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About Botswana Botswana is roughly the size of France or Kenia, at 581 730 square kilometer. The population is about 1.6 million, one of the lowest densities in Africa. The Batswana are the largest tribal group in the country, forming about 50% of the population. Botswana is a landlocked country situated in southern Africa. The climate can be described as arid to semi-arid, with a wide range of temperatures and rainfall. In terms of the economy, Botswana is the wealthiest non-oil-producing countries on the African continent. Tourism is becoming more significant as an earner of foreign revenue and is currently third on the list after diamonds and beef. The wildlife of Botswana is of the very best in Africa. Formation of the Eastern Hardveld Much of Botswana is underplayed by Karoo sediments and younger Stormberg lavas. Tuli area The Tuli block is quite different to anywhere else in Botswana. It is generally referred to as the ‘hardveld’, consisting of rocky outcrops and a network of dry riverbeds. Characteristics of the Tuli landscape is the abundance of inselbergs or outcrops formed from a large variety of rock types – truly a geologist’s paradise! The Tuli block is situated on the Limpopo mobile belt which can be best explained as the image of a tortoise shell, which separates the Zimbabwean craton in the north from the Kaapvaal craton in the south. The Limpopo mobile belt is the oldest known mobile belt in the world, with rocks varying in age from 2 700 million to 3 700 million years. The Tuli block is about 10km to 20km wide and about 350km long. Makgadigadi Pans About 3 million years ago strong easterly winds caused the formation of dunes orientated east to west across the middle Kalahari. Wetter times followed and the flow of the rivers was guided by these dunes, causing the water to flow in one direction, into a huge depression known as Lake Makgadigadi. One has not enjoyed the full charm of Botswana without having had a taste of the magic of the Makgadigadi Pans. The Makgadikgadi Pans consist of two main pans, namely Ntwetwe and Sowa Pan, both of which are surrounded by a myriad of smaller pans. Its remoteness, inaccessibility and danger, all add to the mystique. The Makgadikgadi Pans National Park is an ideal stop-over enroute to the Okavango. Only one-fifth of the reserve comprises salt pans and the rest consists mainly of rolling grasslands which yield very nutritious grasses. ![]() About 20
000 years ago this lake was filled to capacity and forced its way
northwards and the eastwards, causing the middle and lower Zambezi to
connect, an event that resulted in the formation of the Maun The gateway to the Okavango
Delta is Maun.
There is something
about this hot and dusty town that makes one simply fall in love with …
It is the best place to buy Mopane Worms and it is generally accepted
that you have not fully experienced The
best season to visit the
The
birdlife in the ![]() The
central Okavango Delta
is one of the most beautiful places in It comprises almost one-third of the delta and it is completely buffered by wildlife management areas and consists of permanent swamp, seasonal swamp areas and dry land. Kasane Kasane is the ideal place to
end a Kasane is strategically
situated at the
entrance to the The There are four main tourist areas in Chobe namely: The
Chobe river front, Savuti, Nogatsaa and Linyanti.
-
- Savuti: In sharp contrast to the lush Chobe river front is the almost desert-like landscape of the Savuti during the dry season. The most typical feature of the landscape is the dead trees – evidence of the erratic flow of the Savuti channel over the years.
-
Nogatsaa: When the
pans in the Nogatsaa area have water, game viewing is good.
The area is not
spectacular as far as scenery goes and consists mainly of Mopane
woodland and mixed Cumbersome veld and some - Linyanti: Unfortunately, there are only 7km of river front that can be used by visitors for game drives. This is more suited for the more adventurous visitor as the drive is long and difficult. |
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