Draa River

The Draa is Morocco's longest river, at. It is formed by the confluence of the Dadès River and Imini River. It flows from the High Atlas mountains, initially south-eastward to Tagounite, and from Tagounite mostly westwards to its mouth in the Atlantic Ocean somewhat north of Tan-Tan. In 1971, the Mansour Eddahabi dam was constructed to service the regional capital of Ouarzazate and to regulate the flow of the Draa. Most of the year the part of the Draa after Tagounite falls dry.
In the first half of the 20th century, the lowest course of the Draa marked the boundary between the French protectorate of Morocco and the area under Spanish rule.
The valley contains the Fezouata formations, which are Burgess shale-type deposits dating to the Lower Ordovician, filling an important preservational window between the common Cambrian lagerstätten and the Late Ordovician Soom shale. In the fossilized fauna were numerous organisms previously thought to have died out after the mid-Cambrian.

History

Prehistory

Human occupation in the Draa valley and adjacent mountains dates at least to the Lower Paleolithic, as attested by Oldowan and Acheulean tools found near Tamegroute. Middle Paleolithic sites are widespread.
Neolithic-era rock art can be found throughout the Draa valley, depicting hunting scenes as well as domesticated cattle. The chronology of these sites is uncertain, but the earliest may date to the 3rd millennium BCE.

Before 1054

The Draa River was also well known to the ancient Romans. It figures on the first world map in history made by Ptolemy.

Wattasids

During the reign of the Wattasid Abu al-Abbas Ahmad ibn Muhammad, Askia Ishaq I of the Songhai Empire sent Tuareg raiders into the Draa valley to avenge a diplomatic insult where Morocco had demanded the cession of the valuable Taghaza salt mine.

Saadi

Alaouites

Four of the sons of Ismail Ibn Sharif have been khalifa of the Draa:

Mulay Muhammad as-Sharif bin Ismail as-Samin. Khalifa of the Draa 1703.
Mulay 'Abdu'l-Malik bin Ismail as-Samin. b. ca. 1677. Khalifa of the Draa. He was k. for plotting against his father, 1696.
Mulay Nasir bin Ismail as-Samin. Khalifa of Draa 1702–1703, and of Tafilalt. Rebelled in 1711–1712. He was k. 1714.
H.M. Sultan 'Abu Marwan Mulay 'Abdu'l Malik, Sultan of Morocco, etc. b. at Meknes, after 1696, son of H.M. Sultan 'Abul Nasir Mulay Ismail as-Samin bin Sharif, Sultan of Morocco, educ. privately. Khalifa of the Draa 1701–1703, and of Sus 1717–1718. Proclaimed Sultan on the deposition of his elder half-brother 13 March 1728. Deposed at Meknes 18 July 1728. Fled to Fez and arrested there 23 December 1728. He was k. at Meknes, 2 March 1729.

Language

Two languages are spoken in the area: a local variety of Colloquial Arabic which is closely related to Hassaniya, and Shilha or Tashelhiyt, a Berber language.

Oases

The Upper Draa River valley, about long, consists of six stretches of oases/palm groves from north to south:

The Mezguita oasis, with the Agdz and Auriz and south of it the Tamsikht dam
The oasis of Tinzouline, with Ouled Lagraier, Tinzouline, Ouled Yaoub and a dam south of it
The Ternata oasis with Zagora
The Fezouata oasis with Tamegroute and south of it the Azagha dam
The Ktaoua oasis with Tagounite, Blida, Tiraf and the Bounou dam south of it
The oasis of Mhamid el Ghuzlan with Mhamid el Ghuzlan
Ksour

in the Mezguita

in Tinzouline

in Ternata

in the Fezouata

in the Ktaoua/Ktwawa

This is the southern stretch of the valley between the Azagha and the Bounou dam near Tagounite. There are 55 villages, mostly consisting of ksour '':
Source : Recensement général du Maroc, 1994.

Exploration

The Draa has attracted the attention of a number of notable explorers including Frenchman Charles de Foucauld who travelled throughout Morocco disguised as a Jewish merchant in the 1800s, and Jeffrey Tayler who wrote a book about his experiences.