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The population density of Africa as of 2000. North Africa (sometimes Northern Africa) is a region encompassing the northern portion of the African continent. There is no singularly accepted scope for the region, and it is sometimes defined as stretching from the Atlantic shores of the Western Sahara in the west, to Egypt and Sudan's Red Sea coast in the east.
When the Roman Empire began to collapse, North Africa was spared much of the disruption until the Vandal invasion of 429 AD. The Vandals ruled in North Africa until the territories were regained by Justinian of the Eastern Empire in the 6th century. Egypt was never invaded by the Vandals because there was a thousand-mile buffer of desert and ...
The Middle East–North Africa region comprises 20 countries and territories with an estimated Muslim population of 315 million or about 23% of the world's Muslim population. [47] The term "MENA" is often defined in part in relation to majority-Muslim countries located in the region, although several nations in the region are not Muslim ...
Ancient Greek geography of North Africa (3 C, 20 P) E. Geography of Egypt (23 C, 32 P) L. Geography of Libya (18 C, 14 P) M. Maghreb (13 C, 54 P) Mediterranean (10 C ...
The Maghreb is a region of northwest Africa encompassing the coastlands and Atlas Mountains of Morocco, Algeria, and Tunisia. The Sahara Desert is the massive sparsely populated region in North Africa that contains the world's largest hot deserts; Sub-Saharan Africa is the area of the African continent which lies south of the Sahara.
Satellite view of Africa 1916 physical map of Africa. The average elevation of the continent approximates closely to 600 m (2,000 ft) above sea level, roughly near to the mean elevation of both North and South America, but considerably less than that of Asia, 950 m (3,120 ft).
When the North African Monsoon is at its strongest, annual precipitation and consequently vegetation in the Sahara region increase, resulting in conditions commonly referred to as the "green Sahara". For a relatively weak North African Monsoon, the opposite is true, with decreased annual precipitation and less vegetation resulting in a phase of ...
African vegetation during the Last Glacial Maximum (~12,000 BCE). Human habitation in North Africa has been greatly influenced by the climate of the Sahara (currently the world's largest warm desert), which has undergone enormous variations between wet and dry over the last few hundred thousand years. [2]