95 / 220
81
phyllite, mudstone and shale rock systems. The Karagwe-Ankolean phyllites
cover a wide stretch (ridges, and represent the climax of the Kooki hills,
presumably due to being more resistant than shale and mudstone. The
climax is representative of Katabaluka and Katiarizo hills in Kibanda, which
rise to 1,542 m and 1,540 m above sea level, respectively. These bare hills
as seen in the image of 1984 are constantly burnt in the dry seasons.
Bare hills in Kagamba sub county, Rakai District