Slab-pull
Slab-pull
as the subducting plate skins into the mantle, friction between the mantle and lithosphere will oppose plate motion.
An ocean plate is subducting if it is flowing under a less dense plate at a convergent plate boundary.
convergent boundary
Slab-pull
convection
Slab-pull
as the subducting plate skins into the mantle, friction between the mantle and lithosphere will oppose plate motion.
The foci basically outline or emanate from the subducting slab (plate). Multiple foci locations can be used to tell the degree of dip/position of the subducting slab. The distribution patterns also give depth at which melting of slab occurs because earthquakes don't emanate from a partially melted slab, so the deepest earthquake may indicate last solid state of slab.
subducting slab begins to descend beneath another lithospheric slab. Trenches are generally parallel to a volcanic island arc, and about 200 km (120 mi) from a volcanic arc. hence the age of ocean floor is usually greatest in subduction zones
Rock around a subducting slab is heated to extreme temperatures as a result of sliding friction. Much of the rock eventually melts and enters the convection currents in the mantle.
An ocean plate is subducting if it is flowing under a less dense plate at a convergent plate boundary.
volcanoes
Supended slab are slab not sit on the ground directlySuspended slab is a slab supported by beams.
convergent boundary
a clay slab is a slab made of clay