Yes, the sea floor near the mid-ocean ridge is young. As magma rises along the ridge, it solidifies to form new crust, creating a continuous process of crust formation and pushing older crust away from the ridge. This results in the oldest sea floor being farthest from the mid-ocean ridges.
Ocean floor is primarily created at mid-ocean ridges where tectonic plates move apart, allowing magma to rise from the mantle and solidify as new oceanic crust. This process, known as seafloor spreading, results in the formation of new crust that eventually spreads away from the ridge and contributes to the growth of the ocean floor.
an oceanic ridge
Sea-floor spreading occurs at mid-ocean ridges where tectonic plates move apart, allowing magma to rise from the mantle and solidify into new oceanic crust. Evidence for sea-floor spreading includes magnetic stripes on the ocean floor that show alternating patterns of normal and reversed polarity, matching ages of rocks on either side of mid-ocean ridges, and the presence of young volcanic activity along ridges.
Over a long period of time things can move suck as ROCK can move in the ocean from high and low tides, pressure, and waves only up to 3 ft....
fault line
The Young Ocean Floor is the part of the mantle showing between the 2 split tectonic plates.
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.
yes young rocks are found at mid ocean ridges not old rocks.
The youngest rocks on the ocean floor are typically found along mid-ocean ridges. These areas are where new oceanic crust is formed through volcanic activity and the process of seafloor spreading. As the magma cools and solidifies, it creates new rocks that are relatively young compared to rocks found in other parts of the ocean floor.
Mid-ocean ridges are basically underground volcanoes that lava from the Earth's Mantle can breach. The ocean, however, freezes the lava and that in turn forms rock. If this happens repeatedly, then the older rock gets pushed away from the source, and the younger, just formed rock is, therefore, closer to the ridge. So the younger rock being formed by the ridge is pushing away the older, previously made, igneous rock.
The age of rocks on the ocean floor increases with distance from the Mid-Atlantic ridge due to seafloor spreading. As new oceanic crust is formed at the ridge, older crust is pushed away from the ridge. This results in a pattern of young rocks near the ridge and progressively older rocks farther away.