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Published online by Cambridge University Press: 01 May 2009
In the Summer of 1902 I commenced an exploration of the chalk-pits on the eastern border of the Lincolnshire Wolds, starting at Louth and working northward. Mr. W. Hill had previously visited this locality, and had proved the existence of the zone of Holaster planus at Boswell, three miles north-west of Louth, and also at Kirmington, much farther north. Mr. Jukes - Browne suggested to me that I should try and obtain fossils from the intermediate pits, and thus extend the work commenced by Mr. Hill. As the result of visits to about thirty pits, ranging from near Louth to Barrow-on-Humber, I have obtained further evidence of the zone of Holnster planus, and also some indications of the zone of Mieraster enrtestudinarium.
page 172 note 1 “The Red Rocks of the South Devon Coast,” by Alexander Soniervail (Transactions of Devonshire Association for the Advancement of Science, etc., vol. xxxv, pp. 617–630).
page 172 note 2 Hill, W., “ Note on the Upper Chalk of Lincolnshire ”: Geol. Mag., Dec. IV, Vol. IX (1602), p. 404.Google Scholar
page 173 note 1 “ Geology of part of East Lincolnshire,” p. 69.