When two plates move toward each other, they create a convergent boundary. At convergent boundaries, one plate is forced beneath the other in a process known as subduction. This collision can lead to the formation of mountain ranges, deep sea trenches, and volcanic activity.
The force that pulls tectonic plates toward each other is known as "slab pull." This occurs when a dense oceanic plate descends into the mantle at a subduction zone, generating a gravitational force that pulls the rest of the plate along with it.
When two tectonic plates slide past each other, it can result in horizontal movement along a fault line, causing earthquakes. This is known as a transform boundary. The friction between the plates can build up tension, which is released suddenly in the form of seismic waves.
The beam of alpha particles is deflected toward the negatively charged plate. This is because alpha particles are positively charged, and opposite charges attract each other.
gravity is a force that pulls object toward each other
The attraction between any two objects is called gravity. It is a force that pulls objects toward each other based on their mass and distance.
A convergent boundary occurs when two plates move toward each other. This movement can result in subduction, where one plate is forced beneath the other, or it can create mountain ranges and volcanic activity.
seafloor spreading occurs when oceans widen and continents separate.convergent plate movements occurs when two plates collide toward each other.divergent plate movement is the moving away of plates from each other.transform plate movement occurs when two plates are sliding horizontally with each other.:)
seafloor spreading occurs when oceans widen and continents separate.convergent plate movements occurs when two plates collide toward each other.divergent plate movement is the moving away of plates from each other.transform plate movement occurs when two plates are sliding horizontally with each other.:)
The force that pulls tectonic plates toward each other is known as "slab pull." This occurs when a dense oceanic plate descends into the mantle at a subduction zone, generating a gravitational force that pulls the rest of the plate along with it.
convergant plate boundries
When 2 oceanic plates and 2 continental plates move towards each other, subduction occurs. The denser oceanic plate sinks beneath the less dense continental plate, creating deep ocean trenches and volcanic arcs. This process can lead to the formation of mountain ranges and earthquakes.
When tintanic plates obstruct with each other
all volcanoes are caused by the earths plates moving toward each other and that is called convergent boundaries.
When crustal plates move toward each other, they can form convergent boundaries where one plate is forced beneath the other in a process called subduction. This can result in the formation of mountain ranges, deep ocean trenches, and volcanic activity in the area.
They are the contact points between plates that are moving toward each other.
Convergence Boundary.
When plates slide past each other, move toward each other, and move away from each other.