Both continental and oceanic plates float on the top surface of the mantle, which is divided into convection cells. The movement of these convection cells drag the plates along: where convection causes the mantle material to fall the plates are pushed together and where convection causes the mantle material to rise the plates are pulled apart.
convergent boundary
Convection ridge push and slab pull work together to produce tectonic plate movement. Convection currents in the mantle create forces that push plates apart at mid-ocean ridges (ridge push), while the sinking of denser oceanic plates into the mantle at subduction zones generates a pulling force (slab pull). Together, these processes drive the dynamic movement of Earth's lithospheric plates, contributing to phenomena such as earthquakes, volcanic activity, and the formation of mountain ranges.
Slab-pull and ridge-push acting together
Mountain ranges formed by the pushing together of tectonic plates are called fold mountains. Examples include the Himalayas and the Alps, where the collision of plates has caused the Earth's crust to fold and create towering mountain peaks.
The movement of the Earth's tectonic plates is primarily caused by convection currents in the mantle, where hotter, less dense material rises while cooler, denser material sinks. This process creates forces that push and pull the plates in various directions. Additionally, slab pull and ridge push contribute to the movement, where descending oceanic plates pull on the rest of the plate and mid-ocean ridges push plates apart. Together, these mechanisms drive the dynamic activity of plate tectonics.
When tectonic plates push together, they converge, forming a convergent boundary.
when plates push together, it forms new land.
in
Compressed
convergent boundary
Volcanoes or sometimes earthquake!
yes it does
The plates push and pull and grind against each other they push together the force goes up and they form large mountains!
A deep ocean trench is likely to form where two oceanic plates push together in a convergent boundary. This is because one of the plates subducts beneath the other, creating a deep trench.
stromboli mountains
The differences are that when the earth's plates push together
the plates push together an to make mountins