Sea floor spreading: Flat spaces are formed in the opposite direction of two plates on the divergent edges. In these empty spaces, the magma rises above the convection function and the lava gets deposited above, which creates new styles.
The continuation of this process keeps the order of forming the new shell crust. As a result, the ocean bottom is expanding. Like lava on both sides of the mid – Atlantic ridge is creating new scarf, which is spreading the Atlantic Ocean. With the expansion of the ocean bottom, the concept of the continent and ocean mobility is also proved.
