Veld

Etymology

The word veld (Dutch pronunciation: [fɛlt]) comes from the Afrikaans word for 'field'.

The etymological origin is older Dutch veldt, a spelling that the Dutch abandoned in favour of veld during the 19th century, decades before the first Afrikaans dictionary. Subsequent addition of the terminal "t" in the spelling "veldt" seems to have been mainly an English confusion with the already obsolete Dutch usage; it never was an Afrikaans form.

Climate

The climate of the veld is highly variable, but its general pattern is mild winters from May to September and hot or very hot summers from November to March, with moderate or considerable variations in daily temperatures and abundant sunshine. Precipitation mostly occurs in the summer months in the form of high-energy thunderstorms.

Over most of the South African Highveld, the average annual rainfall is between 15 and 30 inches (380 and 760 mm), decreasing to about 10 inches (250 mm) near the western border and increasing to nearly 40 inches (1,000 mm) in some parts of the Lesotho Highlands; the South African Lowveld generally receives more precipitation than the Highveld. Temperature is closely related to elevation. In general, the mean July (winter) temperatures range between 45 °F (7 °C) in the Lesotho Highlands and 60 °F (16 °C) in the Lowveld. January (summer) temperatures range between 65 °F (18 °C) and 80 °F (27 °C).

In Zimbabwe the precipitation averages around 30 to 35 inches (760 to 900 mm) on the Highveld, dropping to less than 15 inches in the lowest areas of the Lowveld. Temperatures are slightly higher than in South Africa.

Over the entire veld, seasonal and annual average rainfall variations of up to 40 percent are common. Damaging drought affects at least half the area about once every three or four years; it reduces plant and animal biomass to sustainable levels again. Everywhere the average number of hours of annual sunshine varies from 60 to 80 percent of the total amount possible.

Definitions

Veld can be loosely compared to the Australian terms outback or "the bush", to the prairie of North America, to the pampas lowlands of South America, or to the steppe of Central Asia. Someone from Yorkshire might equate "wandering across the moors" to "walking through the veld."

By extension, the veld can be compared to the "boondocks" or those places "beyond the black stump" in Australia. There is a sense in which it refers in essence to unimproved land (and is therefore not the equivalent of the English paddock) and does not include areas used both for pastoral activities and the planting of crops. These areas are referred to as fields. The word is less appropriate for land that is heavily forested, mountainous, or urban. The simplest explanation will be to say the word "veld" means "natural vegetation"; excluding vegetation like swamps and forests. It does include mountains with vegetation but not deserts or mountains without natural vegetation.

The veld definition may encompass different natural environments, both humid and dry, such as Coastal plain, Coastal prairie, Flooded grasslands and savannas, Grassland, Prairie, Savanna, Steppe, Meadow, Water-meadow, Flood-meadow, Wet meadow, as well as agricultural fields. Whereas mountainous peaks and thick forests do not really fit in with the term veld, bushes are acceptable. The area then becomes Bosveld, a term that is used mainly to describe Die Bosveld ("The Bushveld"), which is both a loose botanical classification and a specific geographical part of what used to be known as the Transvaal, as described for example in the story Jock of the Bushveld.

Other uses

Highveld

Much of the interior of Southern Africa consists of a high plateau, the higher portions 1,500–2,100 m (4,900–6,900 ft) of which are known as the Highveld, starting at the Drakensberg escarpment, 220 km (140 mi) to the east of Johannesburg, and sloping gradually downwards to the west and south west, as well as to the north, through the Bushveld towards the Limpopo river. These higher, cooler areas (generally more than 1,500 metres (4,900 ft) above sea level) are characterised by flat or gently undulating terrain, vast grasslands and a modified tropical or subtropical climate. To the east, the Highveld's border is marked by the Great Escarpment, or the Mpumalanga Drakensberg, but in the other directions the boundary is not obvious, and often arbitrary. The blesbok and quagga were among the large animals that once roamed on the highveld in great numbers. Nowadays there still is a sizeable population of springbok in some areas, though much of the area is devoted to commercial farming, and South Africa's largest conurbation (Gauteng Province).

Lowveld

The lowlands, below about 500 m (1,640 ft) altitude, along South Africa's northern border with Botswana and Zimbabwe, where a 180-million-year-old failed rift valley cuts into Southern Africa's central plateau and locally obliterates the Great Escarpment is known as the Lowveld. The Limpopo and Save rivers run from the central African highlands via the Lowveld into the Indian Ocean to the east. The Limpopo Lowveld extends southwards, east of the Drakensberg escarpment through Mpumalanga Province and ultimately into eastern Swaziland. This southern limb of the Lowveld is bounded by South Africa's border with Mozambique to the east, and the north-eastern part of the Drakensberg to the west. This region is generally hotter and less intensely cultivated than the Highveld.

Thornveld

Thornveld (also thorn veld or thornveldt), often referred to as "acacia thornveld", is a type of semi-arid savanna in which grassland with thorny acacia and certain species of thorny bushes predominate. The predominant plant species are usually different in the thornveld of the plains or in the hill thornveld, where, for example, species of genus Balanites are common. Some of the characteristic species in the thornveld include:

Sandveld

Sandveld, in the general sense of the word, is a type of veld characterised by dry, sandy soil, typical of certain areas of the Southern African region. It usually absorbs all water from the seasonal rains, although aquatic habitats, largely seasonal, may be also found in specific places in the sandveld. Only certain hardy plant species thrive in the sandveld environment. These consist especially of grasses forming clumps and certain kinds of trees and shrubs. The sandveld vegetation has a particular pattern of growth, rarely covering the whole terrain and thus leaving patches of sandy soil exposed on the surface. Some of the typical sandveld species are Acacia haematoxylon, A. luederitzii, Boscia albitrunca, Terminalia sericea, Lonchocarpus nelsii, Bauhinia petersiana and Baphia massaiensis.

Hardveld

Hardveld is a term applied to certain areas of rocky soils in Botswana, located mostly in the eastern part of the country. The landscape is an undulating plain with scattered rocky hill ranges. There are areas of hardveld also in South Africa in the mountainous central Kamiesberg of the Northern Cape with hilly escarpments and deep river valleys. The soil of the hardveld is characterised by rocky outcrops, as well as an abundance of stones and pebbles of different shapes and sizes.

The flora of the hardveld is typical of rocky savanna, with denser vegetation, and thus less denuded patches than in the sandveld, as well as taller trees. There is also a higher diversity of species in the hardveld compared with the sandveld. Peltophorum africanum, Acacia nigrescens, A. tortilis, Combretum apiculatum and Colophospermum mopane are some of the representative species of the northern hardveld.

See also

External links