Myeik, Myanmar

Myeik (Burmese: မြိတ်မြို့; MLCTS: mrit mrui., pronounced: [mjeɪʔ mjo̰] or [beɪʔ mjo̰]; Mon: ဗိက်, [pòik]; Thai: มะริด, rtgs: Marit, pronounced [má(ʔ).rít]; formerly Mergui) is a city in Tanintharyi Region in Myanmar (Burma), located in the extreme south of the country on the coast of an island on the Andaman Sea. As of 2010 the estimated population was over 209,000. The area inland from the city is a major smuggling corridor into Thailand. The Singkhon Pass, also known as the Maw-daung Pass, has an international cross-border checkpoint.

History

Myeik was the southernmost part of the Pagan Kingdom between the 11th and 13th centuries. After the Pagan Empire's collapse in 1287, Myeik became part of successive Thai kingdoms from the late 13th century to the middle of 18th century: first the Sukhothai Kingdom and later the Ayutthaya Kingdom. A brief period of Bamar rule interrupted this between 1564-93.

From the 16th century on, the city was an important seaport and trading center with the Europeans, who would land at Myeik (then called Mergui), travel upriver to Tanintharyi (Tenasserim) and then cross the mountains to reach Ayutthaya. The French officer Chevalier de Beauregard was made Governor of the city of Myeik after the Siam-England war (1687) that resulted in the English being expelled from Siam. De Beauregard was named Governor by Narai, the king of the Ayutthaya Kingdom, replacing an Englishman, Samuel White. The French were then expelled from Myeik following the Siamese revolution of 1688.

Mergui Archipelago

The Mergui Archipelago (also Myeik Archipelago or Myeik Kyunzu; Burmese: မြိတ်ကျွန်းစု) is an archipelago in far southern Myanmar (Burma) and is part of the Tanintharyi Region. It consists of more than 800 islands, varying in size from very small to hundreds of square kilometres, all lying in the Andaman Sea off the western shore of the Malay Peninsula near its landward (northern) end where it joins the rest of Indochina. Occasionally the islands are referred to as the Pashu Islands because the Malay inhabitants are locally called Pashu. A five-star casino and golf resort, the Andaman Club now operates on Thahtay Kyun Island.

Environment

Geologically, the islands are characterized mainly by limestone and granite. They are generally covered with thick tropical growth, including rainforest, and their shorelines are punctuated by beaches, rocky headlands, and in some places, mangrove swamps. Offshore are extensive coral reefs.

The archipelago's virtual isolation from most of mankind's influence on the natural environment has given the islands and the surrounding waters of the Andaman Sea a great diversity of flora and fauna, contributing to the region's growing popularity as a diving destination, representing megafaunas such as whale sharks and even killer whales.

Andaman Sea

The Andaman Sea (Bengali: আন্দামান সাগর; Hindi: अंडमान सागर) is a body of water to the southeast of the Bay of Bengal, south of Myanmar (Burma), west of Thailand, north-west of Malay Peninsula, north of Sumatra and east of the Andaman Islands, India, from which it takes its name; it is part of the Indian Ocean.

The sea has been traditionally used for fishery and transportation of goods between the coastal countries and its coral reefs and islands are popular tourist destinations. The fishery and tourist infrastructure was severely damaged by the 2004 Indian Ocean earthquake and tsunami.

Extent

At its southeastern reaches, the Andaman Sea narrows to form the Straits of Malacca, which separate the Malay Peninsula from the island of Sumatra.

The International Hydrographic Organization defines the limits of the "Andaman or Burma Sea" as follows:

On the Northwest. The Eastern limit of the Bay of Bengal [A line running from Cape Negrais (16°03'N) in Burma [Myanmar] through the larger islands of the Andaman group, in such a way that all the narrow waters between the islands lie to the Eastward of the line and are excluded from the Bay of Bengal, as far as a point in Little Andaman Island in latitude 10°48'N, longitude 92°24'E].

Similan Islands

The Similan Islands (Thai: หมู่เกาะสิมิลัน, Thai pronunciation: [mùː kɔ̀ʔ si.mi.lan], Malay: Pulau Sembilan سمبيلن ڤولاو) is a group of islands in the Andaman Sea off the coast of, and part of, Phang Nga Province, southern Thailand. It is a national park which was established in 1982.

Similan Islands National Park was established after a one-year exploration by the forestry department. The park is an archipelago consisting of nine islands named Ko Tachai, Ko Bon, Ko Bangu, Ko Similan, Ko Payu, Ko Hok, Ko Ha, Ko Miang, Ko Payan, Ko Payang, and Ko Huyong. Recently, the park was expanded to include two remote islands named Ko Bon and Ko Tachai. The Similans are situated 70 kilometres from Phang Nga town. "Similan" is a Yawi word which means "nine". Bon and Tachai islands were added to the national park in 1998.

The islands are at 8°39′09″N 97°38′27″E / 8.65250°N 97.64083°E / 8.65250; 97.64083

Attractions

Ko Similan

Ko Similan is the largest island. There are a total of 11 islands. The sea in the area has an average depth of 60 feet. Underwater it is full of rock formations and coral reefs in several shapes and forms, resembling such things as deer, leaves, brains, and mushrooms.

Archipelago

An archipelago (ⁱ/ɑːrkᵻˈpɛləɡoʊ/ ark-i-PEL-ə-goh), sometimes called an island group or island chain, is a chain, cluster or collection of islands. The word archipelago is derived from the Greek ἄρχι- – arkhi- ("chief") and πέλαγος – pélagos ("sea") through the Italian arcipelago. In Italian, possibly following a tradition of antiquity, the Arcipelago (from medieval Greek *ἀρχιπέλαγος and Latin archipelagus) was the proper name for the Aegean Sea and, later, usage shifted to refer to the Aegean Islands (since the sea is remarkable for its large number of islands). It is now used to refer to any island group or, sometimes, to a sea containing a small number of scattered islands.

Types

Archipelagos may be found isolated in bodies of water or neighboring a large land mass. For example, Scotland has more than 700 islands surrounding its mainland which constitute an archipelago. Archipelagos are often volcanic, forming along island arcs generated by subduction zones or hotspots, but may also be the result of erosion, deposition, and land elevation. Depending on their geological origin, islands forming archipelagos can be referred to as oceanic islands, continental fragments, and continental islands. Oceanic islands are mainly of volcanic origin. Continental fragments correspond to land masses that have separated from a continental mass due to tectonic displacement. Finally, sets of islands formed close to the coast of a continent are considered continental archipelagos when they form part of the same continental shelf so islands are just exposed continental shelf.