The Full Wiki

More info on Suruga Bay

Suruga Bay: Map

Advertisements
  

Wikipedia article:

Map showing all locations mentioned on Wikipedia article:





Suruga Bay (駿河湾, Suruga-wan) is a bay on the Pacificmarker coast of Honshūmarker in Shizuoka Prefecturemarker, Japanmarker. It is situated north of an imaginary line joining Omaezakimarker Point and Irōzaki Point at the tip of the Izu Peninsulamarker and surrounded by Honshū to the southwest and west and the Izu Peninsula to the east.

Geology

Suruga Bay is a place of contrasts. Japan's loftiest peak, Mount Fujimarker at 3,776 m (12,388 ft), rises from the 2,500-m depth of the Suruga Trough running up the middle of the bay, which makes it Japan's deepest. Numerous rivers—especially the major Fujimarker, the Ōimarker, and Abemarker Rivers—empty into its western portion, giving that area of the bay a seabed rich in submarine canyons and other geographical features, whereas at the bay's easternmost end, only the Kano Rivermarker empties into a pocket (called Uchiura-wan) at Numazu where the Izu Peninsula connects to Honshūmarker, giving the water greater transparency and leaving the seabed largely flat except for a number of small rocky islands, some joined to the mainland by tombolos. This seabed variety coincides with coastline differences as well: The western and central sections of the Suruga Bay coastline, roughly from Shizuoka to Numazu, are characterized by sandy beaches such as those at Yuigahama and Tagonoura, whereas the eastern and northeastern stretches from Numazu down the southwestern coast of the Izu Peninsula to Irōzaki, are generally rocky.

The bay is open to the Philippine Seamarker/Pacific Oceanmarker to the south, but is mostly protected from oceanic waves by Izu Peninsula. This, coupled with the seabed and water characteristics mentioned above, results in conditions favorable to fishing, sailing, windsurfing, swimmingand research on deep-sea organisms [203490]. An undersea plateau at the bay's southwest end, known as Senoumi, is especially well known as a rich fishing ground.

Suruga Bay was formed by tectonic subduction of the Philippine Sea Platemarker and the Eurasian Plate at the Suruga Trough, making it a source of considerable seismic activity, [203491][203492] and giving the bay its extreme depth.

Transport

Suruga Bay can be reached by car from Tokyomarker via Numazu in two to five hours depending on traffic conditions on the Tomei Expressway or in Numazu.

A Google map of the bay is available here.

Sources

In addition to the sources cited in the text, this article draws on the content of the corresponding article in the Japanese Wikipedia, as well as Japanese articles corresponding to other English Wikipedia articles linked to in the text.


Embed code:
Advertisements






Got something to say? Make a comment.
Your name
Your email address
Message