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IV.—Chloritic Mahl and Warminster Greensand

Published online by Cambridge University Press:  01 May 2009

Extract

In the year 1878 there was a short controversy between us respecting these beds in the pages of this Magazine. Since that date we have both enlarged our knowledge of the beds at the junction of Chalk and Greensand, and recently we have had an opportunity of meeting at Seaton in Devon, and of examining the Whitecliff and Beer Head sections together. The result of this and of friendly discussion is that we have both modified our views and have come to an agreement on the most important points about which we differedin1878. Under these circumstances we think it will save trouble and facilitate future enquiry if we jointly express our present views on the subject so far as we are in agreement.

1. Chloritic Marl.—As far as we can ascertain, this name was first applied to certain beds at the junction of the Chalk and Greensand in the Isle of Wight It was subsequently adopted by Prof. E. Forbes, for a bed which occupied a similar position in Dorset, and has since been used for any bed lying at the base of the Chalk Marl and containing fossils and green grains.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1894

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References

page 494 note 1 Ibbetson, , “Notes on the Strata of the Isle of Wight.” London, 1849. 8vo.Google Scholar

page 494 note 2 It has been recorded from the Chloritic Marl, but we believe that this is a mistake; at any rate, the find has never been confirmed.

page 495 note 1 Quart. Journ. Geol. Soc. vol. xxx. p. 369.Google Scholar

page 495 note 2 GEOL. MAO. Dec. II. Vol. V. pp. 547551, 12, 1878.Google Scholar