The Morley-Vine-Matthews hypothesis predicted that this phenomenon would result in symmetric  patterns in rocks at certain locations, providing the first strong support for this notion.
The Morley-Vine-Matthews hypothesis predicted that this phenomenon would result in symmetric  patterns in rocks at certain locations, providing the first strong support for this notion. These patterns record the reversals of the earth's magnetic field. First proposed by Harry Hess, it describes a process that can occur at a triple junction or a divergent boundary. FTP, identify this now widely- accepted theory that helps explain continental drift, a process in which new oceanic crust is formed at mid-ocean ridges.
The Morley-Vine-Matthews hypothesis predicted that this phenomenon would result in symmetric  patterns in rocks at certain locations, providing the first strong support for this notion.
seafloor spreading