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Morocco, a North African country bordering the Atlantic Ocean and Mediterranean Sea, is distinguished by its Berber, Arabian and European cultural influences. Marrakesh’s medina, a mazelike medieval quarter, offers entertainment in its Djemaa el-Fna square and souks (marketplaces) selling ceramics, jewelry and metal lanterns. The capital Rabat’s Kasbah of the Udayas is a 12th-century royal fort overlooking the water, Explore Atlas Mountain Day Trip From Marrakech To Ourika Valley
The Atlas Mountains are a mountain range in the Maghreb in North Africa. It separates the Sahara Desert from the Mediterranean Sea and the Atlantic Ocean; the name “Atlantic” is derived from the mountain range, which stretches around 2,500 km (1,600 mi) through Morocco, Algeria and Tunisia. The range’s highest peak is Toubkal, which is in central Morocco, with an elevation of 4,167 metres (13,671 ft).[2] The Atlas Mountains are primarily inhabited by Berber populations.[3]
The terms for ‘mountain’ are Adrar and adras in some Berber languages, and these terms are believed to be cognates of the toponym Atlas. The mountains are home to a number of animals and plants which are mostly found within Africa but some of which can be found in Europe. Many of these species are endangered and a few are already extinct. The weather is generally cool but summers are sunny, and the average temperature there is 25 °C.[4]The Atlas Mountains have earned a reputation as a trekkers’ den, attracting adventurers year-round
The basement rock of most of Africa was formed during the Precambrian supereon and is much older than the Atlas Mountains lying on the continent. The Atlas was formed during three subsequent phases of Earth’s geology.
The first tectonic deformation phase involves only the Anti-Atlas, which was formed in the Paleozoic Era (~300 million years ago) as the result of continental collisions. North America, Europe and Africa were connected millions of years ago.
The Anti-Atlas Mountains are believed to have originally been formed as part of the Alleghenian orogeny. These mountains were formed when Africa and America collided and were once a chain rivaling today’s Himalayas. Today, the remains of this chain can be seen in the Fall Line region in the Eastern United States. Some remnants can also be found in the later formed Appalachians in North America.