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Structurally, the geology of Uganda is strongly influenced by fold belts and shear zones, as well as the East Africa Rift related crustal downwarping in the Pleistocene that formed Lake Victoria. The Aswa Shear Zone is one example of several Neoproterozoic shear zones in Precambrian rocks, running for 300 kilometers on a northwestern trend.
Name Elevation Location Last eruption meters feet Coordinates; Bufumbira: 2440: 8005: Holocene Bunyaruguru Field: 1554: 5098: Holocene Mount Elgon: 4321: 14,178: Fort Portal Field
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The history of Uganda comprises the history of the people who inhabited the territory of present-day Uganda before the establishment of the Republic of Uganda, and the history of that country once it was established.
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The hill is located in Buyende county, Buyende District, in Uganda's Eastern Region. [2] This is about 42 kilometres (26 mi) north-east of Kamuli, the nearest town. [3] Kagulu hill. Kagulu is approximately 106 kilometres (66 mi) north of Jinja, the largest city in the Busoga sub-region. [4]
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Uganda has a warm tropical climate with temperatures falling in the 25 to 29 °C (77.0 to 84.2 °F) range on an average. The months from December to February are the hottest, but even during this season the evenings can be pleasant with temperatures in the 17 to 18 °C (62.6 to 64.4 °F) range.