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VI.—The Descriptive Nomenclature of Ripple-Mark

Published online by Cambridge University Press:  01 May 2009

A. R. Hunt
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Extract

Over twenty years ago, in 1882, I ventured to controvert a doctrine which was at the time maintained with remarkable unanimity by all geologists, and which was taught in all the current textbooks. It was that the ordinary ripple-mark of the seashore was formed by continuous water-currents of some kind; the current of water taking the place and performing the office of the current of wind which ripples the surface of sand-dunes.

Type
Original Articles
Information
Geological Magazine , Volume 1 , Issue 8 , August 1904 , pp. 410 - 418
Copyright
Copyright © Cambridge University Press 1904

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References

page 410 note 1 This is the type-species of Bayle's Goniotenthis. Explication de la carte géologique de la France, publiée par ordre de M. le Ministre des travaux publics, Tome quatrième, Atlas, Première partie—Fossiles principaux des terrains, E. Bayle, 1878, pl. xxiii, figs. 6–8.

page 410 note 2 Proc. Geol. Assoc., vol. xviii, pt. 4 (1904), p. 271, fig. 12.

page 415 note 1 Proc. Roy. Soc., 1883, p. 2.