location and extent of sahara desert
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Location
Blanketing much of the northern third of the African Continent, or some 3.5 million square miles, the Sahara Desert extends eastward from the Atlantic Ocean some 3,000 miles to the Nile River and the Red Sea, and southward from the Atlas Mountains of Morocco and the Mediterranean shores more than 1,000 miles to the savannah called the Sahel. More than 16 times the size of France, the Sahara Desert blankets nearly all of Mauritania, Western Sahara, Algeria, Libya, Egypt and Niger; the southern half of Tunisia; and the northern parts of Mali, Chad and Sudan.

Landscape
The Sahara's topographical features, said "The Living Africa," include not only the iconic sand dune fields, but also arid mountains, plateaus, sand- and gravel-covered plains, shallow basins and large oasis depressions. Its highest point is Chad's Mount Koussi (an extinct volcanic crater that rises 11,204 feet above sea level at the peak), and its lowest, Egypt's Qattera Depression (an oasis depression that lies 436 feet below sea level at the deepest point).

The Sahara's fabled dune fields, which cover only about 15 percent of the entire desert's surface, lie primarily in the north central region, in the countries of Algeria and Libya. Most sand dunes -- mounds and ridges of sand sculpted by wind and gravity -- have a windward or "backslope" surface and a leeward or "slipface" surface. Prevailing winds drive sand up the backslope until it reaches a crest and then collapses under the pull of gravity, cascading down the slipface. The wind may leave rippled surfaces in its wake.

Saharan dunes as seen from the eastern edge of Morocco.
The dunes take on varied and complex forms. A few examples include:
Crescent dunes, which have arms or "horns" that point downwind and embrace the slip face. These dunes form under winds that have blown from the same direction for an extended period.Linear dunes, which have long, straight or slightly sinuous forms, that may extend for miles. They develop under winds that blow from either of two directions.Transverse dunes, which have sharply crested, roughly saber-shaped forms that lie parallel and may reach to nearly a thousand feet in height and extend for over a hundred miles in length. They form in alignment with a prevailing wind that has changed direction for a prolonged period and redistributed the sands of earlier dunes.Star dunes, which have central pyramidal mounds with three or more radiating arms, each with a backslope and a slipface. The star dunes form under winds that blow from several directions.Dome dunes, which have circular- or oval-shaped mounds, which, surprisingly, have no backslope or slipface. Comparatively rare, they tend to form at the upwind edges of dune fields.
The dunes, with their various forms, raise many questions about the dynamics of their formation
.
Here is your Answer
.
Location
Blanketing much of the northern third of the African Continent, or some 3.5 million square miles, the Sahara Desert extends eastward from the Atlantic Ocean some 3,000 miles to the Nile River and the Red Sea, and southward from the Atlas Mountains of Morocco and the Mediterranean shores more than 1,000 miles to the savannah called the Sahel. More than 16 times the size of France, the Sahara Desert blankets nearly all of Mauritania, Western Sahara, Algeria, Libya, Egypt and Niger; the southern half of Tunisia; and the northern parts of Mali, Chad and Sudan.

Landscape
The Sahara's topographical features, said "The Living Africa," include not only the iconic sand dune fields, but also arid mountains, plateaus, sand- and gravel-covered plains, shallow basins and large oasis depressions. Its highest point is Chad's Mount Koussi (an extinct volcanic crater that rises 11,204 feet above sea level at the peak), and its lowest, Egypt's Qattera Depression (an oasis depression that lies 436 feet below sea level at the deepest point).

The Sahara's fabled dune fields, which cover only about 15 percent of the entire desert's surface, lie primarily in the north central region, in the countries of Algeria and Libya. Most sand dunes -- mounds and ridges of sand sculpted by wind and gravity -- have a windward or "backslope" surface and a leeward or "slipface" surface. Prevailing winds drive sand up the backslope until it reaches a crest and then collapses under the pull of gravity, cascading down the slipface. The wind may leave rippled surfaces in its wake.

Saharan dunes as seen from the eastern edge of Morocco.
The dunes take on varied and complex forms. A few examples include:
Crescent dunes, which have arms or "horns" that point downwind and embrace the slip face. These dunes form under winds that have blown from the same direction for an extended period.Linear dunes, which have long, straight or slightly sinuous forms, that may extend for miles. They develop under winds that blow from either of two directions.Transverse dunes, which have sharply crested, roughly saber-shaped forms that lie parallel and may reach to nearly a thousand feet in height and extend for over a hundred miles in length. They form in alignment with a prevailing wind that has changed direction for a prolonged period and redistributed the sands of earlier dunes.Star dunes, which have central pyramidal mounds with three or more radiating arms, each with a backslope and a slipface. The star dunes form under winds that blow from several directions.Dome dunes, which have circular- or oval-shaped mounds, which, surprisingly, have no backslope or slipface. Comparatively rare, they tend to form at the upwind edges of dune fields.
The dunes, with their various forms, raise many questions about the dynamics of their formation
Answered by
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It is located on the African continent. It is the hottest desert in the world. It extends towards the east from the atlantic ocean and south from the mountain of Morocco and Mediterranean Sea. The Sahara desert covers almost a million square kilometers.
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