List Of Earthquakes In Egypt
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List Of Earthquakes In Egypt
This is a list of earthquakes in Egypt, including earthquakes that either had their epicenter in Egypt, or caused significant damage in Egypt. Seismic hazard Seismic hazard in Egypt is highest at the southern end of the Gulf of Suez, the northern Red Sea and around the Gulf of Aqaba, the location of the active plate boundaries. The highest risk is the southern end of the Dead Sea Transform. Notable earthquakes See also * Geology of Egypt References Further reading * {{DEFAULTSORT:List Of Earthquakes In Egypt Earthquakes 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 Medit ...
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Turkey Seismic Hazard
Turkey ( tr, Türkiye ), officially the Republic of Türkiye ( tr, Türkiye Cumhuriyeti, links=no ), is a list of transcontinental countries, transcontinental country located mainly on the Anatolia, Anatolian Peninsula in Western Asia, with a East Thrace, small portion on the Balkans, Balkan Peninsula in Southeast Europe. It shares borders with the Black Sea to the north; Georgia (country), Georgia to the northeast; Armenia, Azerbaijan, and Iran to the east; Iraq to the southeast; Syria and the Mediterranean Sea to the south; the Aegean Sea to the west; and Greece and Bulgaria to the northwest. Cyprus is located off the south coast. Turkish people, Turks form the vast majority of the nation's population and Kurds are the largest minority. Ankara is Turkey's capital, while Istanbul is its list of largest cities and towns in Turkey, largest city and financial centre. One of the world's earliest permanently Settler, settled regions, present-day Turkey was home to important Neol ...
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1754 Cairo Earthquake
A locally devastating earthquake rocked the city of Cairo in the Ottoman Empire (present-day Egypt) on 18 October 1754. Major damage occurred in the city, and an estimated 40,000 people were killed. Nicholas Ambraseys, a Greek seismologist, estimated the felt area magnitude () at 6.6 and assigned a maximum intensity of VII–IX (''Very strong–Violent''). Damage The quake was particularly destructive in the City of the Dead, Boulaq, and regions of present-day New Cairo. Many homes were destroyed, killing many residents. The Saint Catherine's Monastery was damaged and required repairs. About two-thirds of the buildings in Cairo fell. Shaking was felt for an area of 150,000 km2. Some historians have misdated the event to September 2, 1754, in confusion with another earthquake in Anatolia. At least 40,000 people died due to the shallow depth of focus and location in a densely populated area. The high death toll figure is disputed. See also *List of historical earthquakes *Lis ...
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Earthquakes In Egypt
An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves. Earthquakes can range in intensity, from those that are so weak that they cannot be felt, to those violent enough to propel objects and people into the air, damage critical infrastructure, and wreak destruction across entire cities. The seismic activity of an area is the frequency, type, and size of earthquakes experienced over a particular time period. The seismicity at a particular location in the Earth is the average rate of seismic energy release per unit volume. The word ''tremor'' is also used for Episodic tremor and slip, non-earthquake seismic rumbling. At the Earth's surface, earthquakes manifest themselves by shaking and displacing or disrupting the ground. When the epicenter of a large earthquake is located offshore, the seabed may be displaced sufficiently to cause ...
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Geology Of Egypt
The geology of Egypt includes rocks from Archaean - early Proterozoic times onwards. These oldest rocks are found as inliers in Egypt’s Western Desert. In contrast, the rocks of the Eastern Desert are largely late Proterozoic in age. Throughout the country this older basement is overlain by Palaeozoic sedimentary rocks. Cretaceous rocks occur commonly whilst sediments indicative of repeated marine transgression and regression are characteristic of the Cenozoic Era. Economic geology While gold has been mined since Pharaonic times, it is not of sufficient quality to be economically viable. Copper is another resource available, but is also of a poor grade. There is iron located in the Western Desert, and the railway linking the mines to a city near Cairo was restored in the early 1990s. Black sand placers, which are deposits of minerals formed by gravity separation due to sedimentary processes, that are located along the Mediterranean coast contain ilmenite, hematite, magnetit ...
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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 set ...
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1992 Cairo Earthquake
The 1992 Cairo Earthquake, also known as the 1992 Dahshur earthquake, occurred at 15:09 local time (13:09 UTC) on 12 October, with an epicenter in the Western Desert near Dahshur, Giza, south of Egypt's capital and most populous city, Cairo. The earthquake had a magnitude of either 5.8 or 5.9, but was unusually destructive for its size, causing 561 deaths and injuring 12,392 people. It also made over 30,000 families homeless in tens of cities and villages across 16 governorates, in Greater Cairo, the Delta, and northern Upper Egypt. It was the most damaging seismic event to affect Egypt since 1847. Geology Cairo is sited within a diffuse zone of faulting that transfers extension from the Gulf of Suez Rift to the Manzala rift beneath the Nile delta. Damage The areas of greatest damage were in Old Cairo, Bulaq and southwards along the Nile as far as Girza, on the west bank. 350 buildings were completely destroyed and 9,000 other severely damaged. 216 mosques and 350 schools were ...
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Dahshur
DahshurAlso transliterated ''Dahshour'' (in English often called ''Dashur'' ar, دهشور ' , ''Dahchur'') is a royal necropolis located in the desert on the west bank of the Nile approximately south of Cairo. It is known chiefly for several pyramids, two of which are among the oldest, largest and best preserved in Egypt, built from 2613 to 2589 BC. Pyramids The Dahshur pyramids were an extremely important learning experience for the Egyptians. It provided them with the knowledge and know-how to transition from step-sided pyramids to smooth-sided pyramids. Ultimately their breadth of experience would allow them to build the Great Pyramid of Giza; the last of the Seven Wonders of the Ancient World still standing to this date. The first of the Dahshur pyramids was the Bent Pyramid (2613–2589 BC), built under the rule of King Sneferu. The Bent Pyramid was the first attempt at building a smooth sided pyramid, but proved to be an unsuccessful build due to the miscalculati ...
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1969 Sharm El Sheikh Earthquake
The 1969 Sharm El Sheikh earthquake occurred on March 31 off the southern Sinai Peninsula in northeastern Egypt. The epicenter was located near Shadwan island, southwest of the city of Sharm El Sheikh, at the confluence of the Red Sea and the Gulf of Suez. This normal-slip shock measured 6.6 on the moment magnitude scale, had a maximum reported intensity of VII (''Very strong'') on the Mercalli intensity scale, and was responsible for several deaths and injuries. Tectonic setting This portion of Egypt is adjacent to the African and Arabian tectonic plates. The Red Sea divides the two and splits, with one branch turning north along the Gulf of Aqaba into the Dead Sea Transform system, and the main trend continuing along the Gulf of Suez. While the earthquake activity in the Gulf of Aqaba is characterized by left-lateral strike-slip faulting, the Gulf of Suez is primarily influenced by extensional tectonics, with increasing extension from north to south. Earthquake Although an unr ...
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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, Saint Catherine, Egypt, St. Catherine and Mount Sinai. The city and holiday resort is a significant centre for tourism in Egypt, while also attracting many Conference#Conferences topics, 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 Conference, International Peace Conferences that have been held there. Amongst Egyptians and also many visitors, the name of the city is commonly shortened to "Sharm" (), whic ...
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1955 Alexandria Earthquake
The 1955 Alexandria earthquake occurred on September 12 at 06:09 UTC. The epicenter was located in the eastern Mediterranean, offshore of Alexandria, Egypt. The earthquake had a magnitude of Ms 6.3. Damage was reported in the Nile Delta between Alexandria and Cairo. About 300 adobe houses were badly damaged around Lake Idku. The earthquake caused 18 deaths and 89 injuries, with 40 houses completely collapsed and about 420 houses ruined. The earthquake could also be felt in Cyprus, Palestine, Syria, and Greece. See also * List of earthquakes in 1955 * List of earthquakes in Egypt This is a list of earthquakes in Egypt, including earthquakes that either had their epicenter in Egypt, or caused significant damage in Egypt. Seismic hazard Seismic hazard in Egypt is highest at the southern end of the Gulf of Suez, the northe ... References External links * {{Earthquakes in Africa Alexandria earthquake, 1955 Alexandria earthquake Alexandria earthquake Earthquake, 1955 Ea ...
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Alexandria
Alexandria ( or ; ar, ٱلْإِسْكَنْدَرِيَّةُ ; grc-gre, Αλεξάνδρεια, Alexándria) is the second largest city in Egypt, and the largest city on the Mediterranean coast. Founded in by Alexander the Great, Alexandria grew rapidly and became a major centre of Hellenic civilisation, eventually replacing Memphis, in present-day Greater Cairo, as Egypt's capital. During the Hellenistic period, it was home to the Lighthouse of Alexandria, which ranked among the Seven Wonders of the Ancient World, as well as the storied Library of Alexandria. Today, the library is reincarnated in the disc-shaped, ultramodern Bibliotheca Alexandrina. Its 15th-century seafront Qaitbay Citadel is now a museum. Called the "Bride of the Mediterranean" by locals, Alexandria is a popular tourist destination and an important industrial centre due to its natural gas and oil pipelines from Suez. The city extends about along the northern coast of Egypt, and is the largest city on t ...
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1856 Heraklion Earthquake
The 1856 Heraklion earthquake, also known as the Crete earthquake or Rhodes earthquake occurred on the morning of October 12 at 02:45 am local time. This extremely catastrophic earthquake had an estimated magnitude of 7.7 to 8.3 at a depth of approximately 61 to 100 km. The earthquake was felt over a very wide area extending from Sicily, Italy to the Levant and North Africa. On the Greek island of Crete, the effects of the earthquake were cataclysmic, over 500 bodies were recovered in the city of Heraklion. Shockwaves from the earthquake were felt intensely, covering all of the Ottoman Empire; present-day Turkey, Cyprus and the Middle East where damage and human losses were reported. In Malta, the earthquake collapsed the Għajn Ħadid Tower—a coastal watchtower built around the year 1638. In Cairo, Egypt, the earthquake destroyed buildings, created seiches in canals, and killed several people. Off the Egyptian and Italian coasts, sailors reported feeling a seaquake. Tecton ...
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