Repository logo
  • English
  • Català
  • Čeština
  • Deutsch
  • Español
  • Français
  • Gàidhlig
  • Italiano
  • Latviešu
  • Magyar
  • Nederlands
  • Polski
  • Português
  • Português do Brasil
  • Srpski (lat)
  • Suomi
  • Svenska
  • Türkçe
  • Tiếng Việt
  • Қазақ
  • বাংলা
  • हिंदी
  • Ελληνικά
  • Српски
  • Yкраї́нська
  • Log In
    New user? Click here to register. Have you forgotten your password?
Repository logo
  • Colleges, Institutes & Collections
  • Browse AAU-ETD
  • English
  • Català
  • Čeština
  • Deutsch
  • Español
  • Français
  • Gàidhlig
  • Italiano
  • Latviešu
  • Magyar
  • Nederlands
  • Polski
  • Português
  • Português do Brasil
  • Srpski (lat)
  • Suomi
  • Svenska
  • Türkçe
  • Tiếng Việt
  • Қазақ
  • বাংলা
  • हिंदी
  • Ελληνικά
  • Српски
  • Yкраї́нська
  • Log In
    New user? Click here to register. Have you forgotten your password?
  1. Home
  2. Browse by Author

Browsing by Author "Ayalew, Teklewold"

Now showing 1 - 1 of 1
Results Per Page
Sort Options
  • No Thumbnail Available
    Item
    Relation Ship Sbetween Geology, Mor Phology and Soil Associations of Bichena Area ( S. E. GOJAM )
    (Addis Ababa Universty, 1981-10) Ayalew, Teklewold
    The study investigates the extent of influence of the geolog- ical history , essentially parent rock * topography and time , on soil formation and distribution in Bichena , Southeastern Gojjam * Lithostratigraphy of the Mesozoic sedimentary sequence and Cenozoic volcanics is described * An attempt has been made to reconstruct the morphologic evolution of the area * Four soil mapping units in close relationship with the parent material and geomorphology have been differentiated: Vertisol, Mollisol, Alfisol and Entisol Orders 0 The soils are found to assume different states when the above considered soil forming factors are changed * The vertisol development from aphanitic basalts is determined by the evolution of the structural plateau geomorphic surface through lateral planation, which has allowed for two cycles of pedogenesis* The Mollisols have developed from porphyritic plagio- clase-Olivine basalt* These indicate that soil parent materials with similar mineralogy give way to soil varieties * A lateral variat- ion in some soil properties of the Mollisol order is found to be strongly explained in terms of the slope gradient * The study shows that the Plio-Pleistocene neotectonic uplift and subsequent develop- ment of a deep canyon including morphogenetic threshold slopes has resulted in lack of sufficient time for pedogenic horizons to develop in Alfisols and Entisols *

Home |Privacy policy |End User Agreement |Send Feedback |Library Website

Addis Ababa University © 2023