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Continental-continental, continental-oceanic and oceanic- oceanic convergent boundaries.
Oceanic-Oceanic, Oceanic-Continental, and Continental-Continental are all sub types of convergent plate boundaries.
if i thing if gago abno yudipota ka
There are three primary types of tectonic plate boundaries. They pertain of Divergent boundaries, Convergent boundaries and Transform-fault boundaries.
The three types of convergent boundaries are when two plates meet and two oceanic plate meet, or where an oceanic and continental plate meet.the three types of convergent boundaries are continent boundaries , continent - ocean boundaries, and last but not least............. ocean boundaries
divergent plate boundary- a boundary where two plates move apart from each other. convergent plate boundary- a boundary where two plates move towards each other so that one plate can sink beneath the other. transform plate boundary- a boundary where one plate slips along side another plate.
Convergent (or destructive): Where two plates are moving toward each other. Collisions between oceanic plates results in subduction of the more dense plate. Collisions between an oceanic plate and a continental plate may result in the subduction of the oceanic plate because oceanic plates are more dense than continental plates. Collisions between two continental plates results in uplift and mountain formation where neither plate subducts.Divergent (or constructive): Where two plates are moving away from each other. Divergent plate boundaries are the site of new crust formation, particularly at the mid-ocean ridges, where spreading plates are infilled with basaltic magma from the asthenosphere.Transform (or conservative): Where two plates slide (actually 'grind') alongside each other and neither plate subducts. Earthquakes are common at transform faults due to the grinding and snapping movements of the plates as they move.
The three types of boundaries are Convergent Boundary, Divergent Boundary, and Transform Boundary.......
the three types of plate boundaries are : -convergent plate boundaries -divergent plate boundaries -transformed plate boundaries
the three types of plate boundaries are : -convergent plate boundaries -divergent plate boundaries -transformed plate boundaries
The three types of convergent boundaries are when two plates meet and two oceanic plate meet, or where an oceanic and continental plate meet.the three types of convergent boundaries are continent boundaries , continent - ocean boundaries, and last but not least............. ocean boundaries
Three types of plate boundaries are spreading boundaries, colliding boundaries, and sliding boundaries. um actually they are divergent, convergent, and transform
The three types of convergent plate boundaries are Oceanic-Oceanic, Continental-Continental, Continental-Oceanic.
Plate boundaries are places where two tectonic plates meet. There are three major types of plate boundaries. These are divergent, convergent, and transform plate boundaries.
There are three primary types of tectonic plate boundaries. They pertain of Divergent boundaries, Convergent boundaries and Transform-fault boundaries.
Three types of plate boundaries are spreading boundaries, colliding boundaries, and sliding boundaries. um actually they are divergent, convergent, and transform
The three types of convergent boundaries are when two plates meet and two oceanic plate meet, or where an oceanic and continental plate meet.the three types of convergent boundaries are continent boundaries , continent - ocean boundaries, and last but not least............. ocean boundaries
The four types of plate boundaries are divergent boundaries (plates moving apart), convergent boundaries (plates moving together), transform boundaries (plates sliding past each other), and subduction zones (one plate sinking beneath another).
the three types of plate boundaries are : -convergent plate boundaries -divergent plate boundaries -transformed plate boundaries
Oceanic-Oceanic, Oceanic-Continental, and Continental-Continental are all sub types of convergent plate boundaries.