| dc.description.abstract | Lake Naivasha, (0. 45ºS, 36. 26ºE) lies in the Kenyan rift approximately 80km NW of Nairobi. It
lies at 1,890m (a.s.l) and an average depth of 6m with the deepest part being the crescent island
crater at a maximum depth of 30m. There are two smaller lakes within the vicinity of Lake
Naivasha; Oloiden and Sonachi. The lake is a fresh water lake situated within that part of Eastern
Africa that is influenced by the monsoonal systems of Asia and Indian Ocean with Rainfall
averaging from 450-900mmy-1. The lake is underlain by flood basalts (Miocene), phonolites
(Pleistocene), trachytes (Quaternary), volcaniclastics, Quaternary deposits , and their weathering
products (Olago et al., 2009).
Lake Naivasha and aquifer surrounding the lake are important water resources in the area and
they are used extensively for agriculture mainly in the booming flower industry and domestic
water supplies. However in the last 100 years, there have been large variations in the lake level
with the past four decades indicating a steady decline of the lake waters. This has been attributed
in part to climate variations as well as the vast human activities taking place at the shores of the
lake. Studies in the lake of the past millennium (Verschuren et al., 2000; Olago et al., 2009;
Olaka et al., 2010) have showed climatic induced fluctuations in the lake level associating the
fluctuations with periods of lowstands (Medival Warm Period ~AD 900-1300) and periods
highstands (Little Ice Age ~1300-1900). More studies on the anthropogenic impacts in the lake
(Odada et al., 2005) have showed a steady decline in the lake waters. Therefore the research
reveals that collective impacts of both climate change and human activities have exerted
profound effects to the declining waters of Lake Naivasha. | en |
