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Module:Location map/data/South Africa is a location map definition used to overlay markers and labels on an equirectangular projection map of South Africa. The markers are placed by latitude and longitude coordinates on the default map or a similar map image.
This is a list of the extreme points of South Africa, the points that are farther north, south, east or west than any other location in the country. Including the Prince Edward Islands Northernmost Point: Over Vlakte farm, Vhembe District Municipality , Limpopo Province ( 22°7′40″S 29°39′20″E / 22.12778°S 29.65556°E ...
Wonderboom is a northern residential suburb of Pretoria, South Africa.The suburb includes the Wonderboom Nature Reserve site of the famous Wonderboom [2] (Afrikaans for "Marvel tree" or "Wonder tree"), on the northern slopes of the Magaliesberg mountains, just east of the Apies River.
Equestria is bordered by four routes, namely the N4 (north), M6 (south), M10 (east) and M12 (west). The N4 is the major national route and highway connecting Pretoria Central to the west with eMalahleni to the east. The M6 (Lynnwood Drive) connects Lynnwood to the west with Onbekend to the south-east.
Shere is a residential area to the east of Pretoria, South Africa. It lies wedged between the Bronberg and Magaliesberg mountains. References This page was last ...
The City of Tshwane is the second largest municipality in Gauteng and is among the six biggest metropolitan municipalities in South Africa. The following towns and townships form part of the Municipality's area: Pretoria, Centurion, Akasia, Soshanguve, Mabopane, Atteridgeville, Ga-Rankuwa, Winterveld, Hammanskraal, Temba, Crocodile River and ...
Lynnwood Ridge is a suburb of the city of Pretoria, South Africa. It is a well-developed area, lying to the east of the city centre. Together with Brooklyn and Menlo Park, it was most likely named after American counterparts. Today these suburbs are known as the old east and boast to have some of the city's most high-end residential properties.
About 180 million years ago, a mantle plume under southern Gondwana caused bulging of the continental crust in the area that would later become southern Africa. [2] Within 10–20 million years, rift valleys formed on either side of the central bulge and flooded to become the proto-Atlantic Ocean and proto-Indian Ocean more or less along the present southern African coastline and separating ...