Northern circuit
Arusha Town
The Safari Capital
Arusha is a city in north eastern Tanzania and the capital of the Arusha Region, with a population of 416,442 plus 323,198 in the surrounding Arusha District (2012 census). Located below Mount Meru on the eastern edge of the eastern branch of the Great Rift Valley, Arusha has a temperate climate. The city is close to the Serengeti National Park, the Ngorongoro Conservation Area, Lake Manyara National Park, Olduvai Gorge, Tarangire National Park, Mount Kilimanjaro, and Mount Meru in the Arusha National Park and is thus considered the safari capital of Tanzania.
Arusha National Park
On The Base of Mountain
Arusha National Park covers Mount Meru, a prominent volcano with an elevation of 4566 m, in the Arusha Region of north eastern Tanzania. The park is small but varied with spectacular landscapes in three distinct areas. In the west, the Meru Crater funnels the Jekukumia River; the peak of Mount Meru lies on its rim. Ngurdoto Crater in the south-east is grassland. The shallow alkaline Momella Lakes in the north-east have varying algal colours and are known for their wading birds
Mount Meru is the second highest peak in Tanzania after Mount Kilimanjaro, which is just 60 km away and forms a backdrop to views from the park to the east. Arusha National Park lies on a 300-kilometre axis of Africa's most famous national parks, running from Serengeti and Ngorongoro Crater in the west to Kilimanjaro National Park in the east.
The park is just a few kilometres north east of Arusha, though the main gate is 25 km east of the city. It is also 58 km from Moshi and 35 km from Kilimanjaro International Airport (KIA).
Arusha National Park has a rich variety of wildlife, but visitors shouldn't expect the same game-viewing experience they find in other national parks of Tanzania's northern circuit. Despite the small size of the park, common animals include giraffe, Cape buffalo, zebra, warthog, the black-and-white colobus monkey, the blue monkey, flamingo, elephant, bushbuck and many other African animals. Leopard populations are present, but rarely seen. Birdlife in the forest is prolific, with many forest species more easily seen here than elsewhere on the tourist route - Narina trogon and bar-tailed trogon are both possible highlights for visiting birders, whilst the range of starling species provide somewhat less gaudy interest.
Tarangire National Park
Exceeding Expectations
Tarangire National Park is a national park in Tanzania's Manyara Region. The name of the park originates from the Tarangire River that crosses the park. The Tarangire River is the primary source of fresh water for wild animals in the Tarangire Ecosystem during the annual dry season. The Tarangire Ecosystem is defined by the long-distance migration of wildebeestand zebras. During the dry season thousands of animals concentrate in Tarangire National Park from the surrounding wet-season dispersal and calving areas.
It covers an area of approximately 2,850 square kilometers (1,100 square miles.) The landscape is composed of granitic ridges, river valley, and swamps. Vegetation is a mix of Acaciawoodland, Combretum woodland, seasonally flooded grassland, and baobab trees.
Lake Manyara National Park
Lion Climbing Trees
Lake Manyara National Park is a protected area in Tanzania's Arusha and Manyara Regions, situated between Lake Manyara and the Great Rift Valley. It is administered by the Tanzania National Parks Authority, and covers an area of 325 km2 (125 sq mi) including about 230 km2 (89 sq mi) lake surface. More than 350 bird species have been observed on the lake.
Since the 1920s, Lake Manyara area was used for sports hunting. In 1957, a game reserve was established. In 1960, it was given National Park status and in 1974 about 550 ha (1,400 acres) were added to the southern end. The majority of the land area of the park is a narrow strip running between the Gregory Rift wall to the west and Lake Manyara, an alkaline lake, to the east.The national park only includes the northwest quadrant of the lake, about 200 km2 (77 sq mi). It is part of the much larger Lake Manyara Biosphere Reserve, established in 1981 by UNESCO as part of its Man and the Biosphere Programme.
VegetationThe flora of Lake Manyara National Park is diverse, with over 670 flowering plant and fern species documented. Most are widespread species; there are few rare or endemic species.
The park has a variety of diverse habitats. Rivers flowing off the escarpment and perennial springs below the rift wall support tall, evergreen groundwater forests dominated by Trichilia roka with Broad-Leaved Croton (Croton macrostachyus), sycamore fig (Ficus sycomorus), quinine tree (Rauvolfia caffra) and forest toad-tree (Tabernaemontana ventricosa). Trees are densest in gorges, along the edge of streams and in areas where springs emerge. Growing at the edge of the groundwater forest are dense stands of yellow fever trees (Acacia xanthophloea) and the palm Phoenix reclinata.
Woodlands on the western shore of the lake dominated by Acacia and Commiphora species are also supported by groundwater. Trees are spaced irregularly; densest in zones of seepage and along drainage channels. The dominant tree, Acacia tortilis, grows to about 10m tall with a flat-topped canopy. There is a patchy and diverse understory shrub layer.
Extensive swamps have formed where the Simba River and its tributaries flow into the north end of Lake Manyara and smaller swamps have formed elsewhere, associated with the minor rivers flowing off the walls of the rift valley. A number of aquatic species have been documented, including two species of water lily (Nymphaea caerulea and N.lotus) and extensive mats of water lettuce (Pistia stratiotes). Cattails (Typha sp.) forms pure stands in the northern swamps and various Cyperus species are found around the edges of the swamps. Cyperus immensus forms dense clumps in areas with flooding by fresh water. Cyperus laevigatus is prominent along the lake shore in areas where the alkaline water table is high, in areas of shallow lagoons enclosed behind sand ridges and flanking river deltas.
Grasslands are dominated by Cynodon dactylon in dry locations, or by Sporobolus spicatus, often in association with Sporobolus consimilis on the alkaline lake flats. Sporobolus spicatus is dominant on exposed lakebed and can be very extensive during low lake levels, becoming restricted to a narrow zone above the high water make when lake levels are high. There are extensive areas of Psilolemma jaegeri grasslands outside the park, along the eastern shore of the lake. Vegetation on the escarpment is characterized by Ruellia megachlamys and African baobab trees (Adansonia digitata).
Lake Manyara National Park is known for flocks of thousands flamingos that feed along the edge of the lake in the wet season. In 1991 there were an estimated 1,900,000 non-breeding Lesser Flamingo (Phoeniconaias minor) individuals and 40,000 Greater Flamingo (Phoenicopterus roseus). Great white pelican (Pelecanus onocrotalus) can also be present in large numbers (an estimated 200,000 individuals in 1991) and in all there has been an estimated 1,000,000-2,499,999 individual water birds, however, only 78,320 birds were counted in 1994. The groundwater forest to the north of the lake, and largely within the National Park, is a well-known breeding site for thousands of pink-backed pelican (Pelecanus rufescens) and yellow-billed stork (Mycteria ibis) along with smaller numbers of Marabou stork (Leptoptilos crumeniferus) and grey heron (Ardea cinerea). Over 40 species of birds of prey are documented, including palm-nut vulture (Gypohierax angolensis) and Ayre's hawk eagle (Hieraaetus ayresii). In all, more than 390 species of birds have been documented in the national park, although in the dry season, flamingos and other water birds are usually found only in small numbers.
MammalsPopulation of large migratory mammals that are concentrated primarily in Tarangire National Park, but also move through Lake Manyara National Park include wildebeest, zebra, Thomson's gazelle and Grant's gazelle. Large herds of wildebeest and other plains game from the Mto wa Mbu Game Controlled Area enter the park from the north for short periods. Wildebeest exclusively graze the alkaline grasslands around the lake, and numbers are highest during the dry season, dropping to small resident populations in the wet season. Herbivores of Lake Manyara National Park include zebra, bushbuck, waterbuck, Grant's gazelle, impala, Thomson's gazelle, Cape buffalo, giraffe, hippopotamus, baboon, warthog, and elephant.
Studies in the 1980s found this to be one of the areas with the highest wildlife biomass in Africa, but elephant numbers had fallen by 75% between 1985 and 1991 as a result of illegal hunting, with numbers rebounding to around 200 in 1996. Lake Manyara was also once known for its high population of black rhinoceros,but none were present by 1996. Similarly, reedbuck were present in 1984, but no individuals were found in a 1996 census. Predators of Lake Manyara National Park include lion, leopard, African wild cat, spotted hyena, black-backed jackal, bat-eared fox, serval, honey badger, African civet, genet (Genetta) species and several mongoose species. Cheetah and African golden cat are sighted occasionally.
FishLake Manyara is the type locality for the endangered fish Oreochromis amphimelas, a species of in the cichlid family. It is endemic to Tanzania, and also lives in a few more saline lakes with closed basins. Exploitation is prohibited in the parts of Lake Manyara within the National Park and the protected park areas provide important seed stock for the replenishment of fished populations.
ButterfliesOver 180 species of butterflies have been documented in the park.
Ngorongoro Conservation Area (Crater)
The World Heaven
Ngorongoro Conservation Area is in northern Tanzania. It’s home to the vast, volcanic Ngorongoro Crater and “big 5” game (elephant, lion, leopard, buffalo, rhino). Huge herds of wildebeests and zebras traverse its plains during their annual migration. Livestock belonging to the semi-nomadic Maasai tribe graze alongside wild animals. Hominin fossils found in the Olduvai Gorge date back millions of years.
Ngorongoro conversation area is a protected area and a World Heritage Site located 180 km (110 mi) west of Arusha in the Crater Highlands area of Tanzania. The area is named after Ngorongoro Crater (caldera), a large volcanic caldera within the area. The conservation area is administered by the Ngorongoro Conservation Area Authority, an arm of the Tanzanian government, and its boundaries follow the boundary of the Ngorongoro Division of the Arusha Region.
The 2009 Ngorongoro Wildlife Conservation Act placed new restrictions on human settlement and subsistence farming in the Crater, displacing Maasai pastoralists, most of whom had been relocated to Ngorongoro from their ancestral lands to the north when the British colonial government established Serengeti National Park in 1959.
The name of the crater has an onomatopoeic origin; it was named by the Maasai pastoralists after the sound produced by the cowbell (ngoro ngoro). Based on fossil evidence found at the Olduvai Gorge, various hominid species have occupied the area for 3 million years.
Hunter-gatherers were replaced by pastoralists a few thousand years ago. The Mbulu came to the area about 2,000 years ago and were joined by the Datooga around the year 1700. Both groups were driven from the area by the Maasai in the 1800s.
No Europeans are known to have set foot in the Ngorongoro Crater until 1892, when it was visited by Oscar Baumann. Two German brothers (Adolph and Friedrich Siedentopf) farmed in the crater until the outbreak of World War I, after leasing the land from the administration of German East Africa. The brothers regularly organized shooting parties to entertain their German friends. They also attempted to drive the wildebeest herds out of the crater.
In 1921, the first game preservation ordinance was passed, which restricted hunting to permit holders throughout Tanzania. In 1928, hunting was prohibited on all land within the crater rim, except the former Siedentopf farms. The National Park Ordinance of 1948 (implemented in 1951) created the Serengeti National Park (SNP). This, however, caused problems with the Maasai and other tribes, resulting in the Ngorongoro Conservation Area Ordinance (1959) that separated the conservation area from the national park. Maasai pastoralists living in Serengeti National Park were systematically relocated to Ngorongoro, increasing the population of Maasai and livestock living in the Crater. The Ngorongoro Conservation Area Authority was established by the Game Park Laws (miscellaneous amendments) Act, 1976 and owns the majority of Ngorongoro Conservation Area land, including the Crater. The area became a UNESCO World Heritage Site in 1979.The Wildlife Conservation Act of 2009 further restricted human use of Ngorongoro Crater and created a legal framework to politically disenfranchise and forcibly displace traditional pastoralists.:57–59 The restriction on land use generates tension between the local Maasai communities and conservation authorities. Currently, the International Union for Conservation of Nature (IUCN) is seeking solutions to ease conflict and improve collaborative efforts towards conservation with the locals.
Land in the conservation area is multi-use and unique because it is the only conservation area in Tanzania that protects wildlife while allowing human habitation. Land use is controlled to prevent negative effects on the wildlife population. For example, cultivation is prohibited at all but subsistence levels.
The area is part of the Serengeti ecosystem and, to the northwest, adjoins the SNP and is contiguous with the southern Serengeti plains. These plains also extend to the north into the unprotected Loliondo division and are kept open to wildlife through transhumance pastoralism practiced by the Maasai. The south and west of the area are volcanic highlands, including the famous Ngorongoro Crater and the lesser known Empakaa Crateri. The southern and eastern boundaries are approximately defined by the rim of the East African Rift wall, which also prevents animal migration in these directions.The main feature of the Ngorongoro Conservation Authority is the Ngorongoro Crater, the world's largest inactive, intact and unfilled volcanic caldera. The crater, which formed when a large volcano exploded and collapsed on itself two to three million years ago, is 610 metres (2,000 feet) deep and its floor covers 260 square kilometres (100 square miles).Estimates of the height of the original volcano range from 4,500 to 5,800 metres (14,800 to 19,000 feet) high. The crater floor is 1,800 metres (5,900 feet) above sea level. The crater was voted by Seven Natural Wonders as one of the Seven Natural Wonders of Africa in Arusha, Tanzania in February 2013. The Ngorongoro volcano was active from about 2.45 to 2 million years ago.
The volcanic eruptions like that of Ngorongoro, which resulted in the formation of Ngorongoro Crater in Tanzania, were very common. Similar collapses occurred in the case of Olmoti and Empakaai, but they were much smaller in magnitude and impact.
Out of the two recent volcanoes to the northeast of the Empakaai caldera, Kerimasi and Ol Doinyo Lengai, Doinyo Lengai is still active and had major eruptions in 2007 and 2008. Smaller ash eruptions and lava flows continue to slowly fill the current crater. Its name is Maasai language for ‘Mountain of God.The Munge Stream drains Olmoti Crater to the north, and is the main water source draining into the seasonal salt lake in the center of the crater. This lake is known by two names: Makat as the Maasai called it, meaning salt; and Magadi. The Lerai Stream drains the humid forests to the south of the Crater, and it feeds the Lerai Forest on the crater floor - when there is enough rain, the Lerai drains into Lake Magadi as well. Extraction of water by lodges and Ngorongoro Conservation Area headquarters reduces the amount of water entering Lerai by around 25%.
The other major water source in the crater is the Ngoitokitok Spring, near the eastern crater wall. There is a picnic site here open to tourists and a huge swamp fed by the spring, and the area is inhabited by hippopotamus, elephants, lions and many others. Many other small springs can be found around the crater's floor, and these are important water supplies for the animals and local Maasai, especially during times of drought. Masai were previously permitted to graze their cattle within the crater, but as of 2015 were restricted from doing so.The Ngorongoro Conservation Area has a healthy resident population of most species of wildlife. The Ndutu Lake area to in the west of the conservation area has particularly strong cheetah and lion populations. Common in the area are hartebeest (Alcelaphus buselaphus), spotted hyena (Crocuta crocuta), and jackals. The population of African wild dog may have declined recently.[when? Servals occur widely on the plains to the west of the Ngorongoro Crater.
The annual ungulate migration passes through the Ngorongoro Conservation Area, with 1.7 million wildebeest, 260,000 zebra, and 470,000 gazelles moving south into the area in December and moving north in June. This movement changes seasonally with the rains, but the migration traverses almost the entire plains in search of food.Approximately 25,000 large animals, mostly ungulates, live in the crater. Large mammals in the crater include the black rhinoceros (Diceros bicornis michaeli), the local population of which declined from about 108 in 1964-66 to between 11–14 in 1995, the African buffalo or Cape buffalo (Syncerus caffer), and the hippopotamus (Hippopotamus amphibius). There also are many other ungulates: the blue wildebeest (Connochaetes taurinus) (7,000 estimated in 1994), Grant's zebra (Equus quagga boehmi) (4,000), the common eland (Taurotragus oryx), and Grant's (Nanger granti) and Thomson's gazelles (Eudorcas thomsonii) (3,000). Waterbucks (Kobus ellipsiprymnus) occur mainly near Lerai Forest.
Absent are giraffe, impala (Aepyceros melampus), topi (Damaliscus lunatus), oribi (Ourebia oribi), crocodile (Crocodylus niloticus).
Cheetah (Acinonyx jubatus raineyi), East African wild dog (Lycaon pictus lupinus), and African leopard (Panthera pardus pardus) are rarely seen. Spotted hyenas (Crocuta crocuta) have been the subject of a long-term research study in the Ngorongoro Conservation Area since 1996.
Although thought of as "a natural enclosure" for a very wide variety of wildlife, 20 percent or more of the wildebeest and half the zebra populations vacate the crater in the wet season, while Cape buffalo (Syncerus caffer) stay; their highest numbers are during the rainy season.
Since 1986, the crater's wildebeest population has fallen from 14,677 to 7,250 (2003-2005). The numbers of eland and Thomson's gazelle also have declined while the buffalo population has increased greatly, probably due to the long prevention of fire which favors high-fibrous grasses over shorter, less fibrous types.
Serval (Leptailurus serval) occurs widely in the crater.
Lake Magadi, a large lake in the southwest of the crater, is often inhabited by thousands of mainly lesser flamingoes.The crater has one of the densest known population of lions, numbering 62 in 2001.
A side effect of the crater being a natural enclosure is that the lion population is significantly inbred. This is due to the very small amount of new bloodlines that enter the local gene pool, as very few migrating male lions enter the crater from the outside. Those who do enter the crater are often prevented from contributing to the gene pool by the crater's male lions, who expel any outside competitors.
Long-term data imply that lions in the crater were struck by four deadly disease outbreaks between 1962 and 2002. Drought in 1961 and rains throughout the 1962 dry season caused a massive build-up of blood-sucking stable flies (Stomoxys calcitrans) by May 1962. They drained blood and caused painful skin sores that became infected, causing lion numbers to crash from 75-100 to 12. The population recovered to around 100 by 1975 and remained stable until 1983, when a persistent decline began. Numbers have generally remained below 60 animals since 1993, reaching a low of 29 in 1998. In 2001, 34 percent of the lion population died between January and April from a combination of tick-borne disease and canine distemper.
The lion population is also influenced to some extent by the takeover of prides by incoming males, which typically kill small cubs. The biggest influence, however, appears to be disease, particularly canine distemper.Come and explore the world heaven.
Serengeti National Park
The Endless Plain
The Serengeti National Park is a Tanzanian national park in the Serengeti ecosystem in the Mara and Simiyu regions. It is famous and well known for its annual migration of over 1.5 million white-bearded (or brindled) wildebeest and 250,000 zebra and for its numerous Nile crocodile and honey badger.
The Maasai people had been grazing their livestock in the open plains of eastern Mara Region, which they named "endless plains," for around 200 years when the first European explorer, Austrian Oscar Baumann, visited the area in 1892.The name "Serengeti" is an approximation of the word used by the Maasai to describe the area, siringet, which means "the place where the land runs on forever".
The first American to enter the Serengeti, Stewart Edward White, recorded his explorations in the northern Serengeti in 1913. He returned to the Serengeti in the 1920s and camped in the area around Seronera for three months. During this time, he and his companions shot 50 lions.
Because the hunting of lions made them scarce, the British colonial administration made a partial game reserve of 800 acres (3.2 km2) in the area in 1921 and a full one in 1929. These actions were the basis for Serengeti National Park, which was established in 1951.
The Serengeti gained more fame after the initial work of Bernhard Grzimek and his son Michael in the 1950s. Together, they produced the book and film Serengeti Shall Not Die, widely recognized as one of the most important early pieces of nature conservation documentary.
To preserve wildlife, the British evicted the resident Maasai from the park in 1959 and moved them to the Ngorongoro Conservation Area. There is still considerable controversy surrounding this move, with claims made of coercion and deceit on the part of the colonial authorities.
The park is Tanzania's oldest national park and remains the flagship of the country's tourism industry, providing a major draw to the Northern Safari Circuit encompassing Lake Manyara National Park, Tarangire National Park, Arusha National Park and the Ngorongoro Conservation Area. It has over 2,500 lions and more than 1 million wildebeest.The park is worldwide known for its abundance of wildlife and high biodiversity.
The migratory - and some resident - wildebeest, which number over 1.5 million individuals, constitute the largest population of big mammals that still roam the planet. They are joined in their journey through the Serengeti-Mara ecosystem by 200,000 plains zebras, 300,000 Thomson's gazelles and Grant's gazelle, and tens of thousands of topi and Coke's hartebeest. Masai giraffe, waterbuck, impala, common warthog and hippopotamus are also abundant. Some rarely seen species of antelope are also present in Serengeti National Park, such as common eland, klipspringer, roan antelope, bushbuck, lesser kudu, fringe-eared oryx and dik dik.
Perhaps the most popular animals among tourists are the Big Five, which include:
Lion: the Serengeti is believed to hold the largest population of lions in Africa due in part to the abundance of prey species. More than 3,000 lions live in this ecosystem.African leopard: these reclusive predators are commonly seen in the Seronera region but are present throughout the national park with the population at around 1,000.African bush elephant: the herds have recovered successfully from population lows in the 1980s caused by poaching, numbering over 5,000 individuals,and are particularly numerous in the northern region of the park.Eastern black rhinoceros: mainly found around the kopjes in the centre of the park, very few individuals remain due to rampant poaching. Individuals from the Masai Mara Reserve cross the park border and enter Serengeti from the northern section at times. There's currently a small but stable population of 31 individuals left in the park.Cape buffalo: the most numerous of the Big Five, with around 53,000 individuals inside the park.Carnivores -aside from the Big Five- include the 225 cheetah which is widely seen due to the abundance of gazelle -, about 3,500 spotted hyena, two species of jackals, African golden wolf, honey badger, striped hyena, serval, seven species of mongooses, two species of otters and the East African wild dog of 300 individuals, which recently reintroduced (locally extinct since 1991).Apart from the safari staples, primates such as yellow and olive baboons and vervet monkey, black-and-white colobus are also seen in the gallery forests of the Grumeti River.
Other mammals include aardvark, aardwolf, bat-eared fox, ground pangolin, crested porcupine, three species of hyraxes and cape hare.
Serengeti National Park has also great ornithological interest, boasting about more than 500 bird species,including Masai ostrich, secretarybird, kori bustards, helmeted guineafowls, Grey-breasted spurfowl, southern ground hornbill, crowned cranes, marabou storks, yellow-billed stork, lesser flamingo, martial eagles, lovebirds, oxpeckers, and many species of vultures.
Reptiles in Serengeti National Park include Nile crocodile, leopard tortoise, serrated hinged terrapin, rainbow agama, Nile monitor, chameleons, African python, black mamba,black-necked spitting cobra, puff adder.
Since 2005, the protected area is considered a Lion Conservation Unit together with Maasai Mara National Reserve and a lion stronghold in East Africa
Southern Circuit
Travel Made Easy
Saadani National Park
Wildlife meets the ocean
Saadani National Park is Tanzania's 13th National Park. Tourists can view animals basking along the Indian Ocean shores. It has an area of 1062 km2 and was officially gazetted in 2005, from a game reserve which had existed from 1969. It is the only wildlife sanctuary in Tanzania bordering the sea.Gazetted in 2005, it encompasses a preserved ecosystem including the former Saadani game reserve, the former Mkwaja ranch area, the Wami River as well as the Zaraninge Forest. In the late 1960s Saadani Village – the village after which the park has been named – and particularly its sub-village Uvinje, invited the Tanzania Wildlife Division (WD) to help them to prevent the indiscriminate killing of wildlife prevalent in the area. From this partnership Saadani village and the Wildlife Division established the Saadani Game Reserve (SGR), with the agreement to respect the land rights of the coastal sub-villages of Saadani, including Uvinje and Porokanya sub-villages, while also addressing the needs of wildlife.
As such, conservation interventions in the Saadani landscape have taken place since the mid-1960s and have been supported by villagers traditionally inhabiting the Saadani landscape, but it is only recently that state-managed conservation has become a growing concern among the villages adjacent to the park.
In the late 1990s, Mr. Domician Njao, from Tanzania National Parks Authority (TANAPA) came in to "upgrade" the reserve to a National Park, and create the first and only coastal national park of Tanzania. In doing so, park authorities redrew the boundaries of the reserve to include Uvinje’s and Porokanya’s prime coastal lands as if they have always been a part of the reserve [in so doing changing the agreement with those villagers. Compelling research shows how after this TANAPA proceeded to gazette most of Saadani’s coastal lands as part of the Saadani National Park in 2005, arguing that they have always being a part of the former reserve and belonged to the Park. Spatial analysis on the area of the former Saadani Game reserve, illustrates TANAPA's strategy to gazette Saadani's prime coastal lands as if they have always been a part of the SGR (See various maps of the SGR)The total extent of SGR is said to have been approximately 209 km², however, the SGR official gazette document states that it comprised approximately 300 km², while some of TANAPA’s official documents indicate it was 260 km² . Spatial analysis conducted as part of the present research suggest that the total game reserve area was of about 200Km2
The vagueness of the language used in the reserve’s official gazette, but also TANAPA’s early interventions to develop its own map of the reserve, and its interests in Saadani’s sub-villages’ prime coastal lands have come to challenge Saadani’s coastal sub-villages’ rights to lawfully inhabit their traditional territories, and have led to chronic political and other battles to demand presently gazetted park lands rescinded, the reestablishment of land rights to traditional inhabitants, and to demand from TANAPA to honour commitments made earlier by Wildlife Division.Saadani wildlife population is increasing during recent years after it has been gazetted as a National Park and was a hunting block beforehand. Wildlife in Saadani includes four of the Big Five, namely lions, African bush elephants, Cape buffaloes and leopards. Masai giraffes, Lichtenstein's hartebeest, waterbucks, blue wildebeests, bohor reedbucks, common and red duikers, Dik-Diks, yellow baboons, vervet monkeys, blue monkeys, Colobus monkeys, mongooses, genets, porcupines, sable antelopes, warthogs, hippopotamuses, crocodiles, nile monitors are also found in the park.
Since 2005, the protected area is considered a Lion Conservation Unit.
Ruaha National Park
The Largest Park in East Africa
Ruaha National Park is a national park in Tanzania. The addition of the Usangu Game Reserve and other important wetlands to the park in 2008 increased its size to about 20,226 km2 (7,809 sq mi), making it the largest protected area in Tanzania and East Africa.
The park is about 130 kilometres (81 mi) west of Iringa. The park is a part of the 45,000 square kilometres (17,000 sq mi) Rungwa-Kizigo-Muhesi ecosystem, which includes the Rungwa Game Reserve, the Kizigo and Muhesi Game Reserves, and the Mbomipa Wildlife Management Area.
The name of the park is derived from the Great Ruaha River, which flows along its southeastern margin and is the focus for game-viewing. The park can be reached by car on a dirt road from Iringa and there are two airstrips – Msembe airstrip at Msembe (park headquarters), and Jongomeru Airstrip, near the Jongomeru Ranger Post.Germany gazetted the Saba Game Reserve in 1910. British colonial authorities changed the name to the Rungwa Game Reserve in 1946. In 1964, the southern portion of the reserve was excised and elevated to full park status.
More than 571 species of birds have been identified in the park. Among the resident species are hornbills.Many migratory birds visit the park.
Other noted animals found in this park are East African cheetah and lion, African leopard and wild dog, spotted hyena, giraffe, hippopotamus, African buffalo, and sable antelope.
Since 2005, the protected area is considered a Lion Conservation Unit.
Mikumi National Park
The Wildlife Circuit
The Mikumi belongs to the circuit of the wildlife parks of Tanzania, less visited by international tourists and better protected from the environmental point of view. Most of the routes that cross the Mikumi proceed in the direction of the Ruaha National Park and the Selous. The recommended season for visiting the park is the dry season between May and November, warm weather and beautiful sites that are a once-in-a-lifetime experience.
Mikumi National Park borders Selous Game Reserve on the south, the two areas forming a unique ecosystem. Two other natural areas bordering the national park are the Udzungwa Mountains and Uluguru Mountains. Malundwe Mountain is within the park, the highest of a belt of hills that run east and west through the park, connecting the Uluguru Mountains to the northeast with the Uvidunda and Udzungwa mountains to the west. Malundwe Mountain consists of three peaks along a ridge running north and south. Malundwe's south peak is the highest point in the park, reaching 1290 meters elevation.
The landscape of Mikumi is often compared to that of the Serengeti. The road that crosses the park divides it into two areas with partially distinct environments. The area north-west is characterized by the alluvial plain of the river basin Mkata. The vegetation of this area consists of savannah dotted with acacia, baobab, tamarinds, and some rare palm. In this area, at the furthest from the road, there are spectacular rock formations of the mountains Rubeho and Uluguru. The southeast part of the park is less rich in wildlife, and not very accessible.
The fauna includes many species characteristic of the African savannah. According to local guides at Mikumi, chances of seeing a lion who climbs a tree trunk is larger than in Manyara (famous for being one of the few places where the lions exhibit this behavior). The park contains a subspecies of giraffe that biologists consider the link between the Masai giraffe and the reticulated or Somali giraffe. Other animals in the park are elephants, zebras, impala, eland, kudu, black antelope, baboons, wildebeests and buffaloes. At about 5 km from the north of the park, there are two artificial pools inhabited by hippos. More than 400 different species of birds also inhabit the park.The Mikumi belongs to the circuit of the wildlife parks of Tanzania, less visited by international tourists and better protected from the environmental point of view. Most of the routes that cross the Mikumi proceed in the direction of the Ruaha National Park and the Selous. The recommended season for visiting the park is the dry season between May and November, warm weather and beautiful sites that are a once-in-a-lifetime experience.
Selous Game Reserve
The World Heritage Site
The Selous Game Reserve is a protected area in southern Tanzania. It covers a total area of 50,000 km2 (19,000 sq mi) and has additional buffer zones. It was designated a UNESCO World Heritage Site in 1982 due to its wildlife diversity and undisturbed nature. Some of the typical wildlife of the miombo inhabits the reserve, such as African bush elephant, black rhino, hippopotamus, lion, East African wild dog, Cape buffaloes, Masai giraffe, Plains zebra, and Nile crocodile. Permanent human habitation is not permitted within the reserve. All human entry and exit is controlled by the Wildlife Division of the Tanzanian Ministry of Natural Resources and Tourism.
The area was first designated a protected area in 1896 by the German Governor of Tanganyika Hermann von Wissmann, and became a hunting reserve in 1905. The reserve was named after Frederick Selous, a famous big game hunter and early conservationist, who died at Beho Beho in this territory in 1917 while fighting against the Germans during World War I. Scottish explorer and cartographer Keith Johnston had died at Beho Beho in 1879 while leading a Royal Geographical Society expedition to the Great Lakes of Africa with Joseph Thomson.
Since 2005, the protected area is considered a Lion Conservation Unit.
A boundary change to allow the use of uranium deposits has been approved. The approval for the boundary change was given by the UNESCO and seriously criticized by environmentalists and organizations e.g., Uranium-Network and Rainforest Rescue.
Tanzania president John Magufuli has given an approval of constructing a new Stiegler's Gorge Hydroelectric Power Station of 2,115MW over the Rufiji River.The power station will result to an additional 2,100 megawatts of electricity, more than tripling Tanzania's installed hydropower capacity of 562 megawatts.The project started on 26 July 2019 and should be completed by 2022. The International Union for Conservation of Nature (IUCN) has criticised the Government of Tanzania for failing to consider, the impact of the flooding of nearly 1,000 km2 will have, on both the people and biodiversity of the reserve. Thousands of people are dependent on the river for fishing and agriculture.
Interesting places in the park include the Rufiji River, which flows into the Indian Ocean opposite Mafia Island and the Stiegler Gorge, a canyon of 100 metres depth and 100 metres width. Habitats include grassland, typical Acacia savanna, wetlands and extensive Miombo woodlands. Although total wildlife populations are high, the reserve is large and densities of animals are lower than in the more regularly visited northern tourist circuit of Tanzania. In 1976, the Selous Game Reserve contained about 109,000 elephants, then the largest population in the world. By 2013, the numbers had dropped to about 13,000 – including a 66% drop from 2009 to 2013. Sources blame corrupt politicians, officials and businessmen who help poachers.
Most of the reserve remains set aside for game hunting through a number of privately leased hunting concessions, but a section of the northern park along the Rufiji River has been designated a photographic zone and is a popular tourist destination. There are several high end lodges and camps mainly situated along the river and lake systems in this area. Rather difficult road access means most visitors arrive by small aircraft from Dar es Salaam, though train access is also possible. Walking safaris are permitted in the Selous, and boat trips on the Rufiji are a popular activity.
Udzungwa Mountain National Park
The Largest Biodiversity
Udzungwa Mountains National Park is a national park in Tanzania with a size of 1,990 km2 (770 miles2). The habitats contained within the national park include tropical rainforest, mountain forest, miombo woodland, grassland and steppe. There is a vertical height range of 250–2,576 metres (the peak of Lohomero), which incorporates the Udzungwa Mountains part of the Eastern Arc Mountains. There are more than 400 bird species, 2500 plant species (25% of which are endemics) and 6 primate species. It has the second largest biodiversity of a national park in Africa.
Six primate species have been recorded in the park, five of which are endemic. The Iringa red colobus and Sanje crested mangabey are only found in the Udzungwa Mountains National Park, the mangabey species was undetected by biologists prior to 1979.
Tourism in the Udzungwa Mountains national Park revolves around hiking and trekking, as the park has no roads and is accessible only on foot. The hiking trails range in difficulty from the short one-hour Sonjo trek to the extremely challenging 6-day camping trek the Lumemo Trail. The most common walk is the Sanje Waterfalls trail which takes approximately four hours to complete and allows the visitor access to the stunning 170 m waterfall and includes swimming in the waterfall plunge pools as part of the activity.
Accommodation for visitors within the park is only possible on a camping basis as there are no lodges within the park borders. Within the nearby village of Mang'ula there are also a couple of local guesthouses providing a budget option.
Mountain Climbing
Get to the Top with us
Kilimanjaro Mountain
The Roof of Africa
Mount Kilimanjaro is a dormant volcano in Tanzania. It has 3 volcanic cones: Kibo, Mawenzi and Shira. It is the highest mountain in Africa and the highest single free-standing mountain in the world: 5,895 metres (19,341 ft) above sea level and about 4,900 metres (16,100 ft) above its plateau base.Kilimanjaro is the 4th most topographically prominent peak on Earth. The first people known to have reached the summit were Hans Meyer and Ludwig Purtscheller, in 1889. It is part of Kilimanjaro National Park and is a major climbing destination. Because of its shrinking glaciers and disappearing ice fields, it has been the subject of many scientific studies.
The origin of the name Kilimanjaro is not known, but a number of theories exist. European explorers had adopted the name by 1860 and reported that Kilimanjaro was the mountain's Kiswahili name.The 1907 edition of The Nuttall Encyclopædia also records the name of the mountain as Kilima-Njaro.
Johann Ludwig Krapf wrote in 1860 that Swahilis along the coast called the mountain Kilimanjaro. Although he did not offer any support, he claimed that Kilimanjaro meant either mountain of greatness or mountain of caravans. Under the latter meaning, kilima meant mountain and jaro meant caravans.Jim Thompson claimed in 1885, again without support, that the term Kilima-Njaro "has generally been understood to mean" the mountain (kilima) of greatness (njaro). He also suggested "though not improbably it may mean" the white mountain.
Njaro is an ancient Kiswahili word for shining.Similarly, Krapf wrote that a chief of the Wakamba people, whom he visited in 1849, "had been to Jagga and had seen the Kima jajeu, mountain of whiteness, the name given by the Wakamba to Kilimanjaro....More correctly in the Kikamba language this would be kiima kyeu, and this possible derivation has been popular with several investigators.
Others have assumed that kilima is Kiswahili for mountain. The problem with this assumption is that kilima actually means hill and is, therefore, the diminutive of mlima, the proper Kiswahili word for mountain. However, It is ... possible ... that an early European visitor, whose knowledge of [Kiswahili] was not extensive, changed mlima to kilima by analogy with the two Wachagga names: Kibo and Kimawenzi. A different approach is to assume that the kileman part of Kilimanjaro comes from the Kichagga kileme, which means that which defeats, or kilelema, which means that which has become difficult or impossible. The jaro part would "then be derived from njaare, a bird; or, according to other informants, a leopard; or, possibly from jyaro, a caravan". Considering that the name Kilimanjaro has never been current among the Wachagga people, it is possible that the name was derived from Wachagga saying that the mountain was unclimbable, kilemanjaare or kilemajyaro, and porters misinterpreting this as being the name of the mountain.
In the 1880s, the mountain became a part of German East Africa and was called Kilima-Ndscharo in German following the Kiswahili name components.On 6 October 1889, Hans Meyer reached the highest summit on the crater ridge of Kibo. He named it Kaiser-Wilhelm-Spitze (Kaiser Wilhelm peak).That name was used until Tanzania was formed in 1964,when the summit was renamed Uhuru Peak, meaning freedom peak in Kiswahili.
Meru Mountain
A Dormant Stratovolcano
Mount Meru is a dormant stratovolcano located 70 kilometres (43 mi) west of Mount Kilimanjaro in the country of Tanzania. At a height of 4,562.13 metres (14,968 ft), it is visible from Mount Kilimanjaro on a clear day, and is the fifth-highest of the highest mountain peaks of Africa, dependent on definition.
Mount Meru is located just north of the city of Arusha, in the Arusha Region of Tanzania. It is the second-highest mountain in Tanzania, after Mount Kilimanjaro. The Momella route – which starts at Momella gate, on the eastern side of the mountain – is used to climb Mount Meru.
Much of its bulk was lost about 7,800 years ago due to a summit collapse. Mount Meru most recently had a minor eruption in 1910. The several small cones and craters seen in the vicinity probably reflect numerous episodes of volcanic activity. Mount Meru's caldera is 2.2 miles (3.5 km) wide.
Mount Meru is the topographic centerpiece of Arusha National Park. Its fertile slopes rise above the surrounding savanna and support a forest that hosts diverse wildlife, including nearly 400 species of birds, and also monkeys and leopards.
Oldonyo Lengai Mountain
The Mountain of God
Ol Doinyo Lengai (Oldoinyo Lengai), "Mountain of God" in the Maasai language is an active volcano located in the Gregory Rift, south of Lake Natron within the Arusha Region of Tanzania, Africa. Part of the volcanic system of the East African Rift, it uniquely produces natrocarbonatite lava. The 1960 eruption of Ol Doinyo Lengai led to geological investigations that finally confirmed the view that carbonatite rock is derived from magma.
Ol Doinyo Lengai is unique among active volcanoes in that it produces natrocarbonatite lava, a unique occurrence of volcanic carbonatite. A few older extinct carbonatite volcanoes are located nearby, including Homa Mountain.
LavaWhere as most lavas are rich in silicate minerals, the lava of Ol Doinyo Lengai is a carbonatite. It is rich in the rare sodium and potassium carbonates, nyerereite and gregoryite. Due to this unusual composition, the lava erupts at relatively low temperatures of approximately 510 °C (950 °F). This temperature is so low that the molten lava appears black in sunlight, rather than having the red glow common to most lavas. It is also much more fluid than silicate lavas, often less viscous than water. The sodium and potassium carbonate minerals of the lavas erupted at Ol Doinyo Lengai are unstable at the Earth's surface and susceptible to rapid weathering, quickly turning from black to grey in colour. The resulting volcanic landscape is different from any other in the world.
The carbonatite ash spread over the surrounding grasslands leads to a uniquely succulent, enriched pasture. This makes the area a vital stage on the annual wildebeest migration, where it becomes the nursery for the birth of several thousand calves.
Eruptive activity1883-1915EditThe record of eruptions on the mountain dates to 1883. Flows were recorded between 1904 and 1910 and between 1913 and 1915.1917 A major eruption in June 1917 deposited volcanic ash up to 48 kilometres (30 mi) away.1926 An eruption took place for several months in 1926.
1940 An eruption between July and December 1940 deposited ash as far as Loliondo, 100 kilometres (62 mi) away.
1950s Several minor eruptions of lava were observed in 1954, 1955, and 1958.
1960s Minor eruptions of lava were observed in the early 1960s.
A major eruption occurred on 14 August 1966. Geologists J. B. Dawson and G. C. Clark visited the crater a week later and reported seeing "a thick column of black ash" that rose for approximately 1,000 metres (3,000 ft) above the volcano and drifted away northwards towards Lake Natron. When they climbed the cone-shaped vent, they reported seeing a continuous discharge of gas and whitish-grey ash and dust from the centre of the pit.
2007 Volcanic activity in the mountain caused daily earth tremors in Kenya and Tanzania from 12 July 2007 until 18 July 2007 at 8.30pm in Nairobi. The strongest tremor measured 6.0 on the Richter scale. Geologists suspected that the sudden increase of tremors was indicative of the movement of magma through the Ol Doinyo Lengai. The volcano erupted on 4 September 2007, sending a plume of ash and steam at least 18 kilometres (11 mi) downwind and covering the north and west flanks in fresh lava flows.
2008 The 2007 eruption continued intermittently into 2008. At the end of February it was reported to be gathering strength, with a major outburst taking place on 5 March. Periods of inactivity were followed by eruptions on 8 and 17 April. Eruptive activity continued until late August 2008. A visit to the summit in September 2008 discovered that lava emission had resumed from two vents in the floor of the new crater. Visits to the crater in March/April 2009 showed that this activity appeared to have ceased.
2010 In October 2010, two separate lava flows and a small lava lake were photographed in an overflight.
2013 The volcano resumed natrocarbonatite lava flow which started to fill the large crater from the 2007-2008 eruption. As of July 2013, there is a large active hornito on the western edge of the crater floor. During June, residents near the volcano reported several earthquakes. The new crater is inaccessible and climbers have only occasionally glimpsed into it.