Skip to main content
×
×
Home

III.—Secular Straining of the Earth in Relation to the deep Phenomena of Volcanic Action

  • T. Mellard Reade
Extract

The application by Dr. Johnston-Lavis of the theory of the secular straining of the Earth, with which my name and Mr. Davison's is connected, to an explanation of the deeper phenomena of volcanic action, is ingenious and suggestive. It will, therefore, I trust, be of some use if I am allowed to discuss and criticize the principles and propositions that appear to me to be necessarily involved in the views put forth by Dr. Johnston-Lavis. Before doing this, I feel it incumbent upon me to point out that Mr. O. Fisher's position with regard to the question seems to have been misunderstood. So far from occupying an antagonistic position, he has done much to mathematically develop the theory; and it is only when we come to its practical application to the explanation of geological phenomena, that he, myself and Mr. Davison differ.

Copyright
References
Hide All

page 344 note 5 Geol. Mag. June, 1890.

page 345 note 1 Origin of Mountain Ranges, chap. xi.

page 345 note 2 Physics of the Earth's Crust, second edition, p. 106.

page 345 note 3 Origin of Mountain Ranges, p. 125.

page 346 note 1 See note by me appended to the paper by the Rev. F. Grensted entitled “Theory of the Airless and Waterless Condition of the Moon,” Proceedings of the Liverpool Geol. Soc. Session 1887–8.

Recommend this journal

Email your librarian or administrator to recommend adding this journal to your organisation's collection.

Geological Magazine
  • ISSN: 0016-7568
  • EISSN: 1469-5081
  • URL: /core/journals/geological-magazine
Please enter your name
Please enter a valid email address
Who would you like to send this to? *
×

Metrics

Full text views

Total number of HTML views: 0
Total number of PDF views: 2 *
Loading metrics...

Abstract views

Total abstract views: 31 *
Loading metrics...

* Views captured on Cambridge Core between September 2016 - 12th June 2018. This data will be updated every 24 hours.