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Qattara
The Qattara Depression ( ar, منخفض القطارة, Munḫafaḍ al-Qaṭṭārah) is a depression in northwestern Egypt, specifically in the Matruh Governorate. The depression is part of the Western Desert of Egypt. The Qattara Depression lies below sea level, and its bottom is covered with salt pans, sand dunes, and salt marshes. The depression extends between the latitudes of 28°35' and 30°25' north and the longitudes of 26°20' and 29°02' east.El Bassyony, Abdou. 1995. ''"Introduction to the geology of the Qattara Depression,"'' International Conference on the Studies and Achievements of Geosciences in Egypt, 69 (85-eoa) The Qattara Depression was created by the interplay of salt weathering and wind erosion. Some west of the depression lie the oases of Siwa in Egypt and Jaghbub in Libya in smaller but similar depressions. The Qattara Depression contains the second lowest point in Africa at an elevation of below sea level, the lowest point being Lake Assal in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Qattara Depression R01
The Qattara Depression ( ar, منخفض القطارة, Munḫafaḍ al-Qaṭṭārah) is a depression in northwestern Egypt, specifically in the Matruh Governorate. The depression is part of the Western Desert of Egypt. The Qattara Depression lies below sea level, and its bottom is covered with salt pans, sand dunes, and salt marshes. The depression extends between the latitudes of 28°35' and 30°25' north and the longitudes of 26°20' and 29°02' east.El Bassyony, Abdou. 1995. ''"Introduction to the geology of the Qattara Depression,"'' International Conference on the Studies and Achievements of Geosciences in Egypt, 69 (85-eoa) The Qattara Depression was created by the interplay of salt weathering and wind erosion. Some west of the depression lie the oases of Siwa in Egypt and Jaghbub in Libya in smaller but similar depressions. The Qattara Depression contains the second lowest point in Africa at an elevation of below sea level, the lowest point being Lake Assal i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Qattara Depression (March 2007)
The Qattara Depression ( ar, منخفض القطارة, Munḫafaḍ al-Qaṭṭārah) is a depression in northwestern Egypt, specifically in the Matruh Governorate. The depression is part of the Western Desert of Egypt. The Qattara Depression lies below sea level, and its bottom is covered with salt pans, sand dunes, and salt marshes. The depression extends between the latitudes of 28°35' and 30°25' north and the longitudes of 26°20' and 29°02' east.El Bassyony, Abdou. 1995. ''"Introduction to the geology of the Qattara Depression,"'' International Conference on the Studies and Achievements of Geosciences in Egypt, 69 (85-eoa) The Qattara Depression was created by the interplay of salt weathering and wind erosion. Some west of the depression lie the oases of Siwa in Egypt and Jaghbub in Libya in smaller but similar depressions. The Qattara Depression contains the second lowest point in Africa at an elevation of below sea level, the lowest point being Lake Assal i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Siwa Oasis
The Siwa Oasis ( ar, واحة سيوة, ''Wāḥat Sīwah,'' ) is an urban oasis in Egypt; between the Qattara Depression and the Great Sand Sea in the Western Desert (Egypt), Western Desert, 50 km (30 mi) east of the Libyan Egypt–Libya border, border, and 560 km (348 mi) from the capital. Its fame primarily from its ancient role as the home to an oracle of Ammon, the ruins of which are a popular tourist attraction which gave the oasis its ancient name Oasis of Amun Ra, a List of Egyptian deities#Amun, major Egyptian deity. Geography The Siwa oasis is in a deep Depression (geology), depression that reaches below sea level, to about . To the west the Jaghbub, Libya, Jaghbub oasis rests in a similar depression and to the east , the large Qattara Depression is also below sea level. Name The Ancient Egyptian name of the oasis was ''sḫt jꜣmw'', meaning "Field of Trees". The native Libyan toponym may be preserved in the Egyptian ''t̠ꜣ(j) n d̠rw “tꜣ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moghra Oasis
The Moghra Oasis is an uninhabited oasis in the northeastern part of the Qattara Depression in the Western Desert (Egypt), Western Desert of Egypt. It has a lake containing brackish water, salt marshes and a swamp with Phragmites, reeds. Geography The Qattara Depression is about below sea level and is shaped like a teardrop, with Moghra Oasis in its northeastern corner. The floor of the Depression consists of salt marshes and dry lake beds that flood occasionally and there are also large areas of windblown sand. Moghra Oasis consists of a lake containing brackish water some below sea level. Adjoining it are salt marshes and some ''Phragmites'' swamps. To the south and west there are sand dunes near the lake and extensive sheets of sand beyond. Geology The water rises to the surface from an aquifer in the Nubian Sandstone, Nubian sandstone, but its precise source is unclear as the Nubian Sandstone Aquifer System is at great depths in this area. Just to the north of the oasis is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Qara Oasis
The Qara Oasis (also spelt Cara or Gara; ar, واحة القارة; also Qarat Umm El Sagheir, i.e. ) is an inhabited oasis in Egypt, with a population of only 363 (as of the 11 November 2006 census). This oasis is often disregarded when it comes to counting the number of Egyptian oases as it is very small compared to the others. In local folklore, if a newborn arrives, an elder will die shortly after, thus keeping the population constant. It lies at the northwest edge of the Qattara Depression, northeast of Siwa Oasis, and belongs to Siwa District within Matrouh Governorate. It is connected to an asphalted sub-road of approximately in length, in an area called “Bir al-Nisf” located on the Matrouh–Siwa road. History Originally, the inhabitants lived atop a neighbouring mountain which acted as a natural fortress, but today they live in simple houses beneath. At first, the people of the village built a fortress on top of a nearby rocky mountain, which was a defensive pos ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Mediterranean Sea to the north, the Gaza Strip of Palestine and Israel to the northeast, the Red Sea to the east, Sudan to the south, and Libya to the west. The Gulf of Aqaba in the northeast separates Egypt from Jordan and Saudi Arabia. Cairo is the capital and largest city of Egypt, while Alexandria, the second-largest city, is an important industrial and tourist hub at the Mediterranean coast. At approximately 100 million inhabitants, Egypt is the 14th-most populated country in the world. Egypt has one of the longest histories of any country, tracing its heritage along the Nile Delta back to the 6th–4th millennia BCE. Considered a cradle of civilisation, Ancient Egypt saw some of the earliest developments of writing, agriculture, ur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salt Pan (geology)
Natural salt pans or salt flats are flat expanses of ground covered with salt and other minerals, usually shining white under the sun. They are found in deserts and are natural formations (unlike salt evaporation ponds, which are artificial). A salt pan forms by evaporation of a water pool, such as a lake or pond. This happens in climates where the rate of water evaporation exceeds the rate of that is, in a desert. If the water cannot drain into the ground, it remains on the surface until it evaporates, leaving behind minerals precipitated from the salt ions dissolved in the water. Over thousands of years, the minerals (usually salts) accumulate on the surface. These minerals reflect the sun's rays (through radiation) and often appear as white areas. Salt pans can be dangerous. The crust of salt can conceal a quagmire of mud that can engulf a truck. The Qattara Depression in the eastern Sahara Desert contains many such traps which served as strategic barriers during World ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Western Desert (Egypt)
The Western Desert of Egypt is an area of the Sahara that lies west of the river Nile, up to the Libyan border, and south from the Mediterranean Sea to the border with Sudan. It is named in contrast to the Eastern Desert which extends east from the Nile to the Red Sea. The Western Desert is mostly rocky desert, though an area of sandy desert, known as the Great Sand Sea, lies to the west against the Libyan border. The desert covers an area of which is two-thirds of the land area of the country. Its highest elevation is in the Gilf Kebir plateau to the far south-west of the country, on the Egypt-Sudan-Libya border. The Western Desert is barren and uninhabited save for a chain of oases which extend in an arc from Siwa, in the north-west, to Kharga in the south. It has been the scene of conflict in modern times, particularly during the Second World War. Administratively the Western Desert is divided between various governorates; in the north and west, the Matrouh Governorate adm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jaghbub, Libya
Jaghbub ( ar, الجغبوب) is a remote desert village in the Al Jaghbub Oasis in the eastern Libyan Desert. It is actually closer to the Egyptian town of Siwa than to any Libyan town of note. The oasis is located in Butnan District and was the administrative seat of the Jaghbub Basic People's Congress. Supported by reservoirs of underground water and date production, the town is best known for its hard-won self-sufficiency. Idris of Libya was born in Jaghbub on 12 March 1890. Geography The Jaghbub oasis is located in a deep depression that extends below sea level. This depression, an area lower than the surrounding region, reaches to about -10 m. To the east the Siwa Oasis lies in a similar depression and even further east the large Qattara Depression also lies below sea level. History It was once the headquarters of the Senussi Movement and home of a long disappeared Islamic university and the former Senussi palace (which is now in rubble). Jaghbub was a part of Egypt un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Endorheic Basin
An endorheic basin (; also spelled endoreic basin or endorreic basin) is a drainage basin that normally retains water and allows no outflow to other external bodies of water, such as rivers or oceans, but drainage converges instead into lakes or swamps, permanent or seasonal, that equilibrate through evaporation. They are also called closed or terminal basins, internal drainage systems, or simply basins. Endorheic regions contrast with exorheic regions. Endorheic water bodies include some of the largest lakes in the world, such as the Caspian Sea, the world's largest inland body of water. Basins with subsurface outflows which eventually lead to the ocean are generally not considered endorheic; they are cryptorheic. Endorheic basins constitute local base levels, defining a limit of erosion and deposition processes of nearby areas. Etymology The term was borrowed from French ''endor(rh)éisme'', coined from the combining form ''endo-'' (from grc, ἔνδον ''éndon'' 'wit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mediterranean Sea
The Mediterranean Sea is a sea connected to the Atlantic Ocean, surrounded by the Mediterranean Basin and almost completely enclosed by land: on the north by Western and Southern Europe and Anatolia, on the south by North Africa, and on the east by the Levant. The Sea has played a central role in the history of Western civilization. Geological evidence indicates that around 5.9 million years ago, the Mediterranean was cut off from the Atlantic and was partly or completely desiccated over a period of some 600,000 years during the Messinian salinity crisis before being refilled by the Zanclean flood about 5.3 million years ago. The Mediterranean Sea covers an area of about , representing 0.7% of the global ocean surface, but its connection to the Atlantic via the Strait of Gibraltar—the narrow strait that connects the Atlantic Ocean to the Mediterranean Sea and separates the Iberian Peninsula in Europe from Morocco in Africa—is only wide. The Mediterranean Sea e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Matruh Governorate
Matrouh Governorate ( ar, محافظة مطروح ) is one of the governorates of Egypt. Located in the north-western part of the country, it borders Libya. Its capital is Mersa Matruh. Municipal divisions The governorate is divided into municipal divisions with a total estimated population as of July 2017 of 429,370. Overview The interior of the Matrouh Governorate is part of Egypt's Western Desert, including the Siwa Oasis, in antiquity known for its shrine to Amun. In the center of the Governorate is the Qattara Depression, descending to 133 metres below sea level. Marsa Matrouh is the ancient grc-koi, Παραιτόνιον ''Paraitónion'', Latin ''Paraetonium''. It was the westernmost city of the Ptolemaic Kingdom in the Hellenistic period. The city of Apis, some 18 km to the west of Paraetonium, marked the boundary to Libycus nome, and the Halfaya Pass (at Sallum) marked the boundary to Marmarica proper. Matrouh Governorate contains many historical sites r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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