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The geomorphology of Southeast Kenya
Titre : The geomorphology of Southeast Kenya
Auteur : Oosterom, A.P.
Université de soutenance : Wageningen Universiteit
Grade : PhD thesis 1988
Résumé
A geomorphological map of an area of 66 500 km 2 in the southeastern part of Kenya has been prepared. In the littoral zone eight major terrace levels occurring between the present shore and approximately 160 m +MSL have been described. Analysis of radiometric datings and uplift rates of the coastal succession suggested that the formation of the terraces extends over the last 1.4 my of the Pleistocene. Soil development indicate a climatic change from humid to savannah conditions at approximately 800 ky BP. Three sedimentary levels occurring in the landward part of the coastal region have been linked with the three highest littoral terraces. In the interior region, the denudation of the vast plains east of the 38° 15’ meridian was correlated with the deposition of Plio-Pleistocene deposits in the Lamu embayment and the coast.
Mots clés : geomorphology / horizons / kenya / land evaluation / soil suitability / soil surveys
Page publiée le 19 mars 2009, mise à jour le 30 mai 2022