According to www.geology.com: the Mid-Atlantic Ridge at Iceland, East Africa, and the Red Sea.
RE:
HEY.
I ASKED THE QUESTION> anyway. thanks for looking it up for me
luv you babe
lol
your are a sweetie.
=)
Oceanic-continental convergence: Oceanic plates sink beneath continental plates, creating subduction zones and mountain ranges. Oceanic-oceanic convergence: When two oceanic plates collide, one plate is subducted beneath the other, leading to trench formation and volcanic island arcs. Continental-continental convergence: Two continental plates collide, resulting in the uplift of crust and the formation of mountain ranges.
The mechanism responsible for producing new oceanic crust between two diverging plates is seafloor spreading. Magma rises up from the mantle at mid-ocean ridges, solidifies upon reaching the seafloor, and forms new crust. As the plates move apart, this process continuously adds new material to the ocean floor.
Divergent plates are tectonic plates that are moving away from each other. As they move apart, magma rises from the mantle and creates new crust at the mid-ocean ridges. This process is responsible for seafloor spreading and the formation of new oceanic crust.
The mechanism responsible for producing new seafloor between two diverging plates is seafloor spreading. Magma rises from the mantle to fill the gap created by the plates moving apart, solidifies upon contact with seawater, and forms new oceanic crust. This process results in the continuous growth of the ocean floor.
oceanic convergence is when two oceanic plates subduct beneath one another.
Diverging Plate Boundary
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.
Oceanic-continental convergence: Oceanic plates sink beneath continental plates, creating subduction zones and mountain ranges. Oceanic-oceanic convergence: When two oceanic plates collide, one plate is subducted beneath the other, leading to trench formation and volcanic island arcs. Continental-continental convergence: Two continental plates collide, resulting in the uplift of crust and the formation of mountain ranges.
The mechanism responsible for producing new oceanic crust between two diverging plates is seafloor spreading. Magma rises up from the mantle at mid-ocean ridges, solidifies upon reaching the seafloor, and forms new crust. As the plates move apart, this process continuously adds new material to the ocean floor.
Divergent plates are tectonic plates that are moving away from each other. As they move apart, magma rises from the mantle and creates new crust at the mid-ocean ridges. This process is responsible for seafloor spreading and the formation of new oceanic crust.
The mechanism responsible for producing new seafloor between two diverging plates is seafloor spreading. Magma rises from the mantle to fill the gap created by the plates moving apart, solidifies upon contact with seawater, and forms new oceanic crust. This process results in the continuous growth of the ocean floor.
The two types of tectonic plates are continental and oceanic.
oceanic convergence is when two oceanic plates subduct beneath one another.
in ghfh fgh in ghfh fgh
Oceanic plates are denser and thinner, found beneath the oceans, while continental plates are thicker and less dense, making up the Earth's landmasses. These two types of tectonic plates interact at boundaries, influencing processes like earthquakes and volcanic eruptions.
oceanic convergence is when two oceanic plates subduct beneath one another.
oceanic convergence is when two oceanic plates subduct beneath one another.