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.
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∙ 12y ago- Continental - Continental Collision
- Oceanic - Oceanic subduction
- Oceanic - Continental subduction
Oceanic-Oceanic, Oceanic-Continental, and Continental-Continental are all sub types of convergent plate boundaries.
The three types of plate boundaries are divergent, convergent, and transform boundaries. Divergent boundaries have normal faults, convergent boundaries have thrust faults, and transform boundaries have strike-slip faults.
The three main types of plate boundaries are convergent boundaries, where plates move toward each other, divergent boundaries, where plates move away from each other, and transform boundaries, where plates slide past each other horizontally.
The three types of faults are normal, reverse, and strike-slip faults. Normal faults are associated with divergent plate boundaries, reverse faults with convergent plate boundaries, and strike-slip faults with transform plate boundaries.
The three main types of plate boundaries are divergent boundaries (plates move apart), convergent boundaries (plates move toward each other), and transform boundaries (plates slide past each other horizontally). At divergent boundaries, new crust is formed as magma rises to the surface, while at convergent boundaries, crust is destroyed as one plate is subducted beneath another. Transform boundaries are characterized by earthquakes as the plates grind past each other.
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 three types of plate boundaries are : -convergent plate boundaries -divergent plate boundaries -transformed plate boundaries
Three types of plate boundaries are spreading boundaries, colliding boundaries, and sliding boundaries. um actually they are divergent, convergent, and transform
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the three types of plate boundaries are : -convergent plate boundaries -divergent plate boundaries -transformed plate boundaries
Oceanic-continental: Oceanic plate is subducted beneath continental plate, creating volcanic arcs and mountain ranges. Oceanic-oceanic: One oceanic plate is subducted beneath another, forming deep ocean trenches and volcanic island arcs. Continental-continental: Collision of two continental plates, leading to intense folding and faulting, creating high mountain ranges.
Three types of plate boundaries are spreading boundaries, colliding boundaries, and sliding boundaries. um actually they are divergent, convergent, and transform
divergent, conservative and convergent
The three types of boundaries in science are convergent boundaries (where two plates move towards each other), divergent boundaries (where two plates move away from each other), and transform boundaries (where two plates slide past each other horizontally). These boundaries are important in understanding processes like plate tectonics.
The main types of tectonic plate boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates move toward each other; and transform boundaries, where plates slide past each other horizontally.
The three types of convergent plate boundaries are oceanic-continental, oceanic-oceanic, and continental-continental boundaries. Oceanic-continental boundaries occur when an oceanic plate subducts beneath a continental plate. Oceanic-oceanic boundaries happen when one oceanic plate subducts beneath another oceanic plate. Continental-continental boundaries involve the collision of two continental plates.
The three types of plate boundaries are divergent boundaries, where plates move away from each other; convergent boundaries, where plates move towards each other; and transform boundaries, where plates slide past each other horizontally.