Hostname: page-component-cd9895bd7-jkksz Total loading time: 0 Render date: 2024-12-23T15:10:25.150Z Has data issue: false hasContentIssue false
  • English
  • Français

Carbonatite Structure: Tororo Hills, Eastern Uganda

Published online by Cambridge University Press:  01 May 2009

C. E. Williams
C. E. Williams
Affiliation:
Geological Survey of Uganda, P.O. Box 9, Entebbe, Uganda.
Get access Rights & Permissions [Opens in a new window]

Abstract

The carbonatite plugs of Eastern Uganda represent the final phase of Elgon type volcanoes. The types of structure observed in the carbonatites are discussed and a general description of the structural components of the Tororo Hills is given. It is suggested that the ring features originated through the congealing in the conduit of the central portion of the carbonate mass.

Type
Articles
Information
Geological Magazine , Volume 89 , Issue 4 , August 1952 , pp. 286 - 292
Copyright
Copyright © Cambridge University Press 1952

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

REFERENCES

Davies, K. A., 1951. Geol. Surv. Uganda, Mem. vii. In the press.Google Scholar
Eckermann, H. Von, 1948. The Alkaline District of Alnö Island. Sveriges Geol. Undersok., Series Ca., no. 36.Google Scholar
King, B. C., 1948. The Napak Area of Southern Karamoja, Uganda. Geol. Surv. Uganda, Mem. V.Google Scholar
Strauss, C. A., and Truter, F. C., 1950. The Alkali Complex at Spitskop, Sekukuniland, Eastern Transvaal. Trans. Geol. Soc. S. Africa, liii, 81–125.Google Scholar