Sea floor spreading 2 oceanic plates coming apart
The Mid-Atlantic Ridge is a spreading center located in the middle of the Atlantic Ocean.
sea floor-spreading..;)
Consider. In sea-floor spreading, the plates are spreading apart; in other words diverging. So sea-floor spreading occurs at a divergent boundary,
Spreading center earthquakes are always shallow, subduction zone earthquakes can be very deep.Spreading center earthquakes are typically of lower magnitude than subduction zone earthquakes.
divergent plate boundary
Volcanoes at spreading centers is referred to as spreading center volcanism. This usually takes place on mid-oceanic ridges where the plates diverge.
As you travel from a spreading center towards a coastline, the age of the sea floor rocks increases. Newly formed rocks at the spreading center are younger, while older rocks are found further away from the center, as they have been pushed away over time by the continuous process of seafloor spreading. This results in a pattern where the youngest rocks are closest to the ridge, and the oldest are nearer to the continental margins.
It is a center at the bottom of the ocean that occurs at mid-ocean ridges
It is a center at the bottom of the ocean that occurs at mid-ocean ridges
The center of a ripple is called the focal point. This is where the disturbance that creates the ripple originates, spreading outwards in concentric circles.
some can see how its spreading because no one knows
It is important for the model to have identical patterns of stripes on both sides of the center slit because it demonstrates that new crust is being formed at the center of the ridge and spreading out equally in opposite directions. This helps support the theory of plate tectonics and the process of sea floor spreading. If the stripes were not symmetrical, it would suggest irregularities in the process and raise questions about the validity of the model.