Mountain And Alpine Reserves Codexery

Ennedi Plateau

Mountain range in the central Sahara, home to the Toubou people and the highest peak in the Sahara.

Ennedi Plateau

The Tibesti Mountains are a mountain range in the central Sahara, primarily located in the extreme north of Chad, with a small portion located in southern Libya. The highest peak in the range, Emi Koussi, lies to the south at a height of 3,415 meters (11,204 ft) and is the highest point in both Chad and the Sahara. The central third of the Tibesti is of volcanic origin and consists of five volcanoes topped by large depressions: Emi Koussi, Tarso Toon, Tarso Voon, Tarso Yega and Toussidé. Major lava flows have formed vast plateaus that overlie Paleozoic sandstone. The volcanic activity was the result of a continental hotspot that arose during the Oligocene and continued in some places until the Holocene, creating fumaroles, hot springs, mud pools and deposits of natron and sulfur.

UNESCO World Heritage Status
Added in July 2016

Lore & Background

Tibesti, which means 'place where the mountain people live', is the domain of the Toubou people. The Toubou live mainly along the wadis, on rare oases where palm trees and limited grains grow. They harness the water that collects in gueltas, the supply of which is highly variable from year-to-year and decade-to-decade. The plateaus are used to graze livestock in the winter and harvest grain in the summer. Temperatures are high, although the altitude ensures that the range is cooler than the surrounding desert. The Toubou, who were settled in the range by the 5th century BC, adapted to these conditions and turned the range into a large natural fortress. They arrived in several waves, taking refuge in times of conflict and dispersing in times of prosperity, although not without intense internal hostility at times.

Reader's Guide

The Toubou came into contact with the Carthaginians, Berbers, Tuaregs, Ottomans and the Arabs, as well as the French colonists who first entered the range in 1914 and took control of the area in 1929. The independent spirit of the Toubou and the geopolitics of the region has complicated the exploration of the range as well as the ascent of its peaks. Tensions continued after Chad and Libya gained independence in the mid-20th century, with hostage-taking and armed struggles occurring amid disputes over the allocation of natural resources. The geopolitical situation and the lack of infrastructure has hampered the development of tourism. The Saharomontane flora and fauna, which include the rhim gazelle and Barbary sheep, have adapted to the mountains, yet the climate has not always been as harsh. Greater biodiversity existed in the past, as evidenced by scenes portrayed in rock and parietal art found throughout the range, which date back several millennia, even before the arrival of the Toubou.

Did You Know?

Volcanic Architecture & Geological Formation

The central third of the Tibesti is of volcanic origin and consists of five volcanoes topped by large depressions: Emi Koussi, Tarso Toon, Tarso Voon, Tarso Yega and Toussidé. Major lava flows have formed vast plateaus that overlie Paleozoic sandstone. The volcanic activity was the result of a continental hotspot that arose during the Oligocene and continued in some places until the Holocene, creating fumaroles, hot springs, mud pools and deposits of natron and sulfur. Erosion has shaped volcanic spires and carved an extensive network of canyons through which run rivers subject to highly irregular flows that are rapidly lost to the desert sands. The range includes five shield volcanoes with broad bases whose diameter can reach 80 km (50 mi): Emi Koussi; Tarso Toon, which rises 2,575 m (8,448 ft) above sea level; Tarso Voon; Tarso Yega; and Tarso Toussidé, which culminates in the peak of the same name. Several of these peaks are topped with large calderas. Tarso Yega has the largest caldera, with a diameter of 19 to 20 km (12 to 12 mi) and a depth of approximately 300 m (980 ft), while Tarso Voon has the deepest caldera, with a depth of approximately 1,000 m (3,300 ft) and a diameter of 12 to 13 km (7.5 to 8.1 mi).

The Toubou & Mountain Life

Tibesti, which means 'place where the mountain people live', is the domain of the Toubou people. The Toubou live mainly along the wadis, on rare oases where palm trees and limited grains grow. They harness the water that collects in gueltas, the supply of which is highly variable from year-to-year and decade-to-decade. The plateaus are used to graze livestock in the winter and harvest grain in the summer. Temperatures are high, although the altitude ensures that the range is cooler than the surrounding desert. The Toubou, who were settled in the range by the 5th century BC, adapted to these conditions and turned the range into a large natural fortress. They arrived in several waves, taking refuge in times of conflict and dispersing in times of prosperity, although not without intense internal hostility at times. The Tibesti Mountains are named for the Toubou people, also written Tibu or Tubu, that inhabit the area. In the Kanuri language, tu means 'rocks' or 'mountain' and bu means 'a person' or 'dweller,' and thus Toubou roughly translates to 'people of the mountains' and Tibesti to the 'place where the mountain people live'.

Geopolitical History & Colonial Encounters

The Toubou came into contact with the Carthaginians, Berbers, Tuaregs, Ottomans and the Arabs, as well as the French colonists who first entered the range in 1914 and took control of the area in 1929. The independent spirit of the Toubou and the geopolitics of the region has complicated the exploration of the range as well as the ascent of its peaks. Tensions continued after Chad and Libya gained independence in the mid-20th century, with hostage-taking and armed struggles occurring amid disputes over the allocation of natural resources. The geopolitical situation and the lack of infrastructure has hampered the development of tourism.

Ecology, Rock Art & Cultural Imagination

The Saharomontane flora and fauna, which include the rhim gazelle and Barbary sheep, have adapted to the mountains, yet the climate has not always been as harsh. Greater biodiversity existed in the past, as evidenced by scenes portrayed in rock and parietal art found throughout the range, which date back several millennia, even before the arrival of the Toubou. The isolation of the Tibesti has sparked the cultural imagination in both art and literature.

Frequently Asked Questions

What is the Ennedi Plateau?

It is a sandstone massif in northeastern Chad that forms part of the larger Ennedi Massif within the Sahelian belt. The site spans two administrative regions, Ennedi-Ouest and Ennedi-Est.

Where exactly is the Ennedi Plateau located?

The plateau sits in the northeastern part of Chad, straddling the Ennedi-Ouest and Ennedi-Est regions. It belongs to the broader Ennedi Massif, which falls within the country's Sahelian zone.

What makes the Ennedi Plateau's rock art significant?

The plateau bears extensive petroglyphs nearly 7,000 years old, primarily depicting cattle. These images reflect the deep economic, environmental, and cultural importance that herds held for both hunter-gatherer and pastoralist communities of the past.

When did the Ennedi Plateau gain UNESCO World Heritage status?

It was inscribed on the UNESCO World Heritage List in July 2016. The designation recognizes the site's ancient rock art alongside its unique fauna.

Who inhabits the Ennedi Plateau region today?

Semi-nomadic Muslim communities currently live in the area, sustaining themselves through herds of camels, donkeys, sheep, and goats. Their pastoral way of life continues a tradition of animal husbandry that stretches back millennia.

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