the boundary is called a convergent boundary
A convergent boundary of two plates will push together. If it is two continental crusts, then they will both push upward, forming mountains. If it is a continental crust pushing against an oceanic crust, then the oceanic crust will go underneath, melt, and be recycled because the oceanic crust is less dense than the continental crust.
Convergent tectonic plates are plates that are moving toward each other.
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
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.
Continental boundary.
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.
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.
Convergence Boundary.
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.
Convergent boundary.
A convergent boundary of two plates will push together. If it is two continental crusts, then they will both push upward, forming mountains. If it is a continental crust pushing against an oceanic crust, then the oceanic crust will go underneath, melt, and be recycled because the oceanic crust is less dense than the continental crust.
Convergent tectonic plates are plates that are moving toward each other.
when tectonic plates move toward each othe forms
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.
is a boundary between two plates that are moving toward each other, or converging.