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Suguta Valley
The Suguta Valley, also known as the Suguta Mud Flats, is an arid part of the Great Rift Valley in Kenya (Africa), directly south of Lake Turkana. Location The Suguta valley today is one of the driest parts of Kenya, with annual rainfall below . Lake Logipi seasonally fills a small part of the northern end of the valley. The valley has a relatively flat floor about above sea level. It is bordered by land to the east and west rising to and dotted with volcanic cinder cones. The Barrier Volcano, a broad volcanic complex, separates the valley from Lake Turkana. Mount Ngiro rises to the east of the Suguta valley. The Losiolo Escarpment, rising above the valley floor on the east side near Maralal provides one of the most dramatic views of the Kenyan rift valley. Namarunu, a volcano active in historic times, extends into the valley from the western wall. The Suguta Valley lies along the axis of the Gregory Rift, which has been faulting in this area since the Pliocene along a belt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Namarunu
Namarunu is a shield volcano located in the Great Rift Valley, Kenya. Location Namarunu is located in the Suguta Valley, a section of the Kenyan Rift Valley just south of Lake Turkana. It extends from the western side of the rift past the center. The mountain forms a broad shield. The large basal part is about deep, made up of outward-dipping trachytic lavas, breccias and tuffs. A few thousand years ago the Suguta was filled by a major lake, but now it is extremely dry and hot, with only the small Lake Logipi at the northern end. Some of the recent cones on the floor of the rift valley and on the eastern side of the rift below the Tirr Tirr Plateau contain hot springs. Evolution Namarunu was mainly formed during the upper Pliocene, but has some material from the Holocene. It is a trachytic shield volcano topped by more recent parasitic cones and lava flows. The basal trachyte dates to roughly 6.8 million years ago, while the uppermost basalts date to around 500,000 years ag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trachyte
Trachyte () is an extrusive igneous rock composed mostly of alkali feldspar. It is usually light-colored and aphanitic (fine-grained), with minor amounts of mafic minerals, and is formed by the rapid cooling of lava enriched with silica and alkali metals. It is the volcanic equivalent of syenite. Trachyte is common wherever alkali magma is erupted, including in late stages of ocean island volcanismMacDonald 1983, pp. 51-52 and in continental rift valleys, above mantle plumes,Philpotts and Ague 2009, pp. 390-394 and in areas of back-arc extension. Trachyte has also been found in Gale crater on Mars. Trachyte has been used as decorative building stone and was extensively used as dimension stone in the Roman Empire and the Republic of Venice. Chemical composition Trachyte has a silica content of 60 to 65% and an alkali oxide content of over 7%. This gives it less SiO2 than rhyolite and more (Na2O plus K2O) than dacite. These chemical differences are consistent with the positio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Rift Valley
The Great Rift Valley is a series of contiguous geographic trenches, approximately in total length, that runs from Lebanon in Asia to Mozambique in Southeast Africa. While the name continues in some usages, it is rarely used in geology as it is considered an imprecise merging of separate though related rift and fault systems. This valley extends northward for 5,950 km through the eastern part of Africa, through the Red Sea, and into Western Asia. Several deep, elongated lakes, called ribbon lakes, exist on the floor of this rift valley: Lakes Malawi, Rudolf and Tanganyika are examples of such lakes. The region has a unique ecosystem and contains a number of Africa's wildlife parks. The term Great Rift Valley is most often used to refer to the valley of the East African Rift, the divergent plate boundary which extends from the Afar Triple Junction southward through eastern Africa, and is in the process of splitting the African Plate into two new and separate plates. Geologi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baragoi
Baragoi is a market town in Kenya, lying north of Maralal and east of the Suguta Valley. It is located in Samburu County. The entire Baragoi division has a population of nearly 20,000 (1999 census) comprising mostly people from the Samburu and Turkana tribes. The main access road to Baragoi is the A4 road from Rumuruti-Maralal-Baragoi, which as of 2019 was being tarmaced from Rumuruti up to Maralal. The stretch of 108 km from Maralal to Baragoi is still unpaved. See also *Baragoi Clashes In November 2012, a series of ethnic clashes between the Samburu and Turkana tribes of Kenya's Samburu County resulted in the deaths of at least 46 people including police officers sent to quell the violence. Cause of conflict Tribal rivalry a ... References Populated places in Samburu County {{RiftValleyKE-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kenya Police
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Turkana People
The Turkana are a Nilotic people native to the Turkana County in northwest Kenya, a semi-arid climate region bordering Lake Turkana in the east, Pokot, Rendille and Samburu people to the south, Uganda to the west, and South Sudan and Ethiopia to the north. Overview According to the 2019 Kenyan census, Turkana number 1,016,174, or 2.14% of the Kenyan population, making the Turkana the third largest Nilotic ethnic group in Kenya, after the Kalenjin and the Luo, slightly more numerous than the Maasai, and the tenth largest ethnicity in all of Kenya. Although this figure was initially controversial and rejected as too large by Planning Minister Wycliffe Oparanya, a court ruling (February 7, 2012) by Justice Mohammed Warsame stated that the Kenyan government accepts the 2009 census figures for Turkana. They refer to themselves as ''ŋiTurkana'' (i.e. ngiTurkana, meaning the Turkana, or people of Turkan) and to their land as "Turkan". The language of the Turkana, an Eastern Nilot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pokot People
The Pokot people (also spelled ''Pökoot'') live in West Pokot County and Baringo County in Kenya and in the Pokot District of the eastern Karamoja region in Uganda. They form a section of the Kalenjin ethnic group and speak the Pökoot language, which is broadly similar to the related Marakwet, Nandi, Tuken and other members of the Kalenjin language group. History Origins Pokot identity formed in the Kerio Valley perhaps as early as the late 18th and certainly not later than the mid 19th century. It emerged from the assimilation of the Sirkwa era Chok by the Pokotozek section of the Maliri. Assimilation Early 20th century accounts of the Pokot identify two distinct branches of the community with the caveat that much as two ways of life are detailed, they were one people. Beech (1911) identified significant differences between agricultural and pastoral sections of the Pokot in; oaths, punishment for murder and homicide, punishment for assault, punishment for witchcraft, punis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flamingo
Flamingos or flamingoes are a type of Wader, wading bird in the Family (biology), family Phoenicopteridae, which is the only extant family in the order Phoenicopteriformes. There are four flamingo species distributed throughout the Americas (including the Caribbean), and two species native to Afro-Eurasia. A group of flamingoes is called a "flamboyance." Etymology The name ''flamingo'' comes from Portuguese language, Portuguese or Spanish language, Spanish ("flame-colored"), which in turn comes from Old Occitan, Provençal – a combination of ("flame") and a Germanic-like suffix ''wikt:-ing#Etymology 3, -ing''. The word may also have been influenced by the Spanish ethnonym ("Fleming" or "Flemish"). The name of the genus, ''Phoenicopterus'', is from the Greek , ); other genera names include ''Lesser flamingo, Phoeniconaias,'' which means "crimson/red Naiad, water nymph (or naiad)", and ''Phoenicoparrus,'' which means "crimson/red bird (though, an unknown bird of om ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Playa Lake
Playa (plural playas) may refer to: Landforms * Endorheic basin, also known as a sink, alkali flat or sabkha, a desert basin with no outlet which periodically fills with water to form a temporary lake * Dry lake, often called a ''playa'' in the southwestern United States Populated places United States * Playas, New Mexico, an unincorporated community in New Mexico * Playa, Añasco, Puerto Rico, a barrio in the municipality of Añasco, Puerto Rico * Playa, Guayanilla, Puerto Rico, a barrio in the municipality of Guayanilla, Puerto Rico * Playa, Ponce, Puerto Rico, a barrio of Ponce, Puerto Rico * Playa, Santa Isabel, Puerto Rico, a barrio in the municipality of Santa Isabel, Puerto Rico * Playa, Yabucoa, Puerto Rico, a barrio in the municipality of Yabucoa, Puerto Rico Cuba * Playa, Havana, one of the 15 municipalities of the City of Havana, Cuba Ecuador * Playas Canton, Ecuador ** Playas, Ecuador, the administrative center of the Playas Canton Other * The Playa, Black Rock Des ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Suguta River
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 Suguta River originates in a stream of near-boiling water that emerges from the side of Mount Silali, an extinct volcano. Some geologists speculate that the Kapedo hot spring, which drops through a set of waterfalls to the Sugutu river, is the outlet from Lake Baringo Lake Baringo is, after Lake Turkana, the most northern of the Kenyan Rift Valley lakes, with a surface area of and an elevation of . The lake is fed by several rivers: the Molo, Perkerra and Ol Arabel. It has no obvious outlet; the waters ar ... to the south. At one point the Suguta River passes between two volcanoes and is fed from both sides by hot springs. In places the banks of the Suguta River are lined wit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
African Humid Period
The African humid period (AHP) (also known by other names) is a climate period in Africa during the late Pleistocene and Holocene geologic epochs, when northern Africa was wetter than today. The covering of much of the Sahara desert by grasses, trees and lakes was caused by changes in Earth's orbit around the Sun; changes in vegetation and dust in the Sahara which strengthened the African monsoon; and increased greenhouse gases. During the preceding Last Glacial Maximum, the Sahara contained extensive dune fields and was mostly uninhabited. It was much larger than today, but its lakes and rivers such as Lake Victoria and the White Nile were either dry or at low levels. The humid period began about 14,600–14,500 years ago at the end of Heinrich event 1, simultaneously to the Bølling–Allerød warming. Rivers and lakes such as Lake Chad formed or expanded, glaciers grew on Mount Kilimanjaro and the Sahara retreated. Two major dry fluctuations occurred; during the Youn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Suguta
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. The lake existed a number of times during history, most recently during the early and middle Holocene when a stronger monsoon caused increased precipitation in the basin of the lake. The lake then reached a top elevation of above sea level, when it overflowed into the Kerio River and then into Lake Turkana. The lake possibly ultimately drained into the Nile. Between 8,000 and 5,000 years ago the lake progressively dried up; today only the small Lake Logipi occupies the area. Geography and geology Lake Suguta lies in the Kenya Rift, which is part of the East African Rift. Starting with the Miocene, plate tectonics resulted in the pulling apart of the crust and the formation of the rift valley along with volcanoes; these include The Barrier volcano which starting from 1.3 million years ago and defini ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
-_Breeding_plumage_W2_IMG_8770.jpg "Click for more on -> Flamingo")
