Bushveld in the context of North West (South African province)


Bushveld in the context of North West (South African province)

⭐ Core Definition: Bushveld

The Bushveld (from Afrikaans: bosveld, Afrikaans: bos 'bush' and Afrikaans: veld) is a sub-tropical woodland ecoregion of Southern Africa. The ecoregion straddles the Tropic of Capricorn and constitutes the southern part of the Zambezian region. It encompasses most of Limpopo and a small part of North West in South Africa, the Central and North-East Districts of Botswana and the Matabeleland South and part of Matabeleland North provinces of Zimbabwe. The Kruger National Park has a number of 'Bushveld' camps, but these are strictly speaking in the lowveld, as these terms are sometimes used interchangeably. Although their limits are somewhat blurred, lowveld is generally restricted to the more easterly parts of South Africa and Zimbabwe.

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Bushveld in the context of Veld

Veld (/vɛlt/ or /fɛlt/, Afrikaans and Dutch: veld, field), also spelled veldt, is a type of wide-open, rural landscape in Southern Africa. Particularly, it is a flat area covered in grass or low scrub, especially in the countries of South Africa, Namibia, Lesotho, Eswatini, Zimbabwe, and Botswana. A certain subtropical woodland ecoregion of Southern Africa has been officially defined as the Bushveld by the World Wide Fund for Nature. Trees are not abundant; frost, fire, and grazing animals allow grass to grow, but prevent the build-up of dense foliage.

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Bushveld in the context of Chromite

Chromite is a crystalline mineral composed primarily of iron(II) oxide and chromium(III) oxide compounds. It can be represented by the chemical formula of FeCr2O4. It is an oxide mineral belonging to the spinel group. The element magnesium can substitute for iron in variable amounts as it forms a solid solution with magnesiochromite (MgCr2O4). Substitution of the element aluminium can also occur, leading to hercynite (FeAl2O4). Chromite today is mined particularly to make stainless steel through the production of ferrochrome (FeCr), which is an iron-chromium alloy.

Chromite grains are commonly found in large mafic igneous intrusions such as the Bushveld in South Africa and India. Chromite is iron-black in color with a metallic luster, a dark brown streak and a hardness on the Mohs scale of 5.5.

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