An accretionary wedge is a typical feature found along subduction zones.

Question

Quizplus · Accepted Answer

An accretionary wedge is a common feature found along subduction zones where the oceanic plate is subducting beneath a continental plate. As the oceanic plate slides beneath the continental plate, sediment and rock are scraped off the top of the subducting plate and accumulate in a wedge-shaped deposit known as an accretionary wedge. Over time, this sediment can become compressed and deformed, creating complex geological structures and rock formations within the wedge.

An Accretionary Wedge Is a Typical Feature Found Along Subduction