Understanding the structure, permeability and activity of faults in and around the Rwenzori mountains, Albertine rift system, Uganda.

1Daniel Koehn, 2Kevin Aanyu, 1Allan Hollinsworth, 1Roderick Brown, 2Andreas Schuman

1School of Geographical and Earth Sciences, University of Glasgow, UK

2Department of Geology and Petroleum Studies   

Makerere University, Kampala, Uganda

The East African Rift System (EARS) has intrigued scientists for decades as it is the archetype of a continental rift and is believed to be the cradle of humankind. However, our current understanding of this geological feature is still clouded with mystery. In this project we focus on rift faults in the western branch of the EARS in and around the Rwenzori mountains, and aim at an understanding of why and how a basement block was uplifted during extension of the crust. The EARS represents one of the most variable environments on Earth being an area of active tectonics, dynamic topography with deep lakes, high mountains and active volcanoes. The variability of this changing landscape, its local climate and its richness in natural resources poses opportunities as well as challenges for local communities and consequently regional and global interests. We are working together with researchers from Makerere University, Uganda Wildlife Authority and local community guides to develop an understanding of the geology, faulting and rock uplift as well as science communication and local community development.

This research is funded by the NERC Oil and Gas CDT and supported by the Ugandan Council for Science and Technology (UNCST) and Uganda Wildlife Authority (UWA). We thank NERC, UNCST and UWA for their support.


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