2004 Battagram Earthquake
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2004 Battagram Earthquake
An earthquake struck Khyber Pakhtunkhwa Province, Pakistan on February 14, 2004. Extensive damage occurred and 24 people lost their lives. Tectonic setting Northern Pakistan lies at the southern margin of the broad zone of continental collision between the Eurasian and Indian Plates. The rate of convergence between these plates near this location is 38 mm per year. The main structures involved in accommodating this convergence are large thrust faults, such as the Main Central Thrust and the Main Frontal Thrust. Within the frontal thrust zone, there are many individual thrust faults. Many damaging earthquakes have resulted from movement on such thrust faults, such as the 2005 Kashmir earthquake which caused the deaths of around 87,000 people. Impact Eleven people were killed and 63 were injured by collapsing houses. Thirteen others were also killed and one was left missing when a landslide hit a minibus and fell into a deep ravine in Battagram. 564 houses were destroyed and ...
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Pakistan
Pakistan ( ur, ), officially the Islamic Republic of Pakistan ( ur, , label=none), is a country in South Asia. It is the world's List of countries and dependencies by population, fifth-most populous country, with a population of almost 243 million people, and has the world's Islam by country#Countries, second-largest Muslim population just behind Indonesia. Pakistan is the List of countries and dependencies by area, 33rd-largest country in the world by area and 2nd largest in South Asia, spanning . It has a coastline along the Arabian Sea and Gulf of Oman in the south, and is bordered by India to India–Pakistan border, the east, Afghanistan to Durand Line, the west, Iran to Iran–Pakistan border, the southwest, and China to China–Pakistan border, the northeast. It is separated narrowly from Tajikistan by Afghanistan's Wakhan Corridor in the north, and also shares a maritime border with Oman. Islamabad is the nation's capital, while Karachi is its largest city and fina ...
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2005 Kashmir Earthquake
The 2005 Kashmir earthquake occurred at on 8 October in Pakistani-administered Azad Kashmir. It was centred near the city of Muzaffarabad, and also affected nearby Balakot in Khyber Pakhtunkhwa and some areas of Indian-administered Jammu and Kashmir. It registered a moment magnitude of 7.6 and had a maximum Mercalli intensity of XI (''Extreme''). The earthquake was also felt in Afghanistan, Tajikistan, India, and the Xinjiang region. The severity of the damage caused by the earthquake is attributed to severe upthrust. Over 86,000 people died, a similar number were injured, and millions were displaced. It is considered the deadliest earthquake in South Asia, surpassing the 1935 Quetta earthquake. Earthquake Kashmir lies in the area of collision of the Eurasian and Indian tectonic plates. The geological activity born out of this collision, also responsible for the birth of the Himalayan mountain range, is the cause of unstable seismicity in the region. The United States Geolo ...
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2004 Earthquakes
4 (four) is a number, numeral and digit. It is the natural number following 3 and preceding 5. It is the smallest semiprime and composite number, and is considered unlucky in many East Asian cultures. In mathematics Four is the smallest composite number, its proper divisors being and . Four is the sum and product of two with itself: 2 + 2 = 4 = 2 x 2, the only number b such that a + a = b = a x a, which also makes four the smallest squared prime number p^. In Knuth's up-arrow notation, , and so forth, for any number of up arrows. By consequence, four is the only square one more than a prime number, specifically three. The sum of the first four prime numbers two + three + five + seven is the only sum of four consecutive prime numbers that yields an odd prime number, seventeen, which is the fourth super-prime. Four lies between the first proper pair of twin primes, three and five, which are the first two Fermat primes, like seventeen, which is the third. On ...
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List Of Earthquakes In Pakistan
Pakistan is one of the most seismically active countries in the world, being crossed by several major faults. As a result, earthquakes in Pakistan occur often and are destructive. Geology Pakistan geologically overlaps both the Eurasian and Indian tectonic plates. Balochistan, the Federally Administered Tribal Areas, Khyber Pakhtunkhwa and Gilgit-Baltistan provinces lie on the southern edge of the Eurasian Plate on the Iranian Plateau. Sindh, Punjab and Azad Jammu & Kashmir provinces lie on the north-western edge of the Indian plate in South Asia. Hence this region is prone to violent earthquakes, as the two tectonic plates collide. Earthquakes See also *List of faults in Pakistan * National Disaster Management Authority *Earthquake Reconstruction & Rehabilitation Authority References Sources * * Further reading * External linksNorthern Pakistan 1974 December 28 12:11:43 UTC Magnitude 6.2 USGS accessed Jan 2009 {{DEFAULTSORT:List of Earthquakes in Pakistan ...
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List Of Earthquakes In 2004
This is a list of earthquakes in 2004. Only earthquakes of magnitude 6 or above are included, unless they resulted in significant damage or casualties, or were notable for some other reason. All dates are listed according to UTC time. The year 2004 had the most major earthquakes since 1999. In total, there were 16 magnitude 7.0+ earthquakes this year, 6 of them were in Indonesia. Most of the earthquake deaths in 2004 were caused by the magnitude 9.1–9.3 earthquake off the west coast of Sumatra in December. Most of the deaths were caused by a devastating tsunami that spread across the Indian Ocean. There were several other deadly and destructive earthquakes, including Morocco's largest earthquake to date, which caused 628 deaths. Japan was hit by a magnitude 6.6 earthquake, which caused 68 deaths and $28 billion in damages, making it the fourth costliest earthquake in history. Compared to other years Overall By death toll * Note: At least 10 dead By magnitude * ...
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Pakistani Rupee
The Pakistani rupee ( ur, / ALA-LC: ; sign: Re (singular) and Rs (plural); ISO code: PKR) is the official currency of Pakistan since 1948. The coins and notes are issued and controlled by the central bank, namely State Bank of Pakistan. In Pakistani English, large values of rupees are counted in thousands; lakh (100,000); crore (ten-millions); Arab (billions); kharab (100 billion). Numbers are still grouped in thousands (123,456,789 rather than 12,34,56,789 as written in India) History The word ''rūpiya'' is derived from the Sanskrit word ''rūpya'', which means "wrought silver, a coin of silver", in origin an adjective meaning "shapely", with a more specific meaning of "stamped, impressed", whence "coin". It is` derived from the noun ''rūpa'' "shape, likeness, image". ''Rūpaya'' was used to denote the coin introduced by Sher Shah Suri during his reign from 1540 to 1545 CE. The Pakistani rupee was put into circulation in Pakistan after the dissolution of the ...
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ReliefWeb
ReliefWeb is a humanitarian information portal founded in 1996. The portal now hosts more than 720,000 humanitarian situation reports, press releases, evaluations, guidelines, assessments, maps and infographics. The portal is an independent vehicle of information, designed specifically to assist the international humanitarian community in effective delivery of emergency assistance or ''relief''. It provides information as humanitarian crises unfold, while emphasizing the coverage of "forgotten emergencies" at the same time. Origin and development ReliefWeb was founded in October 1996 and is administered by the United Nations Office for the Coordination of Humanitarian Affairs (OCHA). The project began under the US Department of State, Bureau of International Organization Affairs, which had noticed during the Rwanda crisis how poorly critical operational information was shared between NGOs, UN Agencies and Governments. In 1995, the Department's Senior Policy Adviser on Disas ...
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Battagram
Battagram ( ur, , ps, ) is a city and Union Council of Battagram District in Khyber Pakhtunkhwa Province of Pakistan. It is located at 34°41'N 73°1'E and has an altitude of 1038 metres (3408 feet). Climate With a mild and generally warm and temperate climate, Battagram features a humid subtropical climate A humid subtropical climate is a zone of climate characterized by hot and humid summers, and cool to mild winters. These climates normally lie on the southeast side of all continents (except Antarctica), generally between latitudes 25° and 40° ... (''Cfa'') under the Köppen climate classification. The average temperature in Battagram is , while the annual precipitation averages . June is the hottest month of the year with an average temperature of . The coldest month, January, has an average temperature of . Education The schools are being built with the help of several NGOs and foreign funds to improve the literacy rate of the people. 2005 earthquake ...
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Main Frontal Thrust
The Main Frontal Thrust (MFT), also known as the Himalayan Frontal Thrust (HFT) is a geological fault in the Himalayas that defines the boundary between the Himalayan foothills and Indo-Gangetic Plain. The fault is well expressed on the surface thus could be seen via satellite imagery. It is the youngest and southernmost thrust structure in the Himalaya deformation front. It is a splay branch of the Main Himalayan Thrust (MHT) as the root décollement. It runs parallel to other major splays of the MHT; Main Boundary Thrust (MBT) and Main Central Thrust (MCT). The Sunda Megathrust, which extends from the Banda Islands to Myanmar is joined with the MFT. The fault strikes in a NW-SE direction and dips at an angle of 20° to 30° in the north. Main Boundary Thrust The Main Boundary Thrust (MBT) is another major thrust fault in the Himalaya orogenic wedge that was active in the Cenozoic The Cenozoic ( ; ) is Earth's current geological era, representing the last 66million ...
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Peak Ground Acceleration
Peak ground acceleration (PGA) is equal to the maximum ground acceleration that occurred during earthquake shaking at a location. PGA is equal to the amplitude of the largest absolute acceleration recorded on an wikt:accelerogram, accelerogram at a site during a particular earthquake. Earthquake shaking generally occurs in all three directions. Therefore, PGA is often split into the horizontal and vertical components. Horizontal PGAs are generally larger than those in the vertical direction but this is not always true, especially close to large earthquakes. PGA is an important parameter (also known as an intensity measure) for earthquake engineering, The design basis earthquake ground motion (DBEGM) is often defined in terms of PGA. Unlike the Richter magnitude scale, Richter and Moment magnitude scale, moment magnitude scales, it is not a measure of the total seismic scales#Magnitude and intensity, energy (magnitude, or size) of an earthquake, but rather of how hard the earth shake ...
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Main Central Thrust
The Main Central Thrust is a major geological fault where the Indian Plate has pushed under the Eurasian Plate along the Himalaya. The fault slopes down to the north and is exposed on the surface in a NW-SE direction (strike). It is a thrust fault that continues along 2900 km of the Himalaya mountain belt.Upreti, B. N.An overview of the stratigraphy and tectonics of the Nepal Himalaya ''Journal of Asian Earth Sciences'' 17.5 (1994): 577–606. The generally accepted definition of the Main Central Thrust is that it is a ductile shear zone along which the High-grade Great Himalayan Crystalline complex was placed above the low-grade to unmetamorphosed Lesser Himalayan Sequence.Helm, A., and A. Gansser. "Central Himalaya, Geological observations of the Swiss expedition 1936." ''Memoires de la Societe Helvetique des Sciences Naturelles'' 73.1,245 (1939). However, this definition is not perfect because of many difficulties and complications defining the Main Central Thrust. Many geo ...
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Thrust Fault
A thrust fault is a break in the Earth's crust, across which older rocks are pushed above younger rocks. Thrust geometry and nomenclature Reverse faults A thrust fault is a type of reverse fault that has a dip of 45 degrees or less. If the angle of the fault plane is lower (often less than 15 degrees from the horizontal) and the displacement of the overlying block is large (often in the kilometer range) the fault is called an ''overthrust'' or ''overthrust fault''. Erosion can remove part of the overlying block, creating a ''fenster'' (or ''window'') – when the underlying block is exposed only in a relatively small area. When erosion removes most of the overlying block, leaving island-like remnants resting on the lower block, the remnants are called ''klippen'' (singular ''klippe''). Blind thrust faults If the fault plane terminates before it reaches the Earth's surface, it is referred to as a ''blind thrust'' fault. Because of the lack of surface evidence, blind thr ...
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