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Uganda Atlas of Our Changing Environment - GRID-Arendal

Uganda Atlas of Our Changing Environment - GRID-Arendal

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Aerial view <strong>of</strong> Kabale-Iyamuriro wetland<br />

Lake Bunyonyi<br />

The lake was formed due to a combination <strong>of</strong> intense<br />

rifting and back tilting <strong>of</strong> the landscape by earth<br />

movements that occurred in this area during the Tertiary<br />

times, in association with formation <strong>of</strong> the Western Rift<br />

valley in East Africa; and later the volcanic lava damming<br />

<strong>of</strong> rivers flowing on the raised and tilted landscape. As a<br />

result, Lake Bunyonyi occupies one <strong>of</strong> the deepest and<br />

long winding narrow valleys, characteristic <strong>of</strong> this Kigezi<br />

94<br />

region and a reminiscent <strong>of</strong> the intense Tertiary rifting<br />

in this part <strong>of</strong> the country. The entire lake is encircled<br />

by towering ridges and hills, with very steep slopes that<br />

abruptly drop to the very narrow lake shores. Water from<br />

rivers filled a drowned deep and moderately wide streak<br />

valley which was then dammed by lava to form one <strong>of</strong><br />

the deepest lakes in Africa. The lake covers an area <strong>of</strong> 46<br />

km 2 and has an average depth <strong>of</strong> 39m (Langlands 1974).<br />

Credit...................... NEMA 2007

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