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Pegu Yomas
The Pegu Range ( my, ပဲခူးရိုးမ; Pegu Yoma or Bago Yoma) is a range of low mountains or hillsSeekins, Donald M. (2006) ''Historical dictionary of Burma (Myanmar)'' Scarecrow Press, Lanham, Marylandpage 357 and uplands between the Irrawaddy and the Sittaung River in central Burma (Myanmar). The range runs from Mount Popa in the north to Singuttara Hill (Theingottara Hill) in the south. Both the Pegu River and the Sittaung River originate in the Pegu Range. High points Among the notable peaks or hilltops are high Mount Popa, a stratovolcano,Moore, Elizabeth H. (2007) ''Early landscapes of Myanmar'' River Books, Bangkok, page 44, Binhontaung ,topographic map, 1:250,00Thayetmyo, Burma, NE 46-4 Series U542, United States Army Map Service, October 1959 Kodittaung , Phoe-Oo Taung and Singguttara Hill (Theingottara Hill). Geology The Pegu Range consists of folded and faulted Paleogene marine sediments combined with more recent volcanics. History The Shwed ... [...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 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: �mjænmɑː, ˈbɜːmə So the pronunciation of the last syllable of Myanmar as ɑːror of Burma as ɜːrməby 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 ''ah'' () in "father". If the Burmese name my, မြန်မာ, label=none were spelled "Myanma" in English, this would be pronounced at the end by al ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Teak
Teak (''Tectona grandis'') is a tropical hardwood tree species in the family Lamiaceae. It is a large, deciduous tree that occurs in mixed hardwood forests. ''Tectona grandis'' has small, fragrant white flowers arranged in dense clusters ( panicles) at the end of the branches. These flowers contain both types of reproductive organs ( perfect flowers). The large, papery leaves of teak trees are often hairy on the lower surface. Teak wood has a leather-like smell when it is freshly milled and is particularly valued for its durability and water resistance. The wood is used for boat building, exterior construction, veneer, furniture, carving, turnings, and other small wood projects. ''Tectona grandis'' is native to south and southeast Asia, mainly Bangladesh, India, Indonesia, Malaysia, Myanmar, Thailand and Sri Lanka, but is naturalised and cultivated in many countries in Africa and the Caribbean. Myanmar's teak forests account for nearly half of the world's naturally occurring t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Communist Party Of Burma
The Communist Party of Burma (CPB), also known as the Burma Communist Party (BCP), is a clandestine communist party in Myanmar (Burma). It is the oldest existing political party in the country. Founded in 1939, the CPB initially fought against British colonial forces before joining them in a temporary alliance to expel the invading Imperial Japanese Army from Myanmar during World War II. In the final years of the war, the CPB helped establish a leftist political and military coalition called the Anti-Fascist People's Freedom League (AFPFL). However, the CPB fell out of favour with the more moderate socialists within the AFPFL due to differing views on how an independent Myanmar should be governed. The moderate faction of the AFPFL became the dominant political force in Myanmar's government following the country's independence in 1948. The CPB was subsequently expelled from the AFPFL and the government cracked down on the party's political activities, prompting the CPB's l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tharrawaddy, Burma
Tharrawaddy ( my, သာယာဝတီ) is a city in Bago Region of lower Myanmar. It is the administrative seat of Tharrawaddy District and Tharrawaddy Township. It locates on the main Yangon-Pyay road and 76 miles away at the north of Yangon Yangon ( my, ရန်ကုန်; ; ), formerly spelled as Rangoon, is the capital of the Yangon Region and the largest city of Myanmar (also known as Burma). Yangon served as the capital of Myanmar until 2006, when the military government .... History The current city was built when the region was under British rule, in the first British temporary seat at Thonze. However, Thonze is populated for district offices. Therefore, the city was moved two miles north of Thonze and the new district city was built in 1878. The name of the city called Tharrawaddy as the old Burmese name. Climate References Populated places in Tharrawaddy District {{Bago-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Rule In Burma
( Burmese) , conventional_long_name = Colony of Burma , common_name = Burma , era = Colonial era , event_start = First Anglo-Burmese War , year_start = 1824 , date_start = 5 March , event_end = Independence declared , year_end = 1948 , date_end = 4 January , life_span = 1824–1948 , event1 = Anglo-Burmese Wars , date_event1 = 1824–1826, 1852–1853, 1885 , event2 = Separation from British India , date_event2 = 1937 ( Government of Burma Act) , event3 = Japanese and Thai occupation , date_event3 = 1942–1945 , p1 = British Raj , flag_p1 = British_Raj_Red_Ensign.svg , p2 = Konbaung Dynasty , flag_p2 = Flag of Konbaung Dynasty (Nonrectangular).svg , p3 = State of Burma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saya San
Saya San also spelled Hsaya (original name Yar Kyaw, my, ဆရာစံ, ; 24 October 1876 – 28 November 1931) was a physician, former monk and the leader of the Saya San Rebellion of 1930-1932 in British Burma. The series of uprisings that have been called the Saya San Rebellion has been regarded as one of Southeast Asia's quintessential anti-colonial movements. Because of its national and historical nature, discussions about Saya San and the rebellion associated with him has persisted to this day, particularly within academic spheres. Saya San’s life Saya San was a native of Shwebo, a centre of nationalist-monarchist sentiment in north-central Burma that was the birthplace of the Konbaung (or Alaungpaya) dynasty, which controlled Myanmar from 1752 until the end of the Third Anglo-Burmese War in 1886. He was born on 24 October 1876. His original name was Yar Kyaw. His parents were U Kyaye and Daw Hpet, who lived with their five children in the rural agricultural vil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shwedagon Pagoda
The Shwedagon Pagoda (, ); mnw, ကျာ်ဒဂုၚ်; officially named ''Shwedagon Zedi Daw'' ( my, ရွှေတိဂုံစေတီတော်, , ) and also known as the Great Dagon Pagoda and the Golden Pagoda is a gilded stupa located in Yangon, Myanmar. The Shwedagon is the most sacred Buddhist pagoda in Myanmar, as it is believed to contain relics of the four previous Buddhas of the present kalpa. These relics include the staff of Kakusandha, the water filter of Koṇāgamana, a piece of the robe of Kassapa, and eight strands of hair from the head of Gautama. Built on the high Singuttara Hill, the tall pagoda stands above sea level,The pagoda's pinnacle height (to the tip of its ''hti'') is tall per (UNESCO 2018), and is built on the Singuttara Hill, which is tall per , and tall above sea level per and dominates the Yangon skyline. Yangon's zoning regulations, which cap the maximum height of buildings to above sea level (75% of the pagoda's sea l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marine Sediments
Marine sediment, or ocean sediment, or seafloor sediment, are deposits of insoluble particles that have accumulated on the seafloor. These particles have their origins in soil and rocks and have been transported from the land to the sea, mainly by rivers but also by dust carried by wind and by the flow of glaciers into the sea. Additional deposits come from marine organisms and chemical precipitation in seawater, as well as from underwater volcanoes and meteorite debris. Except within a few kilometres of a mid-ocean ridge, where the volcanic rock is still relatively young, most parts of the seafloor are covered in sediment. This material comes from several different sources and is highly variable in composition. Seafloor sediment can range in thickness from a few millimetres to several tens of kilometres. Near the surface seafloor sediment remains unconsolidated, but at depths of hundreds to thousands of metres the sediment becomes lithified (turned to rock). Rates of sediment ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Popa
Mount Popa (, ) is a dormant volcano 1518 metres (4981 feet) above sea level, and located in central Myanmar in the region of Mandalay about southeast of Bagan (Pagan) in the Pegu Range. It can be seen from the Ayeyarwady (Irrawaddy) River as far away as in clear weather. Mount Popa is a pilgrimage site, with numerous Nat temples and relic sites atop the mountain. Name The name ''Popa'' is believed to come from the Pali/Sanskrit word ''puppha'' meaning flower.Htin Aung, Maung "Folk Elements in Burmese Buddhism", Oxford University Press: London, 1962. Geology The main edifice of the volcano is composed of basalt and basaltic andesite lava flows, along with pyroclastic deposits and scoriaceous material, originating from strombolian eruptions which are thought to have made up the later stages of the volcano's growth. The volcano also contains a wide and deep caldera that is breached to the northwest and is thought to have formed due to failure of the volcano's slo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleogene
The Paleogene ( ; also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago ( Mya) to the beginning of the Neogene Period Mya. It is the beginning of the Cenozoic Era of the present Phanerozoic Eon. The earlier term Tertiary Period was used to define the span of time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognised as a formal stratigraphic term, 'Tertiary' is still widely found in earth science literature and remains in informal use. Paleogene is often abbreviated "Pg" (but the United States Geological Survey uses the abbreviation PE for the Paleogene on the Survey's geologic maps). During the Paleogene, mammals diversified from relatively small, simple forms into a large group of diverse animals in the wake of the Cretaceous–Paleogene extinction event that ended the preceding ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratovolcano
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volcano ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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