During the time of Pangea, Africa joined Europe at the region now known as the Mediterranean Sea. Geological evidence supporting this includes the presence of similar rock formations, fossil distributions, and the alignment of mountain ranges such as the Atlas in Africa and the Alps in Europe, which indicate they were once part of the same landmass. Additionally, paleomagnetic studies show that the continents have shifted over time, providing further confirmation of their past connection.
Africa has valuable natural resources for which Europe has many uses.
Africa
Europe and Asia
Africa and Europe do not share any common border. Southern Spain and the northern parts of Morocco are separated by the straights of Gibraltar, and this is as close as Africa and Europe get to be. To the east, Europe joins Asia. Some geographers call the combination of the two continents Eurasia (Europe and Asia). If you use the definition of Eurasia then Eurasia joins Africa in Egypt, which is on both sides of the Suez Canal, the separation of the two land masses.
Europe colonized Africa during the Age of Imperialism in the 19th century.
Europe and Asia
What happened to the earth's continents during Permian Period is Pangea, Pangea is when the used to be one big super continent broke apart created our separate continents today.
Europe
Black death struck in Africa, Asia, and Europe.
Slaves from Africa to America, Cotton and Sugar from America to Europe, Textiles and manufactured goods to Africa.
Homo Habilis is believed to have originated in East Africa, specifically in regions such as Ethiopia, Kenya, and Tanzania. Some evidence suggests they may have migrated to other parts of Africa as well.
Pangea was a supercontinent that existed about 335 to 175 million years ago during the late Paleozoic and early Mesozoic eras. It was surrounded by a single large ocean called Panthalassa and eventually broke apart due to tectonic plate movements, leading to the formation of the continents we have today. The theory of Pangea was proposed by Alfred Wegener in 1912, based on the fit of the continents, matching rock formations, and fossil evidence.