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2012 Shwebo Earthquake
The 2012 Shwebo earthquake occurred at 07:42 local time (01:12 UTC) on 11 November in Myanmar. It had a magnitude of 6.8 on the moment magnitude scale and a maximum perceived intensity of VIII (''Severe'') on the Mercalli intensity scale. The epicenter was near the town of Male, 52 km NNE of the city of Shwebo, 64 km west of Mogok and 120 km north of Mandalay. Significant damage and possible casualties have been reported from near the epicenter, with up to 26 people dead and many more injured. Part of a bridge under construction fell into the Irrawaddy River near Shwebo and a gold mine collapsed at Sintku. An aftershock with a magnitude of 5.8 followed at 17:24 local time (10:54 UTC). Tectonic setting Central Burma lies within the complex zone of collision between the Indo-Australian Plate and the Eurasian Plate. In this area the collision is highly oblique and much of the plate convergence is accommodated by right lateral strike slip faults, of which the lar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burma
Myanmar, ; UK pronunciations: US pronunciations incl. . Note: Wikipedia's IPA conventions require indicating /r/ even in British English although only some British English speakers pronounce r at the end of syllables. As John C. Wells, John Wells explains, the English spellings of both Myanmar and Burma assume a non-rhotic variety of English, in which the letter r before a consonant or finally serves merely to indicate a long vowel: [ˈmjænmɑː, ˈbɜːmə]. So the pronunciation of the last syllable of Myanmar as [mɑːr] or of Burma as [bɜːrmə] by some speakers in the UK and most speakers in North America is in fact a spelling pronunciation based on a misunderstanding of non-rhotic spelling conventions. The final ''r'' in ''Myanmar'' was not intended for pronunciation and is there to ensure that the final a is pronounced with the broad a, broad ''ah'' () in "father". If the Burmese name my, မြန်မာ, label=none were spelled "Myanma" in English, this would b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Indo-Australian Plate
The Indo-Australian Plate is a major tectonic plate that includes the continent of Australia and the surrounding ocean and extends northwest to include the Indian subcontinent and the adjacent waters. It was formed by the fusion of the Indian and the Australian Plates approximately 43 million years ago. The fusion happened when the mid-ocean ridge in the Indian Ocean, which separated the two plates, ceased spreading. Regions India, Australia, New Guinea, Tasmania, New Zealand, and New Caledonia are all fragments of the ancient supercontinent of Gondwana. As the ocean floor broke apart, these land masses fragmented from one another, and for a time these centers were thought to be dormant and fused into a single plate. However, research in the early 21st century indicates plate separation of the Indo-Australian Plate may have already occurred. Characteristics The eastern side of the plate is the convergent boundary with the Pacific plate. The Pacific plate sinks below the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Earthquakes In Myanmar
Myanmar (also known as Burma) is the northwesternmost country of mainland Southeast Asia located on the Mainland Southeast Asia, Indochinese peninsula. With an area of 261,228 sq mi (676,578 sq km), it is the second largest country in Southeast Asia and the largest on mainland Southeast Asia. The kite-shaped country stretches from 10'N to 20'N for 1,275 miles (2,050 km) with a long tail running along the western coast of the Malay Peninsula. Myanmar lies along the Indian Plate, Indian and Eurasian Plates, to the southeast of the Tibetan Plateau. To its west is the Bay of Bengal and to its south is the Andaman Sea. The country is nestled between several mountain ranges with the Arakan Mountains on the west and the Shan Plateau dominating the east. The central valley follows the Irrawaddy River, the most economically important river to the country with 39.5 million people, including the largest city Yangon, living within its basin. The country is home to many diverse ethnic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
2012 Earthquakes
This is a list of earthquakes in 2012. Only earthquakes of magnitude 6 or above are included, unless they result in damage or casualties, or are notable for some other reason. All dates are listed according to UTC time. Two huge 8 magnitude earthquakes (8.6 and 8.2) struck Indonesia in April, but caused little damage, and no tsunami. The deadliest quake occurred in Iran, while other destructive tremors were observed in Philippines, China, or Afghanistan. Compared to other years Overall By death toll * Note: At least 10 casualties By magnitude * Note: At least 7.0 magnitude By month January * A magnitude 6.8 earthquake struck Izu Islands, Japan, on January 1, at a depth of 348.5 km. * A magnitude 5.5 earthquake struck Peravia Province, Dominican Republic, on January 5, at a depth of 39.8 km. One person died of a cardiac arrest in Santo Domingo, as well as minor damage was reported. * A magnitude 6.6 earthquake struck Santa Cruz Islands, on January 8, at a dep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Earthquakes In Myanmar
Myanmar is one of the most seismically active regions in the world. Oblique subduction, block rotation, and a 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 Rahkine State, the Sunda Megathrust, where the Indian Plate dives beneath the Burma Plate is capable of producing large events and tsunamis like the 2004 earthquake. Intermediate depth earthquakes east of the Chin Range also pose a risk to people. The Shan Plateau is another source of earthquakes, hosting many active strike-slip faults that accommodate block rotation of the Sunda Plate. Notable earthquakes in the history of Myanmar include the following: Earthquakes Tsunamis affecting Myanmar * 1881 Nicobar Islands earthquake * 1941 Andaman Islands earthquake * 2004 Indian Ocean earthquake See also *Geology of Myanmar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Earthquakes In 2012
This is a list of earthquakes in 2012. Only earthquakes of magnitude 6 or above are included, unless they result in damage or casualties, or are notable for some other reason. All dates are listed according to UTC time. Two huge 8 magnitude earthquakes (8.6 and 8.2) struck Indonesia in April, but caused little damage, and no tsunami. The deadliest quake occurred in Iran, while other destructive tremors were observed in Philippines, China, or Afghanistan. Compared to other years Overall By death toll * Note: At least 10 casualties By magnitude * Note: At least 7.0 magnitude By month January * A magnitude 6.8 earthquake struck Izu Islands, Japan, on January 1, at a depth of 348.5 km. * A magnitude 5.5 earthquake struck Peravia Province, Dominican Republic, on January 5, at a depth of 39.8 km. One person died of a cardiac arrest in Santo Domingo, as well as minor damage was reported. * A magnitude 6.6 earthquake struck Santa Cruz Islands, on January 8, at a dept ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thabeikkyin
Thabeikkyin is a town in the Mandalay Region of central Myanmar. It is alleged by the Democratic Voice of Burma that a secret nuclear facility is located there See also *Thabeikkyin District Thabeikkyin District ( my, သပိတ်ကျင်း ခရိုင်) is the district of Mandalay Region, Myanmar. It's principal town is Thabeikkyin. __TOC__ Townships The townships, cities, towns that are included in Thabeikkyin Distric ... References External linksSatellite map at Maplandia.com Populated places in Pyin Oo Lwin District Township capitals of Myanmar {{Mandalay-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aftershock
In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in the same area of the main shock, caused as the displaced crust adjusts to the effects of the main shock. Large earthquakes can have hundreds to thousands of instrumentally detectable aftershocks, which steadily decrease in magnitude and frequency according to a consistent pattern. In some earthquakes the main rupture happens in two or more steps, resulting in multiple main shocks. These are known as doublet earthquakes, and in general can be distinguished from aftershocks in having similar magnitudes and nearly identical seismic waveforms. Distribution of aftershocks Most aftershocks are located over the full area of fault rupture and either occur along the fault plane itself or along other faults within the volume affected by the strain associated with the main shock. Typically, aftershocks are found up to a distance equal to the rupture length away from the fault plane. The patte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tagaung
Tagaung is a town in Mandalay Region of Myanmar (Burma). It is situated on the east bank of the Ayeyarwady River, 127 miles north of Mandalay. Etymology "Tagaung" derives from the Shan language term "Takawng" ( shn, တႃႈၵွင်; ), which means "drum ferry." Transport The Ayeyarwady remains the principal means to reach Tagaung. It is linked to Mandalay and to Kachin State in the north also by the Mandalay-Tagaung- Shwegu-Bhamo-Myitkyina Union Highway. History Pre-Christian era and first millennium The 19th-century chronicle ''Hmannan Yazawin'' introduces Tagaung as the very first capital of Burma, along with the adage ''Myanmar asa Tagaung ga'' (Myanmar starts from Tagaung), and it was the ancient capital of the Pyu, who were the forerunners of the Burmese people. Its history is steeped in myth and legend. The city is said to have been founded in 850 BC by King Abhiraja of the Sakya clan from Kapilavastu in India, before the time of the Buddha. It has a very impo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Singu
Singu is a town in the Mandalay Region of central Myanmar. It is the capital of Singu Township. Geography Singu is located by the Irrawaddy about 55 km to the south of Letha Taung Letha Taung, also known as the Singu Plateau, is a small volcanic plateau in central Burma (Myanmar). Geography Letha Taung is located near Nweyon, Singu Township, Pyinoolwin District, Mandalay Division, about 3 km west of National Highwa ..., also known as the Singu Plateau. References External linksSatellite map at Maplandia.com Populated places in Mandalay Region Township capitals of Myanmar {{Mandalay-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sagaing Fault
The Sagaing Fault is a major fault in Burma, a mainly continental right-lateral transform fault between the Indian Plate and Sunda Plate. It links the divergent boundary in the Andaman Sea with the zone of active continental collision along the Himalayan front. It passes through populated cities of Mandalay, Yamethin, Pyinmana, the capital Naypyidaw, Toungoo and Pegu before dropping off into the Gulf of Martaban, running for a total length of over 1200 kilometers. Geomorphology The Sagaing Fault begins offshore in the Andaman Sea before passing through the central Myanmar basin. The fault has a relatively low topographical relief for most of its length compared to the Shan Scarp Fault to the west. Slip rate and displacement The total slip rate across the Indian–Sunda Plate boundary is about 35 mm/yr, of which 18 mm/yr is accommodated by the Sagaing Fault, according to GPS data. The measured maximum displacement along the fault is about 100 km, although several au ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
