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The geology of South Sudan is founded on Precambrian igneous and metamorphic rocks, that cover 40 percent of the country's surface and underlie other rock units. The region was affected by the Pan-African orogeny in the Neoproterozoic and extensional tectonics in the Mesozoic that deposited very thick oil-bearing sedimentary sequences in rift ...
Mesozoic rift basins including Muglad develop oblique to East African Rift.. The Muglad Basin is a large rift basin in Northern Africa.The basin is situated within southern Sudan and South Sudan, and it covers an area of approximately 120,000 square kilometres (46,000 sq mi) across the two nations.
Oil fields in South Sudan (5 P) Pages in category "Geology of South Sudan" The following 6 pages are in this category, out of 6 total.
South Sudan (/ s uː ˈ d ɑː n,-ˈ d æ n /), officially the Republic of South Sudan, is a landlocked country in East Africa. [16] It is bordered on the north by Sudan; on the east by Ethiopia; on the south by the Democratic Republic of the Congo, Uganda and Kenya; and on the west by the Central African Republic.
Geology of South Sudan (2 C, 6 P) Grasslands of South Sudan (3 P) L. Landforms of South Sudan (6 C, 2 P) N. Natural disasters in South Sudan (3 P) O. Oil fields in ...
The geography of South Sudan describes the physical features of South Sudan, a country in East Africa. South Sudan is a landlocked country and borders – clockwise – Sudan from the north, Ethiopia from the east, Kenya , Uganda and the Democratic Republic of the Congo from the south and the Central African Republic from the west.
The Sudd stretches from Mongalla to just outside the Sobat River confluence with the White Nile just upstream of Malakal as well as westwards along the Bahr el Ghazal.The shallow and flat inland delta lies between 5.5 and 9.5 degrees latitude north and covers an area of 500 kilometres (310 mi) south to north and 200 kilometres (120 mi) east to west between Mongalla in the south and Malakal in ...
Sudan experienced extensive pediplanation, a form of sheet flow erosion that scours away overlying sediments, leaving a gently inclined bedrock surface. Because of this, the country has hardly any unmetamorphosed rocks from the Paleozoic or early Mesozoic , with the exception of a few 530 million year old Early Cambrian rocks at Sabaloka.