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The Drakensberg that form the northeastern and eastern borders of Lesotho, as well as the Eastern Cape Drakensberg, are composed of a thick layer of basalt (lava) that erupted 180 million years ago. [ 5 ] [ 8 ] That layer rests on the youngest of the Karoo Supergroup sediments, the Clarens sandstone , which was laid down under desert conditions ...
The uKhahlamba-Drakensberg Park is also in the List of Wetlands of International Importance (under the Ramsar Convention). Adjacent to the park is the Cathkin Estates Conservation and Wildlife Sanctuary, which spans 1,044 ha (10 km 2 ) of virgin grassland and represents the largest privately-owned game park in the KwaZulu-Natal Drakensberg region.
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 ...
The Maloti-Drakensberg Park is a World Heritage Site, established on 11 June 2001 by linking the Sehlabathebe National Park in the Kingdom of Lesotho and the uKhahlamba Drakensberg Park in KwaZulu-Natal, South Africa. [1] The highest peak is Thaba Ntlenyana rising to 3,482 metres.
The Amphitheatre with the Tugela River. The Amphitheatre is one of the geographical features of the Northern Drakensberg, South Africa.The cliff face of the Amphitheatre is roughly three times the size of the total combined area of all the cliff faces in Yosemite's famous El Capitan, and more than 10 times the size of El Capitan's most famous (South Western) face.
The Drakensberg alti-montane grasslands and woodlands ecoregion, in green (WWF, 2001) Vegetation in the Maloti is known to vary with the surface geomorphic features beneath it, such as the soil's grain size, carbon content, and depth. [12] Flora communities are composed largely of tussock grasses and ericoid shrubs.
Tugela Falls (uThukela in Zulu [citation needed]) is a complex of seasonal waterfalls located in the Drakensberg (Dragon's Mountains) of Royal Natal National Park in KwaZulu-Natal Province, Republic of South Africa. According to some measurements, it is the world's tallest waterfall.
The main features of the park are the Drakensberg Amphitheatre, a rock wall 5 kilometres (3.1 mi) long and up to 1,200 metres (3,900 ft) high, Mont-Aux-Sources peak where the Orange and Tugela rivers have their source, [4] and the 948-metre (3,110 ft) Tugela Falls, the world's tallest waterfall. [5]