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History of Kenya

History of Kenya

Kenya is an East African country known for its beautiful surroundings and extensive animal reserves. For many years, its coast on the Indian Ocean provided historically important ports. Through which the products of Arab and Asian traders entered the continent. Along this coast, which offers some of the best beaches in Africa, are predominantly Swahili Muslim towns like Mombasa.

A historic capital that has contributed much to the country’s musical and culinary history. Inland, the inhabited highlands are famous for their tea plantations, which were an important source of income. During the British colonial era, as well as a variety of animal species, including lions, elephants, leopards, rhinos, and hippopotamuses. The western provinces of Kenya are wooded, with lakes and rivers. While a small area in the north is arid and semi-desert. Kenya’s unique wildlife and beautiful environment attract a large number of European and North American tourists, and tourism is a significant contribution to the country’s economy. Everyone visit kenya.

Nairobi, Kenya’s capital, is a big city and. Like many other African capitals, is a study in contrast, with contemporary skyscrapers dotting gigantic shantytowns in the distance. Many of which are home to refugees left by civil strife in neighboring countries. The old and more affluent neighborhoods are ethnically diverse and well supplied with amenities and other amenities.

Culture

Kenya has a rich heritage of oral and written literature, including many anecdotes that speak of determination and resilience, which are key qualities and are generally preserved given the country’s experience during the war for independence. Outsiders are familiar with many of the peoples of Kenya, due to the desire of the British colonial administration to study them. For years, anthropologists and other sociologists have studied the lifestyles of the Maasai, Luhya, Lo, Kalenjin, and Kikuyu peoples, to name a few. Immigrants from a variety of European and Asian countries add to the country’s ethnic diversity. Kenyans are proud of their cultures and customs, but they are also aware of the necessity of national unity.

The Climate of Kenya

Large-scale pressure systems in the western Indian Ocean and surrounding land masses control seasonal weather fluctuations. Northeast winds blow north of the equator from December to March, while south to southeast winds prevail in the south. Although it may rain locally during these months, the weather is generally dry. The rainy season in both hemispheres runs from late March to May, with air entering from the east. From June to August, there is minimal precipitation, southwest winds north of the equator prevail, and southeast winds from the equator predominate.

Annual precipitation in the Lake Victoria Basin ranges from 40 inches (1,000 mm) along the shoreline to more than 70 inches (1,800 mm) in the eastern regions. Since 20 to 35 inches (500 to 900 mm) of rain falls most years, the beach has good agricultural potential. Maximum daily temperatures range from 80°F (27°C) in July to 90°F (32°C) between October and February. Average temperatures in the Rift Valley drop from over 84°F (29°C) in the north to just over 61°F (16°C) in Lake Nakuru and Naivasha in the south. Nearby elevations are usually temperate, with average temperatures ranging from 56 to 65 degrees Fahrenheit (13 to 18 degrees Celsius). The bottom of the rift valley is usually dry, but the highlands get more than 30 inches (760 mm) of rain each year.

Rainfall in Kenya

The Mau Escarpment’s consistent rainfall and good soil provide the basis for a strong agricultural sector. Although agriculture is limited by the highly variable rainfall in the eastern plateau region, the average annual rainfall ranges from 20 to 30 inches (500 to 760 mm) in most locations. High temperatures but intermittent rainfall characterize the semi-arid and arid regions of northern, northeastern and southern Kenya. The average temperature in most locations is 85 degrees Fahrenheit (29 degrees Celsius), and annual precipitation ranges from about 10 inches (250 mm) in the north to less than 20 inches (500 mm) in the south. Average temperatures in most places on the coast exceed 80 degrees Fahrenheit (27 degrees Celsius), and relative humidity is high throughout the year.

Average temperatures in most places of the coast reach 80 degrees Fahrenheit (27 degrees Celsius), and relative humidity is high all year. Rainfall declines westward from the west coast, where annual precipitation ranges between 30 and 50 inches (760 and 1,270 mm), to roughly 20 inches (500 mm) every year. Precipitation is only regular enough for successful agriculture on the southern shore.

Plant and Animal life

The classic highland environment between elevations of 7,000 and 9,000 feet (2,100 and 2,700 metres). Consists of areas of evergreen forest separated by wide plains of short grass. Where no human encroachment has occurred. The forest contains trees of commercial importance such as cedars (Juniperus procera) and poodoo species. The bamboo area extends about 10,000 feet (3,000 m) above the forest, where there are mountain bogs with treetops. Tree floors (basewood of the genus Senesio), and giant lobelia (a widely distributed herbaceous plant).

The forests give place to low trees distributed across an equal layer of short grass east and west of the hills. Baobab trees grow in semi-desert locations less than 3,000 feet (900 m) in height. Desert scrub grows in the drier northern parts, showing dry soil. The vegetation in the Sahel region is mainly grasslands with areas of the landscape remaining. While forest remains can still be found along the northern shore, they have been practically destroyed in the south by centuries of human settlement. The Green Belt Movement, launched by ecologist. Wangari Maathai (2004 Nobel Peace Prize laureate) in 1977, had planted 30 million trees by the early 2000s in an effort to halt deforestation and desertification. Tsetse flies and mosquitoes, which are responsible for the spread of sleeping sickness (trypanosomiasis) and malaria, invade about a third of Kenya, particularly the western regions and the coastal belt.

Majority of Kenya

The vast majority of Kenya’s wildlife population lives outside of the country’s many national parks and game reserves. Baboons and zebras, for example, can be seen near human settlements and urban centers along the Nairobi-Nakuru road. This led to human-animal conflict.

The Kenya Wildlife Service started a “parks out of parks” scheme in the mid-1990s to try to resolve the situation. The vegetation cover of each region is closely related to the differentiation and distribution of wildlife in it. Elephants and rhinos are two of the most common large animals found in the highland rainforests. However both species have experienced significant declines due to poaching and deforestation. There are also shrub, colobus monkeys, and glagos (bush babies) to be found. The Bamboo area is home to many species of duikers as well as a few species of birds. Lions, tigers, and wild cats are among the highland predators.

Waterbuck, impala, eland, warthog, and buffalo among others. Lions, spotted hyenas, leopards, leopards and other predators feed on these animals. Elephant, rhinoceros, lions, leopards, giraffes, giraffes, impalas, cockatoos. Many varieties of kudus live in the bushes and woodlands of desert regions. While sunny antelopes, buffaloes, and elephants live in the coastal forest. Huge rivers are home to hippopotamuses, crocodiles, and a variety of fish, while the coastal waters are rich in marine life, including butterfly fish, angelfish, rock cod, barracuda, and spiny lobsters.

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