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List Of Earthquakes In Myanmar
Myanmar is one of the most seismically active countries in Southeast Asia. As it is on the Indian and Eurasian plate boundary, it is notorious for devastating earthquakes. Oblique subduction, block rotation, and a Transform fault, transform margin has been responsible for the seismic activities of the country. The Sagaing Fault is one of the largest sources of earthquakes in the country, having produced deadly quakes in the past centuries. Along the western coast, offshore Rakhine State, Rahkine State, the Sunda megathrust, Sunda Megathrust, where the Indian plate dives beneath the Burma plate is capable of producing large events and tsunamis like the 2004 Indian Ocean earthquake and tsunami, 2004 earthquake. Intermediate depth earthquakes east of the Chin Hills, Chin Range also pose a risk to people. The Shan Hills, Shan Plateau is another source of earthquakes, hosting many active Fault (geology), strike-slip faults that accommodate block rotation of the Sunda plate. The latest ea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1839 Ava Earthquake
The 1839 Ava earthquake, also known as the Amarapura earthquake or Inwa earthquake, was a disastrous seismic event that struck present-day central Myanmar on March 23. This earthquake with an estimated moment magnitude as high as 8.3, was one of the largest in the country, since 1762 Arakan earthquake, 1762. It was assigned a maximum of XI (''Extreme'') on the Modified Mercalli intensity scale, and was felt in Yangon, Rangoon and Bhamo. Damage was enormous in Ava, resulting in the death of hundreds. Tectonic setting Myanmar is wedged between four tectonic plates; the Indian plate, Indian, Eurasian plate, Eurasian, Sunda plate, Sunda, and Burma plates, that interact due to active Plate tectonics, geological processes. Along the west coast of the Coco Islands, off the Rahkine coast, and into Bangladesh, is a highly oblique convergent boundary known as the Sunda megathrust. This large fault marks the boundary between the Indian and Burma plates. The megathrust emerges from the seaflo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rakhine State
Rakhine State ( ; , ; ), formerly known as Arakan State, is a Administrative divisions of Myanmar, state in Myanmar (Burma). Situated on the western coast, it is bordered by Chin State to the north, Magway Region, Bago Region and Ayeyarwady Region to the east, the Bay of Bengal to the west and the Chittagong Division, Chattogram Division of Bangladesh to the northwest. It is located approximately between latitudes 17°30' north and 21°30' north and longitudes 92°10' east and 94°50' east. The north–south Arakan Mountains or Rakhine Yoma separate Rakhine State from central Myanmar. Off the coast of Rakhine State there are some fairly large islands such as Ramree Island, Ramree, Cheduba and Myingun Island, Myingun. Rakhine State has an area of and its capital is Sittwe (formerly known as Akyab). Names The state was historically known as Arakan in English until the Burmese government adopted the English name Rakhine in 1989. History The history of the region of Arakan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mohnyin District
Mohnyin District () is a Districts of Burma, district of the Kachin State in northern Myanmar. The administrative center is Mohnyin. Townships The district contains the following three Townships of Burma, townships: *Mongyaung Township *Mohnyin Township *Hpakant Township, Hpakant Township (Kamaing Township) See also *Mongyang State, a Shan state in what is today Burma; the main town was Mohnyin Districts of Myanmar Kachin State {{Kachin-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ayeyarwady Region
Ayeyarwady Region ( , , ; formerly Ayeyarwady Division and Irrawaddy Division) is a region of Myanmar, occupying the delta region of the Ayeyarwady River (Irrawaddy River). It is bordered by the Rakhine State to the northwest, the Bago Region to the north, Bago Region and Yangon Region to the east, and the Bay of Bengal to the south and west. The region lies between approximately latitude 15° 40' and 18° 30' north and between longitude 94° 15' and 96° 15' east. It has an area of . The estimated 2022 population is more than 6.5 million. According to the 2014 Burmese National Census the population of the Ayeyarwady Region was 6,184,829, making it the second most populous of Burma's states and regions after Yangon Region. Ayeyarwady Region is flanked by the Rakhine Yoma (Arakan Mountains) range in the west. Large areas have been cleared for paddy cultivation, leading to its preeminent position as the main rice producer in the country, a position it has retained into the 21st ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sagaing
Sagaing (, ) is a town in the Sagaing Region of Myanmar. It is located on the Irrawaddy River, to the south-west of Mandalay on the opposite bank of the river. Sagaing, with its numerous Buddhist monasteries, is an important religious and monastic centre. The pagodas and monasteries crowd the numerous hills along the ridge running parallel to the river. The central pagoda, Soon U Ponya Shin Pagoda, is connected by a set of covered staircases that run up the hill. Today, with about 70,000 inhabitants, the city is part of Mandalay metropolitan area, home to more than 1,022,000 inhabitants as of 2011. It is a frequent tourist destination for day trippers, usually as part of the "three former capitals" itinerary alongside Amarapura and Innwa. The city is home to five institutions of higher learning: the Sagaing Institute of Education, Sagaing Education College, Sagaing Technological University, Sagaing University of Co-operative and Management, and Sagaing Universit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mercalli Intensity Scale
The Modified Mercalli intensity scale (MM, MMI, or MCS) measures the effects of an earthquake at a given location. This is in contrast with the seismic magnitude usually reported for an earthquake. Magnitude scales measure the inherent force or strength of an earthquake — an event occurring at greater or lesser depth. (The "" scale is widely used.) The MMI scale measures intensity of shaking, at any particular location, on the surface. It was developed from Giuseppe Mercalli's Mercalli intensity scale of 1902. While shaking experienced at the surface is caused by the seismic energy released by an earthquake, earthquakes differ in how much of their energy is radiated as seismic waves. They also differ in the depth at which they occur; deeper earthquakes have less interaction with the surface, their energy is spread throughout a larger volume, and the energy reaching the surface is spread across a larger area. Shaking intensity is localised. It generally diminishes with dist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Earthquakes
An earthquakealso called a quake, tremor, or tembloris the shaking of the Earth's surface resulting from a sudden release of energy in the lithosphere that creates seismic waves. Earthquakes can range in intensity, from those so weak 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. The seismicity at a particular location in the Earth is the average rate of seismic energy release per unit volume. In its most general sense, the word ''earthquake'' is used to describe any seismic event that generates seismic waves. Earthquakes can occur naturally or be induced by human activities, such as mining, fracking, and nuclear weapons testing. The initial point of rupture is called the hypocenter or focus, while the ground level directly above it is the epi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sunda Plate
The Sunda plate is a minor tectonic plate straddling the equator in the Eastern Hemisphere on which the majority of Southeast Asia is located. The Sunda plate was formerly considered a part of the Eurasian plate, but the GPS measurements have confirmed its independent movement at 10 mm/yr eastward relative to Eurasia. Extent The Sunda plate includes the South China Sea, the Andaman Sea, southern parts of Vietnam, Myanmar, Laos and Thailand along with Malaysia, Singapore, Cambodia, southern Philippines, and the islands of Bali, Lombok, West Nusa Tenggara, Borneo, Sumatra, Java, and part of Sulawesi in Indonesia. The Sunda is bounded in the east by the Philippine Mobile Belt, Molucca Sea Collision Zone, Molucca Sea plate, Banda Sea plate and Timor plate; to the south and west by the Australian plate; and to the north by the Burma plate, Eurasian plate; and Yangtze plate. The Indo-Australian plate dips beneath the Sunda plate along the Sunda Trench also known as Jav ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fault (geology)
In geology, a fault is a Fracture (geology), planar fracture or discontinuity in a volume of Rock (geology), rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust (geology), crust result from the action of Plate tectonics, plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction, 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 (geometry), 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 geological maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shan Hills
The Shan Hills (; ''Shan Yoma''), also known as Shan Highland, is a vast mountainous zone that extends through Yunnan to Myanmar and Thailand. The whole region is made up of numerous peaks separated mostly by narrow valleys, as well as a few broader intermontane basins. The ranges in the area are aligned in such a way that they link to the foothills of the Himalayas further to the northwest. The highest point is Loi Leng, at an elevation of . Other peaks are the Mong Ling Shan, Doi Inthanon and m Loi Pangnao. All are ultra prominent peaks of Southeast Asia. Etymology The name of the massif or system of ranges, is derived from the Shan State and its peoples, said in its turn to be derived from the word "Siam", that occupies most of the Shan Highland area. Since it was relatively unexplored until recent times, the Shan mountainous region was referred to as the "Shan Plateau" in geographic works of the British colonial period, a name that is still sometimes used. Howe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chin Hills
The Chin Hills are a range of mountains in Chin State, northwestern Burma (Myanmar), that extends northward into India's Manipur state. Geography The highest peak in the Chin Hills is Khonu Msung, Nat Ma Taung, or Mount Victoria, in southern Chin State, which reaches . The Chin Hills–Arakan Yoma montane forests ecoregion has diverse forests with pine, camellia and teak. Falam is the largest town in the Chin Hills, lying at their southern edge. The Chin Hills are the eastern part of the Patkai Range, which includes the Lushai Hills and runs through Nagaland in India, as well as part of Burma. The Lushai Hills are frequently discussed with the Chin Hills as the topography, people's culture and history are similar. The southern prolongation of the Chin Hills is the Arakan Range (Arakan Yoma), stretching as well from north to south. History Historically the area of the range has been populated by the Chin people who like their neighbours to the west are a Laimi people. I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
2004 Indian Ocean Earthquake And Tsunami
On 26 December 2004, at 07:58:53 local time ( UTC+7), a major earthquake with a magnitude of 9.2–9.3 struck with an epicentre off the west coast of Aceh in northern Sumatra, Indonesia. The undersea megathrust earthquake, known in the scientific community as the Sumatra–Andaman earthquake, was caused by a rupture along the fault between the Burma plate and the Indian plate, and reached a Mercalli intensity of IX in some areas. A massive tsunami with waves up to high, known as the Boxing Day Tsunami after the Boxing Day holiday, or as the Asian Tsunami, devastated communities along the surrounding coasts of the Indian Ocean, killing an estimated 227,898 people in 14 countries, violently in Aceh (Indonesia), and severely in Sri Lanka, Tamil Nadu (India), and Khao Lak (Thailand). The direct result was major disruption to living conditions and commerce in coastal provinces of surrounding countries. It is the deadliest natural disaster of the 21st century, one of the d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
