The Ngorongoro Conservation Area covers 8,292 square kilometers. It is one of the three divisions that comprise the Ngorongoro District in the Arusha Region.
The short rains are from November to December and the long rains from February to April, the latter generally being considered the offseason. However, the rainy season is a very exciting time of year as this is when animals congregate on the Short Grass Plains to have their young. Late February, early March is usually a good time to see the migration on the plains. In turn, this attracts a large number of predators and results in spectacular interactions between predators and prey. Keep in mind that part of the Serengeti Plains falls within the NCA.
The dry season holds its own beauty. In Africa, the dry season is the best time for game viewing because the animals are concentrated along with permanent water sources. Within the Crater game viewing is excellent during this time. However, keep in mind that the Short Grass Plains become completely devoid of the game during this season. This is the best time of the year to visit Empakaai and Ndutu, which has a resident game that remains around the lake all year round
The NCCA’s wildlife and land have been a UNESCO site since 1979 and now its cultural heritage is to be included. The NCA is the only site in the world with a high concentration of wildlife living in harmony with human communities. The multiple land-use systems in this area are among the earliest to be established around the world as a means of reconciling human development and conserving natural resources. The
NCA also contains numerous paleontological, archaeological, and anthropological sites of exceptional quality.
Had it not become the world’s sixth-largest unbroken caldera, then what is now known as the Ngorongoro crater could have been a towering volcanic mountain, as high as Kilimanjaro.
The crater is the flagship tourism feature for the Ngorongoro Conservation Area. It is a large, unbroken, un-flooded caldera, formed when a giant volcano exploded and collapsed some three million years ago. The Ngorongoro crater sinks to a depth of 610 meters, with a base area covering 260 square kilometers. The height of the original volcano must have ranged between 4,500 to 5,800 meters high. Apart from the main caldera, Ngorongoro also has two other volcanic craters: Olmoti and Empakai, the former famous for its stunning waterfalls, and the latter holding a deep lake and lush, green walls.
On the leeward of the Ngorongoro highlands protrudes the iconic Oldonyo Lengai, an active volcano, and Tanzania’s third highest peak after Kilimanjaro and Meru. Known to local people as the Mountain of God, Mount Lengai’s last major eruption occurred in 2007. At the mountain’s foot is Lake Natron, East Africa’s major breeding ground for flamingoes.
Flora and Fauna: Wildlife
The area contains over 25,000 large animals including 26 black rhinoceros. There are 7,000 wildebeests, 4,000 zebras, 3,000 eland and 3,000 Grant’s and Thomson’s gazelles. The crater also has the densest known population of lions, numbering 62. Higher up, in the rainforests of the crater rim, are leopards, about 30 large elephants, mountain reedbuck, and more than 4,000 buffalos, spotted hyenas, jackals, rare wild dogs, cheetahs, and other felines.
The legendary annual wildebeest and zebra migration also passes through Ngorongoro, when the 1.7 million ungulates move south into the area in December then move out heading north in June. The migrants passing through the plains of the reserve include 1.7 million wildebeest, 260,000 zebra, and 470,000 gazelles. The Lake Ndutu area to the west has significant cheetah and lion populations. Over 500 species of birds have been recorded within the NCA. These include ostrich, white pelican, and greater and lesser flamingo on Lake Magadi within the crater, Lake Ndutu, and in the Empakaai Crater Lake, where a vast bird population can be observed.
Ngorongoro is home to lush green, rain-watered vegetation, as well as desert plants. The area has uncultivated lowland vegetation, arid and semi-arid plant communities, abundant short grass used for grazing, and highland forests.
Scrub heath, grasslands, high open moorland, and the remains of dense evergreen forests cover the steep slopes of the crater, while highland trees including Peacock Flower, Yellow-Wood, Kousso (Hagenia abyssinica), and Sweet Olive can also be found. There are also extensive stretches of pure bamboo on Oldeani Mountain, and Pencil Cedar on Makarut Mountain to the west. Dove- weeds dominate the lower slopes, while the upland woodlands contain Red Thorn Acacia and Gum Acacia that are critical for protecting the watershed.
The crater basin is covered by open short grass plains with fresh and brackish water lakes, marshes, swamps, and two patches of Acacia woodland. The Lerai Forest is home to the Yellow Fever tree and Acacia, while Laiyanai Forest has Pillar Wood and Acacia Lahai. The undulating plains to the west are grass-covered with occasional Umbrella Acacia and Commiphora Africana trees. Blackthorn Acacia and Zebrawood dominate in the drier conditions beside Lake Eyasi. These extensive grasslands and bush are rich, relatively untouched by cultivation, and support very large animal populations.
At the far end of the NCA stands the Olduvai Gorge archaeological site, widely regarded as the cradle of mankind and the most important prehistoric site in the world. It is at Olduvai where remains of Zinjanthropus, the world’s first humans, were discovered by Dr. Louis and Mary Leakey over 50 years ago. The earliest known specimens of the human genus, Homo-habilis, as well as early hominids such as Paranthropus boisei have also been found there. The Olduvai Gorge is a steep-sided ravine in the Great Rift Valley, stretching along eastern Africa. The windswept Olduvai is about thirty miles long, lying within the rain shadow of the Ngorongoro highlands. The gorge is named after oldupaai, the Maasai word for the wild sisal plant.
Millions of years ago, the site comprised of a large lake, the shores of which were covered with successive deposits of volcanic ash. Some 500,000 years ago seismic forces diverted a nearby stream, which began to cut down into the sediments, revealing the seven main layers in the walls of the gorge. Based on fossil evidence found at the Olduvai Gorge, it is believed that various hominid species have been occupying the crater continuously for the past three million years of Ngorongoro’s existence. Native hunters and gatherers who initially lived in the vicinity were replaced by pastoralists a few thousand years ago.
About 450,000 tourists visit Ngorongoro every year, accounting for 60 percent of the average 770,000 tourists visiting Tanzania per annum. Famous visitors include former US President Bill Clinton, the Queen of Denmark Margrethe II, former American Human Rights Activist the Rev Jesse Jackson, Hollywood film star Chris Tucker, John Wayne, Prince William, and the entire delegation attending the 2008 Leon Sullivan Summit which took place in Arusha.
Some scenes from the Oscar-winning Out of Africa and John Wayne’s Hatari were filmed in Ngorongoro.
In addition to the above-mentioned attractions, visitors can also sample cultural tourism or eco-tourism in various Maasai bomas and settlements. Gibbs Farm, located near Karatu along the NCA perimeters, specializes in this. There are also the Enduro River nature trail expeditions, conducted within the Northern Highland Forest Reserve, where visitors can see elephant caves, waterfalls (150 meters high), enjoy bird watching and learn about the local flora.
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