Misplaced Pages

Sea of Japan

Article snapshot taken from Wikipedia with creative commons attribution-sharealike license. Give it a read and then ask your questions in the chat. We can research this topic together.

This is an old revision of this page, as edited by Sola4lang (talk | contribs) at 21:52, 16 November 2006 (Physical characteristics). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Revision as of 21:52, 16 November 2006 by Sola4lang (talk | contribs) (Physical characteristics)(diff) ← Previous revision | Latest revision (diff) | Newer revision → (diff)

Template:Sea of Japan Infobox The Sea of Japan (East Sea) is a marginal sea of the western Pacific Ocean. Like the Mediterranean Sea, it has almost no tides due to its nearly complete enclosure.

Physical characteristics

The sea is bound by Russian mainland and Sakhalin island to the north, North Korea and South Korea to the west, and Japan.

It is connected to other seas by five shallow straits: the Strait of Tartary between the Asian mainland and Sakhalin; La Perouse Strait between the islands of Sakhalin and Hokkaido; the Tsugaru Strait between the islands of Hokkaido and Honshu; the Kanmon Straits between the islands of Honshu and Kyushu; and the Korea Strait between the Korean Peninsula and the island of Kyushu. The Korea Strait is composed of the Western Channel and the Tsushima Strait, on either side of Tsushima Island.

  • Deepest point: 3,742 metres below sea level
  • Mean depth: 1,752 metres
  • Surface area: about 978,000 km²

The sea has three major basins: the Yamato Basin in the southeast; the Japan Basin in the north; and the Tsushima Basin (Ulleung Basin) in the southwest. The Japan Basin has the deepest areas of the sea, while the Tsushima Basin has the shallowest.

On the eastern shores, the continental shelves of the sea are wide, but on the western shores, particularly along the Korean coast, they are narrow, averaging about 30 kilometres wide.

The Tsushima Warm Current, a branch of Kuroshio Current, flows northward through the Korea Strait along the Japanese shore, and the Liman Cold Current flows southward through the Strait of Tartary along the Russian shore.

It was once a landlocked sea when the land bridge of East Asia existed. .

Economy

The areas in the north and the southeast are rich fishing grounds. The importance of the fishery in the sea is well illustrated by the dispute between South Korea and Japan over Dokdo (Takeshima). The sea is also important for its mineral deposits, particularly magnetite sands. There are also believed to be natural gas and petroleum fields. With the growth of East Asian economies, the Sea of Japan has become an increasingly important commercial waterway.

Naming

Main article: Sea of Japan naming dispute
 Regarding East Sea-the sea of Japan, both Korea and Japan reveal different points of view. 

Japan takes a position of being ignorant toward the Korea's claim, judging that her aggressive reactions toward the Korea's raising the problem against the naming of the 'Sea of Japan' which is internationally used would rather highlight the Korea's position. On the other hand, the Korean side raises an objection the naming of the 'Sea of Japan' on the basis that domestic or foreign historical material, mainly old maps, that indicate the sea as 'East Sea'.


Categories: