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The Farafra depression ( ar, واحة الفرافرة, ) is a geological depression, the second biggest by size in Western
Egypt Egypt ( ar, مصر , ), officially the Arab Republic of Egypt, is a transcontinental country spanning the northeast corner of Africa and southwest corner of Asia via a land bridge formed by the Sinai Peninsula. It is bordered by the Med ...
and the smallest by population, near latitude 27.06° north and longitude 27.97° east. It is in the large Western Desert of Egypt, approximately midway between Dakhla and Bahariya oases. Farafra has an estimated 5,000 inhabitants (2002) mainly living in the town of Farafra and is mostly inhabited by the local Bedouins. Parts of the town have complete quarters of traditional architecture, simple, smooth, unadorned, all in mud colour — local culture and traditional methods of building and carrying out repairs have been supported by its tourism. Often grouped within Farafra are the
hot springs A hot spring, hydrothermal spring, or geothermal spring is a spring produced by the emergence of geothermally heated groundwater onto the surface of the Earth. The groundwater is heated either by shallow bodies of magma (molten rock) or by c ...
at Bir Sitta (the sixth well) and the El-Mufid lake.


Etymology

The word al-Farafra (''al-Farafira'' in local pronunciation, ''al-Farfarun'' in
Middle Ages In the history of Europe, the Middle Ages or medieval period lasted approximately from the late 5th to the late 15th centuries, similar to the post-classical period of global history. It began with the fall of the Western Roman Empire ...
) is a broken plural form of ''farfar'' meaning "fizzy spring". The Ancient Egyptian name of the oasis was , "the land of cattle".


History

Archaeological evidence suggests that Farafra region was inhabited since late
Pleistocene The Pleistocene ( , often referred to as the '' Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed ...
. Farafra was known in ancient Egyptian history at least since the Middle Kingdom. In the Ptolemaic period, the region was under the administration of the Oxyrhynchite nome (19th Upper Egyptian nome).


White Desert

A main geographic attraction of Farafra is its White Desert (known as '' Sahara el Beyda'') — a national park of Egypt and north of the town of Farafra, the main draw of which is its rock type colored from snow-white to cream. It has massive
chalk rock Chalk is a soft, white, porous, sedimentary carbonate rock. It is a form of limestone composed of the mineral calcite and originally formed deep under the sea by the compression of microscopic plankton that had settled to the sea floor. Chalk i ...
formations that are textbook examples of ventifact and which have been created as a result of occasional sandstorm in the area. The White Desert is a typical place visited by some schools in Egypt, as a location for camping trips.


Wells

Due to its geographical location and geological formation it has more than 100 wells spread out over the lands of the Farafra, many of which are natural. Most of these wells are used in aggregation of the cultivated land in the oasis. Some of the wells in Farafra have become a favorite tourist destination. Bir Sitta, (well 6 in Arabic), Bir Sab'a (well 7) and Bir Ithnian wa ishrin (well 22) are the most important. Because of the water's warm temperature and a slight percentage of
sulfur Sulfur (or sulphur in British English) is a chemical element with the symbol S and atomic number 16. It is abundant, multivalent and nonmetallic. Under normal conditions, sulfur atoms form cyclic octatomic molecules with a chemical formul ...
, these wells are favorable for swimming and relaxation. There is a large lake touristic well named Abu Nus 15 kilometers north of the edge of the Farafra.


Climate

Köppen-Geiger climate classification system classifies its climate as hot desert (BWh).


Gallery

File:WhiteDesertEgypt@FarafraOasis2007jan6-93 byDanielCsorfoly.JPG File:Weisse Wüste.jpg, Limestone rock formation File:White Desert, Al-Farafra-Al-Bahariya road through the desert, Egypt.jpg, Al-Farafra - Al-Bahariya road File:White Desert, Rock formation, Egypt.jpg, Rock formation File:White Desert, Karst rock formations 2, Egypt.jpg, Rock formations File:White Desert, Karst rock formations, Egypt.jpg, Distant view


References


Bibliography

* Frank Bliss: 'Oasenleben. Die ägyptischen Oasen Bahriya und Farafra in Vergangenheit und Gegenwart'. Die ägyptischen Oasen Band 2. Bonn 2006. * Frank Bliss: 'Artisanat et artisanat d’art dans les oasis du désert occidental égyptien'. "Veröffentlichungen des Frobenius-Instituts". Köln 1998. * Beadnell, Hugh J. L
The Farafra Oasis: Its Topography and Geology.
Geological Survey Report. Part 3 Egypt. Maṣlaḥat al-Misāḥah. 1901. * Fakhry, Ahmed. 1974. Bahriyah and Farafra. Reissue of the Classic History and Description. Illustrated, reprint. Publisher: American Univ. in Cairo Press, 1974. , 9789774247323. 189 pages.


External links


Farafra oasis on Wikivoyage
{{Authority control Populated places in New Valley Governorate Oases of Egypt Western Desert (Egypt)