The continuing movement along these plate boundaries occur at a depth of about 8, metres 26, ft. In addition, the trench is crooked off Erimo cape, Hokkaido. It is considered the bend of the trench causes complex shape of the plate boundary. Japan has been situated in the convergent plate boundary during long geohistorical ages. This means that the Japanese islands are built under the subduction tectonics.
The Japanese islands are characterized as the grown-up continental margin formed by the subduction of the oceanic plate. It includes many lesser faults in addition to the San Andreas Fault. The obvious trench to the east and the mountains and volcanoes of the Japanese islands indicate that this is a convergent margin. The Pacific plate is moving westward and being subducted beneath the northern part of Japan, which is on the Okhotsk Plate.
The tectonic plates and their boundaries surrounding Japan. When two continental plates converge, they smash together and create mountains. World Agents for Change. Health Long-Term Care. For Teachers. NewsHour Shop. About Feedback Funders Support Jobs. Close Menu. Email Address Subscribe. Yes Not now. By — Jenny Marder Jenny Marder. Leave your feedback. Share on Facebook Share on Twitter. Its geological features are as follows.
Contact Site Map Location Japanese. Geological Map of Japan top Subduction and Japan Japan has been situated in the convergent plate boundary during long geohistorical ages. Numbers of accretionary complexes accumulate in order and part of them are re-arranged by later tectonism. Age of the basement rocks is generally older in the continental side and younger in the ocean side.
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