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 The Great African Rift Valley

 

The great Rift ValleyThe Great Rift Valley is a geologic depression (rift) that extends from Syria in south western Asia to Mozambique in south eastern Africa. It takes the form of a series of valleys and bodies of water that are bounded by parallel fault lines. The Great Rift Valley is widening slowly but surely, in the process causing many volcanic eruptions and earthquakes in the area. The great Rift valley is also visible from outer space as a rift of two parallel lines.

Some 20 million years ago, the earth's crust weakened and tore itself apart creating a jagged rift, thousands of kilometres long, across the Eastern end of the African continent. The land on either side erupted creating great volcanic mountains, while the valley floor gradually sank into a low flat plain. This geologic phenomena, dubbed the Great Rift Valley by the Scottish explorer John Walter Gregory, divides Kenya neatly down the length of the country essentially separating east from west.

Today, The Rift Valley is characterized by uninhabitable desert and fertile farmland, flat arid plains and steep escarpments. The great Rift Valley is also the home to millions of wildlife and hosts the worlds most renowned game parks and reserves (the Maasai Mara in kenya and The Serengeti in Tanzania). In some places this natural divide is up to 100 km (60 miles) wide, while it reaches its narrowest point just north of Nairobi at 45 km wide.

The valley floor is at its lowest near Lake Turkana where there is virtually no distinction between the Great Rift and the surrounding desert. As it heads south, however, the valley walls form sheer cliffs rising to 1,900 km (6,232 ft) at Lake Naivasha. After Naivasha, the valley descends again to 580 meters (1,902 feet) at the Tanzanian border.

 

Subterranean movement is common today as the Rift Valley is home to thirty active and semi-active volcanoes and countless hot springs along its length. This string of alkaline lakes and boiling springs northwest of Nairobi includes Lake Baringo, Lake Bogoria, Lake Nakuru, Lake Elementaita, Lake Naivasha, and Lake Magadi in the south. In the noth is lake Turkana.

 

Rift Valley Safaris

 

       >>>Safaris

       5 Days Lake Nakuru| Lake Naivasha| Masai Mara

        5 Days Masai Mara| Lake Nakuru

        6 Days Amboseli| Lake Naivasha| Masai Mara

 

 

      >>>Short Excursions - Rift Valley adventure tours

       2 days Lake Nakuru          2 days Lake Naivasha        

       A visit to Lake Baringo       A visit to Lake Bogora      

       A Visit to Lake Magadi        A visit to Lake Elementata

        Lake Turkana

These lakes are unique because their water is highly concentrated in sodium carbonate. This situation is caused by the high alkalinity from the surrounding volcanic rocks coupled with poor drainage outlets due to the steep sides of the valley. The high evaporation of the surface lake water results in sodium carbonate which, in turn, creates an ideal breeding ground for algae. Several species of fish, tilapia in particular, thrive in this environment. As a result, millions of birds flock to these soda lakes to feast on the abundant food supply of algae and fish. Each of the lakes in the East African Rift Valley string have a slightly different water composition ranging from freshwater to extremely alkaline, highly saline to brackish.

Truly Magical Kenya: Africa rift, African rift, east Africa rift, the great rift

the great rift valley

 
 

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East Africa Safari Destinations

    Kenya

 

   Masai Mara Reserve

   Amboseli National Park

   Samburu National park

   The Great Rift Valley

   Laikipia Conservancies


Uganda

 

    Murchison Falls

    Queen Elizabeth

    Bwindi

Northern Tanzania

 

   Serengeti National Park

   Ngorongoro Crater

   Lake Manyara

  Tarangire National Park


Beach Holidays

 

    Zanzibar Beach Holidays

    Mombasa Holidays

    Malindi & Watamu

   

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