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Great Rift Valley: East Africa
built 633 days ago
The formation of the Rift Valley is still continuing. In a few million years, eastern Africa will split off to form a new landmass. The original activity that caused the Rift weakened the Earth's crust. The area is therefore volcanically and seismically active - producing the volcanoes Mount Kilimanjaro, Mount Kenya, Mount Meru, Mount Elgon, and the Crater Highlands in Tanzania.
The complete guide to The Rift Valley; The Great Rift Valley provides the eastern backbone of the African continent, an epic trail of jaw-dropping scenery, stunning safaris and changing cultures. Sarah Barrell uncovers the highlights.(Features)
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Image:Greatrift.jpg The Great Rift Valley is an enormous geographical feature caused by the separation of the African and Arabian tectonic plates around 35 million years ago. It was named by the explorer John Walter Gregory.
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A remarkable and adventurous journey through the Great Rift Valley from the natural and historic wonders of Ethiopia's highlands through the tribal lands of it's southern reaches and into the dusty game-lands of northern Kenya. A rugged journey of contrasts through some of the Africa's most varied and striking scenery.
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The Great Rift still lives. Many of its Volcanos smolder, and some are still erupting. Earthquakes occasionally shake the savannas; the Dead Sea widens a few feet each year. Eventually, in the next few million years, the rift could deepen further, fill with sea water, and cut off the eastern section of Africa to make it a separate landmass. Until then, the Great Rift Valley should continue to offer excellent wildlife viewing and a close look at the inner workings of the planet.
Situated on the equator on Africa's east coast, Kenya has been described as "the cradle of humanity". In the Great Rift Valley palaeontologists have discovered some of the earliest evidence of man's ancestors. In the present day, Kenya's ethnic
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