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Gulf Of Aqaba
The Gulf of Aqaba ( ar, خَلِيجُ ٱلْعَقَبَةِ, Khalīj al-ʿAqabah) or Gulf of Eilat ( he, מפרץ אילת, Mifrátz Eilát) is a large gulf at the northern tip of the Red Sea, east of the Sinai Peninsula and west of the Arabian Peninsula. Its coastline is divided among four countries: Egypt, Israel, Jordan, and Saudi Arabia. Geography The gulf is east of the Sinai Peninsula and west of the Arabian Peninsula. With the Gulf of Suez to the west, it extends from the northern portion of the Red Sea. It reaches a maximum depth of 1,850 m in its central area: the Gulf of Suez is significantly wider but less than 100 m deep. The gulf measures at its widest point and stretches some north from the Straits of Tiran to where Israel meets Egypt and Jordan. Like the coastal waters of the Red Sea, the gulf is one of the world's premier sites for diving. The area is especially rich in coral and other marine biodiversity and has accidental shipwrecks and vessels deliber ...
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Sinai Peninsula
The Sinai Peninsula, or simply Sinai (now usually ) (, , cop, Ⲥⲓⲛⲁ), is a peninsula in Egypt, and the only part of the country located in Asia. It is between the Mediterranean Sea to the north and the Red Sea to the south, and is a land bridge between Asia and Africa. Sinai has a land area of about (6 percent of Egypt's total area) and a population of approximately 600,000 people. Administratively, the vast majority of the area of the Sinai Peninsula is divided into two governorates: the South Sinai Governorate and the North Sinai Governorate. Three other governorates span the Suez Canal, crossing into African Egypt: Suez Governorate on the southern end of the Suez Canal, Ismailia Governorate in the center, and Port Said Governorate in the north. In the classical era the region was known as Arabia Petraea. The peninsula acquired the name Sinai in modern times due to the assumption that a mountain near Saint Catherine's Monastery is the Biblical Mount Sinai. ...
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Straits Of Tiran
The straits of Tiran ( ar, مضيق تيران ') are the narrow sea passages between the Sinai and Arabian peninsulas that connect the Gulf of Aqaba and the Red Sea. The distance between the two peninsulas is about . The Multinational Force and Observers monitors the compliance of Egypt in maintaining freedom of navigation of the straits, as provided under the Egypt–Israel peace treaty. The body is named after Tiran Island, located at its entrance from the Sinai. Sanafir Island lies to the east of Tiran, southeast of the shallow strait between Tiran and Saudi Arabia. The blockade of Israeli passage through the Suez Canal and Straits of Tiran led to two wars, in 1956 and 1967. Background International documents inconsistently refer to both the "Straits of Tiran" and the "Strait of Tiran". There are several passages formed by the islands between Egypt and Saudi Arabia. The westernmost strait, between Egypt and the island of Tiran, overlooked by the Egyptian city S ...
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1995 Gulf Of Aqaba Earthquake
The 1995 Gulf of Aqaba earthquake (also known as Nuweiba earthquake) occurred on November 22 at 06:15 local time (04:15 UTC) and registered 7.3 on the scale. The epicenter was located in the central segment of the Gulf of Aqaba, the narrow body of water that separates Egypt's Sinai Peninsula from the western border of Saudi Arabia. At least 8 people were killed and 30 were injured in the meizoseismal area. The earthquake occurred along the Dead Sea Transform (DST) fault system, an active tectonic plate boundary with seismicity that is characterized by long-running quiescent periods with occasional large and damaging earthquakes, along with intermittent earthquake swarms. It was the strongest tectonic event in the area for many decades and caused injuries, damage, and deaths throughout the Levant and is also thought to have remotely triggered a series of small to moderate earthquakes to the north of the epicenter. In the aftermath of the quake, several field investigations ...
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Fault (geology)
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A '' fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur ...
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Pull-apart Basin
In geology, a basin is a region where subsidence generates accommodation space for the deposition of sediments. A pull-apart basin is a structural basin where two overlapping (en echelon) strike-slip faults or a fault bend creates an area of crustal extension undergoing tension, which causes the basin to sink down. Frequently, the basins are rhombic or sigmoidal in shape. Dimensionally, basins are limited to the distance between the faults and the length of overlap.Frisch, Wolfgang, Martin Meschede, and Ronald C. Blakey. ''Plate tectonics: Continental drift and mountain building''. Springer, 2010. Pull-apart basins are also referred to as overlapping-tension-zones (OTZ). Mechanics and fault configuration The inhomogeneity and structural complexity of continental crust causes faults to deviate from a straight course and frequently causes bends or step-overs in fault paths. Bends and step-overs of adjacent faults become favorable locations for extensional and compressional st ...
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Dead Sea Transform
The Dead Sea Transform (DST) fault system, also sometimes referred to as the Dead Sea Rift, is a series of faults that run from the Maras Triple Junction (a junction with the East Anatolian Fault in southeastern Turkey) to the northern end of the Red Sea Rift (just offshore of the southern tip of the Sinai Peninsula). The fault system forms the transform boundary between the African Plate to the west and the Arabian Plate to the east. It is a zone of left lateral displacement, signifying the relative motions of the two plates. Both plates are moving in a general north-northeast direction, but the Arabian Plate is moving faster, resulting in the observed left lateral motions along the fault of approximately 107 km at its southern end. A component of extension is also present in the southern part of the transform, which has contributed to a series of depressions, or pull-apart basins, forming the Gulf of Aqaba, Dead Sea, Sea of Galilee, and Hula basins. A component of shorteni ...
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Tiran Island
Tiran ( ar, جزيرة تيران ''Jezîret Tīrān'', ''Jazīrat Tīrān''), and ''Yotvat Island'', is a Saudi Arabian island that was formerly administered by Egypt. Sovereignty of the two Red Sea islands, Tiran and Sanafir, was ceded officially to Saudi Arabia as part of a maritime borders agreement between Egypt and Saudi Arabia. The agreement subsequently was approved by the Egyptian Parliament and finally ratified by the Egyptian President on 24 June 2017. The island is located at the entrance of the Straits of Tiran, which connect the Red Sea to the Gulf of Aqaba. It has an area of about . It was part of the Ras Muhammad National Park. The Straits of Tiran are Israel's only access from the Gulf of Aqaba to the Red Sea, and Egypt's blockade of the Straits of Tiran on 22 May 1967 was the casus belli for Israel in the Six-Day War. Tiran Island is of strategic significance in the area, as it forms the narrowest section of the Straits of Tiran, which is an important sea ...
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Requin Island
Requin, shark in French (pl : requins), may refer to : Places * Great Requin River, a river of Grenada * Little Requin River, a river of Grenada People * Édouard Réquin (1879–1953), French soldier * Steve Requin (born 1968), a Canadian cartoonist from Québec * Michèle Bernard-Requin (1943–2019), French lawyer and magistrate * Abderrahim Chafay (born 1977; stagename ''Requin''), Moroccan-French Muay Thai kickboxer. Ships * French ship Requin, a French Navy shipname * Requin-class submarine, a class of submarines of French navy in the mid-1920s ** French submarine Requin (1924) * USS Requin (SS-481), a United States Navy Tench-class submarine * a French submarine seized by Italy during World War II and converted into a cargo submarine * − brig of the French Navy launched in 1794 that the British Royal Navy captured in 1795 and that was wrecked in 1801. Entertainment * ''The Shark'' (1930 film), French film originally released as ''Le Requin'' * '' The Requin' ...
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International Hydrographic Organization
The International Hydrographic Organization (IHO) is an intergovernmental organisation representing hydrography. , the IHO comprised 98 Member States. A principal aim of the IHO is to ensure that the world's seas, oceans and navigable waters are properly surveyed and charted. It does this through the setting of international standards, the co-ordination of the endeavours of the world's national hydrographic offices, and through its capacity building program. The IHO enjoys observer status at the United Nations, where it is the recognised competent authority on hydrographic surveying and nautical charting. When referring to hydrography and nautical charting in Conventions and similar Instruments, it is the IHO standards and specifications that are normally used. History The IHO was established in 1921 as the International Hydrographic Bureau (IHB). The present name was adopted in 1970, as part of a new international Convention on the IHO adopted by the then member nations. ...
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Dahab
Dahab ( arz, دهب, , "gold") is a small Egyptian town on the southeast coast of the Sinai Peninsula in Egypt, approximately northeast of Sharm el-Sheikh. Formerly a Bedouin fishing village, Dahab is now considered to be one of Egypt's most treasured diving destinations. Following the Six-Day War, Sinai was occupied by Israel and Dahab became known as ''Di-Zahav'' ( he, די זהב), after a place mentioned in the Bible as one of the stations for the Israelites during the Exodus from Egypt. The Sinai Peninsula was restored to Egyptian rule under the Egypt–Israel peace treaty in 1982. Egypt's former president, Hosni Mubarak helped the arrival of many local and international tourism companies, hotel chains, and the establishment of many other ancillary facilities has since made the town resorts a popular destination with tourists. Dahab is served by Sharm el-Sheikh International Airport. Masbat (within Dahab) is a popular diving destination, and there are many (50+) dive center ...
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Sharm El-Sheikh
Sharm El Sheikh ( ar, شرم الشيخ, ), commonly abbreviated to Sharm, is an Egyptian city on the southern tip of the Sinai Peninsula, in South Sinai Governorate, on the coastal strip along the Red Sea. Its population is approximately 53,670 . Sharm El Sheikh is the administrative hub of Egypt's South Sinai Governorate, which includes the smaller coastal towns of Dahab and Nuweiba as well as the mountainous interior, St. Catherine and Mount Sinai. The city and holiday resort is a significant centre for tourism in Egypt, while also attracting many international conferences and diplomatic meetings. Name Sharm El Sheikh ("bay of the wise") is also known as the "''City of Peace''"; Egyptian Arabic: "''Madinet Es-Salam''", referring to the large number of International Peace Conferences that have been held there. Amongst Egyptians and also many visitors, the name of the city is commonly shortened to "Sharm" (), which is its common name in Egyptian Arabic. The name is also someti ...
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