The mid-ocean ridges are the buoyant, hot solidified magma that has formed from the decompressed, melting rock of the upper mantle where the oceanic plates are separating.
The Mid-Ocean Ridge is an oceanic mountain chain. Lava seeps out it producing new sea floor. This process is called sea floor spreading.
Ferrous deposits show magnetic banding that corresponds with the flipping of the earth's magnetic poles.
The ages of the rocks become older the farther the way they are from the ridges. The closer they are the younger it is. This leaves evidence to the seafloor spreading theory.
Seafloor spreading at midoceanic ridges.
Magnetic alignment of rocks, in alternating strips that run parallel to ridges, indicates reversals in Earth's magnetic field and provides further evidence of seafloor spreading.
The ages of the rocks become older the farther the way they are from the ridges. The closer they are the younger it is. This leaves evidence to the seafloor spreading theory.
The ages of the rocks become older the farther the way they are from the ridges. The closer they are the younger it is. This leaves evidence to the seafloor spreading theory.
mid-ocean ridges
Mid-oceanic ridges
Mid-Ocean ridges.
It is the mid-ocean ridges.
The magnetic properties of rocks along the mid-oceanic ridges change alignment in a symmetrical manner.
The seafloor rocks vary in different places. Rock samples near ocean ridges are younger than rocks at deep sea trenches
The typical rates of seafloor spreading is 5 centimeters per year. Seafloor spreading is a process that occurs at mid ocean ridges.