XVIII. Radioactivity and Earth Movements

@article{Holmes1931XVIIIRA,
  title={XVIII. Radioactivity and Earth Movements},
  author={Arthur Holmes},
  journal={Transactions of the Glasgow Geological Society},
  year={1931},
  volume={18},
  pages={559 - 606}
}
  • A. Holmes
  • Published 1931
  • Geology
  • Transactions of the Glasgow Geological Society
I.—TECTONIC HYPOTHESES. Both external and internal geological processes are controlled by gravity and the earth's bodily movements. The circulations of matter which constitute the external processes are maintained by energy derived from the sun, whereas the internal processes derive much of their energy from the earth's internal heat, the latter being partly an inheritance, and partly an income supplied by atomic disintegration. Hypotheses relating to the physical causes of earth movements must… 

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References

SHOWING 1-10 OF 109 REFERENCES
The Surface-History of the Earth
A BOOK which has for its chief object the exposition of a group of geological hypotheses of a highly speculative character is likely soon to become out-of-date as geophysical evidence accumulates and
Some Problems of Physical Geology and the Earth's Thermal History
In a recent paper I stated that the hypothesis of a continuously cooling earth had “consistently failed to lead to any adequate explanations of fissure eruptions and other volcanic and tension
The Origin of Continents and Oceans
THE wide appeal of Prof. Wegener's theory of the arrangement of ocean and continent is shown by, the issue of a third greatly revised edition and of this excellent English translation. His theory is
Radioactivity and the Floor of the Oceans
Recently a mechanism allowing the escape of the heat generated by radioactivity in the basaltic under-crust of the earth has been proposed by Dr. Holmes, and a very similar one by Dr. Joly has gained
Contributions to the Theory of Magmatic Cycles
It is quite clear that Professor Joly's presentation of his theory of basaltic cycles is, taken alone, far too simple to match the complex details of geological history. In a former paper I attempted
Our Mobile Earth
PROF. DALY of Harvard once again has presented in book form matter of geological interest gathered from all parts of the world, and has supplied the desirable connective tissue of theory and
Radioactivity and the Heat of the Earth
IN his presidential address to the Geological Society, abridged in NATURE of Jan. 1, Dr. J. W. Evans refers (page 15) to the above topic in the following words: “although the whole of the energy
Physics of the Earth's Crust
MR. FISHER is well known to geologists as the writer of various important papers on Mountain Chains, Terrestrial Heat, and other physical phenomena of the earth. He has in this volume not merely
On the distribution of radium in the Earth's crust and on the Earth’s internal heat
Professor Rutherford has given a calculation which suggests that there may be enough radium in the earth to account for the temperature gradient observed near the surface. The question is of great
Past Climates
THERE are only three factors which can affect the climatic zones of the world: (a) the amount of solar radiation; (b) the horizontal transfer of heat from one part of the earth to another; and (c)
...
1
2
3
4
5
...