The geological survey of Semliki, Kaiso Tonya and Pakwach areas in the Lake Albert Rift Basin
This lecture delves into the geological history of the Albertine Graben, the northernmost basin of the western branch of the East African Rift System (EARS) in Uganda. Spanning over 500km from the Sudan border to the Rwanda border, the graben comprises several sub-basins with depocenters, including the Rhino Camp, Pakwach, Lake Albert, Semliki, and Lake Edward-George basins. These sub-basins have been shaped by active rift processes, featuring fault-bounded basins and uplifted horsts resulting from tectonic activity along the EARS.
A focal point of this lecture is the crucial role of fluvial depositional environments within the Albertine Graben. The presence of river channels, floodplains, and deltaic systems has contributed significantly to the accumulation of thick sedimentary sequences, composed of diverse lithologies such as sandstones, siltstones, and mudstones. These sedimentary records mirror the dynamic nature of the past fluvial systems that once dominated the region.
Particularly, the lecture will present key findings related to the depositional settings within the Semliki, Kaiso Tonya, and Pakwach areas in the Lake Albert Rift basin. By exploring these specific areas, experts aim to shed light on the complex stratigraphy of the Albertine Graben, an ongoing and inconclusive discussion among geological researchers. Attendees will gain valuable insights into the geological processes that have shaped this unique and significant region of East Africa.
Access Passcode: Uq20@46
.