| Kokunye Kyun | |
|---|---|
| Island | |
  Kokunye Kyun | |
| Coordinates: 15°18′0″N97°42′35″E / 15.30000°N 97.70972°E | |
| Country | Myanmar |
| State | Mon |
| Area | |
| • Total | 0.7 km2 (0.3 sq mi) |
| Elevation | 140 m (460 ft) |
| Time zone | Myanmar Standard Time (UTC+6:30) |
Kokunye Kyun is an island in the Andaman Sea, right off the coast of Mon State, in the southern area of Burma. It is located in an area of shoals. This island is 1.4 kilometres (0.87 mi) long and its maximum width is 0.4 kilometres (0.25 mi). It is covered with dense forest and rises to a height of 140 metres (460 ft).
The Andaman Sea is a marginal sea of the eastern Indian Ocean separated from the Bay of Bengal by the Andaman Islands of India and Myanmar and the Nicobar Islands of India and touching Myanmar, Thailand, and the Malay Peninsula. Its southernmost end is defined by Breueh Island, an island just north of Sumatra.
Mon State is an administrative division of Myanmar. It lies between Kayin State to the east, the Andaman Sea to the west, Bago Region to the north and Tanintharyi Region to the south, also having a short border with Thailand's Kanchanaburi Province at its south-eastern tip. The land area is 12,155 km2. The Dawna Range, running along the eastern side of the state in a NNW–SSE direction, forms a natural border with Kayin State. Mon State includes some small islands, such as Kalegauk, Wa Kyun and Kyungyi Island, along its 566 km of coastline. The state's capital is Mawlamyine.
In oceanography, geomorphology, and earth sciences, a shoal is a natural submerged ridge, bank, or bar that consists of, or is covered by, sand or other unconsolidated material, and rises from the bed of a body of water to near the surface. Often it refers to those submerged ridges, banks, or bars that rise near enough to the surface of a body of water as to constitute a danger to navigation. Shoals are also known as sandbanks, sandbars, or gravelbars. Two or more shoals that are either separated by shared troughs or interconnected by past or present sedimentary and hydrographic processes are referred to as a shoal complex.
