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The Kuroshio current is warm, compared to cooler waters in the Yellow Sea, and Sea of Japan. The Kuroshio is a relatively warm ocean current with an annual average sea-surface temperature of about 24 °C (75 °F), is approximately 100 kilometres (62 mi) wide, and produces frequent small to meso-scale eddies.
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 ...
The Oyashio Current (親潮, "Parental Tide"), also known as the Okhotsk Current or Kurile Current, is a cold subarctic ocean current that flows south and circulates counterclockwise in the western North Pacific Ocean. The waters of the Oyashio Current originate in the Arctic Ocean and flow southward via the Bering Sea, passing through the ...
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 ...
Coordinates: 34.0075°N 129.49°E. The map of the Tsushima strait. Tsushima Strait (対馬海峡, Tsushima Kaikyō)[1] or Eastern Channel[2] (동수로 Dongsuro) is a channel of the Korea Strait, which lies between Korea and Japan, connecting the Sea of Japan, the Yellow Sea, and the East China Sea. The strait is the channel to the east and ...
Tsunamis in the Sea of Japan have been observed to arrive faster than those along Japan's Pacific coast. [100] Tsunami modelling executed by the University of Tokyo and Building Research Institute of Japan computed the tsunami to be 3.6 m (12 ft) in Suzu; 3 m (9.8 ft) in Noto; 2.5 m (8 ft 2 in) in Shika and 2 m (6 ft 7 in) in Jōetsu, Niigata.
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 ...
Senkaku Islands dispute. Uotsuri-shima, the largest of the Senkaku Islands at 4.3 km 2 (1.7 sq mi), in an aerial photograph taken in 1978 by the MLIT, the omnibus ministry which operates the Japan Coast Guard. The Senkaku Islands dispute, or Diaoyu Islands dispute, is a territorial dispute over a group of uninhabited islands known as the ...