Hostname: page-component-848d4c4894-wzw2p Total loading time: 0 Render date: 2024-06-01T18:57:58.084Z Has data issue: false hasContentIssue false

V.—Physiography of the Lower Trias

Published online by Cambridge University Press:  01 May 2009

Extract

Free discussion is a valuable aid to research when entered upon in a proper spirit. I am glad to see the contribution of Mr. Jukes-Browne to this subject, together with the letter from Prof. Bonney, in the May Number of the Geological Magazine.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1890

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

page 261 note 1 Geol. Mag. April, 1890.Google Scholar

page 262 note 1 Mr. Hunt asks, “Would Mr. Mellard Reade give his reasons for believing that waves ever cause surface particles in deep water to move in a vertical circle, or an ellipse, not very different from one having the longer axis vertical P” If Mr. Hunt will watch a cork floating in water on which wind waves are generated, he will, I think, see that the vertical oscillatory movement of the cork is as great as or greater than the horizontal. The composition of the two movements will give either a circle or an ellipse. This is no discovery of Mr. Eeade's, but a fact known to every physicist.

page 262 note 1 Kinahan's Manual of the Geology of Ireland, p. 138.

page 262 note 2 Ibid. p. 141.