Gravity
Magnetic stripes can be seen as you move away from ocean ridges.
The type of faulting that characterizes mid-ocean ridges is a transform fault. This type of faulting occurs because transform fault ridges stay in the same fixed location, thus the new ocean sea floor being created at the ridges is pushed away from the ridge.
Harry hess' hypothesis was hot/less dense material rises up the Earth's crust toward the mid-ocean ridges. When the seafloor breaks apart, magma is forced upward and through the cracks. It cools, and becomes a new seafloor. When it moves away from the mid-ocean ridge, it becomes denser and sinks. This helps form ridges.
divergent
away, rifts
Gravity
Magnetic stripes can be seen as you move away from ocean ridges.
The mid-ocean ridges which wrap around the ocean floor like the seam of a baseball, are high topographic features-but as you go away from either side of a ridge, the ocean floor subsides as it cools.
The type of faulting that characterizes mid-ocean ridges is a transform fault. This type of faulting occurs because transform fault ridges stay in the same fixed location, thus the new ocean sea floor being created at the ridges is pushed away from the ridge.
Sorry for this late response,but basically, as the plates move farther away from the mid-ocean ridges, the older it gets..! Hope this helps! ^^
Older, as it moves away from the mid-ocean ridge the sediment gets thicker and older
It spreads away form the ridges
Mid-ocean ridges and seafloor spreading are characteristics of oceanic diverging plates, plates that are moving away from each other.
Harry hess' hypothesis was hot/less dense material rises up the Earth's crust toward the mid-ocean ridges. When the seafloor breaks apart, magma is forced upward and through the cracks. It cools, and becomes a new seafloor. When it moves away from the mid-ocean ridge, it becomes denser and sinks. This helps form ridges.
mid-ocean ridges and volcanoes
gravity
Harry hess' hypothesis was hot/less dense material rises up the Earth's crust toward the mid-ocean ridges. When the seafloor breaks apart, magma is forced upward and through the cracks. It cools, and becomes a new seafloor. When it moves away from the mid-ocean ridge, it becomes denser and sinks. This helps form ridges.