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  2. Island arc - Wikipedia

    en.wikipedia.org/wiki/Island_arc

    Island arcs are long chains of active volcanoes with intense seismic activity found along convergent tectonic plate boundaries. Most island arcs originate on oceanic crust and have resulted from the descent of the lithosphere into the mantle along the subduction zone.

  3. Volcanic arc - Wikipedia

    en.wikipedia.org/wiki/Volcanic_arc

    A volcanic arc (also known as a magmatic arc [1]: 6.2 ) is a belt of volcanoes formed above a subducting oceanic tectonic plate, [2] with the belt arranged in an arc shape as seen from above. Volcanic arcs typically parallel an oceanic trench , with the arc located further from the subducting plate than the trench.

  4. Continental arc - Wikipedia

    en.wikipedia.org/wiki/Continental_arc

    A continental arc is a type of volcanic arc occurring as an "arc-shape" topographic high region along a continental margin.The continental arc is formed at an active continental margin where two tectonic plates meet, and where one plate has continental crust and the other oceanic crust along the line of plate convergence, and a subduction zone develops.

  5. Convergent boundary - Wikipedia

    en.wikipedia.org/wiki/Convergent_boundary

    Volcanic arcs can form as island arc chains or as arcs on continental crust. Three magma series of volcanic rocks are found in association with arcs. The chemically reduced tholeiitic magma series is most characteristic of oceanic volcanic arcs, though this is also found in continental volcanic arcs above rapid subduction (>7 cm/year).

  6. Oceanic trench - Wikipedia

    en.wikipedia.org/wiki/Oceanic_trench

    He proposed the tectogene hypothesis to explain the belts of negative gravity anomalies that were found near island arcs. According to this hypothesis, the belts were zones of downwelling of light crustal rock arising from subcrustal convection currents. The tectogene hypothesis was further developed by Griggs in 1939, using an analogue model ...

  7. Izu–Bonin–Mariana arc - Wikipedia

    en.wikipedia.org/wiki/Izu–Bonin–Mariana_Arc

    The Izu–Bonin–Mariana (IBM) arc system is a tectonic plate convergent boundary in Micronesia.The IBM arc system extends over 2800 km south from Tokyo, Japan, to beyond Guam, and includes the Izu Islands, the Bonin Islands, and the Mariana Islands; much more of the IBM arc system is submerged below sealevel.

  8. Archipelago - Wikipedia

    en.wikipedia.org/wiki/Archipelago

    The Aegean Sea with its large number of islands is the origin of the term archipelago. The Mergui Archipelago in Myanmar. An archipelago (/ ˌ ɑːr k ə ˈ p ɛ l ə ɡ oʊ / ⓘ AR-kə-PEL-ə-goh), [1] sometimes called an island group or island chain, is a chain, cluster, or collection of islands. An archipelago may be in an ocean, a sea, or ...

  9. Category:Island arcs - Wikipedia

    en.wikipedia.org/wiki/Category:Island_arcs

    Pages in category "Island arcs" The following 8 pages are in this category, out of 8 total. This list may not reflect recent changes. ...