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Geography of Eswatini. Eswatini (formerly Swaziland), is a country in Southern Africa lying between Mozambique and South Africa. The country is located at the geographic coordinates 26°30′S 31°30′E. Eswatini has an area of 17,363 square kilometres, of which 160 are water. The major regions of the country are Lowveld, Midveld and Highveld.
Topographic map of Eswatini. A small landlocked kingdom with an area of 17,364 km 2 (6,704 sq mi), Eswatini is located at approximately 26°30'S, 31°30'E [58] and is bordered in the north, west and south by South Africa and by Mozambique in the east.
Google Trikes are also being used for the first time to map popular tourist destinations, such as the scenic Chapman's Peak Drive and Table Mountain in Cape Town, Soccer City in Johannesburg, and the new Moses Mabhida Stadium in Durban. Images of South Africa were made available on Google Street View on June 8, 2010.
East Africa, also known as Eastern Africa or the East of Africa, is a region at the eastern edge of the African continent, distinguished by its geographical, historical, and cultural landscape. Defined in varying scopes, the region is recognized in the United Nations Statistics Division scheme as encompassing 18 sovereign states and 4 territories.
Gold Coast, Slave Coast, Ivory Coast and Pepper Coast. Rhodesia (region) ( Northern Rhodesia, Southern Rhodesia) Mayombe. The Congo Basin is the rainforest region. The Chad Basin is the largest endorheic drainage basin in Africa, centered on Lake Chad. East African Rift. The region contains Tanzania, Kenya, Uganda .
Below is a list of countries in Africa by area. [1] Algeria has been the largest country in Africa and the Arab world since the division of Sudan in 2011. Seychelles is the smallest country in Africa overall, with The Gambia being the smallest country on continental Africa. [2]
The geology of Eswatini formed beginning 3.6 billion years ago, in the Archean Eon of the Precambrian. Eswatini is the only country entirely underlain by the Kaapvaal Craton , one of the oldest pieces of stable continental crust and the only craton regarded as "pristine" by geologists, other than the Yilgarn Craton in Australia.
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