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UKhahlamba

Drakensberg
Maluti, uKhahlamba
Maluti.jpg
Highest point
Peak Thabana Ntlenyana
Elevation 3,482 m (11,424 ft)
Coordinates 29°28′S 29°16′E / 29.467°S 29.267°E / -29.467; 29.267Coordinates: 29°28′S 29°16′E / 29.467°S 29.267°E / -29.467; 29.267
Dimensions
Length 1,000 km (620 mi) SW to NE
Naming
Etymology Dragon's mountain
Geography
Countries South Africa and Lesotho
Geology
Type of rock Basalt and Quartzite

The Drakensberg (Afrikaans: Drakensberge, isiZulu: uKhahlamba, SeSotho: Maluti) is the name given to the eastern portion of the Great Escarpment, which encloses the central Southern African plateau. The Great Escarpment reaches its greatest elevation in this region – 2,000 to 3,000 metres (6,600 to 9,800 feet).

The Drakensberg escarpment stretches for over 1,000 kilometres (600 miles) from the Eastern Cape Province in the South, then successively forms, in order from south to north, the border between Lesotho and the Eastern Cape and the border between Lesotho and KwaZulu-Natal Province. Thereafter it forms the border between KwaZulu-Natal and the Free State, and next as the border between KwaZulu-Natal and Mpumalanga Province. It winds north, through Mpumalanga, where it includes features such as the Blyde River Canyon, Three Rondavels and God's Window. It moves north again above Tzaneen in Limpopo Province, where it includes the Wolkberg Mountains and Iron Crown Mountain, at 2,200 m (7,200 ft) above sea level, the Wolkberg being the highest mountain range in Limpopo. It veers west again and at Mokopane it is known as the Strydpoort Mountains.

The Afrikaans name Drakensberge comes from the name the earliest Dutch settlers to the region gave it. They called them the Drakensbergen, or "Mountains of Dragons". Several possible reasons for this name include the pointy tops giving an appearance similar to that of the back of the mythical European dragon, old local myths of dragons roaming the mountains, and possible findings of dinosaur fossils (which would have been confused with the remains of dragons).


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