No, the wording of you question is not true. However the movement of the lithospheric plates is related to the formation of volcanoes.
True
Convection current occurs due to the difference in densities
skeletal allows movement. No system allows movement of organs LOL
Volcanoes and earthquakes are usually found along plate boundaries because the constant movement allows for lava to flow through easier, and causes release in tension from an earthquake.
The much of the mantle is solid but ductile. This allows it to convect, which aids in plate movement.
true A+
True
Movement of lithospheric plates at convergent boundaries can result in the subduction of one plate beneath another. This subduction creates conditions for magma to form as the subducting plate melts. The rising magma then reaches the surface, leading to the formation of volcanoes.
Convection current occurs due to the difference in densities
Hyperextension is the movement that allows you to gaze at the ceiling.
Volcanoes and earthquakes are usually found along plate boundaries because the constant movement allows for lava to flow through easier, and causes release in tension from an earthquake.
skeletal allows movement. No system allows movement of organs LOL
This is a saddle joint which allows movement in two planes instead of one. It allows the thumb to cross the palm of the hand. This joint allows biaxial movement. This allows movement in the frontal and sagittal planes.
There are six joints that have movement. The plvotal joint is what allows up and down movement.
The mid-ocean ridges are divergent plate boundaries-areas where earth's lithospheric plates are moving away from each other. This movement causes the crust to "thin out". The thinning allows the magma to come to the surface in the form of volcanoes. Mid-ocean ridge volcanism is just one part of the larger, all-encompassing, and evolving theory of plate tectonics. The production of lava and new crust at the mid-ocean ridges is largely a reaction to gravity induced subduction of oceanic crust at convergent plate boundaries. See related question below.
The mid-ocean ridges are divergent plate boundaries-areas where earth's lithospheric plates are moving away from each other. This movement causes the crust to "thin out". The thinning allows the magma to come to the surface in the form of volcanoes. Mid-ocean ridge volcanism is just one part of the larger, all-encompassing, and evolving theory of plate tectonics. The production of lava and new crust at the mid-ocean ridges is largely a reaction to gravity induced subduction of oceanic crust at convergent plate boundaries. See related question below.
The mid-ocean ridges are divergent plate boundaries-areas where earth's lithospheric plates are moving away from each other. This movement causes the crust to "thin out". The thinning allows the magma to come to the surface in the form of volcanoes. Mid-ocean ridge volcanism is just one part of the larger, all-encompassing, and evolving theory of plate tectonics. The production of lava and new crust at the mid-ocean ridges is largely a reaction to gravity induced subduction of oceanic crust at convergent plate boundaries. See related question below.