Sahara Desert example essay topic

Sahara Desert The Sahara Desert is the world's largest desert area. The word Sahara comes from the Arabic word sara', meaning desert. It extends from the Africa's Atlantic Ocean side to the Red Sea and consists of the countries of Morocco, Algeria, Tunisia, Libya, Egypt, Mauritania, Mali, Niger, Chad, and Sudan. It is about 5,200 miles long.

Overall, the Sahara Desert covers 3,500,000 square miles. The geography of the desert is varied. In the west, the Sahara is rocky with varied elevation. It does contain underground rivers, which sometime penetrate the surface, resulting in oases. The central region of the Sahara has more elevation than the other areas, with peaks such as Emi Kou ssi and That. Even though the area lacks rainfall, these peaks are snow capped during the winter.

The Eastern part of the Sahara, the Libyan Desert, is dry with very few oases. The Sahara's landscape features include shallow basins, large oasis depressions, gravel-covered plains, plateaus, and mountains, sand sheets, dunes and sand seas. Sand sheets and dunes cover over 25 percent of the Sahara's surface. The most common types of dunes include tied dunes, blowout dunes, and transverse dunes.

Within the Sahara are several pyramidal dunes that reach over 500 feet in height while others reach over 1,000 feet. Researchers have for many years tried to figure out how these dunes were formed, but the case remains unsolved. The boundaries, however, are not clearly defined and have been shifting for millennia. The Sahara was once a fertile area; millet was cultivated there over 8000 years ago. About 10,000 years ago, the Sahara was used as land for grazing in which elephants, giraffes and other animals thrived. It is estimated that in 4,000 B.C., the climate began to get drier.

The fertile landscape dried up and the desert widened, creating the form that appears today. As conditions gradually became drier, however, and desertification set in, farmers abandoned their land and the animals migrated to other areas. The Sahara's climate is very hot and dry. Although it is very hot during the day, it does become cold at night. On average, it only has 8 inches of rainfall per year. The Sahara's climate consists of basically two sub-climates, a dry subtropical climate in the north and a dry tropical climate in the south.

The dry tropical climate is generally characterized by mild, dry winters, a hot dry season just before the rainy season, and an annual temperature cycle. The dry subtropical climate, however, is characterized by annually high temperature ranges, cold winters, hot summers and two rainy seasons. There is a narrow strip in the western portion of the Sahara, along the coast, which generally has cool temperatures compared to the rest of the Sahara because of the influence of the cold ocean currents. The land is almost entirely without rainfall or surface water but possesses a number of underground rivers that flow from the Atlas and other mountains. Occasionally the waters of these rivers find their way to the surface; in these naturally irrigated oases, plants grow freely. The soil of this region of the Sahara is fertile and, where irrigation is possible, produces excellent crops.

The Libyan Desert is considered the most arid part of the Sahara. Moisture is almost totally absent and few oases exist. The Libyan Desert is virtually devoid of any form of animal or vegetable life. Sandy wastes and large dunes of sand that range to 400 feet or more in height characterize the land. The valley of the Nile River and the mountainous area of the Nubian Desert to the east of the Nile are, geographically, part of the Sahara, but the irrigation afforded by the Nile transforms the desert into fertile agricultural land throughout much of Egypt. Plant and animal life is not as abundant in the Sahara as it is in other deserts.

The grasses, shrubs, and trees that grow in parts of the Sahara have adapted in order to live in the dry conditions there. Plants of the Sahara obtain water in various ways. Some have long roots that reach deep into the soil and absorb moisture. Others take moisture from the air through their leaves. Some of the mammal species found within the Sahara are the gerbil, jerboa, Cape hare, the desert hedgehog, Dorcas gazelle, deer, common jackal, and the mongoose. The Sahara also contains over 300 species of migratory bird populations along with water and shore birds and various other types of birds.

Some of the most common birds are ostriches, raptors, secretary birds, guinea fowl, desert eagles and, sand larks. Numerous types of reptiles - including frogs, toads, and crocodiles - can be found within the Sahara's lakes and pools of water, while lizards, chameleons, skinks, and cobras are to be found among the dunes and rocks. Among the reptiles in the Sahara's rivers and pools can be found snails, brine and algae shrimp, plus other types of crustaceans. Most desert animals can go for long periods of time without water.

They get the water from the plants that they eat. Many of the small animals stay in their burrows during the day to avoid the heat. They search for food at night. The Sahara Desert has only 2.5 million inhabitants, roughly 1 person per square mile, which is one of the lowest population densities on earth. Wherever abundant food and water sources occur, one will find relatively large masses of people and wildlife. On the whole, the Sahara is one of the harshest environments known to man.

The majority of the people living in the Sahara Desert are nomads, which means that these people continuously move from region to region in search of better living conditions. It is believed that the first nomadic peoples came to this region after domestic animals were introduced to the Sahara 7,000 years ago. Evidence suggests that the Sahara accumulated diverse groups that quickly formed dense populations throughout the region. The majority of the groups lived separately, but depended on each other for trade. One of the main problems that are happening to the Sahara desert is the continuing development of the boundaries of the desert.

This is known as desertification. As global warming continues to increase, the probability of more desert regions becoming bigger is more likely.

Bibliography

n. a. web "Sahara Desert" Think Quest 1998.
n. a. web land / saha cl.'s html "People and Places: Sahara Desert" 1998.
s sahara,' Microsoft (R) Encarta (R) 97 Encyclopedia. (c) 1993-1996 Microsoft Corporation.