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Site description
Bishoftu is one of a number of crater lakes near Debre Zeit in East Shewa Zone, 50 km west of the zonal capital, Nazaret. Like all of the volcanic crater lakes in this area, Bishoftu is a closed system, surrounded by very steep and rocky hills and cliffs. The lake is fed directly by rain and by water flowing down from the crater rims. The maximum and minimum depths are 87 m and 55 m respectively. The water is alkaline, with the erosion of basaltic and hyper-alkaline rocks surrounding the lake playing an important role in increasing the alkalinity of the water. The lake does not have enough of a shoreline to attract wading birds. Cliffs and scattered trees that grow on these cliffs make up the major habitats surrounding the lake. The phytoplankton is dominated by blue-green algae, particularly Microcystis aeruginosa and Oscillatoria spp., and there are some fish, although not much fishing is done. Drier slopes around the lake support various Acacia spp.

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