Seafloor spreading occurs at which type s of plate boundary.
Sea floor spreading occurs when.
The process by which the ocean floor sinks into the mantle.
A deep ocean trench is an underwater.
Seafloor spreading occurs at divergent plate boundaries.
Eventually the crust cracks.
Down the middle of underwater mountain ranges is a device that scientist use to map the ocean floor.
Molten material erups the central valley of mid ocean ridges.
The less dense material rises often forming a mountain or elevated area of the seafloor.
As tectonic plates slowly move away from each other heat from the mantle s convection currents makes the crust more plastic and less dense.
This idea played a pivotal role in the development of the theory of plate tectonics which revolutionized geologic thought during the last quarter of the 20th century.
A canyon on the ocean floor where the crust bends downward.
Seafloor spreading is a geologic process where there is a gradual addition of new oceanic crust in the ocean floor through a volcanic activity while moving the older rocks away from the mid oceanic ridge.
Spreading centers end in transform faults or in overlapping spreading center offsets.
The mid ocean ridge is where the seafloor spreading occurs in which tectonic plates large slabs of earth s lithosphere split apart from each other.
Where does sea floor spreading occur.
Seafloor spreading is credited for the formation of the red sea as a result of the movement of the arabian and african tectonic plates away from each other.
A chain of underwater mountains along which seafloor spreading occurs.
Seafloor spreading is a geological process which involves the splitting of tectonic plates and their movement away from each other.