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The Yuri Coast Seawall (由利海岸波除石垣, Yuri kaigan namiyoke ishigaki) is an Edo period (1600-1868) seawall against high waves, salt spray, and strong winds on the Sea of Japan coast in what is now part of the city of Nikaho, Akita. [1] Its remains were designated a National Historic Site of Japan in 1997. [2]
The total surviving length is 640 meters. There are two cut-throughs in the embankment with tide doors. One was made in 1926 and the other in 1980. The earlier Hatakeyama seawall is located in between the Hiromura Embankment and the ocean.The area in between was planted with Japanese black pine and Japanese spindle as well as Japanese lacquer ...
A seawall (or sea wall) is a form of coastal defense constructed where the sea, and associated coastal processes, impact directly upon the landforms of the coast. The purpose of a seawall is to protect areas of human habitation, conservation, and leisure activities from the action of tides, waves, or tsunamis. [1]
A map of Japan's major cities, main towns and selected smaller centers. Japan has a population of 126.3 million in 2019. [20] It is the eleventh-most populous country and the second-most populous island country in the world. [12] The population is clustered in urban areas along the coast, plains, and valleys. [15]
Japan sea map. The earliest known term used for maps in Japan is believed to be kata (形, roughly "form"), which was probably in use until roughly the 8th century.During the Nara period, the term zu (図) came into use, but the term most widely used and associated with maps in pre-modern Japan is ezu (絵図, roughly "picture diagram").
It has three major basins: the Yamato Basin in the south-east, the Japan Basin in the north and the Tsushima Basin (Ulleung Basin) in the south-west. [12] The Japan Basin is of oceanic origin and is the deepest part of the sea, whereas the Tsushima Basin is the shallowest with the depths below 2,300 m (7,500 ft). [13]
In the Edo period, the Seto Inland Sea was one of the busiest transport lines in Japan. It was a part of a navigational route around Japan's islands via the Sea of Japan. Many ships navigated from its coastal areas to the area along the Sea of Japan. Major ports in the Edo period were Osaka, Sakai, Shimotsui, Ushimado, and Tomonoura.
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 ...