Thursday 23 July 2009

11th July..Bye bye Tanzania, Naipenda Tanzania

We left Tarangire in the morning heading back to Arusha.


Laizer, Patricia, Paloma and Martin































From there I had to catch the bus shuttle to Nairobi (around 6 hours) to get my flight back to London late that evening.

It felt weird to leave Arusha...I had only spent there less than 2 weeks of my life but or some strange reason I felt like if I belonged there.
I had the pleasure to admire the views of the Kili from the bus...wow, I had been there!! it was like a dream!

Kilimanjaro seen from Arusha!




Pics taken from the bus












































It was quite chaotic at the border as you can see

















To be able to describe Africa's sunset...you have to be there



10th July, Tarangire

Tarangire National Park is a national park in Tanzania.

Tarangire NP is a quiet, seasonal park with wide views to distant volcanic mountain ranges. Tarangire covers 2600 sq km of grassland and floodplains, and a large proportion of tall acacia woodland just south of the open grass plains of southern Maasailand.

Tarangire National Park is the sixth largest national park after Ruaha, Serengeti, Mikumi, Katavi and Mkomazi. The name of the park originates from the river which crosses at the middle of the park, the river is the only source of water for wild animals during dry seasons. The park is famous for its huge number of elephants, baobab trees and tree climbing African pythons.



Sunset with a baoba tree













It lies a little distance to the south east of Lake Manyara and covers an area of approximately 2,850 square kilometres. It is named after the Tarangire River that flows through the park.

Tarangire has regions of quite dense bush, but with high grasses and huge old baobab trees instead of the green forests of Manyara.


The land is hilly and dominated by the impressive valley of the Tarangire River, which attracts good numbers of migrant animals during the dry months, especially between July and September.

During the dry months the concentration of animals around the Tarangire river is almost as diverse and reliable as in the Ngorongoro Crater, but the ecosystem here is balanced by a localised migration pattern that is followed by most animals other than lion, who don't tend to abandon their territory.

There are a fantastic number of colourful birds swooping and strutting along the rough paths throughout the year, with likely spots including the Paradise Whyder and endearing Yellow-collared lovebirds. There are a few resident lion, which are easier to spot when the migration arrives to excite their taste buds. In other months they look quite mean and lean and slip easily between the lengthening grasses.

The animals mostly disperse during April and May, when there is widespread greenery, vegetation and standing water to encourage all the grazers further afield.


Hienas




Wildebeests





In June, the eland and oryxes begin to return, followed by elephant towards the end of the month. Tarangire is a great spot for elephant gatherings at the end of the rainy season in June, and zebra and wildebeest return together through July.


Family of elephants




















By mid-August all the animals are congregating around their last reliable water source, the Tarangire River.
The calving season falls in the early months of the year, through January, February and March, and so makes the most of the fresh grass during the rainy season.

Male ostrich Giraffes


As Laizer described it, the monkey with 'its stuff " blue

Giraffes







Elephants and female ostrich



Climbing lion








Zebras and giraffes







Male elephant










We stopped on the route a couple of times and during one

I took this pic with some Maasai women

and their children.

9th July Ngorongoro crater


The Ngorongoro Conservation Area or NCA is a conservation area situated 180 km (112 miles) west of Arusha in the Crater Highlands area of Tanzania. 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 Ngorongoro District. It covers an area of 8,288 km² (3,200 square miles) - about the size of Crete.

Based on fossil evidence found at the Olduvai Gorge, it is known that various hominid species have occupied the area for 3 million years. Hunter gatherers were replaced by pastorialists a few thousand years ago. The Mbulu[1] 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. Massive fig trees in the northwest of the Lerai Forest are sacred to the Maasai and Datooga people. Some of them may have been planted on the grave of a Datago leader who died in battlewith the Maasai around 1840.

No Europeans are known to have set foot in the Crater until 1892, when it was visited by Dr. Oscar Baumann. Two German brothers farmed in the Crater until the outbreak of World War I, after leasing the land from the German colonial administration then in control of East Africa. Dr. Baumann shot three rhinos while camped in the crater, and the German brothers regularly organized shooting parties to entertain their German friends. They also attempted to drive the wildebeest herds out of the crater.

The Ngorongoro area originally was part of the Serengeti National Park when it was created by the British in 1951. Maasai continued to live in the newly created park until 1959, when repeated conflicts with park authorities over land use led the British to evict them to the newly declared Ngorongoro Conservation Area.

The Ngorongoro Conservation Area Authority is the governing body regulating use and access to the NCA. The area became a UNESCO World Heritage Site in 1979.

Land in the conservation area is multi-use, it is unique in Tanzania as the only conservation area providing protection status for w

ildlife whilst 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 north-west, it adjoins the Serengeti National Park and is contiguous with the southern Serengeti plains, these plains also extend to the north into unprotected Loliondo division and are kept open to wildlife through trans-human pastoralism practiced by Maasai. The south and west of the area are volcanic highlands, including the famous Ngorongoro Crater and the lesser known Empakai. The southern and eastern boundaries are approximately defined by the rim of the Great Rift Valley wall, which also prevents animal migration in these directions.

The annual ungulate migration passes through the NCA, with wildebeest and zebra moving south into the area in December and moving north in June. This movement changes seasonally with the rains, but the migration will traverse almost the entire plains in search of food. The NCA has a healthy resident population of most species of wildlife, in particular the Ndutu Lake area to the west has strong cheetah and lion populations.

A population of approximately 25,000 large animals, largely ungulates along with reputedly the highest density of mammalian predators in Africa, lives in the crater.


These include the black rhinoceros, whose local population declined from about 108 in 1964-66 to between 11-14 in 1995,










and the hippopotamus, which is very uncommon in the area. There also are many other ungulates: the wildebeest (7,000 estimated in 1994), the zebra (4,000), the eland, and Grant's and Thomson's gazelles (3,000).


The crater has the densest known population of lions, numbering 62 in 2001. On the crater rim are leopards, elephants - numbering 42 in 1987 but only 29 in 1992 - mountain reedbuck, and buffalo (4,000 in 1994).

However, since the 1980s the crater's wildebeest population has fallen by a quarter to about 19,000 and 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.

In summer, enormous numbers of Serengeti migrants pass through the plains of the reserve, including 1.7 million wildebeest, 260,000 zebra, and 470,000 gazelles. Waterbuck occur mainly near Lerai Forest; servals occur widely in the crater and on the plains to the west. Common in the reserve are lions, hartebeest, spotted hyenas and jackals. Cheetahs, although common in the reserve, are scarce in the crater itself. The African Wild Dog has recently disappeared from the crater and may have declined elsewhere in the Conservation Area as well, as well as throughout Tanzania according to C. Michael Hogan.

The main feature of the NCA is the Ngorongoro Crater, which is the world's largest unbroken, unflooded volcanic caldera. The Crater, which formed when a giant volcano exploded and collapsed on itself some two to three million years ago, is 610 m (2,001 ft) deep and its floor covers 260 km² (102 square miles). Estimates of the height of the original volcano range from fifteen to nineteen thousand feet (4500 to 5800 metres) high.

Although thought of as "a natural enclosure" for a very wide variety of wildlife, up to 20% or more of the wildebeest (Connochaetes taurinus) and half the zebra (Equus burchelli) populations vacate the Crater in the wet season. However, an effect of this 'enclosure' situation means that the population of Ngorongoro lions is severely inbred, with many genetic problems passed from generation to generation. This is due to the very small amount of new bloodlines that enter the local gene pool, with very few migrating male lions entering the crater from the outside. Animal populations in the crater include most of the species found in East Africa, but there are no impalas (Aepyceros melampus), topis (Damaliscus lunatus), oribis (Ourebia oribi), giraffes (Giraffa camelopardalis), or crocodiles (Crocodylus niloticus).

The crater highlands on the side facing the easterly trade winds receives 800–1200mm of rain a year and is covered largely in montane forest, while the less-steep west wall receives only 400–600 mm; this side is grassland and bushland dotted with Euphorbia bussei trees. The crater floor is mostly open grassland with two small wooded areas dominated by Acacia xanthophloea.

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 NCA headquarters reduces the amount of water entering Lerai by around 25%.
he 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 floor, and these are important water supplies for the animals and local Masaai, especially during times of drought.

Aside from herds of zebra, gazelle, and wildebeest, the crater is home to the "big five" of rhinoceros, lion, leopard, elephant, and buffalo. The crater plays host to almost every individual species of wildlife in East Africa, with an estimated 25,000 animals within the crater.

Following the recommendations of the ad hoc committee of scientists convened after the 2000 drought, an ecological burning program was implemented in the Crater, which entails annual or biannual controlled burns of up to 20% of the grasslands.Maasai are now permitted to graze their cattle within in the Crater, but must enter and exit daily.

8th July en route to Ngorongoro

In the morning we drove to Olduvai Gorge

The Olduvai Gorge or Oldupai Gorge is commonly referred to as "The Cradle of Mankind." It is a steep-sided ravine in the Great Rift Valley, which stretches along eastern Africa. Olduvai is in the eastern Serengeti Plains in northern Tanzania and is about 30 miles (48 km) long. The gorge is named after the Maasai word for the wild sisal plant Sansevieria ehrenbergii, commonly called Oldupaai.

Olduvai Gorge is one of the most important prehistoric sites in the world and has been instrumental in furthering understanding of early human evolution. Excavation work there was pioneered by Louis and Mary Leakey in the 1950s and continued into the twenty first century by Professor Fidelis Masao of the Open University of Tanzania supported by Earthwatch; there have also been teams from Rutgers University. Millions of years ago, the site was that of a large lake, the shores of which were covered with successive deposits of volcanic ash. Around 500,000 years ago seismic activity diverted a nearby stream which began to cut down into the sediments, revealing seven main layers in the walls of the gorge. The geology of Olduvai Gorge and the surrounding region was studied in detail by Richard L. Hay, who worked at the site between 1961 and 2002.

The stratigraphy is extremely deep and layers of volcanic ash and stones allow radiometric dating of the embedded artifacts, mostly through potassium-argon dating and Argon–argon dating. The base of the Olduvai sediments dates to slightly older than 2 million years, [2] with the first artifacts (pebble tools and choppers) appearing slightly above. Nearby site Laetoli has a much older fossil record.

The earliest archaeological deposit, known as Bed I, has produced evidence of campsites and living floors along with stone tools made of flakes from local basalt and quartz. Since this is the site where these kinds of tools were first discovered, these tools are called Oldowan. It is now thought that the Oldowan toolmaking tradition started about 2.6 million years ago. Bones from this layer are not of modern humans but primitive hominid forms of Paranthropus boisei and the first discovered specimens of Homo habilis.

The site of Frida Leakey Korongo North bears the distinction of having the oldest known evidence of Elephant consumption, attributed to Homo ergaster around 1.8 million years ago. A nearly complete skeleton of the extinct Elephas recki was found in the lowest of its six occupation levels along with stone tools such as choppers and flakes. Large numbers of bone fragments of smaller animals found with it clearly identify FLK North as an early butchering site.

Above this, in Bed II, pebble tools begin to be replaced by more sophisticated handaxes of the Acheulean industry and made by Homo ergaster. This layer has not yet been successfully dated, but likely falls between 1.75 and 1.2 million years.

Beds III and IV have produced Acheulean tools and fossil bones from more than 600,000 years ago.

During a period of major faulting and volcanism roughly 400,000 to 600,000 years ago, the Masek Beds were made.

Beds above these contained tools from a Kenya-Capsian industry made by modern humans and are termed the Masek Beds (600,000 to 400,000 years ago), the Ndutu Beds (400,000 to 32,000 years ago), and the Naisiusiu Beds (22,000 to 15,000 years ago).

We went to visit on the rim of the Gorge the Olduvai Gorge Museum. This Museum presents exhibitions pertaining to the Gorge's history.

It was very interesting and we also had lunch there. Believe it os nor I was the only tourist sunbathing....everyone else was hiding from the sun...and it was not even hot!



After lunch (the packed lunch..not the best) we went to visit a Maasai Village... I was sooooooooooooooooooooooooooooooo excited....I have such a passion about the Maasai culture and finally there I was.... wow, wow!
The received us with a welcoming dance...which to me was just a group of people screaming...
We all felt so out of place....





















Maasai Women





Maasai warriors


















Here I am with the Maasai women...I was sooo over the moon.

and here with a baby....
















I had not felt that happy in ages..

I had kept the peanuts and some cookies from the packed lunch so I was giving them to the Maasai kids.






















They took us to visit the school:

and there was a kid who tried to impress as with the english alphabet...well, he did!

The school desks were a donation.
The teacher was a very young maasai woman.