands and gravels, for which a marine origin had been claimed, was readily explained by accumulation in temporary lakes before the deposition of the main Chalky Boulder-clay of Essex and Suffolk. BAWDSEY NODULE BED.—Frost and rain of the late winter erosed our sea-cliff between East Lane and the post-office in Bawdsey to an unusual extent; Fir-trees and even one or two small concrete forts, relics of the German war, had fallen from its brow to the beach in mid-March. Enormous masses of Rederag and the glacial talus above it had come hurtling down, revealing not only entirely new faces of the former but broad sections o f t h e Nodule-bed of Corpolites at its base, immediately above the Lower Eocene London-clay that is here sometimes ironed into a brilliant crimson colour. Rarely have broader exposures of the Nodule bed been revealed and these were found to average just two feet in depth. This always interesting and prolinc deposit, seen in the annexed photograph by M r . Rumbelow at Ramsholt, was found at Bawdsey to be füll of Mesoplodon-bones (first discovered in this bed by our Society at Trans, iii, p. xxx) with a few palatal teeth of the Ray-fish Myliobatis tumidens, W d w . (loc. cit., p. 131) though none of sharks were noted. In it were very numeruos Mollusca, the species of which were peculiarly few ; in a b n g t h of some twenty yards, no more appeared then Turritella incrassata, Sow., Mytilus edulis, L., Cardium Parkinsoni, Sow., and edulis, L., Pectunculus glycimeris, L.,


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