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island arc

American  

noun

  1. a curved chain of islands, as the Aleutians or Antilles, usually convex toward the ocean and enclosing a deep-sea basin.


island arc British  

noun

  1. an arc-shaped chain of islands, such as the Aleutian Islands or the Japanese Islands, usually lying at the edge of a Benioff zone, indicating volcanic activity where the oceanic lithosphere is descending into the earth's interior

"Collins English Dictionary — Complete & Unabridged" 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

island arc Scientific  
  1. A usually curved chain of volcanic islands bounded on the convex side by a deep oceanic trench. Island arcs form in the overriding tectonic plates of subduction zones as the result of rising melt from the downgoing plate. The arcs are curved because of the curvature of the Earth. The Aleutian Islands, in Alaska, are an island arc. An island arc is a kind of volcanic arc.


Etymology

Origin of island arc

First recorded in 1905–10

Example Sentences

Examples are provided to illustrate real-world usage of words in context. Any opinions expressed do not reflect the views of Dictionary.com.

See Examples For:

The results indicate that the mantle beneath the Kermadec island arc melts in the presence of water and at relatively high temperatures, above the sulfide liquidus.

From Science Daily Jul. 29, 2026

Situated in the northeast of the Caribbean island arc, Anguilla lies perfectly within the North Atlantic hurricane belt.

From BBC Aug. 31, 2025

If the volcanoes rise high enough the reach the ocean surface, the chain of volcanism forms an island arc.

From Textbooks Jan. 1, 2017

With an island arc between Asia and India, there would have been two subduction zones pulling on India, which could explain the high velocity of India.

From New York Times May 18, 2015

We’re in another island arc, where volcanoes erupted and islands with their reefs formed, although this islands’s quite a lot older than the one we just visited.

From Scientific American Mar. 7, 2012

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