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Geology of Lesotho. The geology of Lesotho is built on ancient crystalline basement rock up to 3.6 billion years old, belonging to the Kaapvaal Craton, a section of stable primordial crust. Most of the rocks in the country are sedimentary or volcanic units, belonging to the Karoo Supergroup. The country is notable for large fossil deposits and ...
1,400 m (4,593.2 ft) Lesotho is a mountainous, landlocked country located in Southern Africa. It is an enclave, surrounded by South Africa. The total length of the country's borders is 909 kilometres (565 mi). Lesotho covers an area of around 30,355 square kilometres (11,720 sq mi), of which a negligible percentage is covered with water.
Lesotho ( / lɪˈsuːtuː / ⓘ lih-SOO-too, [6] [7] Sotho pronunciation: [lɪˈsʊːtʰʊ] ), formally the Kingdom of Lesotho, is a landlocked country in Southern Africa. As an enclave of South Africa, with which it shares a 1,106 km (687 mi) border, [8] it is the only sovereign enclave in the world outside of the Italian Peninsula.
The following outline is provided as an overview of and topical guide to Lesotho: Lesotho – sovereign country located in Southern Africa. [1] Lesotho is an enclave completely surrounded by the Republic of South Africa. Formerly Basutoland, it is a member of the Commonwealth of Nations.
The Great Escarpment is a major topographical feature in Africa that consists of steep slopes from the high central Southern African plateau [1] downward in the direction of the oceans that surround southern Africa on three sides. [2] [3] While it lies predominantly within the borders of South Africa, in the east the escarpment extends ...
Geologic formations of Lesotho (1 C, 6 P) M. Mines in Lesotho (1 C) Mining in Lesotho (1 C, 3 P) P. Paleontology in Lesotho (13 P) V.
Pages in category "Geologic formations of Lesotho". The following 6 pages are in this category, out of 6 total. This list may not reflect recent changes . List of fossiliferous stratigraphic units in Lesotho.
A geologic map or geological map is a special-purpose map made to show various geological features. Rock units or geologic strata are shown by color or symbols. Bedding planes and structural features such as faults, folds, are shown with strike and dip or trend and plunge symbols which give three-dimensional orientations features.