Skip to main content
Log in

Some remarks on continental drift

  • Published:
Geofisica pura e applicata Aims and scope Submit manuscript


The continental drift may be explained by an expanding Earth only. In fact, there is a differences in the rate of heat flow between continents and oceans. Principially, there is a possibility of deriving the value of ancient radii by palaeomagnetic and age measurements.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Subscribe and save

Springer+ Basic
EUR 32.99 /Month
  • Get 10 units per month
  • Download Article/Chapter or Ebook
  • 1 Unit = 1 Article or 1 Chapter
  • Cancel anytime
Subscribe now

Buy Now

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others


  1. Jacobs J. A.: Nature, 185, p. 231 (1960).

    Google Scholar 

  2. Egyed L.: Acta Geol. Sc. Hung., IV, pp. 43–83 (1956).

    Google Scholar 

  3. Egyed L.: Geofisica pura e appl., 33, pp. 42–48 (1956).

    Google Scholar 

  4. Egyed L.: Geol. Rundschau, 46, pp. 101–121 (1957).

    Google Scholar 

  5. Egyed L. &Stegena L.: Zeitschrift für Geophysik, 24, pp. 260–267 (1958).

    Google Scholar 

  6. von Herzen R.: Nature, 183, pp. 882 (1953).

    Google Scholar 

  7. Heezen B.: Am. Geoph. Un. Trans., 38, p. 394 (1957).

    Google Scholar 

  8. Contini C.: Annali di Geofisica, IX, pp. 561–575 (1956).

    Google Scholar 

Download references

Author information

Authors and Affiliations


Rights and permissions

Reprints and permissions

About this article

Cite this article

Egyed, L. Some remarks on continental drift. Geofisica Pura e Applicata 45, 115–116 (1960).

Download citation

  • Received:

  • Issue Date:

  • DOI: