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  2. Reiterdenkmal, Windhoek - Wikipedia

    en.wikipedia.org/wiki/Reiterdenkmal,_Windhoek

    The plinth is 5 metres (16 ft) tall and consists of approximately 180 granite rocks from Okahandja. [2] It has a plaque mounted on it that remembers the German soldiers and civilians that died in the Herero and Namaqua War of 1904–1907, as well as in the Kalahari Expedition in 1908. The translation of the inscription is: [3]

  3. Kalahari Craton - Wikipedia

    en.wikipedia.org/wiki/Kalahari_craton

    The Kalahari Craton is a craton, an old and stable part of the continental lithosphere, that occupies large portions of South Africa, Botswana, Namibia and Zimbabwe. It consists of two cratons separated by the Limpopo Belt : the larger Kaapvaal Craton to the south and the smaller Zimbabwe Craton to the north.

  4. List of deserts by area - Wikipedia

    en.wikipedia.org/wiki/List_of_deserts_by_area

    Rank Name Type Image Area (km 2) Area (sq mi) Location [note 1] Nation(s) 1: Antarctic Desert: Polar ice and tundra: 14,200,000 [1]: 5,482,651: Antarctica: N/A 2: Arctic Desert: Polar ice and tundra

  5. Kalahari Desert - Wikipedia

    en.wikipedia.org/wiki/Kalahari_Desert

    The Kalahari Desert is a large semi-arid sandy savanna in Southern Africa extending for 900,000 square kilometres (350,000 sq mi), covering much of Botswana, ...

  6. Caliche - Wikipedia

    en.wikipedia.org/wiki/Caliche

    Caliche fossil forest on San Miguel Island, California. Caliche (/ k ə ˈ l iː tʃ iː /) (unrelated to the street-slang "Caliche" spoken in El Salvador) is a soil accumulation of soluble calcium carbonate at depth, where it precipitates and binds other materials—such as gravel, sand, clay, and silt.

  7. I-type granite - Wikipedia

    en.wikipedia.org/wiki/I-type_Granite

    I-type granites are a category of granites originating from igneous sources, first proposed by Chappell and White (1974). [1] They are recognized by a specific set of mineralogical, geochemical, textural, and isotopic characteristics that indicate, for example, magma hybridization in the deep crust. [ 2 ]

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