TheInfoListRev V5.1.84
Xfr/
SummaryRelatedTreeNews

Related topics

Suruga Trough

Sponsored
Shop Amazon for garden tools
Browse products on Amazon.
Search Amazon →
As an Amazon Associate I earn from qualifying purchases.

The Suruga Trough (駿河トラフ, Suruga Torafu) is a tectonically activetrough off Suruga Bay, Japan, forming the northern extension of the Nankai Trough. As part of the convergent boundary where the Philippine Sea Platesubducts beneath the Japanese islands, it experiences episodic seafloor disturbances . See alsoJapan Median Tectonic LineList of earthquakes in JapanSagami TroughReferences

Nankai TroughNankai TroughThe Nankai Trough (南海トラフ, Nankai Torafu; Southern Sea Trough) is a submarine trough located south of the Nankaidō region of Japan's island of Honshu, extending approximately 900 km (559 mi) offshore. The underlying fault, the Nankai megathrust, is the source of the devastating Nankai megathrust earthquakes, while the trough itself is potentially a major source of hydrocarbonfuel, in the form of methane clathrate.Philippine Sea platePhilippine Sea plateThe Philippine Sea plate or the Philippine plate is a tectonic plate comprising oceanic lithosphere that lies beneath the Philippine Sea, to the east of the Philippines. Most segments of the Philippines, including northern Luzon, are part of the Philippine Mobile Belt, which is geologically and tectonically separate from the Philippine Sea plate.Suruga BaySuruga BaySuruga Bay (駿河湾, Suruga-wan) is a bay on the Pacific coast of Honshū in Shizuoka Prefecture, Japan. It is situated north of a straight line from Omaezaki Point to Irōzaki Point at the tip of the Izu Peninsula and surrounded by Honshū to the southwest and west and the Izu Peninsula to the east. GeologySuruga Bay contains the Suruga Trough which runs up the middle of the bay, Japan's deepest trough.Trough (geology)Trough (geology)In geology, a trough is a linear structural depression that extends laterally over a distance. Although it is less steep than a trench, a trough can be a narrow basin or a geologic rift. These features often form at the rim of tectonic plates. There are various oceanic troughs on the ocean floors. Troughs created by glaciation are called glacial trough.JapanJapanCountry in East AsiaJapan is an island country in East Asia. Located in the Pacific Ocean off the northeast coast of the Asian mainland, it is bordered to the west by the Sea of Japan, the Sea of Okhotsk in the north, and the East China Sea in the south. The Japanese archipelago consists of four major islands alongside over 14,000 smaller islands.TectonicsTectonicsTectonics (from Ancient Greektektonikós'pertaining to building' via Latin) are the processes that result in the structure and properties of Earth's crust and its evolution through time. The field of planetary tectonics extends the concept to other planets and moons.SubductionSubductionDiagram of the geological process of subductionSubduction is a geological process in which the oceanic lithosphere and some continental lithosphere is recycled into the Earth's mantle at the convergent boundaries between tectonic plates. Where one tectonic plate converges with a second plate, the heavier plate dives beneath the other and sinks into the mantle.Japanese archipelagoJapanese archipelagoThe Japanese archipelago (Japanese: 日本列島, Hepburn: Nippon/Nihon Rettō; Japanese pronunciation: [ɲip.pon/ɲi.hon ɾeꜜt.toː]) is an archipelago of 14,125 islands that constitute the sovereign state of Japan.

*As an Amazon Associate I earn from qualifying purchases.

AboutPrivacyContact

TheInfoList organizes topic information and links to original sources.

Loading topic…