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2019 Albania Earthquake
Northwestern Albania was struck by a magnitude 6.4 earthquake with an epicentre 16 kilometres (9.9 mi) west-southwest of Mamurras, at 03:54 CET (UTC+1) on 26 November 2019. The earthquake lasted at least 50 seconds and was felt in Albania's capital Tirana, and in places as far away as Bari, Taranto and Belgrade, 370 kilometres (230 mi) northeast of the epicentre. The maximum felt intensity was VIII (''Severe'') on the Modified Mercalli intensity scale. A total of 51 people were killed in the earthquake, with about 3,000 injured. It was the second earthquake to strike the region in the space of three months. It was the strongest earthquake to hit Albania in more than 40 years, its deadliest earthquake in 99 years and the world's deadliest earthquake in 2019. Tectonic setting Albania lies across the convergent boundary between the Eurasian Plate and the Adriatic Plate, part of the complex collision zone with the African Plate. The structure of the western part o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Durrës
Durrës ( , ; sq-definite, Durrësi) is the second most populous city of the Republic of Albania and seat of Durrës County and Durrës Municipality. It is located on a flat plain along the Albanian Adriatic Sea Coast between the mouths of the Erzen and Ishëm at the southeastern corner of the Adriatic Sea. Durrës' climate is profoundly influenced by a seasonal Mediterranean climate. Durrës was founded by Ancient Greek colonists from Corinth and Corcyra under the name of Epidamnos around the 7th century BC in cooperation with the local Illyrian Taulantii. Also known as Dyrrachium, Durrës essentially developed as it became an integral part of the Roman Empire and its successor the Byzantine Empire. The Via Egnatia, the continuation of the Via Appia, started in the city and led across the interior of the Balkan Peninsula to Constantinople in the east. In the Middle Ages, Durrës was contested between Bulgarian, Venetian and Ottoman dominions. The Ottomans ultimatel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Belgrade
Belgrade ( , ;, ; Names of European cities in different languages: B, names in other languages) is the Capital city, capital and List of cities in Serbia, largest city in Serbia. It is located at the confluence of the Sava and Danube rivers and the crossroads of the Pannonian Basin, Pannonian Plain and the Balkan Peninsula. Nearly 1,166,763 million people live within the administrative limits of the City of Belgrade. It is the third largest of all List of cities and towns on Danube river, cities on the Danube river. Belgrade is one of the List of oldest continuously inhabited cities, oldest continuously inhabited cities in Europe and the world. One of the most important prehistoric cultures of Europe, the Vinča culture, evolved within the Belgrade area in the 6th millennium BC. In antiquity, Thracians, Thraco-Dacians inhabited the region and, after 279 BC, Celts settled the city, naming it ''Singidunum, Singidūn''. It was Roman Serbia, conquered by the Romans under the reign ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Montenegro
) , image_map = Europe-Montenegro.svg , map_caption = , image_map2 = , capital = Podgorica , coordinates = , largest_city = capital , official_languages = Montenegrin , languages2_type = Languages in official use , languages2 = , ethnic_groups = , ethnic_groups_year = 2011 , religion = , religion_year = 2011 , demonym = Montenegrin , government_type = Unitary parliamentary republic , leader_title1 = President , leader_name1 = Milo Đukanović , leader_title2 = Prime Minister , leader_name2 = Dritan Abazović (acting) , leader_title3 = Speaker , leader_name3 = Danijela Đurović , legislature = Skupština , sovereignty_type = Establishment history , established_event1 = Principality of Duklja , established_date1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1979 Montenegro Earthquake
The 1979 Montenegro earthquake occurred on 15 April at 06:19 UTC with a moment magnitude of 6.9 and a maximum Mercalli intensity of X (''Extreme''). It was the most devastating earthquake in SR Montenegro, then part of Yugoslavia,(Montenegrin)Crnogorski zemljotres ukroćen u Skoplju Vijesti and was mostly felt along the Montenegrin and Albanian coastline. It was also felt in other parts of the country (in Podgorica and Dubrovnik with intensity of VII, in Sarajevo and Skopje V-VI, in Belgrade IV, in Zagreb and Ljubljana III-IV). The main earthquake was followed by more than 90 aftershocks stronger than 4.0 on Richter scale, strongest of which occurred on 24 May 1979, with a magnitude of 6.3. Damage Budva's Old Town, one of Montenegro's Cultural Heritage Sites, was heavily devastated. Of the 400 buildings in Budva's Old Town, 8 remained unscathed from the earthquake. The 15th century walls and ramparts protecting the Old Town were severely damaged as well. Praskvica Monastery, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Active Fault
An active fault is a fault that is likely to become the source of another earthquake sometime in the future. Geologists commonly consider faults to be active if there has been movement observed or evidence of seismic activity during the last 10,000 years. * Active faulting is considered to be a geologic hazard - one related to earthquakes as a cause. Effects of movement on an active fault include strong ground motion, surface faulting, tectonic deformation, landslides and rockfalls, liquefaction, tsunamis, and seiches. Quaternary faults are those active faults that have been recognized at the surface and which have evidence of movement during the Quaternary Period. Related geological disciplines for ''active-fault'' studies include geomorphology, seismology, reflection seismology, plate tectonics, geodetics and remote sensing, risk analysis, and others. Location Active faults tend to occur in the vicinity of tectonic plate boundaries, and active fault research has foc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thrust Tectonics
Thrust tectonics or contractional tectonics is concerned with the structures formed by, and the tectonic processes associated with, the shortening and thickening of the crust or lithosphere. It is one of the three main types of tectonic regime, the others being extensional tectonics and strike-slip tectonics. These match the three types of plate boundary, convergent (thrust), divergent (extensional) and transform (strike-slip). There are two main types of thrust tectonics, thin-skinned and thick-skinned, depending on whether or not basement rocks are involved in the deformation. The principle geological environments where thrust tectonics is observed are zones of continental collision, restraining bends on strike-slip faults and as part of detached fault systems on some passive margins. Deformation styles In areas of thrust tectonics, two main processes are recognized: thin-skinned deformation and thick-skinned deformation. The distinction is important as attempts to structur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
African Plate
The African Plate is a major tectonic plate that includes much of the continent of Africa (except for its easternmost part) and the adjacent oceanic crust to the west and south. It is bounded by the North American Plate and South American Plate to the west (separated by the Mid-Atlantic Ridge); the Arabian Plate and Somali Plate to the east; the Eurasian Plate, Aegean Sea Plate and Anatolian Plate to the north; and the Antarctic Plate to the south. Between and , the Somali Plate began rifting from the African Plate along the East African Rift. Since the continent of Africa consists of crust from both the African and the Somali plates, some literature refers to the African Plate as the Nubian Plate to distinguish it from the continent as a whole. Boundaries The western edge of the African Plate is a divergent boundary with the North American Plate to the north and the South American Plate to the south which forms the central and southern part of the Mid-Atlantic Ridge. The A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Collision Zone
A collision zone occurs when tectonic plates meet at a convergent boundary both bearing continental lithosphere. As continental lithosphere is usually not subducted due to its relative low density, the result is a complex area of orogeny involving folding and thrust faulting as the blocks of continental crust ''pile up'' above the subduction zone. This includes the Eastern Anatolian collision zone and Banda Arc–Australian collision zone.Karig, Daniel E., et al., ''Nature and distribution of deformation across the Banda Arc–Australian collision zone at Timor,'' GSA Bulletin; January 1987; v. 98; no. 1; pp. 18–32 See also *List of tectonic plate interactions Tectonic plate interactions are classified into three basic types: * Divergent boundaries are areas where plates move away from each other, forming either mid-ocean ridges or rift valleys. These are also known as constructive boundaries. ... References {{reflist Tectonics ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adriatic Plate
The Adriatic or Apulian Plate is a small tectonic plate carrying primarily continental crust that broke away from the African Plate along a large transform fault in the Cretaceous period. The name Adriatic Plate is usually used when referring to the northern part of the plate. This part of the plate was deformed during the Alpine orogeny, when the Adriatic/Apulian Plate collided with the Eurasian Plate. The Adriatic/Apulian Plate is thought to still move independently of the Eurasian Plate in NNE direction with a small component of counter-clockwise rotation. The fault zone that separates the two is the Periadriatic Seam that runs through the Alps. Studies indicate that in addition to deforming, the Eurasian continental crust has actually subducted to some extent below the Adriatic/Apulian Plate, an unusual circumstance in plate tectonics. Oceanic crust of the African Plate is also subducting under the Adriatic/Apulian Plate off the western and southern coasts of the Italia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eurasian Plate
The Eurasian Plate is a tectonic plate that includes most of the continent of Eurasia (a landmass consisting of the traditional continents of Europe and Asia), with the notable exceptions of the Indian subcontinent, the Arabian subcontinent and the area east of the Chersky Range in eastern Siberia. It also includes oceanic crust extending westward to the Mid-Atlantic Ridge and northward to the Gakkel Ridge. The eastern edge is a boundary with the North American Plate to the north and a boundary with the Philippine Sea Plate to the south and possibly with the Okhotsk Plate and the Amurian Plate. The southern edge is a boundary with the African Plate to the west, the Arabian Plate in the middle and the Indo-Australian Plate to the east. The western edge is a divergent boundary with the North American Plate forming the northernmost part of the Mid-Atlantic Ridge, which is straddled by Iceland. All volcanic eruptions in Iceland, such as the 1973 eruption of Eldfell, the 1783 eruptio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Convergent Boundary
A convergent boundary (also known as a destructive boundary) is an area on Earth where two or more Plate tectonics, lithospheric plates collide. One plate eventually slides beneath the other, a process known as subduction. The subduction zone can be defined by a plane where many earthquakes occur, called the Wadati–Benioff zone. These collisions happen on scales of millions to tens of millions of years and can lead to volcanism, earthquakes, Orogeny, orogenesis, destruction of lithosphere, and Deformation (geology), deformation. Convergent boundaries occur between oceanic-oceanic lithosphere, oceanic-continental lithosphere, and continental-continental lithosphere. The geologic features related to convergent boundaries vary depending on crust types. Plate tectonics is driven by convection cells in the mantle. Convection cells are the result of heat generated by the radioactive decay of elements in the mantle escaping to the surface and the return of cool materials from the surfac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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