When plates move together along a plate boundary, it is known as a convergent boundary. At convergent boundaries, one plate is typically forced beneath the other in a process called subduction, leading to the formation of mountain ranges, deep ocean trenches, and volcanic activity. These interactions are driven by the Earth's tectonic forces and can result in significant geological events such as earthquakes and tsunamis.
Plates move apart along divergent boundaries, where new crust is created through volcanic activity and magma upwelling from the mantle. This process is called seafloor spreading and occurs primarily in mid-ocean ridges.
When two plates move towards each other, it is called convergence. The motion during convergence is usually called subduction if one plate is forced beneath the other, or collision if the two plates collide and form mountain ranges.
When Earth's plates move together, it is called convergent boundary or a collision boundary. This movement can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity.
Fault lines are fractures in the Earth's crust where tectonic plates meet and slide past each other. At faults, tectonic plates can move in three ways: sliding horizontally past each other (transform motion), moving away from each other (divergent motion), or colliding and pushing together (convergent motion).
When two tectonic plates rub together, it can create friction and pressure that causes earthquakes. The plates can become stuck, building up energy until they suddenly release, resulting in seismic activity. The movement along the plate boundary can also result in the formation of mountain ranges or deep ocean trenches.
A convergent boundary is where plates move together.
Transform plates move sideways past each other in opposite directions along a fault line. They are neither moving together nor apart, but rather horizontally in opposite directions.
you get mountians
divergent boundary
convergent boundary
earthquakes
Subduction zone.
Volcanoes that form along a mid-ocean ridge are called volcanic islands. These volcanoes occur when the plates move apart to produce gaps which molten lava rises to fill.
2cm
they break
The plates come together
If plates move together they will make a montinous or a hill side area. If lava is flowing beneath it it can make a volcano and potentialy erupt.