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geologia: African humid period

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They left archaeological sites and artifacts, such as one of the oldest canoes ever discovered and rock paintings such as those in the Cave of Swimmers and in the Acacus Mountains.
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The African humid period (AHP; also known by other names) was a climate period in Africa during the late Pleistocene and Holocene geologic epochs, when North Africa was wetter than it is today. The covering of much of the Sahara by grasses, trees, and lakes was caused by changes in the Earth's axial tilt, changes in vegetation and dust in the Sahara which strengthened the African monsoon, and increased greenhouse gases. During the preceding Last Glacial Maximum, the Sahara contained extensive dune fields and was mostly uninhabited. It was much larger than it is today, and its lakes and rivers, such as Lake Victoria and the White Nile, were either dry or at low levels. The humid period began about 14,600–14,500 years ago at the end of Heinrich event 1, simultaneously with the Bølling–Allerød warming. Rivers and lakes such as Lake Chad formed or expanded, glaciers grew on Mount Kilimanjaro, and the Sahara retreated. Two major dry fluctuations occurred during the Younger Dryas and the short 8.2-kiloyear event. The AHP ended 6,000–5,000 years ago during the Piora Oscillation cold period. While some evidence points to an end 5,500 years ago in the Sahel, Arabia, and East Africa, the end of the period appears to have occurred in several steps, such as the 4.2-kiloyear event. The AHP led to the widespread settlement of the Sahara and the Arabian Desert and had a profound effect on Af…
Kategoria: geologia
Rodzina: geologia
Jakość źródła: 65/100
Próby weryfikacji: 3
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Saharan rock art is a significant area of archaeological study focusing on artwork carved or painted on the natural rocks of the central Sahara desert. The rock art dates from numerous periods starting c. 12,000 years ago. The paintings and carvings of the Sahara are endangered and vulnerable; much of the rock art on uncovered rock has already disappeared. This is due to time and how the area has changed, as well as the improper exploration of this sites in the past. Organizations such as the Trust for African Rock Art are researching and recording as much information about Saharan rock art as possible, while raising awareness of threats to the art itself. New discoveries and ongoing resear…

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Wikipedia ENpomocnicze

Evidence: 48 • authority: 72

The African humid period (AHP; also known by other names) was a climate period in Africa during the late Pleistocene and Holocene geologic epochs, when North Africa was wetter than it is today. The covering of much of the Sahara by grasses, trees, and lakes was caused by changes in the Earth's axial tilt, changes in vegetation and dust in the Sahara which strengthened the African monsoon, and increased greenhouse gases. During the preceding Last Glacial Maximum, the Sahara contained extensive dune fields and was mostly uninhabited. It was much larger than it is today, and its lakes and rivers, such as Lake Victoria and the White Nile, were either dry or at low levels. The humid period began…

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Tunisia, officially the Republic of Tunisia, is a country in the Maghreb region of North Africa. It is bordered by Algeria to the west and southwest, Libya to the southeast, and the Mediterranean Sea to the north and east. Tunisia also shares maritime borders with Italy through the islands of Sicily and Sardinia to the north and Malta to the east. It features the archaeological sites of Carthage dating back to the 9th century BC, as well as the Great Mosque of Kairouan. Known for its ancient architecture, souks, and blue coasts, it covers 163,610 km2 (63,170 sq mi), and has a population of 12.1 million. It contains the eastern end of the Atlas Mountains and the northern reaches of the Sahar…

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