It spreads away form the ridges
Yes, the process that creates oceanic crust on a mid-ocean ridge is called "seafloor spreading". seafloor spreading creates a new oceanic crust that forms on the mid-ocean ridge.
The Mid-Atlantic Ridge has one of the slowest rates of seafloor spreading, averaging about 2.5 cm per year. This ridge is located in the Atlantic Ocean and is less active compared to other spreading ridges like the East Pacific Rise.
The Mid Atlantic Ridge
rift valley
Vine and Matthews
Lawrence W. Morley, Frederick John Vine, and Drummond Hoyle Matthews were the first to tie magnetic stripe anomalies to seafloor spreading. The magnetic anomalies was the first evidence that supported the theory of seafloor spreading.
The evidence that seafloor rocks farther from the mid-ocean ridge are older than those closer to it supports the idea of seafloor spreading by demonstrating that new oceanic crust is created at the ridge and gradually moves outward. As magma rises and solidifies at the ridge, it forms new rock, which pushes the existing rocks away from the ridge over time. This pattern of age distribution aligns with the theory that the ocean floor is continuously being formed and expanded, confirming the dynamic nature of plate tectonics and seafloor spreading.
At any divergent plate margin: The Mid-Atlantic Ridge The boundary between the African Plate and Arabian Plate (the Red Sea) Great Rift Valley West Antarctic Rift East Pacific Rise Pacific-Antarctic Ridge Galapagos Rise Gakkel Ridge
One example would be...the mid-atlantic ridge.
One example would be...the mid-atlantic ridge.
Yes, the process that creates oceanic crust on a mid-ocean ridge is called "seafloor spreading". seafloor spreading creates a new oceanic crust that forms on the mid-ocean ridge.
Seafloor spreading is a process that occurs at mid-ocean ridges, where new oceanic crust is formed through volcanic activity and then gradually moves away from the ridge. Seafloor spreading helps explain continental drift in the theory of plate tectonics.