mid-ocean ridges
Tsunami's can be triggered by earthquakes that happen underneath the ocean floor.
Earthquakes in Japan are caused by the movement of tectonic plates. A tsunami is a large ocean wave that is caused by sudden motion on the ocean floor which can be triggered by earthquakes.
tsunami
earthquakes under seafloor can lead to tsunamis
Slabs of ocean floor return to the mantle in subduction zones
pie
Mid-ocean ridges are not associated with subduction zones. They are divergent plate boundaries where tectonic plates are moving away from each other, leading to the formation of new oceanic crust. Subduction zones, on the other hand, are convergent plate boundaries where one tectonic plate is being forced beneath another.
The continental shelf is the feature that best marks the edge of a continent. It is the shallow, submerged extension of a continent before the ocean floor begins.
The mid ocean ridge is the area of the ocean floor that is associated with the breaking down of the oceanic crust. This area is known for seafloor spreading.
The ocean floor is irregular as to the land we can see. It has mountains and ridges and plains and valleys and volcanoes. It even has underwater earthquakes, and just about every other land feature you could name.
Offshore trenches are deep, elongated depressions on the ocean floor formed by the collision of tectonic plates. They are typically associated with subduction zones where one tectonic plate is forced beneath another, creating a trench-like topographic feature. Offshore trenches play a vital role in plate tectonics and are often sites of earthquakes and volcanic activity.
THE SHELF
shallow areas
New Zealand experiences about 300 earthquakes of Richter 4 to 4.9 each year, (on average); and an average of two in the range Richter 6 to 6.9.There is a huge difference in the distribution of Deep and Shallow earthquakes, and this is illustrated by graphs in the website of gns.cri.nz.Of course, the shallow earthquakes have a very much greater effect on structures.The very deep earthquakes are commonly in Fiordland, where the population is very low. The deep earthquakes in both islands are strongly associated with the subduction of the Pacific plate under the Australian Plate in the north; and the subduction of the Australian plate under the Pacific Plate in the South.As far as deep earthquakes are concerned, there is a quiet zone where these patterns cross over, and this raises the Southern Alps.New Zealand straddles the boundary between these two plates. The Alpine Fault in the South Island may be an extension of a transcurrent fault associated with the Mid Ocean Ridge sea floor spreading in the south Pacific.This fault continues through New Zealand, emerging as the Hikurangi trench, which becomes the Tonga Trench further north again.
Tsunami's can be triggered by earthquakes that happen underneath the ocean floor.
what other ocean floor feature is fromed by movement of earth's plates
Earthquakes in Japan are caused by the movement of tectonic plates. A tsunami is a large ocean wave that is caused by sudden motion on the ocean floor which can be triggered by earthquakes.