By center slit I assume that you mean a mid ocean ridge which is a divergent boundary and the sea floor is very young there. Then be side slit I am assuming that you mean a trench which is a convergent boundary or subduction zone which would be the oldest part of the sea floor.
The ocean floor near the center slit typically shows deeper depths and a more pronounced trench-like formation compared to the ocean floor near the side slit. The center slit is often associated with tectonic plate boundaries, resulting in more significant geological activity and topographical features. In contrast, the side slit may exhibit a shallower gradient and less dramatic relief due to its location away from the main tectonic activity.
The movement of ocean floor on either side of a mid-ocean ridge is known as seafloor spreading. As new oceanic crust is formed at the ridge, it pushes the existing crust away from the ridge in opposite directions, creating a continuous process of plate tectonics.
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 floor the side the ball the pins
On each side of the mid-ocean ridge is a mirror of the striped pattern on the other side. When drawn, these patterns show alternating bands of normal and reverse polarity that match the geomagnetic reversal time scale, scientists can assign ages to the sea-floor rocks. The youngest rocks were at the center, and the older rocks father away. The ages of the sea floor rocks are symmetrical. The only place on the ocean-floor where new rocks are formed are at the rift in mid-ocean ridge. hope this helps :)
The polarities were mirror images on either side of the mid-ocean ridge.
Under the dash - center console. Remove the side cover on the center console on the passenger side and you will see it on the floor board.
On each side of the mid-ocean ridge is a mirror of the striped pattern on the other side. When drawn, these patterns show alternating bands of normal and reverse polarity that match the geomagnetic reversal time scale, scientists can assign ages to the sea-floor rocks. The youngest rocks were at the center, and the older rocks father away. The ages of the sea floor rocks are symmetrical. The only place on the ocean-floor where new rocks are formed are at the rift in mid-ocean ridge. hope this helps :)
Magnetic symmetry in rocks can provide evidence of sea-floor spreading by showing alternating patterns of magnetic polarity on either side of mid-ocean ridges. As new oceanic crust forms at the ridge and spreads outward, minerals in the crust record Earth's changing magnetic field. These symmetrical patterns of magnetic polarity across the ocean floor support the idea that the seafloor is spreading apart at these mid-ocean ridges.
mid-oceanic ridge. its where the plates are shifting away from eachother.
The rocks on either side of a mid-ocean ridge record the direction of the Earth's magnetic field at the time they were formed, and form a pattern of 'magnetic stripes' on either side of the ridge which are symmetrical. It is also now possible to measure ocean widths with sufficient accuracy to show yearly changes.
Submarine Canyons