Tanzania Rift Valley

Document Sample
Tanzania Rift Valley Powered By Docstoc
					Tanzania Rift Valley
Rift valley in Tanzania


Tanzania is a country in far east Africa bordered by nigeria and Uganda on the northern , Rwanda,
Burundi and the Democratic Republic of the Congo for the west, and Zambia, Malawi and
Mozambique on the southern. To the east it edges the Indian Ocean.
The country's name came right after union of Tanganyika, the big mainland territory, and Zanzibar the
offshore archipelago.. The two former British colonies usa in 1964, forming your United Republic of
Tanganyika and Zanzibar, which after the same year was relabeled the United Republic regarding
Tanzania.
Tanzania has 26 regions , twenty-one are on your mainland and five inside Zanzibar for which three
take presctiption Unguja and two are on Pemba. Ninety-eight districts , each using at least one
council, have been made to further increase local expert ; Currently there are 114 councils operating
in 99 districts ; 22 are urban along with 92 are rural.
Tanzania is the world 31st biggest country with about 364,875 m' (945,087 km') it comes after Egypt.

To north of manchester and west of Tanzania there are the Great Lakes regarding Lake Victoria
(Africa's biggest lake) and Lake Tanganyika (Africa's deepest lake). Main Tanzania comprises a large
level of skill , with plains and arable land. The eastern shore is hot and humid, with the isle of
Zanzibar lying merely offshore. Also Tanzania support the famous national parks along with Game
reserve which red flags Tanzania in high level regarding tourism. Many people of Tanzania are
participate mostly inside agriculture, hence large number of people are living in rural area.

As earlier mentioned , the major reasons which makes body of water Tanganyika to be the second
deepest and largest freshwater on the globe , after Lake Baikal inside Siberia , This is because it is
handed by rift valley, your lake is situated within the traditional western Rift of the geographic feature
known as the Great Rift pit formed by the tectonic far east African Rift, and is enclosed by the
mountainous walls in the valley. It is the largest rift lake in Africa as well as the second largest lake
through surface area on the continent. It is the deepest lake in africa and holds the greatest level of
fresh water. It extends pertaining to 673 km in a general north-south direction and earnings 50 km in
width. Your lake covers 32,nine hundred km', with a shoreline of a single ,828km and a mean depth of
570 m along with a maximum depth of 1,470 m in the northern container it holds an estimated 18 ,900
km'. So a rift valley is a linear-shaped lowland between highlands or mountain ranges created by the
act of a geologic rift or fault. This action is evident as crustal extension, a distributing apart of the
surface area which is subsequently further deepened by the forces of erosion. Rifts can occur at all
elevations, from the sea floor to plateaus and mountain runs. They can occur in continental crust or in
oceanic crust. Rift valleys are usually associated with a number of adjoining subsidiary or co-
extensive valleys which are typically regarded geologically part of the principal rift valley. The Rift pit
lakes are a group of waters in the Great Rift pit formed by the East cameras Rift which runs through
the whole eastern side in the African continent from northern to south. These waters include some of
the oldest, biggest and deepest lakes on the globe , and many are freshwater ecoregions of great
biodiversity, although some are alkaline or soda lakes supporting highly specialist organisms.

The Great Rift pit is a vast geographical along with geological feature of far east Africa and southwest
parts of asia created by the rifting along with separation of the African along with Arabian tectonic
plates about 35 million years ago. It had been named by the explorer steve Walter Gregory. The
Great Rift Valley runs north to south for some 5,000 km, from northern Syria to central Mozambique.
Your valley varies in width via 30-100 km and in depth from a few hundred to many thousand metres.
The northernmost part of the Rift forms your valley of the Jordan riv , which flows southward through
the Sea of Galilee inside Israel to the Dead sea. From the Dead Sea southwards, the Rift is busy by
the Wadi Arabah and then the Gulf of Aqaba and the Red Sea. Your southern end of the red Sea
marks a branch in the rift.
in a southwest direction the problem continues as the Great Rift Valley, which split your older
Ethiopian highlands in to two halves. In eastern Africa the valley splits into two, the eastern Rift and
the Western Rift. The Western Rift, also called the Albertine Rift, and possesses the Rift Valley
waters , which include some of the deepest waters in the world (up to 1,470 meters deep at body of
water Tanganyika). Lake Victoria, the second largest lake in the world, is considered the main Rift
Valley system eventhough it actually lies between the a couple of branches. In Kenya your valley is
deepest for the north of Nairobi. Since the valley has no outlet for the sea, its lakes are generally
shallow and have a high mineral content as the evaporation regarding water leaves the salt behind.
For example, Lake Magadi is almost solid soda (salt carbonate), and Lake Elmenteita, Lake Baringo,
Lake Bogoria, and Lake Nakuru are typical strongly alkaline, while body of water Naivasha needs to
be supplied by fresh water springs to support its biological variety. The formation of the Rift Valley
continues: within a few million years, eastern africa will probably split off to type a new landmass. The
original faulting activity that created the Rift weakened the Earth's crust coupled its margins. The area
is therefore volcanically and seismically productive and has produced the volcanic mountains Mount
Kilimanjaro, attach Kenya, Mount Karisimbi, attach Nyiragongo, Mount Meru along with Mount Elgon
as well as the Crater Highlands in Tanzania. Your Ol Doinyo Lengai volcano remains active, and is
the only natrocarbonatite volcano on the globe.

The Rift Valley is a huge rich source of anthropological breakthrough discovery , especially in Olduvai
Gorge. Because the rapidly eroding highlands get filled the valley using sediments, a favourable
environment for the preservation of remains has been produced.

For more information on visiting Tanzania Tanzania safari with Wild Things

For more information on ascending Kilimanjaro or visiting Tanzania's mountains contact Climb
Kilimanjaro with Mountain Kingdom

--
Fred Mlaponi is a Tanzanian college student researcher on work exposure to Wild Things and MK
Safaris in Tanzania http://www.wildthingsafaris.com . http://www.mksafaris.org
For More Info Click Here

				
DOCUMENT INFO
Shared By:
Categories:
Stats:
views:4
posted:7/8/2012
language:
pages:2
Description: 570 m along with a maximum depth of 1,470 m in the northern container it holds an estimated 18 ,900