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  2. Island arc - Wikipedia

    en.wikipedia.org/wiki/Island_arc

    Andesite and basaltic andesite are the most abundant volcanic rock in island arc which is indicative of the calc-alkaline magmas. Some Island arcs have distributed volcanic series as can be seen in the Japanese island arc system where the volcanic rocks change from tholeiite—calc-alkaline—alkaline with increasing distance from the trench. [15]

  3. List of Roblox games - Wikipedia

    en.wikipedia.org/wiki/List_of_Roblox_games

    Blox Fruits (formerly known as Blox Piece), is an action fighting game created by Gamer Robot that is inspired by the manga and anime One Piece. [152] In the game, players choose to be a master swordsman, a powerful fruit user, a martial arts attacker or a gun user as they sail across the seas alone or in a team in search of various worlds and ...

  4. Category:Volcanic arcs - Wikipedia

    en.wikipedia.org/wiki/Category:Volcanic_arcs

    A volcanic arc is a chain of volcanic islands or mountains located near the edge of continents that are formed as the result of tectonic plate subduction. Subcategories This category has the following 7 subcategories, out of 7 total.

  5. Nishinoshima (Ogasawara) - Wikipedia

    en.wikipedia.org/wiki/Nishinoshima_(Ogasawara)

    Nishi-no-shima (Japanese: 西之島, "western island") is a volcanic island located around 940 km (584 mi) south-southeast of Tokyo, [2] that is part of the Volcano Islands arc. Nishinoshima is located about 130 km to the west of the nearest of the Ogasawara islands, hence the name, but the other Ogasawara island groups are aligned north-south.

  6. 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.

  7. Geology of Antigua and Barbuda - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Antigua_and_Barbuda

    The geology of Antigua and Barbuda is part of the Lesser Antilles volcanic island arc. Both islands are the above water limestone "caps" of now inactive volcanoes. The two islands are the surface features of the undersea Barbuda Bank and have karst limestone landscapes. [1] Barbuda is primarily flat and formed from coral reefs.

  8. Coromandel Volcanic Zone - Wikipedia

    en.wikipedia.org/wiki/Coromandel_Volcanic_Zone

    The Coromandel Volcanic Zone (CVZ) is an extinct intraplate volcanic arc stretching from Great Barrier Island in the north, through the Coromandel Peninsula, to the Kaimai Range in the south. The area of transition between it and the newer and still active Taupō Volcanic Zone is now usually separated and is called the Tauranga Volcanic Centre .

  9. Back-arc region - Wikipedia

    en.wikipedia.org/wiki/Back-arc_region

    A back-arc above a subduction zone. The back-arc region is the area behind a volcanic arc. [1] In island volcanic arcs, it consists of back-arc basins of oceanic crust with abyssal depths, which may be separated by remnant arcs, similar to island arcs. [1]