Karst Landform Analysis as Evidence for Climatic Change in the Transvaal
- 1 January 1972
- journal article
- research article
- Published by Taylor & Francis in South African Geographical Journal
- Vol. 54 (1), 152-162
- https://doi.org/10.1080/03736245.1972.10559507
Abstract
Detailed studies in the northeastern Transvaal karst belt have indicated seven fluctuations from wet to dry during the Quaternary period. Precise dating of these events is as yet impossible but a tentative relative chronology is proposed which will in future be tested in other karst regions of South Africa.Keywords
This publication has 1 reference indexed in Scilit:
- Cave Levels and Erosion Surfaces in the Transvaal, South AfricaSouth African Geographical Journal, 1969