the boundary is called a convergent boundary
It is called a convergent boundary and can often result in a chain of mountains. When two plates converge, it is common for the denser plate to sink underneath the other. This process is called subduction.
Most volcanoes on land are caused by the Earth's plates moving toward each other, a process known as convergent plate boundary. When two plates converge, the denser oceanic plate subducts beneath the less dense continental plate, leading to the formation of volcanoes along the subduction zone.
Divergent Plate Boundary: The area where two plates are moving in relatively opposite directions and new crustal material is being created by rising decompressed mantle rock. Examples would be the mid-ocean ridges, and the East African Rift. Convergent Plate Boundary: The area where two tectonic plates are moving toward each other and one of two things happens; either the more dense plate subducts under the lighter plate and heads toward the mantle, or, if the plates are of similar density, they cause uplift and mountain forming events. Examples would be the oceanic to continental crustal collision creating the Andes Mountains, and the continental to continental crustal collision creating the Himalayan Mountains. Transform Plate Boundary: The area where two plates are grinding past each other, snapping into place from elastic rebound as they go, causing numerous earthquakes. The San Andreas Fault is an example of a transform plate boundary between the North American and Pacific plates.
A conversion boundary is a place where 2 tectonic plates are mving toward each other. There are 3 types of convergent boundaries OCEANIC CRUST-OCEANIC CRUST OCEANIC CRUST-CONTINENTAL CRUST CONTINENTAL CRUST-CONTINENTAL CRUST They are classified according to their crust
Convergent plates are two tectonic plates that are colliding as they move toward each other. There are several types of converging plate boundaries.Oceanic to oceanic plate convergence:Where an oceanic plate collides with another oceanic plate, the more dense plate subducts into the mantle. The subduction results in the partial melting of lithospheric rock above the area of the subduction, causing underwater volcanoes to form. If the volcanoes grow to reach the surface, volcanic arc islands are formed.Oceanic to continental plate convergence:Where an oceanic plate collides with a continental plate, the oceanic plate is subducted due to the fact that it is more dense, which can also cause volcanism and mountain building.Continental to continental plate convergence:Where two continental plates collide, neither subducts into the mantle, the crust is thickened, and mountain ranges are formed from the thickening and uplift.
This is called a convergent boundary. A divergent boundary is when plate move away from each other, and a transform boundary is when plates slide past each other.
When tectonic plates move toward each other, it is known as a convergent boundary. This movement can result in subduction, where one plate is forced beneath the other, or in the collision of two plates, leading to the formation of mountain ranges.
Convergence Boundary.
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.
At a convergent boundary two plates move toward each other. At a transform boundary plates slide past each other.
Convergent boundaries , where two plates are moving toward each other, are of three types, depending on the type of crust present on either side of the boundary — oceanic or continental . The types are ocean-ocean, ocean-continent, and continent-continent.
It is called a convergent boundary and can often result in a chain of mountains. When two plates converge, it is common for the denser plate to sink underneath the other. This process is called subduction.
Convergent boundary.
Most volcanoes on land are caused by the Earth's plates moving toward each other, a process known as convergent plate boundary. When two plates converge, the denser oceanic plate subducts beneath the less dense continental plate, leading to the formation of volcanoes along the subduction zone.
Divergent Plate Boundary: The area where two plates are moving in relatively opposite directions and new crustal material is being created by rising decompressed mantle rock. Examples would be the mid-ocean ridges, and the East African Rift. Convergent Plate Boundary: The area where two tectonic plates are moving toward each other and one of two things happens; either the more dense plate subducts under the lighter plate and heads toward the mantle, or, if the plates are of similar density, they cause uplift and mountain forming events. Examples would be the oceanic to continental crustal collision creating the Andes Mountains, and the continental to continental crustal collision creating the Himalayan Mountains. Transform Plate Boundary: The area where two plates are grinding past each other, snapping into place from elastic rebound as they go, causing numerous earthquakes. The San Andreas Fault is an example of a transform plate boundary between the North American and Pacific plates.
When two neighboring plates move toward each other, it is called a convergent boundary. This type of plate boundary can lead to the formation of mountain ranges, volcanic arcs, and deep ocean trenches as one plate is forced beneath the other in a process known as subduction.
A conversion boundary is a place where 2 tectonic plates are mving toward each other. There are 3 types of convergent boundaries OCEANIC CRUST-OCEANIC CRUST OCEANIC CRUST-CONTINENTAL CRUST CONTINENTAL CRUST-CONTINENTAL CRUST They are classified according to their crust