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- Q5535380 subject Q6977665.
- Q5535380 subject Q7288708.
- Q5535380 subject Q8668390.
- Q5535380 abstract "The islands of Japan are primarily the result of several large oceanic movements occurring over hundreds of millions of years from the mid-Silurian to the Pleistocene as a result of the subduction of the Philippine Sea Plate beneath the continental Amurian Plate and Okinawa Plate to the south, and subduction of the Pacific Plate under the Okhotsk Plate to the north.Japan was originally attached to the eastern coast of the Eurasian continent. The subducting plates, being deeper than the Eurasian plate, pulled Japan eastward, opening the Sea of Japan around 15 million years ago. The Strait of Tartary and the Korea Strait opened much later.Japan is situated in a volcanic zone on the Pacific Ring of Fire. Frequent low intensity earth tremors and occasional volcanic activity are felt throughout the islands. Destructive earthquakes, often resulting in tsunamis, occur several times a century. The most recent major quakes include the 2011 Tōhoku earthquake and tsunami, the 2004 Chūetsu earthquake and the Great Hanshin earthquake of 1995. Hot springs are numerous and have been developed as resorts.".
- Q5535380 thumbnail Japan_separation.png?width=300.
- Q5535380 wikiPageExternalLink tatoroyama_no_ki_e.html.
- Q5535380 wikiPageExternalLink japan-map.jpg.
- Q5535380 wikiPageExternalLink GSJ.
- Q5535380 wikiPageExternalLink index.html.
- Q5535380 wikiPageWikiLink Q1072875.
- Q5535380 wikiPageWikiLink Q1091247.
- Q5535380 wikiPageWikiLink Q110802.
- Q5535380 wikiPageWikiLink Q1139220.
- Q5535380 wikiPageWikiLink Q1201001.
- Q5535380 wikiPageWikiLink Q17.
- Q5535380 wikiPageWikiLink Q176318.
- Q5535380 wikiPageWikiLink Q1784278.
- Q5535380 wikiPageWikiLink Q18783.
- Q5535380 wikiPageWikiLink Q205411.
- Q5535380 wikiPageWikiLink Q214866.
- Q5535380 wikiPageWikiLink Q25546.
- Q5535380 wikiPageWikiLink Q27092.
- Q5535380 wikiPageWikiLink Q339748.
- Q5535380 wikiPageWikiLink Q3510594.
- Q5535380 wikiPageWikiLink Q36204.
- Q5535380 wikiPageWikiLink Q481751.
- Q5535380 wikiPageWikiLink Q52052.
- Q5535380 wikiPageWikiLink Q5401.
- Q5535380 wikiPageWikiLink Q543692.
- Q5535380 wikiPageWikiLink Q62412.
- Q5535380 wikiPageWikiLink Q655311.
- Q5535380 wikiPageWikiLink Q6977665.
- Q5535380 wikiPageWikiLink Q7288708.
- Q5535380 wikiPageWikiLink Q7944.
- Q5535380 wikiPageWikiLink Q8070.
- Q5535380 wikiPageWikiLink Q8072.
- Q5535380 wikiPageWikiLink Q8668390.
- Q5535380 comment "The islands of Japan are primarily the result of several large oceanic movements occurring over hundreds of millions of years from the mid-Silurian to the Pleistocene as a result of the subduction of the Philippine Sea Plate beneath the continental Amurian Plate and Okinawa Plate to the south, and subduction of the Pacific Plate under the Okhotsk Plate to the north.Japan was originally attached to the eastern coast of the Eurasian continent.".
- Q5535380 label "Geology of Japan".
- Q5535380 depiction Japan_separation.png.