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The Levante in Spain. The Levante (Spanish:; Catalan: Llevant [ʎəˈβan, ʎəˈvant, ʎeˈβan, ʎeˈvant]; "Levant, East") is a name used to refer to the eastern region of the Iberian Peninsula, on the Spanish Mediterranean coast.
The term Levant appears in English in 1497, and originally meant 'the East' or 'Mediterranean lands east of Italy'. [23] It is borrowed from the French levant 'rising', referring to the rising of the sun in the east, [23] or the point where the sun rises. [24] The phrase is ultimately from the Latin word levare, meaning 'lift, raise'.
The group of over 700 sites of prehistoric Rock art of the Iberian Mediterranean Basin, also known as Levantine art, were collectively declared a World Heritage Site by UNESCO in 1998. The sites are in the eastern part of Spain and contain rock art dating to the Upper Paleolithic or (more likely) Mesolithic periods of the Stone Age .
Levante, Spain, the eastern Iberian coastal region of Spain Riviera di Levante, an Italian name for the eastern section of the Italian Riviera Sestri Levante , an Italian town
Named after its regional range, the Levantine Bronze Age (or Bronze of Levant, or Valencian Bronze) refers to a culture extended over the actual territory of the Valencian Community, in the "Levante" or eastern side of the Iberian peninsula. Its chronological range was between 2200 BC and 1500 BC.
Over recorded history, there have been many names of the Levant, a large area in the Near East, or its constituent parts. These names have applied to a part or the whole of the Levant . On occasion, two or more of these names have been used at the same time by different cultures or sects.
The history of the Mediterranean region and of the cultures and people of the Mediterranean Basin is important for understanding the origin and development of the Mesopotamian, Egyptian, Canaanite, Phoenician, Hebrew, Carthaginian, Minoan, Greek, Persian, Illyrian, Thracian, Etruscan, Iberian, Roman, Byzantine, Bulgarian, Arab, Berber, Ottoman ...
Levant cloud forming against the eastern cliffs of the Rock of Gibraltar. The Rock of Gibraltar is a monolithic promontory. The Main Ridge has a sharp crest with peaks over 400 metres (1,300 ft) above sea level, formed by Early Jurassic limestones and dolomites. [5] It is a deeply eroded and highly faulted limb of an overturned fold.