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Last updated August 26, 2025

The Age of the Sahara: From Green Prairie to Stone Desert

Satellite view of the Sahara Dunes

The Sahara: From the Atlantic Ocean to the Red Sea

The Sahara is today the largest hot desert on the planet, but its history is marked by intense climatic and hydrological cycles. Its formation results from a combination of geological, tectonic, and climatic factors spanning several million years.

Note: The word Sahara comes from the Arabic as-sahraʾ, which literally means "the desert" or "the vast expanse of sand." This term reflects the Arab-Muslim vision of North Africa as a region dominated by arid and desert landscapes. It refers not only to the dunes but to the entire desert ecosystem, including rocky plateaus, regs, oases, and temporary basins.

Geological Origins

The geological structures of the Sahara, including sedimentary basins, peripheral mountain ranges, and stabilized plateaus, testify to long processes: erosion, fluvio-lacustrine deposition, tectonic uplifts, and crustal movements. The formation of dunes and the accumulation of aeolian sediments mainly date back to the Pleistocene, about 2.5 million to 10,000 years ago.

Quaternary Climate Oscillations

During the Quaternary (2.58 million years ago to present), the North African climate was strongly influenced by orbital cycles (precession, obliquity, eccentricity) that modified the seasonal distribution of insolation. These variations caused alternations between humid periods, with lakes and dense vegetation, and arid periods similar to the current Sahara. The humid periods, known as "African Humid Periods," correspond to phases when the African monsoon reached the central Sahara.

The Holocene and the African Humid Period

The main African Humid Period, about 11,500 to 5,500 years ago, allowed the existence of temporary rivers, lakes, and extensive vegetation. Isotopic, sedimentological, and paleoecological analyses show that the Sahara was then a semi-arid to sub-humid environment, favoring the settlement of human populations and animals. The progressive desertification around 4,000 years before our era corresponds to a decline in precipitation and the establishment of the current arid climate.

Chronological Table of Major Events

Chronology and Main Processes of the Sahara
PeriodEvent or PhaseComment
Miocene – Pliocene (23-2.6 Ma)Marine and lacustrine depositsFormation of basins and pre-desert sediments
Pleistocene (2.5 Ma – 10 ka)Gradual establishment of dunesAeolian accumulation linked to glacial and interglacial cycles
Middle QuaternaryAlternating humid periodsActivation of lakes and temporary vegetation, orbital control of insolation
Holocene (11.5 – 5.5 ka)African Humid PeriodExpansion of rivers and lakes, strong human occupation
Around 4 kaFinal desertificationCurrent arid climate, retreat of vegetation and lakes

Future Perspectives for the Sahara

Environmental Challenges

The Sahara, the world's largest hot desert, is at the heart of major environmental challenges. Climate warming is accelerating desertification and threatening fragile ecosystems. However, initiatives are emerging to combat these phenomena:

Economic Opportunities

The Sahara holds natural resources and economic opportunities that are still under-exploited:

Technological Innovations

Technological advances could transform the Sahara into an innovation hub:

Geopolitical Challenges

The stability of the Sahara depends on regional and international cooperation:

Culture and Identity

The Sahara is also a space of cultural and historical diversity:

Scenarios for 2050

By 2050, the Sahara could become:

Table of Ongoing and Planned Projects in the Sahara in 2025

Achievements and Projects in the Sahara in 2025
PeriodCountry / RegionProject / EventComment
2023–2025Western Sahara / DakhlaDakhla Atlantic deep-water portPort capable of accommodating container ships and supertankers, aiming to open up Sahel countries and promote South-South trade. Part of the Moroccan Atlantic Initiative.
2023–2025Western Sahara / DakhlaSeawater desalination plantMeets drinking water needs and supports agricultural and tourist development in the region.
2023–2025North Africa / Central SaharaDesertec project (solar energy)Potential export of solar electricity to Europe and development of green hydrogen. Work continues despite security and governance challenges.
2025Morocco / Dakhla-Oued EddahabRenewable energies and agricultureMultiplication of projects in the solar, wind, agriculture, and tourism sectors, creating local jobs and attracting foreign investment.
2024–2026Algeria / Southern SaharaHassi R’Mel photovoltaic solar parkMajor project for green electricity, aiming to supply cities and reduce dependence on hydrocarbons.
2023–2027Mali / Timbuktu and Saharan regionManagement and valorization of groundwaterMapping of fossil aquifers and installation of boreholes for sustainable agriculture and drinking water supply.
2023–2026Tunisia / Southern SaharaSustainable tourism and ecotourismCreation of protected areas and tourist circuits to develop the local economy while preserving desert ecosystems.
2024–2025Egypt / Western DesertMining exploration and phosphate extractionProjects for the exploitation of mineral deposits, integrating sustainability practices and limiting environmental impact.

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