[Collapse]
Wikipedia relies on your donations: please give today.
$2,876,194
Our Goal: $6 millio
Volcanic arc
From Wikipedia, the free encyclopedia
A volcanic arc is a chain of volcanic islands or mountains formed by plate tectonics as an oceanic tectonic plate subducts under another tectonic plate and produces magma. There are two types of volcanic arcs: oceanic arcs (commonly called island arcs, a type of archipelago) and continental arcs. In the former, oceanic crust subducts beneath other oceanic crust on an adjacent plate, while in the latter case the oceanic crust subducts beneath continental crust. In some situations, a single subduction zone may show both aspects along its length, as part of a plate subducts beneath a continent and part beneath adjacent oceanic crust.
Two classic examples of oceanic island arcs are the Mariana Islands in the western Pacific OceanLesser Antilles in the western Atlantic Ocean. The Cascade Volcanic Arc in western North America and the Andes along the western edge of South America are examples of continental volcanic arcs. The best examples of volcanic arcs with both sets of characteristics are in the North Pacific, with the Aleutian Arc consisting of the Aleutian Islands and their extension the Aleutian Range on the Alaska Peninsula, and the Kuril-Kamchatka Arc comprising the Kuril Islands and southern Kamchatka Peninsula. and the
Contents[hide] |
[edit] Petrology
In the subduction zone, loss of water from the subducted slab induces partial melting of the overriding mantle and generates low-density, calc-alkaline magma that buoyantly rises to intrude and be extruded through the lithosphere of the overriding plate. This loss of water is due to the destabilization of the mineral chlorite at approximately 40-60 km depth.[1][2] This is the reason for island arc volcanism at consistent distances from the subducting slab: because the temperature-pressure conditions for flux-melting volcanism due to chlorite destabilization will always occur at the same depth, the distance from the trench to the arc volcanoes is determined only by the dip angle of the subducting slab.
On the subducting side of the island arc is a deep and narrow oceanic trench, which is the trace at the Earth’s surface of the boundary between the downgoing and overriding plates. This trench is created by the gravitational pull of the relatively dense subducting plate pulling the leading edge of the plate downward. Multiple earthquakes occur along this subduction boundary with the seismic hypocenters located at increasing depth under the island arc: these quakes define the Wadati-Benioff zones.
Ocean basins that are being reduced by subduction are called 'remnant oceans' as they will slowly be shrunken out of existence and crushed in the subsequent orogenic collision. This process has happened over and over in the geologic history of the Earth.
[edit] Examples
[edit] Continental arcs
[edit] Island arcs
- Aleutian Islands
- Kuril Islands
- Japan and Ryukyu Islands
- Izu Islands
- Philippines
- Mariana Islands
- Tonga and Kermadec Islands
- Bonin Islands
- Crete and Dodecanese
- Andaman and Nicobar Islands
- Mentawai Islands
- Sunda Arc
- Lesser Sunda Islands
- Tanimbar and Kai Islands
- Solomon Islands
- South Aegean Volcanic Arc
- Lesser Antilles, including the Leeward Antilles
- South Sandwich Islands
- Mascarene Islands
[edit] Ancient Island arcs
[edit] See also
[edit] References
- ^ Grove, T. L., N. Chatterjee, S. W. Parman, and E. Médard (2006), The Influence of H2O on Mantle Wedge Melting, Earth and Planetary Science Letters, 249, 74-89.
- ^ Grove, T.L., C. B. Till, N. Chatterjee, and E. Médard (submitted 2008), Transport of H2O in subduction zones and its role in the formation and location of arc volcanoes, Nature.
Personal tools
Toolbox
- This page was last modified on 16 November 2008, at 15:46.
- All text is available under the terms of the GNU Free Documentation License. (See Copyrights for details.)
Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc., a U.S. registered 501(c)(3) tax-deductible nonprofit charity. - Privacy policy
- About Wikipedia
- Disclaimers
Donate Now »
[Expand]
Support Wikipedia: a non-profit project
Donate Now »
[Expand]
Support Wikipedia: a non-profit project — Donate Now
Volcanic arc
From Wikipedia, the free encyclopedia
(Redirected from Island arc)
Jump to: navigation, search
"Arcs" redirects here; for other uses, see Arc.
Mariana Islands, an oceanic island arc
Cascade Volcanic Arc, a continental volcanic arc
A volcanic arc is a chain of volcanic islands or mountains formed by plate tectonics as an oceanic tectonic plate subducts under another tectonic plate and produces magma. There are two types of volcanic arcs: oceanic arcs (commonly called island arcs, a type of archipelago) and continental arcs. In the former, oceanic crust subducts beneath other oceanic crust on an adjacent plate, while in the latter case the oceanic crust subducts beneath continental crust. In some situations, a single subduction zone may show both aspects along its length, as part of a plate subducts beneath a continent and part beneath adjacent oceanic crust.
Two classic examples of oceanic island arcs are the Mariana Islands in the western Pacific Ocean and the Lesser Antilles in the western Atlantic Ocean. The Cascade Volcanic Arc in western North America and the Andes along the western edge of South America are examples of continental volcanic arcs. The best examples of volcanic arcs with both sets of characteristics are in the North Pacific, with the Aleutian Arc consisting of the Aleutian Islands and their extension the Aleutian Range on the Alaska Peninsula, and the Kuril-Kamchatka Arc comprising the Kuril Islands and southern Kamchatka Peninsula.
Contents
[hide]
* 1 Petrology
* 2 Examples
o 2.1 Continental arcs
o 2.2 Island arcs
o 2.3 Ancient Island arcs
* 3 See also
* 4 References
[edit] Petrology
In the subduction zone, loss of water from the subducted slab induces partial melting of the overriding mantle and generates low-density, calc-alkaline magma that buoyantly rises to intrude and be extruded through the lithosphere of the overriding plate. This loss of water is due to the destabilization of the mineral chlorite at approximately 40-60 km depth.[1][2] This is the reason for island arc volcanism at consistent distances from the subducting slab: because the temperature-pressure conditions for flux-melting volcanism due to chlorite destabilization will always occur at the same depth, the distance from the trench to the arc volcanoes is determined only by the dip angle of the subducting slab.
On the subducting side of the island arc is a deep and narrow oceanic trench, which is the trace at the Earth’s surface of the boundary between the downgoing and overriding plates. This trench is created by the gravitational pull of the relatively dense subducting plate pulling the leading edge of the plate downward. Multiple earthquakes occur along this subduction boundary with the seismic hypocenters located at increasing depth under the island arc: these quakes define the Wadati-Benioff zones.
Ocean basins that are being reduced by subduction are called 'remnant oceans' as they will slowly be shrunken out of existence and crushed in the subsequent orogenic collision. This process has happened over and over in the geologic history of the Earth.
The Aleutian Arc, with both oceanic and continental parts.
[edit] Examples
[edit] Continental arcs
* Cascade Volcanic Arc
* Alaska Peninsula and Aleutian Range
* Kamchatka
* Andes
o North Volcanic Zone
o Central Volcanic Zone
o South Volcanic Zone
o Austral Volcanic Zone
* Central America Volcanic Arc
[edit] Island arcs
* Aleutian Islands
* Kuril Islands
* Japan and Ryukyu Islands
* Izu Islands
* Philippines
* Mariana Islands
* Tonga and Kermadec Islands
* Bonin Islands
* Crete and Dodecanese
* Andaman and Nicobar Islands
* Mentawai Islands
* Sunda Arc
* Lesser Sunda Islands
* Tanimbar and Kai Islands
* Solomon Islands
* South Aegean Volcanic Arc
* Lesser Antilles, including the Leeward Antilles
* South Sandwich Islands
* Mascarene Islands
[edit] Ancient Island arcs
* Insular Islands
* Intermontane Islands
* Sakhalin island arc
[edit] See also
* Back-arc basin
* Volcanic belt
[edit] References
1. ^ Grove, T. L., N. Chatterjee, S. W. Parman, and E. Médard (2006), The Influence of H2O on Mantle Wedge Melting, Earth and Planetary Science Letters, 249, 74-89.
2. ^ Grove, T.L., C. B. Till, N. Chatterjee, and E. Médard (submitted 2008), Transport of H2O in subduction zones and its role in the formation and location of arc volcanoes, Nature.
* Subduction Zone Volcanism
* Tectonics and Volcanoes of Japan
* USGS: Island-Arc, Oceanic, and Continental Volcanoes
Retrieved from "http://en.wikipedia.org/wiki/Volcanic_arc"
Categories: Volcanic arcs | Volcanology | Plate tectonics | Archipelagoes | Coastal and oceanic landforms
Views
* Article
* Discussion
* Edit this page
* History
Personal tools
* Log in / create account
Navigation
* Main page
* Contents
* Featured content
* Current events
* Random article
Search
Interaction
* About Wikipedia
* Community portal
* Recent changes
* Contact Wikipedia
* Donate to Wikipedia
* Help
Toolbox
* What links here
* Related changes
* Upload file
* Special pages
* Printable version
* Permanent link
* Cite this page
Languages
* Deutsch
* Eesti
* Español
* Français
* עברית
* Italiano
* 日本語
* Nederlands
* Norsk (nynorsk)
* Português
* Русский
* Tiếng Việt
Powered by MediaWiki
Wikimedia Foundation
* This page was last modified on 16 November 2008, at 15:46.
* All text is available under the terms of the GNU Free Documentation License. (See Copyrights for details.)
Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc., a U.S. registered 501(c)(3) tax-deductible nonprofit charity.
* Privacy policy
* About Wikipedia
* Disclaimers
No comments:
Post a Comment