Draa

Draa

The Draa River, stretching across 1,100 kilometers, holds significant historical and geological importance in Morocco. Its origin lies in the confluence of the Dadès and Imini rivers, which merge to form the mighty Draa. Flowing from the majestic High Atlas Mountains, the river initially heads southeast towards Tagounite, before changing its course to the west, ultimately reaching the Atlantic Ocean just north of Tan-Tan. To manage the flow of the Draa and provide water supply to the regional capital of Ouarzazate, the Mansour Eddahabi dam was constructed in 1971. The Draa Valley, through which the river meanders, is not only known for its natural beauty but also for its rich paleontological significance. Within the valley, the Fezouata formations can be found, which are Lower Ordovician Burgess shale-like deposits. The Draa Valley has been inhabited by humans for thousands of years. Evidence of human occupation dates back to the Lower Paleolithic era, with the discovery of Oldowan and Acheulean tools near Tamegroute. Middle Paleolithic sites are also widespread in the area. Additionally, throughout the valley, one can find Neolithic rock art depicting hunting scenes and domesticated animals. Although the exact chronology of these sites remains uncertain, some of the earliest rock art may date back to the 3rd millennium BC. The Upper Draa Valley, spanning approximately 200 kilometers, is characterized by six stretches of oases and palm groves that extend from north to south. These lush green pockets provide a stark contrast to the surrounding arid landscape and have been vital for agriculture and human settlements in the region for centuries.