Lake Magadi, Rift valley, Kenya

Lake Magadi, lake, in the Great Rift Valley, southern Kenya. Lake Magadi is 32 km long and 3 km wide and is located about 240 km east of Lake Victoria. It’s north of Tanzania’s Lake Natron. During the dry season, it is 80% covered by soda and is well known for its wading birds, including flamingos.

It occupies the lowest level of a vast depression, and its bed consists almost entirely of solid or semisolid soda. It was explored by Captain E.G. Smith in 1904, who found the outline irregular and traversed by great ridges.

Several streams, both cold and hot, the latter heavily impregnated with soda, flow into the lake, while all about springs of soda water gush up through the caked crust, dyeing the waters a vivid pink. A railway from Mombasa leads to the lake, from which salt and gypsum are extracted.

Lake Magadi was not always so saline. Several thousand years ago (during the late Pleistocene to mid-Holocene in the African humid period), the Magadi basin held a freshwater lake with many fish, whose remains are preserved in the High Magadi Beds, a series of lacustrine and volcaniclastic sediments preserved in various locations around the present shoreline. Evidence also exists for several older Pleistocene precursor lakes that were much larger than present Lake Magadi. At times, Lake Magadi and Lake Natron were united as a single larger lake.

Lake Magadi is also well known for its extensive deposits of siliceous chert. There are many varieties including bedded cherts that formed in the lake and intrusive dike-like bodies that penetrated through overlying sediments while the silica was soft. Most famous is “Magadi-type chert”, which formed from a sodium silicate mineral precursor magadiite that was discovered at Lake Magadi in 1967.

Magadiite, a rare hydrous sodium-silicate mineral [NaSi₇O₁₃(OH)₃·4(H₂O)], was discovered about 50 years ago in sediments around Lake Magadi, a hypersaline alkaline lake fed by hot springs in the semi-arid southern Kenya Rift Valley. Today this harsh lacustrine environment excludes most organisms except microbial extremophiles, a few invertebrates (mostly insects), highly adapted fish (Alcolapia sp.), and birds including flamingos. Burrows discovered in outcrops of the High Magadi Beds (~25–9 ka) that predate the modern saline (trona) pan show that beetles and other invertebrates inhabit this extreme environment when conditions become more favourable. Burrows (cm-scale) preserved in magadiite in the High Magadi Beds are filled with mud, silt and sand from overlying sediments. Their stratigraphic context reveals upward-shallowing cycles from mud to interlaminated mud-magadiite to magadiite in dm-scale units. The burrows were formed when the lake floor became fresher and oxygenated, after a period when magadiite precipitated in shallow saline waters. The burrows, probably produced by beetles, show that trace fossils can provide evidence for short-term (possibly years to decades) changes in the contemporary environment that might not otherwise be recognised or preserved physically or chemically in the sediment record.

Magadi township lies on the lake’s east shore, and is home to the Magadi Soda factory, owned by Tata India since December 2005. This factory produces soda ash, which has a range of industrial uses.

The lake is featured in Fernando Meirelles’s film The Constant Gardener, which is based on the book of the same name by John le Carré, and is used as a stand-in for Lake Turkana in the north of Kenya, where the book and film are set.

A causeway that crosses the lake provides access to the area west of the lake (Nguruman Escarpment). Recently accommodation for tourists is provided in air conditioned canvas tents