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Nawnghkio Township
Nawnghkio Township is a township of Kyaukme District in the Shan State of eastern Myanmar. The principal town and administrative seat is Nawnghkio. The name 'Nawnghkio' was started to call after a camp near a green lake ( Shan language: nawng = lake or natural pond, hkio = green). The lake is located in the west of 'Haw Taw Monastery' of today's Nawnghkio.[]Nawnghkio Township Profile 2009, Township Peace and Development Council Geography The township lies between 22° 45' and 23° 15' north latitude and 96° 00' and 97° 00' east longitude. Altitude ranges from 700 feet above the sea level in the lowest to 4300 feet in the highest with an average of 2750 feet. Occupying nearly half of the center of the land is highly productive plane surrounded by mountains in north, east, south and west. Mountains of the southern region are the highest. More than half of the surface area is covered by rain forests. Average number of raining days range from 90 to 130 days per year and annual rail ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Townships Of Myanmar
Townships ( my, မြို့နယ်, Mrui.nay; ) are the third-level administrative divisions of Myanmar. They are the sub-divisions of the Districts of Myanmar. According to the Myanmar Information Management Unit (MIMU), as of December 2015, there are 330 townships in Myanmar."Myanmar States/Divisions & Townships Overview Map" Myanmar Information Management Unit (MIMU) Townships are the basic administrative unit of local governance and are the only type of administrative division that covers the entirety of Myanmar. A Township is administered by a Township Administrator, a civil servant appointed through the [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bamar
The Bamar (, ; also known as the Burmans) are a Sino-Tibetan ethnic group native to Myanmar (formerly Burma) in Southeast Asia. With approximately 35 million people, the Bamar make up the largest ethnic group in Myanmar, constituting 68% of the country's population. The geographic homeland of the Bamar is the Irrawaddy River basin. Burmese is the native language of the Bamar, as well as the national language and lingua franca of Myanmar. Ethnonyms In the Burmese language, Bamar (ဗမာ, also transcribed Bama) and Myanmar (မြန်မာ, also transliterated Mranma and transcribed Myanma) have historically been interchangeable endonyms. Burmese is a diglossic language; "Bamar" is the diglossic low form of "Myanmar," which is the diglossic high equivalent. The term "Myanmar" is extant to the early 1100s, first appearing on a stone inscription, where it was used as a cultural identifier, and has continued to be used in this manner. From the onset of British colonial r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shan People
The Shan people ( shn, တႆး; , my, ရှမ်းလူမျိုး; ), also known as the Tai Long, or Tai Yai are a Tai ethnic group of Southeast Asia. The Shan are the biggest minority of Burma (Myanmar) and primarily live in the Shan State of this country, but also inhabit parts of Mandalay Region, Kachin State, and Kayin State, and in adjacent regions of China ( Dai people), Laos, Assam (Ahom people) and Thailand. Though no reliable census has been taken in Burma since 1935, the Shan are estimated to number 4–6 million, with CIA Factbook giving an estimate of five million spread throughout Myanmar which is about 10% of the overall Burmese population. 'Shan' is a generic term for all Tai-speaking peoples within Myanmar (Burma). The capital of Shan State is Taunggyi, the fifth-largest city in Myanmar with about 390,000 people. Other major cities include Thibaw (Hsipaw), Lashio, Kengtung and Tachileik. Etymology The Shan use the endonym Tai (တႆး) in r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Danu People
The Danu people ( my, ဓနု) are a government-recognized ethnic group in Myanmar, predominantly populating the areas near the Pindaya Caves in Shan State. They speak the Danu language. at (18th ed., 2015) Etymology The name ''Danu'' derives from the term ''dhanu'', which means "archer" or "bow." The term ''dhanu'' is a reference to the legend of Prince Kummabhaya, whose bow and arrow rescued seven princesses trapped in the caves by a giant spider.Notable Danu people * |
Ethnic Groups
An ethnic group or an ethnicity is a grouping of people who identify with each other on the basis of shared attributes that distinguish them from other groups. Those attributes can include common sets of traditions, ancestry, language, history, society, culture, nation, religion, or social treatment within their residing area. The term ethnicity is often times used interchangeably with the term nation, particularly in cases of ethnic nationalism, and is separate from the related concept of races. Ethnicity may be construed as an inherited or as a societally imposed construct. Ethnic membership tends to be defined by a shared cultural heritage, ancestry, origin myth, history, homeland, language, or dialect, symbolic systems such as religion, mythology and ritual, cuisine, dressing style, art, or physical appearance. Ethnic groups may share a narrow or broad spectrum of genetic ancestry, depending on group identification, with many groups having mixed genetic ancestry. Ethnic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kayah State
Kayah State ( my, ကယားပြည်နယ်, formerly Karenni State) is a state of Myanmar. Situated in eastern Myanmar, it is bounded on the north by Shan State, on the east by Thailand's Mae Hong Son Province, and on the south and west by Kayin State. It lies approximately between 18° 30′ and 19° 55′ north latitude and between 96° 50′ and 97° 50′ east longitude. The area is . Its capital is Loikaw (also spelt Loi-kaw). The estimated population in 1998 was approximately 207,357, according to UNICEF. It is inhabited primarily by the Karenni ethnic group, also known as Red Karen or Kayah, a Sino-Tibetan people. Geography Karenni (Kayah) State is located in the eastern part of Myanmar. The relief of Karenni (Kayah) State is mountainous with the Dawna Range and the Karen Hills also known as "Karenni-Karen" mountains separated by the Salween River as it flows through Karenni (Kayah) State. Balu Chaung flows from Inle Lake to Than Lwin River and converges with t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aftershocks
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 pattern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Foreshock
A foreshock is an earthquake that occurs before a larger seismic event (the mainshock) and is related to it in both time and space. The designation of an earthquake as ''foreshock'', ''mainshock'' or aftershock is only possible after the full sequence of events has happened. Occurrence Foreshock activity has been detected for about 40% of all moderate to large earthquakes, and about 70% for events of M>7.0. They occur from a matter of minutes to days or even longer before the main shock; for example, the 2002 Sumatra earthquake is regarded as a foreshock of the 2004 Indian Ocean earthquake with a delay of more than two years between the two events. Some great earthquakes (M>8.0) show no foreshock activity at all, such as the M8.6 1950 India–China earthquake. The increase in foreshock activity is difficult to quantify for individual earthquakes but becomes apparent when combining the results of many different events. From such combined observations, the increase before the mai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seismotectonics
Seismotectonics is the study of the relationship between the earthquakes, active tectonics and individual faults of a region. It seeks to understand which faults are responsible for seismic activity in an area by analysing a combination of regional tectonics, recent instrumentally recorded events, accounts of historical earthquakes and geomorphological evidence. This information can then be used to quantify the seismic hazard of an area. Methodology A seismotectonic analysis of an area often involves the integration of disparate datasets. Regional tectonics An understanding of the regional tectonics of an area is likely to be derived from published geological maps, research publications on the geological structure and seismic reflection profiles, where available, augmented by other geophysical data. In order to understand the seismic hazard of an area it is necessary not only to know where potentially active faults are, but also the orientation of the stress field. This is no ... [...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 the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Richter Scale
The Richter scale —also called the Richter magnitude scale, Richter's magnitude scale, and the Gutenberg–Richter scale—is a measure of the strength of earthquakes, developed by Charles Francis Richter and presented in his landmark 1935 paper, where he called it the "magnitude scale". This was later revised and renamed the local magnitude scale, denoted as ML or . Because of various shortcomings of the original scale, most seismological authorities now use other similar scales such as the moment magnitude scale () to report earthquake magnitudes, but much of the news media still erroneously refers to these as "Richter" magnitudes. All magnitude scales retain the logarithmic character of the original and are scaled to have roughly comparable numeric values (typically in the middle of the scale). Due to the variance in earthquakes, it is essential to understand the Richter scale uses logarithms simply to make the measurements manageable (i.e., a magnitude 3 quake factors ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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