Yangon River

The Yangon River (also known as the Rangoon River or Hlaing River) is formed by the confluence of the Pegu and Myitmaka Rivers in Myanmar. It is a marine estuary that runs from Yangon (also known as Rangoon) to the Gulf of Martaban of the Andaman Sea. The channel is navigable by ocean-going vessels, thus plays a critical role in the economy of Myanmar.

Coal divers prepare to dive in the Yangon River
Yangon River
Hlaing River
Yangon River
Native nameလှိုင်မြစ် (Burmese)
Location
CountryMyanmar
CityYangon (also known as Rangoon)
Physical characteristics
Mouth 
  location
Andaman Sea
  elevation
0 m (0 ft)
Discharge 
  locationGulf of Martaban

The Twante Canal connects the Yangon River with the Irrawaddy Delta, once known as 'the rice bowl of Asia'. It consists of 1,000 square miles (3,000 km2) of lush teak plantations and mangrove swamps, many of which have now been cleared for rice production.

References

    16°28′N 96°20′E


    Yangon River, also called Rangoon River, marine estuary in southern Myanmar (Burma), formed at the city of Yangon (Rangoon) by the confluence of the Pegu and Myitmaka rivers. It empties into the Gulf of Martaban of the Andaman Sea, 25 miles (40 km) southeast. Yangon River is about 40 km long. It flows past Thanlyin and Pokataloke.

    Written By Draco

    This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.