It was once part of a larger freshwater lake, joined with the current Lake Baringo.[7]
As shown on the satellite picture at the top of this page, it is divided in three lobes: a large center one and two smaller ones at the north and south extremities. The two narrower areas separating these lobes are shallow, tectonically controlled sills at Nyalibuch and Mwanassis.[1]
There are contradictions regarding its altitude. Unesco's Ramsar gives 963m (3,159ft).[5] More precise — and more prudent —, Renaut & Owen 1991 give c. 990 m as of August 1977, but also indicate that the lake's level fluctuates seasonally by 50 to 100 cm; and that it can vary by several meters for short periods, having fluctuated between c. 988 and c. 996 m during the 20th century.[1] Lake-shore terraces around the shoreline, made of coarse angular gravel and angular orthoconglomerates, mark higher lake levels from the Pleistocene and Holocene.[8] They are visible on 45% of the present level, and some are about 9 m above the present shoreline.[9]
In 1991 the maximum length is 17.6km (10.9mi) and its width ranges from 0.5km (0.31mi) to 3.6km (2.2mi).[1]
In 1978 its maximum depth was recorded as 12m (39ft)[11] or 11.5m (38ft), and Renaut & Owen 1991 precise that this was in the largest sub-basin or lobe; and that the two smaller parts at the north and south extremities were 5.5m (18ft) deep at that time.[1] In 2003 its maximum depth is just over 10m (33ft) in an area of 3,000ha (7,400 acres). This is relatively shallow, but nevertheless deeper — and therefore hydrologically more stable — than the other endorheic lakes in Kenya.[12] The Rift Valley lakes undergo regular (and cyclic) changes in water levels mostly in response to precipitation, which is unreliable and unpredictable.[13] In this region, lake Bogoria is the only alkaline lake that has minimal lake water fluctuations,[5] and is used as a refuge for flamigos and other animals when other relatively shallow lakes dry out.[13]
Its surface is generally 3,300ha (8,200 acres) but this fluctuates, essentially according to the amount of rainfall.[5] Most of the rain falls between April and November, and precipitation ranges average about 700 mm on the Loboi plain and 1200 mm on the adjacent highlands. But El Nino years bring increased rainfall and flooding of the lake shores.[14] For example, in 2020 its area increased to about 4,690ha (11,600 acres):[5] 2020 was one of the hottest years on record, but despite depressed rainfall in the short-rains season (October to December, or OND) it also saw a wetter than normal January and February because of the strong positive Indian Ocean Dipole index during that period, and enhanced rainfall during the long-rains season (March to May, or MAM) (that year, Lake Victoria rose to a new record level).[15]
However, evaporation rate is above 2500 mm,[1][14] thus inducing a water deficit and creating semi-arid conditions over most of the lower parts of the Bogoria basin.[14]
Wetlands
Lake Bogoria
Although the lake is in a semi-arid part of Kenya Rift Valley, it is surrounded by numerous and varied wetlands along its shorelines, along faults where hot, warm and cold springs have developed, and along rivers that run across the rift floor.
Types of wetlands
Six major types of wetland have been defined around lake Bogoria:[16]
proximal hot springs, with small streamlets, exposed ground (carbonate and/or siliciclastics), high water temperatures over 40 ◦C that reach up to 99 ◦C at vents, and microbial mats of bacteria and less common diatoms;[14] These are associated with:
hot spring marshes, found downstream of the proximal hot springs and adjacent to spring streamlets, and dominated by thick clusters of short reeds, mainly Cyperus laevigatus,[14] that stand through a water layer 2 cm high or less and with temperatures ranging between 30–40 ◦C;[17]
artesian blister wetlands[lower-alpha 1] associated with cool springs (30–33 ◦C).[17] The circular blister mounds are about 15 m diameter and 1 to 2 m high.[17] They are formed by cool artesian springs that emerge at the surface,[18] creating a sort of water blister of about 1m3.Ashley et al. 2002 They are capped with an arched semi-permeable cover of short graminoids[18] (mostly less than 10 cm high) such as Cyperus laevigatus,[17]Pycreus mundtii and Leersia hexandra. The edges of these 'blister mounds' are dominated by Leersia hexandra mixed with other grasses and sedges. Further around are some Sporobolus spicatus,[18] and downslope of these mounds and of other water seeps are often found small patches of Typha and wet meadows plants.[17]
the graminoid vegetation is interspersed with cyanobacterial and algal mats. Water from the blister mounds, and other seeps and springs, support wet meadows and Typha swamps. The blister mounds and Typha swamps have a more or less neutral pH, low conductivities and total alkalinity.[18]
Typha and Cyperus papyrus swamps, fed by a mix of surface streams, groundwater seeps or warm springs (25°C to 30◦C). Where water is shallow and ephemeral, these are dominated by tall Typha domingensis (2 m tall or taller); where water is permanent — usually in broad depressions —, the dominant vegetation is floating Cyperus papyrus;[17]
floodplain marshes, with seasonal flooding and populated by short grasses;[17]
hypersaline lake littoral wetlands, found on the lake shores: they are flooded (by more than 10 cm of water), gently sloping, siliciclastic delta margins, often modified by flamingo nesting. Their pH is around 10, with an alkalinity ca. 1000 meq l−1. Hot springs may also feed into some of these sites. There are no macrophytes and few diatoms: cyanobacteria dominate (mainly Spirulina platensis);[17]
freshwater lake littoral wetlands, forming narrow to extensive fringes around the relatively fresh water Lake Baringo (pH ~8.9, alkalinity ca. 13 meq l−1), dominated by a variety of wetland vegetation.[17]
Wetlands areas
The marshes to the north of the lake do not feed any river outlet. They are linked to both Lake Bogoria and adjacent Lake Baringo; both lakes are fed by the Waseges river[5] (or Sandai river), the latter bringing a small permanent flow of the diverted Loboi river.[19] These wetlands are fed by ephemeral or perennial streams, and by springs.[14] In the south, two freshwater springs supply permanent streams. All three (the Wasenge river and the two streams) are used extrensively for drinking, as well as the water from some hot springs streams — some of these being substantially less salty than the lake water.[19] Other streams, such as the Emsos to the south and the Parkirichai to the west, are ephemeral: they flow only after heavy rains.[14]
The Loboi Swamp
This swamp is to the north of the lake. It hugs the base of a horst block (raised fault block bounded by normal faults) oriented north-south. According to radiocarbon datation, it was created only 700 years ago in a former floodplain environment — possibly as a consequence of faulting. In 1969, it spread over 6 km in length; but water was diverted from the Waseges river[20] and by 2001 it was only 3.5 km long and about 0.5 km wide. At least three warm springs, and groundwater inputs, feed it. The Loboi river also contributes to it but that river periodically shifts its bed (avulsions) and that modifies its relative role regarding the swamp. This river is cool and only slightly alkaline. The springs have a similar chemistry but they are warmer, have a higher nitrate content, and are slightly acidic.[17] The resulting waters of the Loboi Swamp are also slightly alkaline, and generally reflect the mixing of fluvial, spring and groundwater inflows.[18] Its areas of semi-permanent or seasonal standing water are dominated by Typha domingensis and also have some Leersia hexandra, Ipomoea aquatica, and other taxa. These areas surround a wetter area populated by near pure stands of Cyperus papyrus that are rooted or floating in water up to 1.5 m deep. Acacia scrub occurs on an adjacent horst block to the west, with grasses such as Sporobolus spicata on adjacent plains.[18]
The Kesubo floodplain marshes
These are also to the north of the lake, east of the Loboi swamp. They rest at the southern end of an extensive alluvial fan formed by the Sandai river. The Kesubo Floodplain Marshes are seasonally flooded and lie between the rift valley boundary faults, to the east, and a small horst block, to the west. The river waters are slightly alkaline, cool, and have a low total alkalinity. The marshes are similar in their general water chemistry, but are slightly acidic and have a distinctly lower NO3 content. Short grasses are the dominant vegetation type and cattle graze the area.[18]
The Campground Wetlands
These lie near the Lake Bogoria National Reserve entrance, to the south of the Loboi swamp, and at the limit dividing faulted volcanic uplands and colluvial-alluvial sediments. They contain several types of habitats.[18]Ashley et al. 2002 defined them as an 'Artesian Blister Wetland' (see Types of wetlands above),[21] and that wetland also includes slightly acidic, nitrate enriched, warm springs.
The Loburu Delta
This is on the western shore of Lake Bogoria. It is composed of silts and gravels, and shows a variety of fluvial, deltaic, and beach settings. It has active hot springs that feed a series of marshes dominated by Cyperus laevigatus. The springs are alkaline, of the Na-HCO3 type, contain a lot of silica and nitrate, and the temperature near the vents is extremely hot (more than 96◦C). The areas immediately adjacent to the vents and in nearby streamlets commonly include microbial mats of Phormidium, Pseudanabaena, Spirulina, Synechococcus and Calothrix, but are devoid of macrophytes. the Cyperus marshes, which have similar water chemistries, are dominated by short reeds less than 20 cm high. Temperatures range from about 32◦C to about 60◦C near the hot spring streamlets that cross the marshes. There are also algal and cyanobacterial mats. The lake shoreline at Loburu (and other shorelines) does not present many aquatic macrophytes. The lake brine is of Na-CO3-HCO3-Cl composition, with a pH range of 9.3–10.6. Some shallow marginal lagoons have salinities exceeding 100 g l−1. Temperature at the time of sampling ranged between 28 and 33 ◦C, but exceed 60 ◦C at sublacustrine hot spring vents. However, cyanobacteria — mainly Spirulina platensis — are abundant and support up to 2 million flamingoes.[18]
Geysers and hot springs
Lake Bogoria is in a geothermally active part of the Kenya Rift Valley,[22] and is famous for geysers and hot springs along the bank of the lake and in the lake. There are about 200 hot springs, most of which are distributed along the shoreline.[1] In four locations around the lake can be observed at least 10 geysers, which erupt up to 5 m high.[23] Geyser activity is affected by the fluctuations of lake level, which may inundate or expose some geysers.
Geysers
Geology
Lake Bogoria occupies an asymmetric basin approximately 20 km long and 10 km wide, bordered by faults. The east and south borders are marked by a major fault,[24] with steep slopes that prevent wetland development[14] (the Siracho Escarpment, to the east[23]). To the west, trachyphonolites (uncommon extrusive igneous rock) are cut through by numerous gently sloping tilt-blocks; rivers oriented north-south feed delta lobes, where spring-fed wetlands have developed. The north opens on a basin with Quaternary silts, sands and gravels; there, the gently sloping Sandai and Loboi plains gradually rise to a drainage divide that separates lake Bogoria and lake Baringo.[14]
The faults control over 200 hot and cold springs and seeps, which bring a significant water input.[14]
Core analysis of the lake floor has revealed two types of sedimentation: a shallow fan–deltaic clastic zone; and a deeper zone where Organic matters alternate with evaporites. The organic muds were formed during periods of relatively high lake level and high microbial productivity; whereas the evaporites were formed during drier periods. The cores attest of many environmental fluctuations during the past 30 000 years, linked to regional climatic changes and to local tectonic and hydrological conditions.[22]
Chemistry, hydrology
Lake Bogoria is a soda lake: it has no surface outlet, its waters are strongly alkaline[22] (pH:10.5). High salt concentrations are also given (40‰) and this increases when the total amount of water decreases (evapoconcentration). Thus, following an extreme draught from March to October 2009, salt saturation reached 48‰.[25] Soda lakes are highly productive ecosystems.
Its waters contain large concentrations of Na+, HCO3−, CO32− et Cl− ions.[1] They originate from inflow from the Sandai and Emsos rivers, and from about 200 alkaline hot springs that are present at three onshore sites: Loburu, Chemurkeu, and a southern group (Ng'wasis, Koibobei, Losaramat).[26] Other springs discharge directly from the lake floor. Lake Bogoria also contains the highest concentration of true geysers in Africa (at least 18 have been active in the 35 years before 2008).[27]
The lake is meromictic (stratified)[22][1] with less dense surface waters lying on a denser more saline bottom waters.
The lake has not always been saline. Sediment cores from the lake floor have shown that freshwater conditions existed for several periods during the past 10,000 years.[citation needed]
Of the ca. 60 hot springs that discharge on Loburu delta plain on the western margin of the lake, travertine appears at 20% of them. Carbonate is actively precipitating at several of these, as shown by calcite-encrusted artefacts. This is unusual, in that this precipitation most probably occurs at temperatures over 80°C.[28]
The geysers are believed by some to have medicinal value.[29]
Flamingos nesting on the shoreline of the lake (1988).
Phytoplankton
One species dominates the phytoplankton: Arthrospira fusiformis, a cyanobacteriumspirulina.[12] But all these wetlands see the occurrence of diatoms in at least parts of them; these diatoms vary in diversity, abundance and species composition. The main factors directing these variables are pH, temperature, and specific conductivity; secondary factors are Si and nitrate. Hot springs generally have a low diversity of diatoms, with variable abundance; they commonly include Anomoeoneis sphaerophora var. guntheri, Navicula tenella, Navicula cuspidata, and Nitzschia invisitata. In other wetland types, distinctive diatom floras variously include Fragilaria brevistriata, Gomphonema parvulum, Navicula tenelloides, Nitzschia communis, N. latens, N. sigma, Rhopalodia gibberula, and Stauroneis anceps.[16]
The lake supports more than 300 waterbird species. It is an important stopover site for a population of up to 1.5 million migratory birds, notably for the lesser flamingo (Phoeniconaias minor).[29]
In the 1990s, two episodes of mass deaths occurred among flamingos, all starting from Lake Bogoria. The first episode, in 1993-1995, saw about 35,000 flamingos dying between August and November 1993 and about 15,000 dying in August 1995. The second episode occurred in 1999-2000; the number of deaths for 2000 was estimated at around 100,000. In both cases, flamingos were the only water bird species falling victim to this unknown phenomenon. The studies on these events were not conclusive as to the main cause of death. Heavy metal poisoning was suggested but such poisoning does not have a periodic effect: its effect are continuous, and in these cases not compatible with the periodic dying; nor was it coherent with that birds of all ages were concerned, whereas such poisoning affects older individuals more than younger ones (ther older ones have had more time to accumulate poison in their bodies). Food poisoning has also been cited. the main food for lesser flamingo is Spirulina platensis, which is abundantly produced in the lakes of that region; but around the years that saw this heavy mortality toll, there had been an important increase of toxic cyanobacteria, especially during periods of algal blooms; and the symptoms of dying flamingos were similar to those of algal toxicity.[13]
Other animals
Greater kudu one of the animals at lake bogoria
Its immediate surroundings are a critical habitat for vulnerable species such as the common hippopotamus (Hippopotamus amphibius) and African lion (Panthera leo); another important species is the greater kudu (Tragelaphus strepsiceros). The lake's stable water level makes it doubly important during periods of drought, when water levels in other East African lakes drop.[29]
Nature protection
The Site is a UNESCO World Heritage Site since 2011[31] and an Important Bird and Biodiversity Area (IBA).[29] The Ramsar site, designated on August 27, 2001,[29] covers the entire National Reserve, with an area of 10,700ha (26,000 acres), shared between the 3,300 ha lake and 7,400 ha of riparian and terrestrial habitats.[5]
Human rights: the Endorois people
Cheptaleel's Prayer. Contemporary illustration of heroine of Kalenjin folklore
The lake area was the traditional home of the Endorois people, who were forced to leave the area in the 1970s and are now challenging their removal at the African Commission on Human and Peoples' Rights. In 2009 the African Commission on Human and Peoples' Rights (ACHPR) made a landmark ruling, ordering the Kenyan government to restore the Endorois to their historic land, compensate them from losses and sharing with them the profits from the Lake Bogoria game reserve. But in 2022, Minority Rights Group reported that that decision had not yet been implemented and has many Endorois were still consigned to 'severe poverty, illiteracy, poor health and a life of destitution.' In 2024 the Endorois allied with the Ogiek people — who have themselves been initially evicted in 1920 from their ancestral grounds in the Mau Forest (south-west Kenya) by the British colonial government. In 2017 the Ogiek also won a court case against the Kenian government, whereby the latter was supposed to restitute the Ogiek ancestral land and pay a compensation of 157,000 Kenyan shillings ($1,026) per person. As of 2024, not only the government has so far failed to implement the court's orders as in the case of the Endorois, but has persisted in further evictions imposed in November 2023 by the Kenyan authorities during the visit of Britain's King Charles III. On 6 February 2024, both ethnies demonstrated together in Nairobi with the support of the International Network for Economic, social and cultural rights to demand the government implement the rulings.[32]
The area is inhabited by Tugen and Jemps pastoralists, and livestock grazing is the main land use in the area.[29]
Tourism
The lake and its surroundings attract 200,000 tourists per year, due to the wildlife, the hot springs, the spectacular cliffs and escarpments and the rich indigenous culture.[29]
Hotel accommodation is available near Loboi village at the north end of the lake. Camping is permitted at the southern end of the lake.[33]
Lake Bogoria panorama: the Loburu delta with proximal hot springs and hot spring marshes[34]
Lake Baringo is, after Lake Turkana, the most northern of the Kenyan Rift Valley lakes, with a surface area of 130 square kilometres (50 sq mi) and an elevation of 970 metres (3,180 ft). The lake is fed by several rivers: the Molo, Perkerra and Ol Arabel. It has no obvious outlet; the waters are assumed to seep through lake sediments into the faulted volcanic bedrock. It is one of the two freshwater lakes in the Rift Valley in Kenya, the other being Lake Naivasha.
The lesser flamingo is a species of flamingo occurring in sub-Saharan Africa and western India. Birds are occasionally reported from further north, but these are generally considered vagrants.
Geysir, sometimes known as The Great Geysir, is a geyser in south-western Iceland, that geological studies suggest started forming about 1150 CE. The English word geyser derives from Geysir. The name Geysir itself is derived from the Icelandic verb geysa. Geysir lies in the Haukadalur valley on the slopes of Laugarfjall lava dome, which is also the home to Strokkur geyser about 50 metres (160 ft) to the south. The Strokkur geyser may be confused with it, and the geothermal field it is in is known usually as either, Geysir or Haukadalur.
Lake Natron is a salt or alkaline lake located in north Ngorongoro District of Arusha Region in Tanzania at the border with Kenya. It is in the Gregory Rift, which is the eastern branch of the East African Rift. The lake is within the Lake Natron Basin, a Ramsar Site wetland of international significance. It is the only regular breeding area for Africa's lesser flamingoes, although this habitat is not protected and is under threat from planned development projects.
The Rift Valley lakes are a series of lakes in the East African Rift valley that runs through eastern Africa from Ethiopia in the north to Malawi in the south, and includes the African Great Lakes in the south. These include some of the world's oldest lakes, deepest lakes, largest lakes by area, and largest lakes by volume. Many are freshwater ecoregions of great biodiversity, while others are alkaline "soda lakes" supporting highly specialised organisms.
Lake Magadi is the southernmost lake in the Kenyan Rift Valley, lying in a catchment of faulted volcanic rocks, 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.
Nakuru is a city in the Rift Valley region of Kenya. It is the capital of Nakuru County, and it is the fourth largest city in Kenya and the largest in the Great Rift Valley, Kenya|Rift Valley region. As of 2019, Nakuru has an urban population of 570,674, making it the largest urban center in the Rift Valley, above Eldoret, Uasin Gishu County. The city lies along the Nairobi–Nakuru Highway, 160 kilometres (99 mi) from Nairobi, the capital city of Kenya.
Lake Nakuru is one of the Rift Valley lakes, located at an elevation of 1,754 m (5,755 ft) above sea level. It lies to the south of Nakuru, in the rift valley of Kenya and is protected by Lake Nakuru National Park.
Lake Abijatta is an alkaline lake in Ethiopia. It lies in the Main Ethiopian Rift valley south of Addis Ababa, in the Abijatta-Shalla National Park.
Lake Manyara National Park is a protected area in Tanzania's Arusha and Manyara Regions, situated between Lake Manyara and the Great Rift Valley. It is administered by the Tanzania National Parks Authority, and covers an area of 325 km2 (125 sq mi) including about 230 km2 (89 sq mi) lake surface. More than 350 bird species have been observed on the lake.
The Kapthurin Formation is a series of Middle Pleistocene sediments associated with the East African Rift Valley. Part of the East African Rift System, it is also an important archaeological site in the study of early humans who occupied the area and left stone tools and animal bones behind. It outcrops in Kenya west of Lake Bogoria and northwest of Lake Baringo in the Kenya Rift Valley, exposed on the surface in a 150 km2 (58 sq mi) area. It also outcrops in portions of the Tugen Hills farther east. The ~125 metres (410 ft) of sediment that comprises the Kapthurin formation represents more than 600,000 years of depositional history. Clastic sediments, tuffs, and carbonate beds, in the Kapthurin give information on past river and lake environments. Additionally, intercalated tuffs and extrusive igneous rocks associated with Rift Valley volcanic activity have allowed for multiple argon–argon dating studies. The high resolution dating enables archaeological studies regarding changing hominin behavior. The Kapthurin Formation has been used to study the Acheulian-Middle Stone Age transition.
Lake Elmenteita is a soda lake, in the Great Rift Valley, about 120 km northwest of Nairobi, Kenya.
The Great Rift Valley is part of an intra-continental ridge system that runs through Kenya from north to south. It is part of the Gregory Rift, the eastern branch of the East African Rift, which starts in Tanzania to the south and continues northward into Ethiopia. It was formed on the "Kenyan Dome", a geographical upwelling created by the interactions of three major tectonics: the Arabian, Nubian, and Somalian plates. In the past, it was seen as part of a "Great Rift Valley" that ran from Madagascar to Syria. Most of the valley falls within the former Rift Valley Province.
Mount Silali is a dormant volcano in the Gregory Rift Valley, near Kapedo, Kenya. Silali is south of the Suguta Valley, which reaches northward to Lake Turkana, and is about 70 kilometres (43 mi) north of Lake Baringo.
Lake Bogoria National Reserve is in the Great Rift Valley, Kenya, covering Lake Bogoria and the land immediately surrounding the lake. It is administered by the Kenya Wildlife Service.
The Waseges River, or Sandai River, is a river in Kenya. Its source is on the slopes of the Nyandarua Plateau below the Aberdare Range; it ends its course in lake Bogoria.
The Olkaria Area is a region located immediately to the south of Lake Naivasha in the Great Rift Valley of Kenya, Africa. It is geothermally active and is being used to generate clean electric power. The region has an estimated potential of 2,000 MW. This is almost double the maximum daily electricity peak demand recorded in 2008/2009 for the entire country.
The Suguta River is a seasonal river in the Great Rift Valley in Kenya (Africa), directly south of Lake Turkana. It flows northward through the Suguta Valley in the rainy season, forming the temporary Lake Alablad, a dry lake that combines with Lake Logipi at the northern end of the valley.
The Southern Ewaso Ng'iro is a river in the Great Rift Valley in Kenya. It plays an important role in the ecology of Lake Natron, the main regular breeding site for near-threatened lesser flamingos. Changes to land use in the river's headwaters or in the marshes before the river enters the lake could have a serious impact on this species.
Lake Suguta is a former lake in Africa. It formed in the Suguta Valley, which is part of the East African Rift, south of Lake Turkana during the Holocene African humid period.
↑ Beccaluva, Luigi; Bianchini, Gianluca; Wilson, Marjorie (2011). Volcanism and Evolution of the African Lithosphere. GSA Special Papers. Vol.478. Geological Society of America. doi:10.1130/SPE478. ISBN978-0-8137-2478-2.
↑ Nilsson, E. (1932). Quarternary glaciations and pluvial lakes in British East Africa (Ph.D. thesis). Stockholm: Centraltryckeriet. Cited in Harper et al. 2003, p.261.
↑ Vareschi, Ekkehard (January 1978). "The ecology of Lake Nakuru (Kenya) I. Abundance and feeding of the lesser flamingo". Oecologia (Berl.). 32 (1): 11–35. doi:10.1007/BF00344687. Cited in Harper et al. 2003, p.261.
↑ Karua, (Minister for water resources management and development) (June 17, 2003). "Diversion of River Waseges". Parliamentary Debates.
↑ Ashley, Gail M.; Goman, Michelle; Hover, Victoria C.; Muasya, A. Muthama; Owen, Richard B.; Renaut, Robin W. (2002). "Artesian blister wetlands, a perennial water resource in the semi-arid rift valley of East Africa". Wetlands. 22 (4): 686–695. doi:10.1672/0277-5212(2002)022[0686:ABWAPW]2.0.CO;2. Cited in Owen et al. 2004, p.65.
Renaut, Robin W.; Owen, R. Bernhart (1991). "Lake Bogoria". In Anadón, P.; Cabrera, Ll; Kelts, K. R. (eds.). Lacustrine facies analysis. John Wiley & Sons. pp.175–194. ISBN0-632-03149-2.
Renaut, Robin W.; Tiercelin, Jean-Jacques (March 1993). "Lake Bogoria, Kenya: soda, hot springs and about a million flamingoes". Geology Today. 9 (2): 56–61. doi:10.1111/j.1365-2451.1993.tb00981.x.
Renaut, Robin W.; Tiercelin, Jean-Jacques (1994). "Lake Bogoria, Kenya Rift Valley: a sedimentological overview". In Renaut, Robin W.; Last, William M. (eds.). Sedimentology and Geochemistry of Modern and Ancient Saline Lakes. Society for Sedimentary Geology, Special Publication, vol. 50. pp.101–123. doi:10.2110/pec.94.50.0101. ISBN9781565761759.
Renaut, Robin W.; Owen, R. Bernhart (2005). "The geysers of Lake Bogoria, Kenya Rift Valley, Africa". GOSA Transactions. 9: 4–18.
Tiercelin, Jean-Jacques; Vincens, Annie; Barton, C. E. (1987). "Le demi–graben de Baringo–Bogoria, Rift Gregory, Kenya. 30,000 ans d'histoire hydrologique et sédimentaire". Bulletin des Centres de Recherches Exploration-Production Elf-Aquitaine (in French). 11 (2): 249–540. ISSN0396-2687.
Tierlin J.J. 1985 Le rift est African vers un nouvel ocean: l'hydrothermalisme marqueur de l'ouverture? Actes 110e Conles nationalize societes sav., 6, 305-316
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