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Ko Samet is part of the Phe (Thai: เพ) Subdistrict of the Amphoe Mueang Rayong (Thai: เมืองระยอง, the capital district, or Amphoe Mueang), of Rayong Province. Ko Samet is the largest and westernmost of a cluster of islands not far from the coast. Ko Samet measures 6.8 kilometres (4.2 mi) from north to south.
The sunset at Khao Laem Ya–Mu Ko Samet National Park. Although the north is hilly, the province consists mostly of low coastal plains. The total forest area is 292 km 2 (113 sq mi) or 8 percent of provincial area. [8] Off the shoreline of Mueang Rayong District is Khao Laem Ya–Mu Ko Samet National Park, consisting of several islands.
In 1981, the Royal Forest Department declared the archipelago of Ko Samet, along with nine other small islands, the headland of Khao Laem Ya, and the 11 kilometre Mae Rampeung Beach to be a national park, and thus these areas are under the jurisdiction of the national parks department. In August 2013 more than 500 national park officials were ...
Khao Sam Roi Yot National Park (Thai: อุทยานแห่งชาติเขาสามร้อยยอด, RTGS: Utthayan Haeng Chat Khao Sam Roi Yot, pronounced [ʔùt.tʰā.jāːn hɛ̀ŋ tɕʰâːt kʰǎw sǎːm rɔ́ːj jɔ̂ːt]) is a marine national park in Kui Buri District, Prachuap Khiri Khan Province, Thailand. [2]
For example, "Ko Phi Phi Island" would be redundant, since "Ko Phi Phi" already means "Phi Phi Island" Various maps commonly spell Thai names differently, using different transliterations. For example, Ko Mak may be seen as Koh Mak, Koh Maak or even Koh Mark.
The area of Mu Ko Lanta National Park is 83,750 rai ~ 134 square kilometres (52 sq mi). [3] It includes Mu Ko Rok, Ko Mai Ngam, Ko Talabeng, parts of Ko Lanta Yai, Ko Ngai, Mu Ko Rokk, Ko Rok Nai, Mu Ko Maa, Ko Hin Dang and the nearby islands of Ko Klang, Ko Lanta Noi [dubious – discuss], and Ko Lanta Yai sub-district, Amphoe Ko Lanta, Krabi Province.
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Due to the collision of the Indian and Eurasian plate 0-66 million years ago, the Himalayas were formed, and what is now Thailand shifted dramatically near the continental divide and the limestone rocks were forced upward creating the dramatic limestone "karsts" for which the region is known today. Finally, melting ice established the river ...