Lesotho Highlands
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The Lesotho Highlands are formed by the
Drakensberg The Drakensberg (Afrikaans: Drakensberge, Zulu: uKhahlambha, Sotho: Maluti) is the eastern portion of the Great Escarpment, which encloses the central Southern African plateau. The Great Escarpment reaches its greatest elevation – within t ...
and Maloti mountain ranges in the east and central parts of the country of
Lesotho Lesotho ( ), officially the Kingdom of Lesotho, is a country landlocked as an enclave in South Africa. It is situated in the Maloti Mountains and contains the highest mountains in Southern Africa. It has an area of over and has a population ...
. Foothills form a divide between the lowlands and the highlands. Snow is common in the highlands in the winter.


Location and description

The Highlands are located to the southeast of the Highveld, encompassing the whole eastern part of Lesotho. The average annual rainfall is nearly 1,000 mm (40 inches) in some parts of the high ranges. Temperature is closely related to elevation in the Lesotho Highlands. In general, the mean July (winter) temperatures stay around 7 °C (45 °F). The Lesotho Highlands form a localized high spot on the Central Plateau of the
Great Escarpment The Great Escarpment is a major topographical feature in Africa that consists of steep slopes from the high central Southern African plateauAtlas of Southern Africa. (1984). p. 13. Reader's Digest Association, Cape Town downward in the directio ...
. This is because it is capped by a 1400 m thick layer of erosion resistant
lava Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or ...
''Geological Map of South Africa, Lesotho and Swaziland''. (1970). Council for Geoscience, Geological Survey of South Africa. which welled up and spread across most of Southern Africa when it was still part of Gondwana.McCarthy t. & Rubidge B. (2005) ''The Story of Earth & Life''. p. 192, 209-269. Struik Publishers, Cape Town. Most of this lava has eroded away together with a layer of Karoo sedimentary rocks several kilometres thick on top of which the lava was poured out 182 million years ago. Only a small patch of this lava remains and covers much of Lesotho. The Lesotho Highlands have been deeply eroded by the tributaries of the
Orange River The Orange River (from Afrikaans/Dutch: ''Oranjerivier'') is a river in Southern Africa. It is the longest river in South Africa. With a total length of , the Orange River Basin extends from Lesotho into South Africa and Namibia to the north ...
which drain these highlands towards the south-west by means of erosion gulleys which turn into deep valleys further downstream. This gives this high region its very rugged, mountainous appearance. There are so many of these tributaries that the whole terrain of the highlands has a very rugged mountainous appearance, both from the ground and from the air. The eastern Lesotho Highlands contain numerous terraces and scarp faces developed on ancient
flood basalt A flood basalt (or plateau basalt) is the result of a giant volcanic eruption or series of eruptions that covers large stretches of land or the ocean floor with basalt lava. Many flood basalts have been attributed to the onset of a hotspot reac ...
. The form and development of terraces is controlled by rock structure. The terraces are
pediment Pediments are gables, usually of a triangular shape. Pediments are placed above the horizontal structure of the lintel, or entablature, if supported by columns. Pediments can contain an overdoor and are usually topped by hood moulds. A pedim ...
s where
cryogenic In physics, cryogenics is the production and behaviour of materials at very low temperatures. The 13th IIR International Congress of Refrigeration (held in Washington DC in 1971) endorsed a universal definition of “cryogenics” and “cr ...
processes are active. The terraces may be referred as cryoplanation terraces albeit this term is controversial. Each scarp represent a flow unit of the flood basalt. During the last glacial period periglacial conditions prevailed in the highlands producing landforms such as
blockfield A blockfieldWhittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 66 and 190. . (also spelt block fieldLeser, Hartmut, ed. (2005). ''Wörterbuch Allgemeine Geographie'', 13th ed., dtv, Munich, pp. 107 and 221. ...
s,
blockstream Blockstream is a blockchain technology company led by co-founder Adam Back, headquartered in Victoria, Canada, with offices and staff worldwide. The company develops a range of products and services for the storage and transfer of Bitcoin and ot ...
s and stone garlands. During the coldest period of the last glacial period—the
last glacial maximum The Last Glacial Maximum (LGM), also referred to as the Late Glacial Maximum, was the most recent time during the Last Glacial Period that ice sheets were at their greatest extent. Ice sheets covered much of Northern North America, Northern Eu ...
— the environment was relatively arid with deep
seasonal freezing A season is a division of the year based on changes in weather, ecology, and the number of daylight hours in a given region. On Earth, seasons are the result of the axial parallelism of Earth's tilted orbit around the Sun. In temperate and ...
. The area is believed to have been free of both permafrost and large snow accumulations. There is some uncertainty if small glaciers ever developed in the shadowy slopes around the highlands.


Flora

There are numerous species of plants in the highlands. The soil cover in the upland areas is discontinuous and immature. Soils in the Lesotho Highlands differ according to the host rock (basalt) and the influence of freeze and thaw processes; generally they are dominated by mollisols. Some sectors of the Lesotho Highlands are part of the Drakensberg alti-montane grasslands and woodlands
ecoregion An ecoregion (ecological region) or ecozone (ecological zone) is an ecologically and geographically defined area that is smaller than a bioregion, which in turn is smaller than a biogeographic realm. Ecoregions cover relatively large areas of ...
.Drakensberg alti-montane grasslands and woodlands - WWF
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Fauna

The Lesotho Highlands are one of the endemic bird areas of the world. The Drakensberg Rockjumper is an
endemic Endemism is the state of a species being found in a single defined geographic location, such as an island, state, nation, country or other defined zone; organisms that are indigenous to a place are not endemic to it if they are also found else ...
bird species of the Lesotho Highlands and areas surrounding them in
South Africa South Africa, officially the Republic of South Africa (RSA), is the southernmost country in Africa. It is bounded to the south by of coastline that stretch along the South Atlantic and Indian Oceans; to the north by the neighbouring coun ...
.


Threats and preservation

The Lesotho Highlands Water Project (LHWP) is an ongoing water supply and hydropower project in the area of the Highlands. Developed in partnership between the governments of Lesotho and South Africa, it comprises a system of several large dams and tunnels throughout the territory of both countries. The project allegedly is said to have had so far negative social and environmental effects.


See also

* Great Escarpment, Southern Africa * Lesotho Highlands Water Project


References


External links


ISS - Environmental change and human security in Lesotho: The role of the Lesotho Highlands Water Project in environmental degradationLate Holocene Neoglacial conditions from the Lesotho highlands, southern Africa: Phytolith and stable carbon isotope evidence from the archaeological site of LikoaengLesotho Flora
{{Coord, 29, 0, 0, S, 28, 30, 0, E, type:landmark_region:ZA, display=title Geography of Lesotho Geography of Southern Africa Afromontane ecoregions Ecoregions of South Africa Environment of South Africa Montane grasslands and shrublands Highlands