The Sahara is dominated by vast sand seas known as ergs. These ergs are characterized by large, undulating dunes that can reach heights of several hundred meters. The sand is composed primarily of quartz, and its color can vary from pale yellow to deep orange. The movement of the sand dunes creates a constantly changing landscape, as the wind shapes and reshapes them over time.
Rocky Plateaus (Hamadas):
Hamadas are elevated rocky plateaus that are found throughout the Sahara. They are formed from ancient sedimentary rocks that have been eroded over time, exposing a flat, barren surface. The hamadas can be extremely inhospitable, with little vegetation and extreme temperature fluctuations.
Gravel Plains (Reg):
Regs are extensive, gently sloping plains that are covered in a layer of small stones and gravel. They are formed by the weathering of rocks and the subsequent erosion of sand and finer sediments. Regs are often found at the edges of ergs and hamadas, and they can be difficult to traverse due to the loose surface material.
Oases:
Oases are areas of vegetation and water that occur in the midst of the desert. They are typically formed around springs or wells, and they provide a vital source of water for humans and animals. Oases are often home to human settlements and agriculture, and they can be important centers of trade and commerce.
Mountain Ranges:
The Sahara Desert is not completely flat, and there are several mountain ranges that rise above the surrounding landscape. The most notable mountain range is the Tibesti Mountains, which are located in the northern part of the desert. The Tibesti Mountains include the highest point in the Sahara, Mount Emi Koussi, which has a peak elevation of 3,415 meters (11,204 feet).
Salt Flats (Chotts):
Chotts are large, flat depressions that are covered with a crust of salt. They are formed when water evaporates from shallow lakes or playas, leaving behind a layer of salt. Chotts can be found in various parts of the Sahara, and they are often associated with oases.