Moksobo
Shwebo ( my, ရွှေဘိုမြို့ ) is a city in Sagaing Region, Burma, 110 km north-west of Mandalay between the Irrawaddy and the Mu rivers. The city was the origin of the Konbaung Dynasty, established by King Alaungpaya in 1752, that was the dominant political force in Burma after the mid-18th century. It served as Alaungpaya's capital from 1752 to 1760. As of 2021, it has a population of 88,914. History Up to 1752, Shwebo was a village, called Moksobo ( my, မုဆိုးဘို ; ) of about 300 houses. It lies near the site of the ancient Pyu city-state of Hanlin. On 29 February 1752, the chief of the village Aung Zeya founded the Konbaung Dynasty to resist the upcoming invasion of Lower Burma-based Hanthawaddy forces. Aung Zeya, who also assumed the royal title of Alaungpaya, gained the allegiance of 46 surrounding villages, and organized defenses building a stockade and digging a moat around Moksobo. He renamed his village, Shwebo (). Over th ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Alaungpaya
Alaungpaya ( my, အလောင်းဘုရား, ; also spelled Alaunghpaya or Alaung-Phra; 11 May 1760) was the founder of the Konbaung Dynasty of Burma (Myanmar). By the time of his death from illness during his campaign in Siam, this former chief of a small village in Upper Burma had unified Burma, subdued Manipur, conquered Lan Na and defeated the French and the British who had given help to the Restored Hanthawaddy Kingdom. He added settlements around Dagon, and called the enlarged town Yangon.Letwe Nawrahta and Maha Sithu of Twinthin 1961: 190–191 He is considered one of the three greatest monarchs of Burma alongside Anawrahta and Bayinnaung for unifying Burma for the third time in Burmese history. Background The future king was born Aung Zeya ( "Victorious Victory") at Moksobo, a village of a few hundred households in the Mu River Valley about northwest of Ava (Inwa) on 24 August 1714 to Min Nyo San () and his wife Saw Nyein Oo (). He was the second ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Naungdawgyi
Dabayin Min ( my, ဒီပဲယင်းမင်း), commonly known as Naungdawgyi ( my, နောင်တော်ကြီး ; 10 August 1734 – 28 November 1763) was the second king of Konbaung Dynasty of Burma (Myanmar), from 1760 to 1763. He was a top military commander in his father Alaungpaya's reunification campaigns of the country. As king, he spent much of his short reign suppressing multiple rebellions across the newly founded kingdom from Ava (Inwa) and Toungoo (Taungoo) to Martaban (Mottama) and Chiang Mai. The king suddenly died less than a year after he had successfully suppressed the rebellions. He was succeeded by his younger brother Hsinbyushin. Early life Naungdawgyi was born Maung Lauk () to Yun San and Aung Zeya (later King Alaungpaya) on 10 August 1736 (Tuesday, 11th waxing of Wagaung 1096 ME) in a small village of Moksobo, about 60 miles northwest of Ava (Inwa).Maung Maung Tin Vol. 1 1905: 263 He was the eldest child of the couple's nine children. ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Konbaung Dynasty
The Konbaung dynasty ( my, ကုန်းဘောင်ခေတ်, ), also known as Third Burmese Empire (တတိယမြန်မာနိုင်ငံတော်) and formerly known as the Alompra dynasty (အလောင်းဘုရားမင်းဆက်, Alaungphra dynasty) and the Hunter dynasty (မုဆိုးမင်းဆက် Mokso dynasty / မုဆိုးဘိုမင်းဆက် Moksobo dynasty), was the last dynasty that ruled Burma/Myanmar from 1752 to 1885. It created the second-largest empire in Burmese history and continued the administrative reforms begun by the Toungoo dynasty, laying the foundations of the modern state of Burma. The reforms, however, proved insufficient to stem the advance of the British, who defeated the Burmese in all three Anglo-Burmese Wars over a six-decade span (1824–1885) and ended the millennium-old Burmese monarchy in 1885. An expansionist dynasty, the Konbaung kings waged campaigns against Mani ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Restored Hanthawaddy Kingdom
The Restored Hanthawaddy Kingdom ( my, ဟံသာဝတီ နေပြည်တော်သစ်), also known as the Neo-Ramanic State () was the kingdom that ruled Lower Burma and parts of Upper Burma from 1740 to 1757. The kingdom grew out of a rebellion by the Mon led population of Pegu, who then rallied the other Mon as well as Delta Bama and Karens of Lower Burma, against the Toungoo Dynasty of Ava in Upper Burma. The rebellion succeeded in expelling Toungoo loyalists and restored the Mon-speaking Kingdom of Hanthawaddy ruled Lower Burma from 1287 to 1539. The restored Hanthawady kingdom also claim heritage to Bayinaung's early Toungoo Empire whose capital was based in Pegu and guaranteed the loyalty of the non-Mon population of Lower Burma. Supported by the French, the upstart kingdom quickly carved out a space for itself in Lower Burma, and continued its push northward. In March 1752, its forces captured Ava, and ended the 266-year-old Toungoo dynasty. A new dynas ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Lower Burma
Lower Myanmar ( my, အောက်မြန်မာပြည်, also called Lower Burma) is a geographic region of Myanmar and includes the low-lying Irrawaddy Delta ( Ayeyarwady, Bago and Yangon Regions), as well as coastal regions of the country ( Rakhine and Mon States and Tanintharyi Region). In the Burmese language, people originating from Upper Myanmar are typically called ''a-nya-tha'' for men and ''a-nya-thu'' for women, whereas those from Lower Myanmar are called ''auk tha'' () for men and ''auk thu'' for women. Historically, Lower Myanmar referred to the part of Myanmar annexed by the British Empire after the end of the Second Anglo-Burmese War in 1852, plus the former kingdom of Arakan and the territory of Tenasserim which the British had taken control of in 1826 through the Treaty of Yandabo. Lower Myanmar was centred at Rangoon, and composed of all of the coast of modern Myanmar, and also the lower basin of the Irrawaddy River, including Prome. Until the early 1 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' i ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Tropical Savanna Climate
Tropical savanna climate or tropical wet and dry climate is a tropical climate sub-type that corresponds to the Köppen climate classification categories ''Aw'' (for a dry winter) and ''As'' (for a dry summer). The driest month has less than of precipitation and also less than 100-\left (\frac \right)mm of precipitation. This latter fact is in a direct contrast to a tropical monsoon climate, whose driest month sees less than of precipitation but has ''more'' than 100-\left (\frac \right) of precipitation. In essence, a tropical savanna climate tends to either see less overall rainfall than a tropical monsoon climate or have more pronounced dry season(s). In tropical savanna climates, the dry season can become severe, and often drought conditions prevail during the course of the year. Tropical savanna climates often feature tree-studded grasslands due to its dryness, rather than thick jungle. It is this widespread occurrence of tall, coarse grass (called savanna) which has led ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Arakan Mountains
The Arakan Mountains ( my, ရခိုင်ရိုးမ), also known as the Rakhine Yoma, are a mountain range in western Myanmar, between the coast of Rakhine State and the Central Myanmar Basin, in which flows the Irrawaddy River. It is the most prominent of a series of parallel ridges that arc through Assam, Nagaland, Manipur, Mizoram and Myanmar. The Arakan Mountains run from Cape Negrais in the south in to Manipur, India in the north. They include the Naga Hills, the Chin Hills, and the Patkai range which includes the Lushai Hills. The mountain chain is submerged in the Bay of Bengal for a long stretch and emerges again in the form of the Andaman and Nicobar Islands. Etymology The word ''Arakan'' is derived from the Sanskrit word ''Rakshasa'' (राक्षस), a term used to refer to the inhabitants of the region. Geology and formation The Arakan Mountains and the parallel arcs to the west and east were formed by compression as the Indian Plate collided with t ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Rain Shadow
A rain shadow is an area of significantly reduced rainfall behind a mountainous region, on the side facing away from prevailing winds, known as its leeward side. Evaporated moisture from water bodies (such as oceans and large lakes) is carried by the prevailing onshore breezes towards the drier and hotter inland areas. When encountering elevated landforms, the moist air is driven upslope towards the peak, where it expands, cools, and its moisture condenses and starts to precipitate. If the landforms are tall and wide enough, most of the humidity will be lost to precipitation over the windward side (also known as the ''rainward'' side) before ever making it past the top. As the air descends the leeward side of the landforms, it is compressed and heated, producing foehn winds that ''absorb'' moisture downslope and cast a broad "shadow" of dry climate region behind the mountain crests. This climate typically takes the form of shrub–steppe, xeric shrublands or even d ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Pagan Min
Pagan Min ( my, ပုဂံမင်း, ; 21 June 1811 – 14 March 1880), was the ninth king of the Konbaung dynasty of Burma. Born Maung Biddhu Khyit, he was granted the title of Prince of Pagan by his father Tharrawaddy in August 1842. Pagan Min became king when Tharrawaddy died on 17 November 1846, with the formal title of His Majesty "Sri Pawara Vijaya Nanda Jatha Maha Dharma Rajadhiraja Pagan Min Taya-gyi". Pagan Min won the power struggle to succeed his father by having his rival brothers killed. His chief ministers Maung Baing Zat and Maung Bhein enriched themselves by executing rich subjects. The Second Anglo-Burmese War broke out during the reign of Pagan Min. In 1851 the governor of Pegu, Maung Ok, charged the captains of two British merchant ships with murder, embezzlement, and evasion of custom duties. He fined them 500 rupees, and required their debts be paid before being authorized to return to Kolkata. After receiving their complaints, Lord Dalhousie, the gov ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mindon Min
Mindon Min ( my, မင်းတုန်းမင်း, ; 1808 – 1878), born Maung Lwin, was the penultimate King of Burma (Myanmar) from 1853 to 1878. He was one of the most popular and revered kings of Burma. Under his half brother King Pagan, the Second Anglo-Burmese War in 1852 ended with the annexation of Lower Burma by the British Empire. Mindon and his younger brother Kanaung overthrew their half brother King Pagan. He spent most of his reign trying to defend the upper part of his country from British encroachments, and to modernize his kingdom. Early life Mindon was born ''Maung Lwin'' in 1808, a son of Tharrawaddy Min and Chandra Mata Mahay, Queen of the south Royal Chamber. He studied at the Maha Zawtika monastic college in Amarapura until the age of 23, and he held deep respect for religion and religious scholarship throughout his entire life. Mindon grew up in the shadow of British control – by 1853, the year of his coronation, Burma had gone through radical ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Crown Prince
A crown prince or hereditary prince is the heir apparent to the throne in a royal or imperial monarchy. The female form of the title is crown princess, which may refer either to an heiress apparent or, especially in earlier times, to the wife of the person styled crown prince. ''Crown prince'' as a descriptive term has been used throughout history for the prince who is first-in-line to a throne and is expected to succeed (i.e. the heir apparent), barring any unforeseen future event preventing this. In certain monarchies, a more specific substantive title may be accorded and become associated with the position of ''heir apparent'' (e.g. Prince of Wales in the United Kingdom or Prince of Asturias in the Spain, Kingdom of Spain). In these monarchies, the term crown prince may be used less often than the substantive title (or never). Until the late twentieth century, no modern monarchy adopted a system whereby females would be guaranteed to succeed to the throne (i.e. absolute pr ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |