Converging plate boundaries
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Accretionary wedges
Hornfels
Thrust faults
Low angle 30°
Andes (ocean-cont)
Shallow Earthquakes (ocean-cont)
Island arcs (ocean-ocean)
Metamorphism in accretionary prism (ocean-ocean)
Caribbean (ocean-ocean)
Monserrat and Lesser Antilles (ocean-ocean)
Faults (all kinds of convergent boundaries)
Thrust fault (low angle) and reverse faults (high angle) In ocean-cont very much in wedge to regional scale
Volcanism/mountains (Continent-continent)
Volcanism common because crust is so thick High mountains
Metamorphism (Continent-continent)
Low grade contact metamorphism Low-high grade regional metamorphism (depending on how deep and close to area of convergence rock is)
Metamorphism (ocean-continent)
Oceanic plate (subducted): Blueschist - eclogite facies Accretionary wedge Zeolite - sub greenschist
Volcanism/mountains (ocean- continent)
High mountains Explosive volcanism (lots of volatiles dragged into mantle wedge)