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Flora Of Myanmar
The wildlife of Myanmar includes its flora and fauna and their natural habitats. Flora Like all Southeastern Asian forests, the forests of Myanmar can be divided into two categories: monsoon forest and rainforest. Monsoon forest is dry at least three months a year, and is dominated by deciduous trees. Rainforest has a rainy season of at least nine months, and are dominated by broadleaf evergreen. In the region north of the Tropic of Cancer, in the Himalayan region, subtropical broadleaf evergreen dominates to an elevation of 2000 m, and from 2000 m to 3000 m, semi-deciduous broadleaf dominates, and above 3000 m, evergreen conifers and subalpine forest are the primary fauna until the alpine scrubland. The area from Yangon to Myitkyina is mostly monsoon forest, while peninsular Malaysia south of Mawlamyine is primarily rainforest, with some overlap between the two. Along the coasts of Rakhine State and Tanintharyi Division, tidal forests occur in ...
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Alpine Climate
Alpine climate is the typical climate for elevations above the tree line, where trees fail to grow due to cold. This climate is also referred to as a mountain climate or highland climate. Definition There are multiple definitions of alpine climate. In the Köppen climate classification, the alpine and mountain climates are part of group ''E'', along with the polar climate, where no month has a mean temperature higher than . According to the Holdridge life zone system, there are two mountain climates which prevent tree growth : a) the alpine climate, which occurs when the mean biotemperature of a location is between . The alpine climate in Holdridge system is roughly equivalent to the warmest tundra climates (ET) in the Köppen system. b) the alvar climate, the coldest mountain climate since the biotemperature is between 0 °C and 1.5 °C (biotemperature can never be below 0 °C). It corresponds more or less to the coldest tundra climates and to the ice cap cli ...
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Myanmar Coast Mangroves
The Burmese or Myanmar Coast mangroves are an ecoregion in Burma, Malaysia, Thailand and Bangladesh where there were once thick forests of mangroves but today most has been cleared, resulting in loss of habitat for wildlife. Location and description Mangroves were once common in the Irrawaddy River Irrawaddy Delta, Delta and today exist in three distinct areas, Rakhine State, Ayeyarwady Region, Ayeyarwady and Tanintharyi Regions, as well as Kutubdia and Moheshkhali islands in Bangladesh Flora The mangrove flora of Burma include ''Rhizophora'' and ''Xylocarpus'' mangrove trees, ''Sonneratias'', other Rhizophoraceae, ''Nypa fruticans'' and ''Phoenix paludosa''. Fauna The remaining mammals include a small group of wild Asian elephants in Rakhine State, while once common species of mammals and reptiles such as the tiger, the saltwater crocodile (''Crocodylus porosus'') and the mangrove terrapin (''Batagur baska'') have either disappeared or seriously reduced in number Bird life how ...
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Low Island
A coral island is a type of island formed from coral detritus and associated organic material. It occurs in tropical and sub-tropical areas, typically as part of a coral reef which has grown to cover a far larger area under the sea. The term low island can be used to distinguish such islands from high islands, which are formed through volcanic action. Low islands are formed as a result of sedimentation upon a coral reef or of the uplifting of such islands. Ecosystem Coral reefs are some of the oldest ecosystems on the planet, over geological time, they form massive reefs of limestone. The reef environment supports more plant and animal species than any other habitat. Coral reefs are vital for life in multiple aspects some of which include structure, ecology, and nutrient cycles which all support biodiversity in the reefs. Coral reefs build massive calcareous skeletons that serve as homes for animals such as fish hiding inside the crooks and crannies of the reef and barnacles ...
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Tidal Creek
A tidal creek or tidal channel is a narrow inlet or estuary that is affected by the ebb and flow of ocean tides. Thus, it has variable salinity and electrical conductivity over the tidal cycle, and flushes salts from inland soils. Tidal creeks are characterized by slow water velocity, resulting in buildup of fine, organic sediment in wetlands. Creeks may often be a dry to muddy channel with little or no flow at low tide, but with significant depth of water at high tide. Due to the temporal variability of water quality parameters within the tidally influenced zone, there are unique biota associated with tidal creeks which are often specialised to such zones. Nutrients and organic matter are delivered downstream to habitats normally lacking these, while the creeks also provide access to inland habitat for salt-water organisms. Terminology A "creek" normally refers to a tidal water channel in British English and in other parts of the Anglosphere. This is the case in many countries ...
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Lagoon
A lagoon is a shallow body of water separated from a larger body of water by a narrow landform, such as reefs, barrier islands, barrier peninsulas, or isthmuses. Lagoons are commonly divided into ''coastal lagoons'' (or ''barrier lagoons'') and ''atoll lagoons''. They have also been identified as occurring on mixed-sand and gravel coastlines. There is an overlap between bodies of water classified as coastal lagoons and bodies of water classified as Estuary, estuaries. Lagoons are common coastal features around many parts of the world. Definition and terminology Lagoons are shallow, often elongated bodies of water separated from a larger body of water by a shallow or exposed shoal, reef, coral reef, or similar feature. Some authorities include fresh water bodies in the definition of "lagoon", while others explicitly restrict "lagoon" to bodies of water with some degree of salinity. The distinction between "lagoon" and "estuary" also varies between authorities. Richard A. Davis J ...
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Estuary
An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime environments and are an example of an ecotone. Estuaries are subject both to marine influences such as tides, waves, and the influx of saline water, and to fluvial influences such as flows of freshwater and sediment. The mixing of seawater and freshwater provides high levels of nutrients both in the water column and in sediment, making estuaries among the most productive natural habitats in the world. Most existing estuaries formed during the Holocene epoch with the flooding of river-eroded or glacially scoured valleys when the sea level began to rise about 10,000–12,000 years ago. Estuaries are typically classified according to their geomorphological features or to water-circulation patterns. They can have many different names, such as ba ...
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Tidal Forests
Tidal is the adjectival form of tide. Tidal may also refer to: * ''Tidal'' (album), a 1996 album by Fiona Apple * Tidal (king), a king involved in the Battle of the Vale of Siddim * TidalCycles, a live coding environment for music * Tidal (service), a music streaming service * '' Tidal: Occupy Theory, Occupy Strategy'', a magazine associated with the Occupy Wall Street movement See also * Tidal flow (traffic), the flow of traffic thought of as an analogy with the flow of tides * Tidal force, a secondary effect of the force of gravity and is responsible for the tides * Tidal power, energy harnessed by converting energy from tides * Tide (other) A tide is the rise and fall of a sea level caused by the Moon's gravity and other factors. Tide(s) may also refer to: Media * The Tide (Nigeria), ''The Tide'' (Nigeria), a newspaper *Tide (TV series), ''Tide'' (TV series), 2019 Irish/Welsh/Scott ...
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Tanintharyi Division
Tanintharyi Region (, ; Mon: or ; formerly Tenasserim Division and Tanintharyi Division) is a region of Myanmar, covering the long narrow southern part of the country on the northern Malay Peninsula, reaching to the Kra Isthmus. It borders the Andaman Sea to the west and the Tenasserim Hills, beyond which lie Thailand, to the east. To the north is the Mon State. There are many islands off the coast, the large Mergui Archipelago in the southern and central coastal areas and the smaller Moscos Islands off the northern shores. The capital of the division is Dawei (Tavoy). Other important cities include Myeik (Mergui) and Kawthaung. The division covers an area of , and had a population of 1,406,434 at the 2014 Census. Names Tanintharyi has historically been known by a number of names, reflecting changes in administrative control throughout history, as the region changed hands from the Kedah Sultanate, to the Hanthawaddy, Ayutthaya and Konbaung kingdoms, and British Burma. The ...
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Rakhine State
Rakhine State ( ; , ; ), formerly known as Arakan State, is a Administrative divisions of Myanmar, state in Myanmar (Burma). Situated on the western coast, it is bordered by Chin State to the north, Magway Region, Bago Region and Ayeyarwady Region to the east, the Bay of Bengal to the west and the Chittagong Division, Chattogram Division of Bangladesh to the northwest. It is located approximately between latitudes 17°30' north and 21°30' north and longitudes 92°10' east and 94°50' east. The north–south Arakan Mountains or Rakhine Yoma separate Rakhine State from central Myanmar. Off the coast of Rakhine State there are some fairly large islands such as Ramree Island, Ramree, Cheduba and Myingun Island, Myingun. Rakhine State has an area of and its capital is Sittwe (formerly known as Akyab). Names The state was historically known as Arakan in English until the Burmese government adopted the English name Rakhine in 1989. History The history of the region of Arakan ...
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Mawlamyine
Mawlamyine (also spelled Mawlamyaing; , ; ; , ), formerly Moulmein, is the fourth-largest city in Myanmar (Burma), ''World Gazetteer'' southeast of Yangon and south of Thaton, at the mouth of Thanlwin (Salween) River. Mawlamyine was an ancient city and the first List of capitals of Myanmar, capital of British Burma. The city is currently the capital and largest city of Mon State and the main trading (commerce), trading centre and seaport in southeastern Myanmar. Etymology and legend The Mon language, Mon name which was previously used for Mawlamyine, ''Moulmein'' (; ) means "damaged eye" or "one-eyed man." According to legend, a Mon people, Mon king had a powerful third eye in the centre of his forehead, able to see what was happening in neighbouring kingdoms. The daughter of one of the neighbouring kings was given in marriage to the three-eyed king and managed to destroy the third eye. The Burmese name "Mawlamyine" is believed to be a corruption of the Mon name. Moulmein was ...
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Myitkyina
Myitkyina (, ; Jingpho language, Jinghpaw: ''Myitkyina'', ; , ''Sèna'') is the capital city of Kachin State in Myanmar (Burma), located from Yangon, and from Mandalay. In Burmese language, Burmese it means "near the big river", and Myitkyina is on the west bank of the Ayeyarwady River, just downstream from Myit-son (Burmese for confluence) of its two headstreams (the Mali River, Mali and N'Mai River, N'mai rivers). It is the northernmost river port and railway terminus in Myanmar. The city is served by Myitkyina Airport. History Myitkyina has been an important trading town between China and Myanmar since ancient times. American Baptist missionary George J. Geis and his wife arrived in Myitkyina in the late 1890s and in 1900 they requested permission to build a mansion in the town. The building was named Geis Memorial Church. It is one of the Kachin Baptist Convention (KBC) churches in Myitkyina. Japanese forces captured the town and nearby airbase during World War II in 1942 ...
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