Singkhon Pass
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Singkhon Pass
Singkhon Pass ( th, ด่านสิงขร), also referred to as Sing Khon and as Maw Daung after the name of the Burmese town west of the border, is a pass across the Tenasserim Hills on the border between Thailand and Myanmar, at an elevation of . The pass is close to the narrowest point of Thailand in Khlong Wan (คลองวาฬ) subdistrict, Mueang Prachuap Khiri Khan District, Prachuap Khiri Khan Province. History Singkhon pass was important during the wars between Siam and the Burmese, and also during World War II, when the Mergui Road was constructed by the Japanese invaders. The pass, on Thai Hwy 1039, about to the west of its junction with Thailand Route 41, was formerly closed, but was informally opened since May 2013 as a result of bilateral agreements. The road on the Burmese side leads to Myeik – via Mawdaung and Tanintharyi Tanintharyi or Taninthayi (widely known during the British occupation and since as Tenasserim) is a small town in Tani ...
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Border Checkpoint
A border checkpoint is a location on an international border where travelers or goods are inspected and allowed (or denied) passage through. Authorization often is required to enter a country through its borders. Access-controlled borders often have a limited number of checkpoints where they can be crossed without legal sanctions. Arrangements or treaties may be formed to allow or mandate less restrained crossings (e.g. the Schengen Agreement). Land border checkpoints (land ports of entry) can be contrasted with the customs and immigration facilities at seaports, international airports, and other ports of entry. Checkpoints generally serve two purposes: * To prevent entrance of individuals who are either undesirable (e.g. criminals or others who pose threats) or simply unauthorized to enter. * To prevent entrance of goods that are illegal or subject to restriction, or to collect tariffs. Checkpoints are usually staffed by a uniformed service (sometimes referred to as customs ...
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Mergui Road
Mergui Road was a transit route in the area of the Singkhon Pass between Burma and Thailand, built and used during World War II by Imperial Japan. The road connected Prachuap Khiri Khan to Mergui via Tenasserim on the Burmese south coast. It was hastily constructed under supervision of the Japanese army as a means of retreat in 1945, as British and American forces advanced and rail lines were severed by bombing. Mergui Road was built by romusha Asian laborers and some Allied prisoners of war under brutal slave labor conditions. See also *Burma Railway The Burma Railway, also known as the Siam–Burma Railway, Thai–Burma Railway and similar names, or as the Death Railway, is a railway between Ban Pong, Thailand and Thanbyuzayat, Burma (now called Myanmar). It was built from 1940 to 1943 ... * Kra Isthmus Railway References External links Mergui RoadThe Forgotten Mergui Road World War II sites in Burma {{Myanmar-hist-stub ...
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Mountain Passes Of Myanmar
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable ...
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Mountain Passes Of Thailand
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable ...
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