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The Sea of Japan (see below for other names) is the marginal sea between the Japanese archipelago, Sakhalin, the Korean Peninsula, and the mainland of the Russian Far East. The Japanese archipelago separates the sea from the Pacific Ocean. Like the Mediterranean Sea, it has almost no tides due to its nearly complete enclosure from the Pacific ...
A dispute exists over the international name for the body of water which is bordered by Japan, Korea (North and South) and Russia. In 1992, objections to the name Sea of Japan were first raised by North Korea and South Korea at the Sixth United Nations Conference on the Standardization of Geographical Names. [1]
The Sea of Japan was considered to be a frozen inner lake because of the lack of the warm Tsushima Current. Various plants and large animals, such as Palaeoloxodon naumanni, migrated into the Japanese archipelago. [76] The Sea of Japan was a landlocked sea when the land bridge of East Asia existed circa 18,000 BCE. During the glacial maximum ...
Seto Inland Sea. The Seto Inland Sea (瀬戸内海, Seto Naikai), sometimes shortened to the Inland Sea, is the body of water separating Honshu, Shikoku, and Kyushu, three of the four main islands of Japan. It serves as a waterway connecting the Pacific Ocean to the Sea of Japan. It connects to Osaka Bay and provides a sea transport link to ...
Approximately 26 [1] The Liancourt Rocks, [2] also known by their Korean name of Dokdo (Korean: 독도) [a] or their Japanese name of Takeshima, [b] are a group of islets in the Sea of Japan between the Korean peninsula and the Japanese archipelago administered by South Korea. The Liancourt Rocks comprise two main islets and 35 smaller rocks ...
South Atlantic. gyre. The Kuroshio Current is the west side of the clockwise North Pacific ocean gyre. The Kuroshio Current (黒潮, "Black Tide"), also known as the Black Current or Japan Current (日本海流, Nihon Kairyū) is a north-flowing, warm ocean current on the west side of the North Pacific Ocean basin. It was named for the deep ...
Liancourt Rocks dispute. The Liancourt Rocks dispute, also called the Takeshima dispute or Dokdo dispute is a territorial dispute between South Korea and Japan [1][2][3][4] regarding sovereignty over the Liancourt Rocks, a group of small islets in the Sea of Japan. The rocks also go by the names Dokdo (Korean: 독도; Hanja: 獨島) and ...
Around 23 million years ago, western Japan was a coastal region of the Eurasia continent. The subducting plates, being deeper than the Eurasian plate, pulled parts of Japan which become modern Chūgoku region and Kyushu eastward, opening the Sea of Japan (simultaneously with the Sea of Okhotsk) around 15-20 million years ago, with likely freshwater lake state before the sea has rushed in. [4 ...