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The Humpata Plateau (Portuguese: Planalto da Humpata) is an elevated plateau and highlands region in southwest Angola, [1] part of the larger Huíla Plateau. [2] It has a semi-humid climate, [3] and acts as an intermediate climactic region between the arid Namib Desert to the west and the wetter Kalahari Basin to the east. [4]
This list of fossil sites is a worldwide list of localities known well for the presence of fossils.Some entries in this list are notable for a single, unique find, while others are notable for the large number of fossils found there.
The geology of Angola includes large areas of Precambrian age rocks. The west of the country is characterized by meta-sedimentary rocks of Proterozoic age including tillites assigned to the Bembe System. Overlying these are a thick pile of limestones and other marine sediments laid down during the Mesozoic and Cenozoic eras.
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Tundavala Gap (Portuguese: Fenda da Tundavala) is a canyon on the escarpment of the Serra da Leba near Lubango, Huíla Province, Angola.The escarpment marks the western limit of the Humpata Plateau, part of the Great Escarpment of Southern Africa, and creates a natural boundary between Huíla Province and Namibe Province.
A synthesis of the paleontology in Angola shows that 1313 fossil species are known in the country, 201 of them are vertebrates [1] and about one tenth of them are species firstly described based on specimens from Angola. Paleontology portal
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It is also the first non-avian dinosaur discovered in Angola. The genus contains a single species, Angolatitan adamastor, known from a partial right forelimb. Angolatitan was a relict form of its time; it was a Late Cretaceous basal titanosauriform, when more derived titanosaurs were far more common. [1]