A UNESCO protected World Heritage Site and an International Biosphere Reserve, the Ngorongoro Conservation Area is situated some 190 km. west of Arusha, between Lake Manyara and Serengeti National Parks. Covering approximately 8,292 square km, the Ngorongoro Conservation Area consists of the Ngorongoro Crater itself, the Olduvai Gorge and Ndutu, the Empakai crater and the Oldonyo Lengai Mountain. The Ngorongoro Conservation Area is a pioneering experiment in multi-purpose land use where people (the Maasai), their livestock and wildlife coexist and share the same protected habitat. Wild animals are protected as in the National Parks. The craters of Ngorongoro and Empakai are reserved exclusively for wildlife, while the rest of the Conservation Area is shared by wildlife, people and livestock. The Maasai, the main residents of Ngorongoro, are pastoralists who move widely with their herds of cattle, sheep, goat and donkeys in search of pasture and water. In recent years the Maasai have been encouraged to work on the land and supplement their traditional diet of milk and meat.
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The Ngorongoro Crater, which is the central attraction in the area, is the largest Caldera in the world that has its walls intact. The Ngorongoro Crater floor, a sheer drop of 610 metres below the crater rim, has an area of 304 sq. km, with a diameter of 19 km. The sight of the Ngorongoro Crater is simply stunning.
“It is impossible to give a fair description of the size and beauty of the Crater, for there is nothing with which one can compare it. It is one of the Wonders of the World…” once wrote Professor Bernhard Grzimek. The crater floor is home to tens of thousands of plains animals, including wildebeest, zebra, gazelles, elands, and a large predator population of lions, hyena and jackal which can all be viewed at close quarters. The rare black rhino can be viewed here, and if you are lucky you can see cheetah and leopard. The rainy season is between November and May. The altitude at the crater rim is about 2286 metres above sea level, and temperatures can get quite chilly in the evening, especially between May to September.
“It is impossible to give a fair description of the size and beauty of the Crater, for there is nothing with which one can compare it. It is one of the Wonders of the World…” once wrote Professor Bernhard Grzimek. The crater floor is home to tens of thousands of plains animals, including wildebeest, zebra, gazelles, elands, and a large predator population of lions, hyena and jackal which can all be viewed at close quarters. The rare black rhino can be viewed here, and if you are lucky you can see cheetah and leopard. The rainy season is between November and May. The altitude at the crater rim is about 2286 metres above sea level, and temperatures can get quite chilly in the evening, especially between May to September.
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The area has been subject to extensive archaeological research for over 80 years and has yielded a long sequence of evidence of human evolution and human-environment dynamics, collectively extending over a span of almost four million years to the early modern era.
This evidence includes fossilized footprints at Laetoli, associated with the development of human bipedalism, a sequence of diverse, evolving hominin species within Olduvai gorge, which range from Australopiths such as Zinjanthropus boisei to the Homo lineage that includes Homo habilis, Homo erectus and Homo sapiens; an early form of Homo sapiens at Lake Ndutu; and, in the Ngorongoro crater, remains that document the development of stone technology and the transition to the use of iron. The overall landscape of the area is seen to have the potential to reveal much more evidence concerning the rise of anatomically modern humans, modern behavior and human ecology
This evidence includes fossilized footprints at Laetoli, associated with the development of human bipedalism, a sequence of diverse, evolving hominin species within Olduvai gorge, which range from Australopiths such as Zinjanthropus boisei to the Homo lineage that includes Homo habilis, Homo erectus and Homo sapiens; an early form of Homo sapiens at Lake Ndutu; and, in the Ngorongoro crater, remains that document the development of stone technology and the transition to the use of iron. The overall landscape of the area is seen to have the potential to reveal much more evidence concerning the rise of anatomically modern humans, modern behavior and human ecology
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