Ndoto Mountains
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Ndoto Mountains
The Ndoto Mountains are a mountain range in northern Kenya. Like Mount Nyiru to the north and the Mathews Range to the south, the Ndoto Mountains consist of Precambrian crystalline basement rock, mostly extremely durable gneisses and granites.Rainer W. Bussmann (2002). "Islands in the Desert—Forest Vegetation of Kenya's Smaller Mountains and Highland Areas (Nyiru, Ndoto, Kulal, Marsabit, Loroghi, Ndare, Mukogodo, Porror, Mathews, Gakoe, Imenti, Ngaia, Nyambeni, Loita, Nguruman, Nairobi)," ''Journal of East African Natural History'', 91(1), 27-79, (1 January 2002) The climate is semi-arid at lower elevations. At higher elevations there are areas of higher rainfall, humidity, and cloud cover which support montane forests Montane ecosystems are found on the slopes of mountains. The alpine climate in these regions strongly affects the ecosystem because temperatures fall as elevation increases, causing the ecosystem to stratify. This stratification is a crucial f ....Benny B ...
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Kenya
Kenya, officially the Republic of Kenya, is a country located in East Africa. With an estimated population of more than 52.4 million as of mid-2024, Kenya is the 27th-most-populous country in the world and the 7th most populous in Africa. Kenya's capital and largest city is Nairobi. Its second-largest and oldest city is Mombasa, a major port city located on Mombasa Island. Other major cities within the country include Kisumu, Nakuru & Eldoret. Going clockwise, Kenya is bordered by South Sudan to the northwest (though much of that border includes the disputed Ilemi Triangle), Ethiopia to the north, Somalia to the east, the Indian Ocean to the southeast, Tanzania to the southwest, and Lake Victoria and Uganda to the west. Kenya's geography, climate and population vary widely. In western, rift valley counties, the landscape includes cold, snow-capped mountaintops (such as Batian, Nelion and Point Lenana on Mount Kenya) with vast surrounding forests, wildlife and ...
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Mount Nyiru
Mount Ng'iro, also known as Mount Nyiru or Mount Nyiro, is a mountain in the north of Kenya overlooking the Suguta Valley, part of the Great Rift Valley, to the west. The mountain is surrounded by desert, but is forested on its upper slopes. It lies in the territory of the Samburu people. Some subclans under the Lmasula phratry cultivate bees on the mountain, and as bee-keepers claim exclusive rights to the land and water. There are 78.9 square kilometres of montane forest on the mountain. African juniper ('' Juniperus procera'') is the predominant tree at lower elevations and in drier areas, growing in pure stands or with ''Myrsine africana''. '' Faurea saligna'' and ''Ilex mitis'' are the predominant trees in more humid high-elevation areas. In high-elevation areas with the most condensing mist the bamboo '' Oldeania alpina'' forms dense thickets 6 to 8 meters tall. '' Lasiosiphon glaucus'' is the dominant tree in summit forests, forming close stands up to 8 meters tall. There a ...
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Mathews Range
The Matthews (or Mathews) Range, also known as the Lenkiyio Hills, is a range of mountains in Kenya. Geography The range is about 150 km long, oriented north–south. It is located in the Laikipia district of the Rift Valley Province in northern Kenya. The town of Wamba lies at the southeastern edge of the range.Rough Guide Map to Kenya Peaks The highest point is Warges, at above sea level, a peak located the southern end of the range, separated by a valley from the rest of the range. There is also a breast-shaped hill locally known as Sweet Sixteen in the range. Table Ecology The area is isolated, and holds montane forests of African juniper (''Juniperus procera'') and cycads. It is home to elephants and other large mammals, and was one of the last places in northern Kenya to have wild Black Rhinos. The last Black Rhino in the Mathew's was poached out in the 1990s. The Mathew's are also home to the Samburu people. The mountain range is a sky island: surrounded by ...
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Gneiss
Gneiss (pronounced ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. This rock is formed under pressures ranging from 2 to 15 kbar, sometimes even more, and temperatures over 300 °C (572 °F). Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct Cleavage (geology), cleavage. Gneisses are common in the ancient crust of Continental Shield, continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description image:Orthogneiss Geopark.jpg, Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct Cleavage (geology), cleavage. In other words, it i ...
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Granite
Granite ( ) is a coarse-grained (phanerite, phaneritic) intrusive rock, intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dike (geology), dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF diagram, QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) conta ...
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East African Montane Forests
The East African montane forests is a montane tropical moist forest ecoregion of eastern Africa. The ecoregion comprises several separate areas above 2000 meters in the mountains of South Sudan, Uganda, Kenya, and Tanzania. Geography The East African montane forests extend across a total of , in 25 separate enclaves, which range in size from 23,700 to 113 square kilometers. The montane forests extend down to approximately 1000 meters elevation, and as high as 3500 meters. The northernmost enclave is on Mount Kinyeti in the Imatong Mountains of South Sudan, extending south through Mount Moroto in eastern Uganda and Mount Elgon on the Kenya-Uganda border. In Kenya and Tanzania, the ecoregion follows the mountains east and west of the Eastern Rift and associated volcanoes, including the Aberdare Range, Mount Kenya, Mount Kulal, Mount Nyiru, Ndoto Mountains, Matthews Range, Mount Marsabit, Cherangany Hills, and the Nguruman Escarpment in Kenya, and Mount Kilimanjaro, Moun ...
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Great Rift Valley
The Great Rift Valley () is a series of contiguous geographic depressions, approximately 6,000 or in total length, the definition varying between sources, that runs from the southern Turkish Hatay Province in Asia, through the Red Sea, to Mozambique in Southeast Africa. While the name remains in some usages, it is rarely used in geology where the term "Afro-Arabian Rift System" is preferred. This valley extends southward from Western Asia into the eastern part of Africa, where several deep, elongated lakes, called ribbon lakes, exist on the rift valley floor, Lake Malawi and Lake Tanganyika being two such examples. 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 sep ...
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Mountains Of Kenya
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains te ...
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