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The Mariana Trench is part of the Izu–Bonin–Mariana subduction system that forms the boundary between two tectonic platesIn this system the western edge of one plate the Pacific Plate is subducted (ie thrust) beneath the smaller Mariana Plate that lies to the west Crustal material at the western edge of the Pacific Plate is some of the oldest oceanic crust on Earth.
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IDM H&S committee meetings for 2022 will be held via Microsoft Teams on the following Tuesdays at 12h3013h30 8 February 2022 31 May 2022 2 August 2022.
Pacific Plate Subduction Beneath The Central Mariana And Izu Bonin Fore Arcs New Insights From An Old Margin Oakley 2008 Geochemistry Geophysics Geosystems Wiley Online Library
Mariana Trench Wikipedia
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