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{{ |
{{Short description|Oceanic tectonic plate to the east of the Philippines}} | ||
{{ |
{{more citations needed|date=March 2017}} | ||
{{Use mdy dates|date=December 2022}} | |||
{{Use Philippine English|date=December 2022}} | |||
{{Infobox tectonic plate | {{Infobox tectonic plate | ||
| image = File:PhilippinePlate.png | | image = File:PhilippinePlate.png | ||
| alt = The Philippine Sea |
| alt = The Philippine Sea plate | ||
| type = ] | | type = ] | ||
| area = 5,500,000 km<sup>2</sup><ref>{{cite web|url=http://geology.about.com/library/bl/blplate_size_table.htm|title=Sizes of Tectonic or Lithospheric Plates |
| area = 5,500,000 km<sup>2</sup><ref>{{cite web|url=http://geology.about.com/library/bl/blplate_size_table.htm<!-- NOTE: as if September 2, 2021, redirects to a page giving no support or information re area -- archived olde version does-->|archiveurl=https://web.archive.org/web/20070209033841/http://geology.about.com/library/bl/blplate_size_table.htm|archivedate=February 9, 2007|title=Sizes of Tectonic or Lithospheric Plates}}</ref> | ||
| move_direction = north-west | | move_direction = north-west | ||
| move_speed = |
| move_speed = 48–84 mm/year | ||
| geo_features = ], ], ] | | geo_features = ], ], ] | ||
}} | }} | ||
The '''Philippine Sea |
The '''Philippine Sea plate''' or the '''Philippine plate''' is a ] comprising oceanic ] that lies beneath the ], to the east of the Philippines. Most segments of the Philippines, including northern ], are part of the ], which is geologically and tectonically separate from the Philippine Sea plate. | ||
The plate is bordered mostly by ]:<ref>{{Cite book |last1=Smoczyk |first1=Gregory M. |last2=Hayes |first2=Gavin P. |last3=Hamburger |first3=Michael W. |last4=Benz |first4=Harley M. |last5=Villaseñor |first5=Antonio H. |last6=Furlong |first6=Kevin P. |title=Open-File Report |date=2013 |chapter=Seismicity of the Earth 1900-2012 Philippine Sea plate and vicinity |chapter-url=https://pubs.usgs.gov/of/2010/1083/m/pdf/of2010-1083m.pdf |location=Reston, VA |doi=10.3133/ofr20101083m}}</ref> To the north, the Philippine Sea plate meets the ] at the ]. The Philippine Sea plate, the ], and the Okhotsk plate meet near ] in Japan. The thickened crust of the Izu–Bonin–Mariana arc colliding with Japan constitutes the Izu Collision Zone. The east of the plate includes the ]–] (Bonin) and the ], forming the ] system. There is also a ] between the Philippine Sea plate and the small ] which carries the Mariana Islands. To the east, the ] ] beneath the Philippine Sea plate at the ]. To the south, the Philippine Sea plate is bounded by the ] and ]. To the west, the Philippine Sea plate subducts under the ] at the ] and the ]. (The adjacent rendition of Prof. Peter Bird's map is inaccurate in this respect.) To the northwest, the Philippine Sea plate meets ] and the ] on the ], and southern Japan on the ]. | |||
Philippine Sea plate is bordered mostly by ]<ref>Smoczyk, G.M., Hayes, G.P., Hamburger, M.W., Benz, H.M., Villaseñor, Antonio, and Furlong, K.P., 2013, : U.S. Geological Survey Open-File Report 2010–1083-M, scale 1:10,000,000, ''<nowiki>https://dx.doi.org/10.3133/ofr20101083m</nowiki>''.</ref>: | |||
It also meets the ] due northwest. | |||
To the north, the Philippine Sea Plate meets the ] at the ]. The Philippine Sea Plate, the ], and the Okhotsk Plate meet at ] in ]. The thickened crust of the Izu-Bonin-Mariana arc colliding with Japan constitutes the Izu Collision Zone. | |||
The east of the plate includes the ]-] (Bonin) and the ], forming the ] system. There is also a ] between the Philippine Sea Plate and the small ] which carries the Mariana Islands. To the east, the ] ] beneath the Philippine Sea Plate at the ]. | |||
To the south, the Philippine Sea Plate is bounded by the ] and ]. | |||
To the west, the Philippine Sea Plate subducts under the ] at the ] and the ]. (The adjacent rendition of Prof. Peter Bird's map is inaccurate in this respect.) | |||
To the northwest, the Philippine Sea Plate meets ] and the ] on the ], and southern Japan on the ]. | |||
] | ] | ||
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==References== | ==References== | ||
{{Reflist}} | {{Reflist}} | ||
* {{ |
* {{citation|doi=10.1029/GM088p0371|chapter=The Philippine Sea Plate: Magnetism and reconstructions|title=Active Margins and Marginal Basins of the Western Pacific|series=Geophysical Monograph Series|year=1995|last1=Hall|first1=Robert|last2=Fuller|first2=Michael|last3=Ali|first3=Jason R.|last4=Anderson|first4=Charles D.|volume=88|pages=371–404|isbn=0-87590-045-3}} | ||
==External links== | ==External links== | ||
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{{SE Asia plates}} | {{SE Asia plates}} | ||
{{East Asia plates}} | {{East Asia plates}} | ||
{{Authority control}} | |||
⚫ | {{coord|26|N|132|E|type:landmark_source:dewiki|display=title}} | ||
⚫ | {{coord|26|N|132|E|type:landmark_source:dewiki|display=title}} | ||
⚫ | {{tectonics-stub}} | ||
] | ] | ||
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] | ] | ||
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Latest revision as of 03:52, 10 November 2024
Oceanic tectonic plate to the east of the PhilippinesThis article needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. Find sources: "Philippine Sea plate" – news · newspapers · books · scholar · JSTOR (March 2017) (Learn how and when to remove this message) |
Philippine Sea plate | |
---|---|
Type | Minor |
Approximate area | 5,500,000 km |
Movement | north-west |
Speed | 48–84 mm/year |
Features | Northern Luzon, Philippine Sea, Taiwan |
Relative to the African plate |
The 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.
The plate is bordered mostly by convergent boundaries: To the north, the Philippine Sea plate meets the Okhotsk microplate at the Nankai Trough. The Philippine Sea plate, the Amurian plate, and the Okhotsk plate meet near Mount Fuji in Japan. The thickened crust of the Izu–Bonin–Mariana arc colliding with Japan constitutes the Izu Collision Zone. The east of the plate includes the Izu–Ogasawara (Bonin) and the Mariana Islands, forming the Izu–Bonin–Mariana Arc system. There is also a divergent boundary between the Philippine Sea plate and the small Mariana plate which carries the Mariana Islands. To the east, the Pacific plate subducts beneath the Philippine Sea plate at the Izu–Ogasawara Trench. To the south, the Philippine Sea plate is bounded by the Caroline plate and Bird's Head plate. To the west, the Philippine Sea plate subducts under the Philippine Mobile Belt at the Philippine Trench and the East Luzon Trench. (The adjacent rendition of Prof. Peter Bird's map is inaccurate in this respect.) To the northwest, the Philippine Sea plate meets Taiwan and the Nansei islands on the Okinawa plate, and southern Japan on the Amurian plate. It also meets the Yangtze plate due northwest.
See also
References
- "Sizes of Tectonic or Lithospheric Plates". Archived from the original on February 9, 2007.
- Smoczyk, Gregory M.; Hayes, Gavin P.; Hamburger, Michael W.; Benz, Harley M.; Villaseñor, Antonio H.; Furlong, Kevin P. (2013). "Seismicity of the Earth 1900-2012 Philippine Sea plate and vicinity" (PDF). Open-File Report. Reston, VA. doi:10.3133/ofr20101083m.
{{cite book}}
: CS1 maint: location missing publisher (link)
- Hall, Robert; Fuller, Michael; Ali, Jason R.; Anderson, Charles D. (1995), "The Philippine Sea Plate: Magnetism and reconstructions", Active Margins and Marginal Basins of the Western Pacific, Geophysical Monograph Series, vol. 88, pp. 371–404, doi:10.1029/GM088p0371, ISBN 0-87590-045-3
External links
- High-resolution map of Tectonic Plate Boundaries
- Map showing Seismicity of the Earth, 1900‒2012: Philippine Sea Plate and Vicinity United States Geological Survey
Tectonic plates of Southeast Asia–New Guinea (Australian plate–Pacific plate convergence zone) | |||||||||||
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Trenches and troughs |
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Subsea plateaus and basins |
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26°N 132°E / 26°N 132°E / 26; 132
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