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MYXOMATOSIS IN EAST SUFFOLK
No major outbreaks have been reported this year, but one diseased rabbit was pickedup in the HerringswellareainMay, 1955. No evidence has been found of foxes doing more damage than usual but the public, in particular poultry keepers, appear to be far more fox conscious than before the spread of myxomatosis. N . W. NEWELL, August, 1955.
THE SUFFOLK CRAG By
D.
F.
W.
BADEN-POWELL,
M.A., B.Sc.,
F.G.S.
As all Suffolk geologists know, the Crag is a much-investigated deposit. The history of research on the subject has been somewhat uneven, as spurts of activity and new discovery have alternated with periods of quiescence. In recent decades there has been an acceleration in our work on these beds, and the purpose of this article is to summarise what has been found out in the last 30 years or so, and to indicate what might be done in the future. Before the nineteenth Century, many writers alluded to the Crag mainly in connection with its importance in agriculture, and it was not until the 1830's that geologists began to pay detailed attention to this formation. About this time Lyell published his famous recognition of the great antiquity of the Crag, based on the presence of extinct shells, and Charlesworth (1835) realised that " the Crag " is not all of one age, and gave the names Coralline Crag, Red Crag and Norwich Crag to the three main divisions ; these designations have been used ever since his time. This period of initial activity was followed by less eventful work which included attempts by Prestwich to identify detailed layers over wide areas. By 1866, Searles Wood had shown that Prestwich's sub-zones could not be followed in the way he suggested, and established three divisions of the Red Crag which could be recognised by their shells ; these are now known to us as the Walton, Newbourne and Butley Crags. The various Monographs of the Palaeontographical Society by Wood, Harmer and others are a record of the diligent collecting of fossils which was carried out between the 1870's and the 1920's ; as early as 1872 (in the " Supplement to the Crag Mollusca ") the main faunal lists had been recorded. No attempt will be made here to give references to the numerous papers on the Crag, a mere list of these would occupy more space than the whole of this article : however, in the following paragraphs a few references will be given to papers which deal with recent research, so that geologists may have some idea of contemporary work.