Forearc

A forearc is a region in a subduction zone between an oceanic trench and the associated volcanic arc. Forearc regions are present along convergent margins and eponymously form 'in front of' the volcanic arcs that are characteristic of convergent plate margins. A back-arc region is the companion region behind the volcanic arc.

Many forearcs have an accretionary wedge which may form a topographic ridge known as an outer arc ridge that parallels the volcanic arc. A forearc basin between the accretionary wedge and the volcanic arc can accumulate thick deposits of sediment, sometimes referred to as an outer arc trough. Due to collisional stresses as one tectonic plate subducts under another, forearc regions are sources for powerful earthquakes.^[1]^[2]

^ Fuller, C. W; Willet, S.D.; Brandon, M.T. (2006). "Formation of forearc basins and their influence on subduction zone earthquakes". Geology. 34 (2): 65–68. Bibcode:2006Geo....34...65F. doi:10.1130/g21828.1.
^ Kearey, Philip; Klepeis, A. Keith; Fredrick, Vine J. (2009). Global Tectonics (3rd ed.). Singapore by Moarkono: J. Wiley. pp. 1–400. ISBN 978-1-4051-0777-8.

[Fuller_et_al._2006-1] Fuller, C. W; Willet, S.D.; Brandon, M.T. (2006). "Formation of forearc basins and their influence on subduction zone earthquakes". Geology. 34 (2): 65–68. Bibcode:2006Geo....34...65F. doi:10.1130/g21828.1.

[Kearey_et_al._2006-2] Kearey, Philip; Klepeis, A. Keith; Fredrick, Vine J. (2009). Global Tectonics (3rd ed.). Singapore by Moarkono: J. Wiley. pp. 1–400. ISBN 978-1-4051-0777-8.

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