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It is one of three distinct physiographic provinces of the African massive physiographic division.The Sahara is mainly rocky hamada (stone plateaus), Ergs (sand seas - large areas covered with sand dunes) form only a minor part, but many of the sand dunes are over 180 metres (590 ft) high.According to the botanical criteria of Frank White the northern limit of the Sahara corresponds to the northern limit of date palm cultivation and the southern limit of the range of esparto, a grass typical of the Mediterranean climate portion of the Maghreb and Iberia.The northern limit also corresponds to the 100 mm (3.9 in) isohyet of annual precipitation.

The Sahara is the world's largest low-latitude hot desert.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 risk of rainfall.These extremely arid areas often receive no rain for years.To the north, the Sahara skirts the Mediterranean Sea in Egypt and portions of Libya, but in Cyrenaica and the Maghreb, the Sahara borders the Mediterranean forest, woodland, and scrub eco-regions of northern Africa, all of which have a Mediterranean climate characterized by hot summers and cool and rainy winters.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.