Saturday, 14 November 2026

AFRICA: DESERTS

(1). Introduction

* Africa is home to the world's largest hot desert – the Sahara Desert.

* Deserts are mainly concentrated in North Africa, the Horn of Africa and Southern Africa.

* African deserts include hot deserts, semi-arid regions and coastal deserts.

* Most African deserts receive very low and irregular rainfall.

(2). Major Deserts of Africa

(1). Sahara Desert

* World's largest hot desert.

* Located in North Africa.

* Covers approximately 9.2 million km².

* Extends from the Atlantic Ocean to the Red Sea.

* Countries include Algeria, Libya, Egypt, Chad, Niger, Mali, Mauritania, Morocco, Tunisia and Sudan.

(2). Libyan Desert

* Located mainly in eastern Libya and western Egypt.

* Forms part of the eastern Sahara.

* Characterised by extensive sand dunes and rocky plateaus.

(3). Nubian Desert

* Located in northeastern Sudan.

* Lies between the Nile River and the Red Sea region.

* Characterised by rocky and sandy terrain.

(4). Namib Desert

* Located along the southwestern coast of Africa, mainly in Namibia.

* One of the world's oldest deserts.

* Influenced by the cold Benguela Current.

* Famous for its enormous sand dunes.

(5). Kalahari Desert

* Located in Southern Africa.

* Extends across Botswana, Namibia and South Africa.

* It is a semi-arid sandy region.

* Supports grasslands, shrubs and wildlife.

(6). Danakil Desert

* Located in the Afar region of Ethiopia, Eritrea and Djibouti.

* Known for extreme heat, salt flats and volcanic landscapes.

* Contains the Danakil Depression.

(7). Ténéré Desert

* Located in central Sahara, mainly in Niger.

* Characterised by vast sand dunes.

* Known as the desert within a desert.

(8). Chalbi Desert

* Located in northern Kenya.

* One of the driest regions of Kenya.

* Contains sandy and rocky surfaces.

(9). Moçâmedes Desert

* Located in southwestern Angola.

* Associated with the Namib Desert system.

* Influenced by the cold Benguela Current.

(10). Bayuda Desert

* Located in northeastern Sudan.

* Lies within the great bend of the Nile.

* Characterised by rocky and sandy landscapes.

(3). Other Important Desert Regions

* Tanezrouft Desert: Located in southern Algeria and northern Mali.

* El Djouf: A desert region of Mauritania and Mali.

* Lompoul Desert: Located in northwestern Senegal.

* Ogaden: An arid region of eastern Ethiopia.

* Guban: A narrow arid coastal region of northern Somalia.

* Grand Bara: Located in Djibouti.

* Nyiri Desert: Located in southern Kenya.

* Great Karoo: A semi-arid plateau region in South Africa.

4 Why Are African Deserts Formed?

Important factors:

* Subtropical High Pressure: Descending dry air around 20°–30° latitude inhibits rainfall.

* Cold Ocean Currents: Benguela Current contributes to dryness along southwestern Africa.

* Continentality: Interior regions receive limited moisture from oceans.

* Rain Shadow Effect: Mountains block moisture-bearing winds in some areas.

* Trade Winds: Dry continental air contributes to arid conditions in certain regions.

6 Important Facts for Competitive Exams:

* Largest hot desert: Sahara Desert.

* Oldest desert: Namib Desert.

* Cold ocean current near Namib: Benguela Current.

* Famous desert depression: Danakil Depression.

* Largest desert region in Southern Africa: Kalahari.

* Ténéré Desert: Part of the Sahara.

* Major desert of Kenya: Chalbi Desert.

* Major desert of Namibia: Namib Desert.

* Tibesti: Mountain massif in the Sahara, not a desert.

* Great Karoo: Semi-arid region of South Africa.

7 Quick Revision:

Remember these distinctions

* Sahara – Largest hot desert.

* Namib – One of the oldest deserts.

* Kalahari – Semi-arid sandy region.

* Danakil – Extreme heat and volcanic landscape.

* Chalbi – Northern Kenya.

* Moçâmedes – Southwestern Angola.

* Benguela Current – Cold current along southwestern Africa.

Exam tip: Do not confuse the Sahara, Kalahari and Namib. Their locations, climatic conditions and geographical characteristics are frequently important in physical geography examinations.

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