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Its when the oceanic crust and the continental crsut colide together.
when 2 oceanic plates move toward(converge)each other they form a lain of VOLCANIC ISLAND ARC.when 2 continenatl plates move toward(converge)each other they form MOUNTAIN BUILDING.
Plates that move toasted each other are detractive plates meeting at a destructive margin. If a continental and an oceanic plate move towards each other, earthquakes and volcanoes occur, this is called a subduction margin, but if the plates are both continental then fold mountains form this is a collision margin
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
The 3 general types are constructive, destructive, and conservative boundaries. Constructive (divergent) - plates move away from each other, typically creating a rift Destructive (convergent) - one plate will be subducted, or continental plates collide Conservative (transform) - plates grind past each other, stalling and slipping
A destructive margin is when the oceanic crust moves towards the continental crust and slip under it (oceanic crust is heavier than the continental crust). This can build up a lot of pressure between the plates.
Its when the oceanic crust and the continental crsut colide together.
when 2 oceanic plates move toward(converge)each other they form a lain of VOLCANIC ISLAND ARC.when 2 continenatl plates move toward(converge)each other they form MOUNTAIN BUILDING.
Plates that move toasted each other are detractive plates meeting at a destructive margin. If a continental and an oceanic plate move towards each other, earthquakes and volcanoes occur, this is called a subduction margin, but if the plates are both continental then fold mountains form this is a collision margin
Oceanic plates are primarily made up of basaltic rock while continental plates are primarily made of granitic rock. Basalt is denser than granite which allows oceanic plates to subduct beneath continental plates.
Plates that move toasted each other are detractive plates meeting at a destructive margin. If a continental and an oceanic plate move towards each other, earthquakes and volcanoes occur, this is called a subduction margin, but if the plates are both continental then fold mountains form this is a collision margin
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
The 3 general types are constructive, destructive, and conservative boundaries. Constructive (divergent) - plates move away from each other, typically creating a rift Destructive (convergent) - one plate will be subducted, or continental plates collide Conservative (transform) - plates grind past each other, stalling and slipping
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.
Converging (destructive) plate boundary: where two plates collide. Diverging (constructive) plate boundary: where two plates move away from each other. Transform plate boundary: where two plates move, or grind, past each other. Like the boundary in California.
Converging (destructive) plate boundary: where two plates collide. Diverging (constructive) plate boundary: where two plates move away from each other. Transform plate boundary: where two plates move, or grind, past each other. Like the boundary in California.
When it is two continental plates, new oceanic crust is formed, and when this continues, more oceanic crust is formed between the plates.