Tanganyika is the second deepest and largest Lake by volume in the world. Inflows are Ruzizi, Malagarasi and Kalambo Rivers, and the outflow is Lukuga River. While the main water influx is rain, and water loss is from evaporation.
Lake was created by tectonic movements. Because of the tectonic movements, the Lake demersal basin structure was changed many times in history. Therefore the inhabitants of the Lake were extinct or adapted quickly to new conditions.
Thanks to adaptive distribution capabilities of the aquatic creatures and massive species diversification;1500 species of fish, invertebrates and plants (600 of them endemic) are living in Lake. Tanganyika is a valuable source for searching unique species and as a microcosm in which to assess the processes of evolution that have led to this diversity.
BIN of Kipili shore is a shallow, and stony habitat contains Phragmites australis and a tree root which directly affected by the rising water level of Lake.(Bib.1-2,Sit.1-6,15,22)
- GPS
- -7.4444442, 30.5922222
- Geographical region
- Eastern Africa
- Drainage Basin
- River catchment
- Water body type
- Lake
- Water body name
- Lake Tanganyika
- Water body part
- Water body course
- Water body: tributary of
- Tributary name