Libyan Desert

When we think of deserts, we conjure up images of sand dunes, barren, arid regions of great heat, and nowhere will you find a higher temperature than that recorded at Al 'Aziziyah in the Libyan Desert, which reached a record 57.8C or 136.0°F in 1922; the highest naturally occurring temperature ever recorded. The Libyan desert, which covers most of eastern Libya and forms part of its north-eastern section, is the most inhospitable of the inhospitable. The Libyan Desert went largely uncharted until 1924 when the explorer Ahmed Hassanein, the grandson of the last Admiral of the Egyptian fleet, undertook a 2200 mile expedition deep into the heart of the desert, discovering the Jebel Uweinat mountain ~ Mountain of Sourcelets ~ on the Egyptian, Libyan and Sudanese border, named after the spring 'Ain Dua' found at the foot of the mountain on its Libyan side.

He also encountered the hostile Senussi, a grouping pledged to fight colonial expansion in the region, particularly Italy, after their Libyan forays that started in 1911. The Grand Senussi's grandson was later to become King Idris I of Libya in 1951 until he was overthrown in a military coup in 1969 by Colonel Gaddafi. Hassanein adventures were published in 1924 in the National Geographic Magazine and a year later in his book 'The Lost Oasis'. Stretching across vast swathes of northeastern Africa, the Libyan Desert is not merely a segment of the Sahara but a distinct and formidable geographic entity. Encompassing western Egypt, eastern Libya, and northern Sudan, this hyper-arid landscape is one of the most uninhabitable yet scientifically fascinating regions on Earth. A realm defined by its extreme aridity, dramatic geological formations, and whispers of ancient civilisations, the Libyan Desert stands as a testament to the raw power of nature and the enduring mysteries of our planet.

The Libyan Desert is almost entirely covered by sand and boulder plains. It’s so dry that no permanent rivers flow through its boundaries. However, water occasionally flows beneath the ground and seeps aboveground into dry streambeds called wadis. Its most iconic features are the immense sand seas, such as the Great Sand Sea, which spans hundreds of kilometres along the Egypt-Libya border, and the Calanshio Sand Sea to its west. These colossal accumulations of sand dunes, some reaching heights of over 100 meters, create a mesmerising, undulating ocean of golden-orange earth. Interspersed with these sandy expanses are vast, rocky plateaus. The most famous among these is the Gilf Kebir (meaning "the Great Barrier" in Arabic) in southwestern Egypt, a massive sandstone massif that rises abruptly from the desert floor, riddled with wadis (dry riverbeds) and prehistoric rock art with the UNESCO-listed Rock-Art Sites of Tadrart Acacus containing thousands of cave paintings dating from 12,000 BC to 100 AD. These ancient artworks provide glimpses into the lives and cultures of prehistoric inhabitants of the region.

Beyond the dunes and plateaus, the desert is punctuated by several significant depressions, many of which host vital oases. In Egypt, these include the Qattara Depression, one of the world's largest natural depressions, and the fertile oases of Siwa, Farafra, Bahariya, Dakhla, and Kharga, which have sustained human life for millennia. These oases, fed by ancient underground aquifers, are islands of green in an otherwise barren expanse, supporting date palms, olive groves, and small communities.

 
 
 
 


Libyan Desert

Libyan Desert

Libyan Desert

Libyan Desert

 


About Africa

About Africa

This article about the Libyan Desert is part of our About Africa series for volunteers. More here!
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Libyan Desert

Libyan Desert

Libyan Desert Facts

The climate of the Libyan Desert is unequivocally one of the harshest on Earth. Rainfall is virtually non-existent, often going years without a single measurable drop. When it does occur, it is typically in localised, intense downpours that quickly evaporate or sink into the parched ground. Temperatures swing wildly, with scorching daytime highs often exceeding 50°C (122°F) in summer, plummeting to near-freezing temperatures at night. The relentless sun and low humidity create an evaporation rate that far outstrips any precipitation. Strong winds are common, often whipping up colossal sandstorms (haboobs) that can obscure visibility for days and reshape the desert's surface. These extreme conditions make the Libyan Desert an invaluable natural laboratory for studying adaptation to aridity and ancient climate patterns.

The geological narrative of the Libyan Desert is exceptionally rich, stretching back millions of years. Much of its surface is composed of Nubian Sandstone, a vast formation laid down during the Mesozoic Era. Beneath this lie older crystalline rocks. The desert's dramatic features are the result of aeons of wind and water erosion, although evidence of past wetter climates, such as ancient river channels and lakebeds, is abundant. This geological history also accounts for some of its most intriguing phenomena, such as Libyan Desert Glass – a rare, naturally occurring tektite, believed to be the by-product of a meteorite impact that occurred some 29 million years ago. This yellowish, translucent glass, found uniquely in this region, adds another layer of scientific intrigue to the desert's mystique.

Despite its formidable nature, the Libyan Desert has not always been devoid of human presence. Archaeological evidence, particularly in the Gilf Kebir and Uweinat regions, reveals a vibrant past. As noted above, cave paintings and rock engravings, some dating back over 7,000 years, depict elephants, giraffes, antelopes, and the daily lives of hunter-gatherers, providing irrefutable proof of a much wetter, greener Sahara during the African Humid Period. These prehistoric artworks serve as a poignant reminder of profound climatic shifts and the adaptability of early human societies.

In more recent history, the Libyan Desert has been a stage for exploration. European explorers like Gerhard Rohlfs (19th century) and Ralph Bagnold (early 20th century) meticulously mapped its vastness, often relying on early motorised vehicles. During World War II, the desert became a crucial theatre for covert operations, most famously by the British Long Range Desert Group (LRDG), whose expertise in navigating these desolate lands was instrumental in intelligence gathering and raiding behind enemy lines. Their exploits further solidified the desert's reputation as a place of immense challenge and strategic importance.

Beyond its historical and geological wonders, the Libyan Desert continues to yield scientific treasures. Meteorite hunters find it a fertile ground due to the lack of vegetation and the well-preserved nature of objects on its surface. Its extreme aridity also makes it an ideal location for studying exogeology, offering insights into the surface conditions of Mars and other arid planets. However, this magnificent wilderness is not without its challenges. Climate change continues to exert pressure, and while its vastness offers some resilience, the precious groundwater resources that sustain its oases are finite. Balancing scientific exploration and the conservation of its unique ecosystems and archaeological heritage remains an ongoing endeavour.

The video explores the Libyan desert and shows examples of its ancient rock art. After you've watched it, why not check out our interactive map of the Libyan Desert below.


 
 


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