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Algeria · Landforms

Mountain Ranges, Deserts and Landforms of Algeria

Africa is the largest of the 17 mountain ranges, deserts and other landforms recorded for Algeria, at 29.41M km², ahead of Sahara at 4.73M km². The full list follows.

How this list is built: Ranked by mapped area. Covers mountain ranges, deserts, plateaus, named glaciers, plains, basins, peninsulas and capes. One that crosses a border is listed under every country it lies in, with the area of the whole feature. It covers the mountain ranges, deserts and other landforms indexed in YearMaps, drawn from open geospatial data, and is not an exhaustive national register.

Landforms Listed
17
Top Ranked
29.41M km²
Africa
Second
4.73M km²
Sahara
Profiled Below
6
Photo, encyclopedia text and figures
Mountain Ranges, Deserts and Landforms of Algeria
#NameArea
1Africa29.41M km²
2Sahara4.73M km²
3Sahel1.02M km²
4Ténéré348,246 km²
5AHAGGAR Mountains185,343 km²
6Tassili oua-n-Ahaggar150,456 km²
7Grand Erg Oriental127,027 km²
8Tassili-n-Ajjer123,986 km²
9Hamada de Tinrhert120,350 km²
10‘Erg Chech111,855 km²
11Grand Erg Occidental89,552 km²
12Plat. du Tademaït82,994 km²
13Atlas Mountains63,011 km²
14‘Erg Iguidi35,106 km²
15Hamada du Drâa11,707 km²
16Atlas Tellien172 km²
17Atlas Saharien133 km²

The Landforms of Algeria in Detail

The 6 mountain ranges, deserts and other landforms above that have an encyclopedia article, in the same order, each with its photograph, figures and the places around it.

Sahara
Image via Wikimedia Commons (author and licence on the file page).

Sahara

Desert · 4.73M km²

Sahara is a desert in Africa, covering an estimated 4.73M km². It extends across Sudan, Libya, Egypt, Chad, Mali, Niger, Algeria, Mauritania, Morocco and Tunisia. It is the largest of the 58 deserts with a mapped extent in YearMaps.

The Sahara (, ) is a desert spanning North Africa. With an area of 9,200,000 square kilometres (3,600,000 sq mi), it is the largest hot desert in the world and the third-largest desert overall, smaller only than the deserts of Antarctica and the northern Arctic.

The desert covers much of North Africa, excluding the fertile region on the Mediterranean Sea coast, the Atlas Mountains of the Maghreb, and the Nile Valley in Egypt and the Sudan.

It stretches from the Red Sea in the east and the Mediterranean in the north to the Atlantic Ocean in the west, where the landscape gradually changes from desert to coastal plains. To the south it is bounded by the Sahel, a belt of semi-arid tropical savanna around the Niger River valley and the Sudan region of sub-Saharan Africa. The Sahara can be divided into several regions, including the western Sahara, the central Ahaggar Mountains, the Tibesti Mountains, the Aïr Mountains, the Ténéré desert, and the Libyan Desert.

Adapted from Wikipedia: Sahara (CC BY-SA 4.0).

Feature class
Desert
Mapped extent
4.73M km²
Size rank
#1 of 58 deserts
Region
Africa
Countries
Sudan, Libya, Egypt, Chad, Mali, Niger, Algeria, Mauritania, Morocco, Tunisia
Coordinates
27.0430°, 22.0108°
Summits:
Tahat (2,908 m), Lalla Khedidja (2,308 m), Djebel Chelia (2,326 m)
Ranges:
Haut Atlas (Africa), Anti Atlas (Africa)
Settlements:
Adrar (403 km), Reggane (451 km), Timimoun (499 km)

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Geography

The Sahara covers large parts of Algeria, Chad, Egypt, Libya, Mali, Mauritania, Niger, Western Sahara and Sudan, and parts of southern Morocco and Tunisia. It covers 9 million square kilometres (3,500,000 sq mi), 31% of the African continent. If all areas with a mean annual precipitation of less than 250 mm (9.8 in) were included, the Sahara would be 11 million square kilometres (4,200,000 sq mi). It is one of three distinct physiographic provinces of the African massive physiographic division. The Sahara is so large and bright that, in theory, it could be detected from other stars as a surface feature of Earth, with near-current technology.

Climate

The Sahara is the world's largest hot desert. It is located in the horse latitudes under the subtropical ridge, a significant belt of semi-permanent subtropical warm-core high pressure where the air from the upper troposphere usually descends, warming and drying the lower troposphere and preventing cloud formation.

The permanent absence of clouds allows unhindered light and thermal radiation. The stability of the atmosphere above the desert prevents any convective overturning, thus making rainfall virtually non-existent. As a consequence, the weather tends to be sunny, dry and stable with a minimal chance of rainfall. Subsiding, diverging, dry air masses associated with subtropical high-pressure systems are extremely unfavorable for the development of convectional showers.

History

Scientists have identified more than 230 humid periods in North Africa over the past eight million years, recurring at intervals of approximately 21,000 years.

A modern laboratory examination of the Uan Muhuggiag child mummy and Tin Hanakaten child have suggested that the Central Saharan peoples from the Epipaleolithic, Mesolithic, and Pastoral periods possessed dark skin complexions. The creators of the Round Head rock art possessed dark skin.

A 2025 study sequenced individuals from Takarkori (7,000 YBP) and discovered that most of their ancestry was from an unknown ancestral North African lineage, related to the African admixture component found in Iberomaurusians.

Sections adapted from Wikipedia: Sahara (CC BY-SA 4.0).

Sahara: Key Facts

Key facts about Sahara
Area9,200,000 km²
Highest pointEmi Koussi

Facts from Wikidata Q6583 (CC0).

Sahel
Image via Wikimedia Commons (author and licence on the file page).

Sahel

Plain · 1.02M km²

Sahel is a plain in Africa, covering an estimated 1.02M km². It extends across Mauritania, Sudan, Niger, Chad, Mali, Egypt, Senegal, South Sudan, Nigeria, Eritrea, the Central African Republic, Cameroon, Burkina Faso and Algeria. It is the 17th-largest of the 231 landforms with a mapped extent in YearMaps.

The Sahel region (; from Arabic ساحل sāḥil [ˈsaːħil], "coast, shore"), or Sahelian acacia savanna, is a biogeographical region in Africa. It is the transition zone between the more humid Sudanian savannas to its south and the drier Sahara to the north. The Sahel has a hot semi-arid climate and stretches across the southernmost latitudes of North Africa between the Atlantic Ocean and the Red Sea. Although geographically located in the tropics, the Sahel does not have a tropical climate.

The Sahel has one of the world's fastest-growing populations due to its high human birthrate, with approximately 80 million people in 2018. The western Sahel in particular has experienced frequent food and water shortages due to droughts caused by its semi-arid climate, as well as high levels of government corruption. Since the 2010s, various coups, insurgencies, terrorist incidents, and foreign interventions have taken place across the Sahel and Françafrique, leading to the region being called the Coup Belt. As a result, the Sahel is viewed as both an ecoregion and a geopolitical space shaped by internal instability and external strategic competition.

Adapted from Wikipedia: Sahel (CC BY-SA 4.0).

Feature class
Plain
Mapped extent
1.02M km²
Size rank
#17 of 231 landforms
Region
Africa
Countries
Mauritania, Sudan, Niger, Chad, Mali, Egypt, Senegal, South Sudan, Nigeria, Eritrea, Central African Republic, Cameroon, Burkina Faso, Algeria
Coordinates
15.5072°, 15.0064°
Summits:
Tahat (2,908 m), Djebel Chelia (2,326 m), Lalla Khedidja (2,308 m)
Ranges:
Marrah Mountains (Africa), Al Jabal al Akhdar (Africa)
Settlements:
Tamanrasset (1,283 km), Arak (1,598 km), I-n-Salah (1,836 km)

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Geography

The Sahel spans 5,900 km (3,670 mi) from the Atlantic Ocean in the west to the Red Sea in the east, in a belt several hundred to a thousand kilometers (c. 600 miles) wide. It covers an area of 3,053,200 square kilometers (1,178,850 sq mi).

Representing a climatic and ecological transition zone with hot semi-desert and steppe conditions, the region borders the more humid Sudanian savannas to its south and the dry Sahara desert to the north. This ecoregion is also called the Sahelian acacia savanna in honour of its most prominent and very drought tolerant genus of tree.

The topography is mainly flat; most of the region lies between 200 and 400 meters (660 and 1,310 ft) in elevation.

History

Around 4000 BC, the climate of the Sahara and the Sahel started to become drier at an exceedingly fast pace. This climate change caused lakes and rivers to shrink significantly and caused increasing desertification. This in turn decreased the amount of land conducive to settlements and caused migrations of farming communities to the more humid climate of West Africa.

The larger Sahelian kingdoms emerged from 750 AD and founded several large cities in the Niger valley region, including Timbuktu, Gao and Djenné.

The kingdom of Alodia was a Christian Nubian Kingdom in the eastern Sahel that reached its zenith from the 9th to 12th century. It was first mentioned in 569, its capital Soba located near modern-day Khartoum.

Sections adapted from Wikipedia: Sahel (CC BY-SA 4.0).

Ténéré
Image via Wikimedia Commons (author and licence on the file page).

Ténéré

Desert · 348,246 km²

Ténéré is a desert in Africa, covering an estimated 348,246 km². It extends across Niger, Algeria and Chad. It is the 6th-largest of the 58 deserts with a mapped extent in YearMaps.

The Ténéré (Tuareg: Tenere, literally: "desert") is a desert region in south central Sahara. It comprises a vast plain of sand stretching from northeastern Niger to western Chad, occupying an area of over 400,000 square kilometres (150,000 sq mi). It is bounded by the Aïr Mountains in the west, the Hoggar Mountains in the north, the Djado Plateau in the northeast, the Tibesti Mountains in the east, and the basin of Lake Chad in the south. The central part of the desert contains the Erg of Bilma, an area of sand dunes. The Neolithic Tenerian culture was centred on the region.

Adapted from Wikipedia: Ténéré (CC BY-SA 4.0).

Feature class
Desert
Mapped extent
348,246 km²
Size rank
#6 of 58 deserts
Region
Africa
Countries
Niger, Algeria, Chad
Coordinates
19.2157°, 13.9936°
Summits:
Tahat (2,908 m), Djebel Chelia (2,326 m), Lalla Khedidja (2,308 m)
Ranges:
Al Jabal al Akhdar (Africa), Moyen Atlas (Africa)
Settlements:
Tamanrasset (410 km), Arak (615 km), I-n-Salah (820 km)

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Climate

The Ténéré has a hot desert climate (Köppen climate classification BWh), typical of the large Sahara Desert. The climate is hyper-arid, extremely hot, sunny and dry year-round and there is virtually no plant life. The average high temperatures are above 40 °C (104 °F) for about 5 months and more in the hottest regions, and record high temperatures as high as 50 °C (122 °F) are highly possible during summer. The annual average high temperature is around 35 °C (95 °F). During "winter" months, the average high temperatures stay above 25 °C (77 °F) and generally hover around 30 °C (86 °F).

History

During the Carboniferous period, the region was beneath the sea; later it was a tropical forest. A major dinosaur cemetery lies southeast of Agadez at Gadoufaoua; many fossils have been found there, having eroded out from the ground. An almost complete specimen of the crocodile-like reptile Sarcosuchus imperator, nicknamed the SuperCroc, was discovered there by paleontologists.

During early human history, this was a fertile land much more congenial to human life than it is now. The region was inhabited by modern humans as long ago as the Paleolithic period some 60,000 years ago. They hunted wild animals and left evidence of their presence in the form of stone tools including tiny, finely carved arrow heads.

Sections adapted from Wikipedia: Ténéré (CC BY-SA 4.0).

Ténéré: Key Facts

Key facts about Ténéré
Area400,000 km²

Facts from Wikidata Q272521 (CC0).

Grand Erg Oriental
Image via Wikimedia Commons (author and licence on the file page).

Grand Erg Oriental

Desert · 127,027 km²

Grand Erg Oriental is a desert in Africa, covering an estimated 127,027 km². It extends across Algeria, Tunisia and Libya. It is the 17th-largest of the 58 deserts with a mapped extent in YearMaps.

The Grand Erg Oriental (English: Great Eastern Sand Sea) is a large erg or "field of sand dunes" in the Sahara Desert. Situated for the most part in Saharan lowlands of northeast Algeria, the Grand Erg Oriental covers an area of some 185,000 sq. km (about the size of North Dakota or twice the size of Portugal). It is the second largest erg in Algeria after Erg Chech.

The erg's northeastern edge spills over into neighbouring Tunisia (about 30,000 sq. km) It borders the Atlas and the Aurès Mountains as well as the mountainous region of Jebel Dahar in Tunisia to the north, and the Hamada of Tinrhert and the Tademait Plateau to the south. - Erg is a Tamachek Berber word, and also a geographic term of art.

Adapted from Wikipedia: Grand Erg Oriental (CC BY-SA 4.0).

Feature class
Desert
Mapped extent
127,027 km²
Size rank
#17 of 58 deserts
Region
Africa
Countries
Algeria, Tunisia, Libya
Coordinates
30.9328°, 8.3934°
Summits:
Djebel Chelia (2,326 m), Lalla Khedidja (2,308 m), Tahat (2,908 m)
Ranges:
Moyen Atlas (Africa), Haut Atlas (Africa)
Settlements:
Ouargla (254 km), Touggourt (331 km), El Oued (347 km)

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Hydrology

The climate is hyper arid, with average annual precipitation of 60 mm in the north of the erg. Further south, it decreases, reaching 25 mm at the southern edge. However, there is a lot of water stored underground: the Aquifer Continental Intercalaire, one of the largest closed aquifers in the world, stores around 60,000 cubic kilometers of water and extends over large areas of the Algerian, Tunisian, and Libyan northern Sahara. Most of this water is fossil water that seeped into the ground during the wet periods of the Pleistocene in the Atlas Mountains and Aurès region, the M'zab ridge west of Touggourt, and the Dahar mountain range in southern Tunisia. These elevations are located in the vicinity of the erg.

Sections adapted from Wikipedia: Grand Erg Oriental (CC BY-SA 4.0).

Grand Erg Oriental: Key Facts

Key facts about Grand Erg Oriental
Area185,000 km²

Facts from Wikidata Q307143 (CC0).

Tassili-n-Ajjer
Image via Wikimedia Commons (author and licence on the file page).

Tassili-n-Ajjer

Desert · 123,986 km²

Tassili-n-Ajjer is a desert in Africa, covering an estimated 123,986 km². It extends across Algeria and Libya. It is the 18th-largest of the 58 deserts with a mapped extent in YearMaps.

Tassili n'Ajjer (Berber: Tassili n Ajjer, Arabic: طاسيلي ناجر, romanized: ṭāssīlī naʾjir; "Plateau of rivers") is a mountain range in the Sahara desert, located in south-eastern Algeria. It holds one of the most important groupings of prehistoric cave art in the world and covers an area of more than 72,000 km2 (28,000 sq mi).

The site has been designated a national park and a Biosphere Reserve, and was inducted into the UNESCO World Heritage Site list in 1982.

The literal English translation of Tassili n'Ajjer is 'plateau of rivers'.

Adapted from Wikipedia: Tassili n'Ajjer (CC BY-SA 4.0).

Feature class
Desert
Mapped extent
123,986 km²
Size rank
#18 of 58 deserts
Region
Africa
Countries
Algeria, Libya
Coordinates
25.6973°, 7.8586°
Summits:
Tahat (2,908 m), Djebel Chelia (2,326 m), Lalla Khedidja (2,308 m)
Ranges:
Moyen Atlas (Africa), Haut Atlas (Africa)
Settlements:
Tamanrasset (398 km), Arak (429 km), I-n-Salah (583 km)

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Geography

Tassili n'Ajjer is a plateau in south-eastern Algeria at the borders of Libya and Niger, covering an area of 72,000 km2. It ranges from 26°20′N 5°00′E east-south-east to 24°00′N 10°00′E. Its highest point is the Adrar Afao that peaks at 2,158 m (7,080 ft), located at 25°10′N 8°11′E. The nearest towns are Djanet on the southeastern edge and Illizi on the northern edge.

The plateau is of great geological and aesthetic interest. Its panorama of geological formations consisting of rock forests, composed of eroded sandstone, resembles a lunar landscape and hosts a range of rock art styles.

Geology

The range is composed largely of sandstone. The sandstone is stained by desert varnish, a thin outer layer of deposited metallic oxides that colour the rock formations variously from near-black to dull red. Erosion in the area has resulted in nearly 300 natural rock arches being formed in the south east, along with deep gorges and permanent water pools in the north.

The Tuareg Shield, an accumulation of terranes that formed during the Neoproterozoic era between 750 and 550 million years ago, encompassed the area of today's Ahaggar Mountains in Algeria, the Aïr Mountains in Niger, and the Adrar des Ifoghas in Mali. To the west lies the West African Craton, to the east the Saharan Metacraton.

Sections adapted from Wikipedia: Tassili n'Ajjer (CC BY-SA 4.0).

Tassili-n-Ajjer: Key Facts

Key facts about Tassili-n-Ajjer
Area72,000 km²
Highest pointJebel Azao

Facts from Wikidata Q190048 (CC0).

Grand Erg Occidental
Image via Wikimedia Commons (author and licence on the file page).

Grand Erg Occidental

Desert · 89,552 km²

Grand Erg Occidental is a desert in Africa, covering an estimated 89,552 km². It is the 23rd-largest of the 58 deserts with a mapped extent in YearMaps.

The Grand Erg Occidental, (also known as the Western Sand Sea), Arabic العرق الغربي الكبير (al-ʿIrq al-Ḡarbī al-Kabīr), is an erg in the northern center of the Algerian Sahara. It is the third largest erg in Algeria after the Erg Chech and the Grand Erg Oriental.

Adapted from Wikipedia: Grand Erg Occidental (CC BY-SA 4.0).

Feature class
Desert
Mapped extent
89,552 km²
Size rank
#23 of 58 deserts
Region
Africa
Coordinates
30.0943°, -0.6347°
Summits:
Jebel Toubkal (4,165 m), Rock of Gibraltar (426 m), Mulhacén (3,479 m)
Ranges:
Haut Atlas (Africa), Moyen Atlas (Africa)
Settlements:
Timimoun (129 km), Béchar (227 km), Adrar (250 km)

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Geography

The Grand Erg Occidental borders the Hamada Bet Touadjine and the Monts des Ksour of the Saharan Atlas to the south. To the west, it is adjacent to the Hamada du Guir, to the south to the Tademait Plateau, and to the east to the Chebka du Mzab. It extends approximately 550 km from east to west and 340 km from north to south, covering an area of approximately 75,000 km². The erg is roughly bordered in the west by National Road (RN) 6 and the Oued Saoura, in the north by RN6B, in the east by RN107, and in the south by RN1 and RN51. It is crossed in a north-south direction by RN118.

Climate

Average annual rainfall varies between 62 mm in the northwest, 47 mm in the east, 36 mm in the southwest, and 33 mm in the center of the erg. These amounts are relatively high compared to other ergs. For example, in the neighboring Erg Er Raoui, they range from 16 mm to 19 mm, and in the Erg Chech from 8 mm to 10 mm.

From December to March, the northeast wind is the strongest (northeast trade winds), from June to September, the east wind dominates, and during the other months, it is mainly the east wind. The strongest winds blow in April and May, and the weakest from October to January.

Hydrology

The erg region forms part of the southwestern edge of the Aquifer Continental Intercalaire, one of the largest closed aquifers in the world. This aquifer layer begins at a depth of approximately 300 to 500 m below the surface of the erg. Above it lies the Grand Erg Occidental aquifer, fed by the oueds of the Saharan Atlas, floods at Jebel El Kehla in Morocco, and rainwater infiltration. The water does not flow through the sand of the erg, but below it, in a limestone formation dating from the Miocene and Pliocene epochs. At the southern edge of the erg, the water table is close to the surface, which allows the Gourara region to be irrigated using the foggara system.

Sections adapted from Wikipedia: Grand Erg Occidental (CC BY-SA 4.0).

Grand Erg Occidental: Key Facts

Key facts about Grand Erg Occidental
Area75,000 km²

Facts from Wikidata Q1537020 (CC0).

More on Algeria

Quick Answers

What is the largest landform in Algeria?
Africa, at 29.41M km². Sahara is second at 4.73M km². Rankings cover the mountain ranges, deserts and other landforms indexed in YearMaps.
How many mountain ranges, deserts and other landforms are there in Algeria?
YearMaps lists 17 mountain ranges, deserts and other landforms for Algeria. This is the number mapped in the atlas, not an official national count.