|
Sittaung River
The Sittaung River ( ; formerly, the Sittang or Sittoung) is a river in south central Myanmar in Bago Division. The Pegu Range separates its basin from that of the Irrawaddy. The river originates at the edge of the Shan Hills southeast of Mandalay, and flows southward to the Gulf of Martaban. Its length is and its mean annual discharge is around per year. Basin Although it flows through fairly flat country, the Sittaung has a notorious tidal bore at its mouth which has precluded any but very small craft navigating the river. The river is navigable for year-round and for during three months of the year. The Sittaung empties into the Gulf of Martaban where the tide-dominated coast is a Ramsar wetland of international importance. The river is used primarily to float timber south for export. Strong currents make the river even less valuable as a means of transport in eastern Burma. Its basin does not have the same richness for agriculture Agriculture encompasse ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Pyinmana
Pyinmana (, ; population: 100,000 (2006 estimate)) is a logging town and sugarcane refinery center in the Naypyidaw Union Territory of Myanmar. The administrative capital of Myanmar was officially moved to a militarized greenfield site (which the leader, Than Shwe, dubbed Naypyidaw, or Royal City) two miles (3.2 km) west of Pyinmana on November 6, 2005. As of 2014, the city has an urban population of 72,010. During World War II, Pyinmana was the base of the Burma Independence Army (later renamed and reorganized into the Burma Defence Army by the Japanese). Climate Pyinmana has a 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 ... with a dry winter (Köppen-Geiger climate type ''Aw''). This means that it has a clear wet season and a clear dry season. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
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] [Amazon] |
Gulf Of Mottama
The Gulf of Martaban () or the Gulf of Mottama is an arm of the Andaman Sea in the southern part of Myanmar (Burma). The gulf is named after the port city of Mottama (formerly known as Martaban). The Sittaung, Salween and Yangon rivers empty into it. A characteristic feature of the Gulf of Martaban is that it has a tide-dominated coastline. Tides ranges between 4–7 m with the highest tidal range at the Elephant Point in the western Gulf of Martaban. During spring tide, when the tidal range is around 6.6 m, the turbid zone covers an area of more than 45,000 km2 making it one of the largest perennially turbid zones of the world's oceans. During neap tide, with tidal range of 2.98 m, the highly turbid zone coverage drops to 15,000 km2. The edge of the highly turbid zone migrates back-and-forth in-sync with every tidal cycle by nearly 150 km. The gulf is home to varieties of species and the Eden's whale was scientifically recognized in the wate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Andaman Sea
The Andaman Sea (historically also known as the Burma Sea) is a marginal sea of the northeastern Indian Ocean bounded by the coastlines of Myanmar and Thailand along the Gulf of Martaban and the west side of the Malay Peninsula, and separated from the Bay of Bengal to its west by the Andaman Islands and the Nicobar Islands. Its southern end is at Breueh Island just north of Sumatra, with the Strait of Malacca further southeast. Traditionally, the sea has been used for fishery and transportation of goods between the coastal countries and its coral reefs and islands, which are popular tourist destinations. The fishery and tourist infrastructure was severely damaged by the December 2004 Indian Ocean earthquake and tsunami. Geography Location The Andaman Sea, which extends over 92°E to 100°E and 4°N to 20°N, occupies a very significant position in the Indian Ocean, yet remained unexplored for a long period. To the south of Myanmar, west of Thailand, and north of Indonesia, t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Bago Region
Bago Region (, ; formerly Pegu Division and Bago Division) is an administrative divisions of Myanmar, administrative region of Myanmar, located in the southern central part of the country. It is bordered by Magway Region and Mandalay Region to the north; Kayin State, Mon State and the Gulf of Martaban to the east; Yangon Region to the south and Ayeyarwady Region and Rakhine State to the west. It is located between 46°45'N and 19°20'N and 94°35'E and 97°10'E. It has a population of 4,867,373 (2014). History According to legend, two Mon people, Mon princes from Thaton founded the city of Bago in 573 AD. They saw a female Hamsa (bird), Hamsa standing on the back of a male Hamsa on an island in a huge lake. Believing this was an auspicious omen, the princes built a city called Hanthawady (Pāli, Pali: ) on the edge of the lake. The Persian Empire, Persian geographer Ibn Khordadbeh mentions the city around 850 AD. The Mon capital was still in Thaton at that time. The Thiruvalang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
River
A river is a natural stream of fresh water that flows on land or inside Subterranean river, caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by the water cycle, the processes by which water moves around the Earth. Water first enters rivers through precipitation, whether from rainfall, the Runoff (hydrology), runoff of water down a slope, the melting of glaciers or snow, or seepage from aquifers beneath the surface of the Earth. Rivers flow in channeled watercourses and merge in confluences to form drainage basins, or catchments, areas where surface water eventually flows to a common outlet. Rivers have a great effect on the landscape around them. They may regularly overflow their Bank (geography), banks and flood the surrounding area, spreading nutrients to the surrounding area. Sedime ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Bago Division
Bago Region (, ; formerly Pegu Division and Bago Division) is an administrative region of Myanmar, located in the southern central part of the country. It is bordered by Magway Region and Mandalay Region to the north; Kayin State, Mon State and the Gulf of Martaban to the east; Yangon Region to the south and Ayeyarwady Region and Rakhine State to the west. It is located between 46°45'N and 19°20'N and 94°35'E and 97°10'E. It has a population of 4,867,373 (2014). History According to legend, two Mon princes from Thaton founded the city of Bago in 573 AD. They saw a female Hamsa standing on the back of a male Hamsa on an island in a huge lake. Believing this was an auspicious omen, the princes built a city called Hanthawady (Pali: ) on the edge of the lake. The Persian geographer Ibn Khordadbeh mentions the city around 850 AD. The Mon capital was still in Thaton at that time. The Thiruvalangadu plate describe Rajendra Chola I, the Chola Emperor from South India, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Pegu Range
The Pegu Range (; 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, Sinnamaung Taung 2,693 feet (820 m), Shwenape Taung 2,631feet (802 m), TALAN Taung 2,050 feet (625 m), 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 ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Irrawaddy River
The Irrawaddy River (, , Ayeyarwady) is the principal river of Myanmar, running through the centre of the country. Myanmar’s most important commercial waterway, it is about 1,350 miles (2,170 km) long. Originating from the confluence of the N'Mai River, N'mai and Mali River, Mali rivers, it flows from north to south before emptying through the Irrawaddy Delta in the Ayeyarwady Region into the Andaman Sea. Its drainage basin of about covers 61% of the land area of Burma, and contains five of its largest cities. As early as the sixth century, the river was used for trade and transport, and an extensive network of irrigation, irrigation canals was developed to support agriculture. The river is still of great importance as the largest commercial waterway of Myanmar. It also provides important Ecosystem service, ecosystem services to different communities and economic sectors, including agriculture, fisheries, and tourism. In 2007, State Peace and Development Council, Myanmar's ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Mandalay
Mandalay is the second-largest city in Myanmar, after Yangon. It is located on the east bank of the Irrawaddy River, 631 km (392 mi) north of Yangon. In 2014, the city had a population of 1,225,553. Mandalay was founded in 1857 by King Mindon Min, Mindon, replacing Amarapura as the new royal capital of the Konbaung dynasty. It was Burma's final royal capital before the kingdom's Third Anglo-Burmese War, annexation by the British Empire in 1885. Under British rule, Mandalay remained commercially and culturally important despite the rise of Yangon, the new capital of British Burma. The city suffered extensive destruction during the Japanese conquest of Burma in the World War II, Second World War. In 1948, Mandalay became part of the newly independent Union of Burma. Today, Mandalay is the economic centre of Upper Myanmar and considered the centre of Burmese culture. A continuing influx of irregular Overseas Chinese, Chinese immigrants, mostly from Yunnan, since the late ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Gulf Of Martaban
The Gulf of Martaban () or the Gulf of Mottama is an arm of the Andaman Sea in the southern part of Myanmar (Burma). The gulf is named after the port city of Mottama (formerly known as Martaban). The Sittaung, Salween and Yangon rivers empty into it. A characteristic feature of the Gulf of Martaban is that it has a tide-dominated coastline. Tides ranges between 4–7 m with the highest tidal range at the Elephant Point in the western Gulf of Martaban. During spring tide, when the tidal range is around 6.6 m, the turbid zone covers an area of more than 45,000 km2 making it one of the largest perennially turbid zones of the world's oceans. During neap tide, with tidal range of 2.98 m, the highly turbid zone coverage drops to 15,000 km2. The edge of the highly turbid zone migrates back-and-forth in-sync with every tidal cycle by nearly 150 km. The gulf is home to varieties of species and the Eden's whale was scientifically recognized in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Tidal Bore
A tidal bore, often simply given as bore in context, is a tidal phenomenon in which the leading edge of the incoming tide forms a wave (or waves) of water that travels up a river or narrow bay, reversing the direction of the river or bay's current. It is a strong tide that pushes up the river, against the current. Description Bores occur in relatively few locations worldwide, usually in areas with a large tidal range (typically more than between high and low tide) and where incoming tides are funneled into a shallow, narrowing river or lake via a broad bay. The funnel-like shape not only increases the tidal range, but it can also decrease the duration of the flood tide, down to a point where the flood appears as a sudden increase in the water level. A tidal bore takes place during the flood tide and never during the ebb tide. A tidal bore may take on various forms, ranging from a single breaking wavefront with a somewhat like a hydraulic jumpto undular bores, compr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
