It's formed in magma before it is oozed up through the ocean floor at the Mid-Atlantic Ridge. While it is still liquid, the iron molecules in the lava can orient themselves along the magnetic lines of force that envelope the earth.
Scientists found that the polarity of the magnetic bands on either side of mid-ocean ridges was symmetrical and mirrored each other. This pattern indicated periods of magnetic reversals, where Earth's magnetic field flipped, creating alternating stripes of normal and reversed polarity. This discovery supported the theory of seafloor spreading, demonstrating that new oceanic crust is formed at the ridges and gradually moves away, carrying the magnetic information with it.
These "stripes" formed the pattern known as magnetic striping. ... They hypothesized that the magnetic striping was produced from the generation of magma at mid-ocean ridges during alternating periods of normal and reversed magnetism by the magnetic reversals of the Earth's magnetic field.
revealed a symmetrical alternation of magnetic orientations on either side of mid-ocean ridges. This suggested that new oceanic crust was being formed at these ridges, with molten magma solidifying and locking in Earth's magnetic field at the time of its creation. By studying these patterns, scientists could map the history of seafloor spreading and plate tectonics.
Mid-Ocean Ridges
They technically don't. They do provide evidence for it, however, in that they occur in pairs on either side of a rift, providing strong evidence that the rocks on either side were deposited at the same time and that the rifts are spreading.
Scientists found that the polarity of the magnetic bands on either side of mid-ocean ridges was symmetrical and mirrored each other. This pattern indicated periods of magnetic reversals, where Earth's magnetic field flipped, creating alternating stripes of normal and reversed polarity. This discovery supported the theory of seafloor spreading, demonstrating that new oceanic crust is formed at the ridges and gradually moves away, carrying the magnetic information with it.
These "stripes" formed the pattern known as magnetic striping. ... They hypothesized that the magnetic striping was produced from the generation of magma at mid-ocean ridges during alternating periods of normal and reversed magnetism by the magnetic reversals of the Earth's magnetic field.
revealed a symmetrical alternation of magnetic orientations on either side of mid-ocean ridges. This suggested that new oceanic crust was being formed at these ridges, with molten magma solidifying and locking in Earth's magnetic field at the time of its creation. By studying these patterns, scientists could map the history of seafloor spreading and plate tectonics.
Mid-Ocean Ridges
True. Magnetic stripes on the ocean floor are created by alternating bands of magnetic polarities in the oceanic crust. These stripes are evidence of seafloor spreading where new crust is formed at mid-ocean ridges, pushing older crust away. Subduction zones are where older crust sinks back into the mantle.
Magnetic stripes can be seen as you move away from ocean ridges.
The pattern of magnetic reversals along the sides of mid-ocean ridges resembles stripes that alternate in polarity, created as new oceanic crust is formed at mid-ocean ridges and records the Earth's changing magnetic field. These magnetic stripes provide evidence for seafloor spreading and plate tectonics.
The primary evidence for seafloor spreading comes from magnetic striping patterns on the ocean floor. These patterns show alternating bands of normal and reversed polarity, indicating that new oceanic crust is being continuously formed at mid-ocean ridges and spreading away from the ridge axis.
Strips of ocean-floor basalt record the polarity of earth's magnetic field at the time the rock formed. These strips form a pattern that is the same on both sides of the mid-ocean ridge. the pattern shows that ocean floor forms along mid-ocean ridges and then moves away from the ridge.
iron bearing minerals can record Earth's magnetic field direction. when Earth's magnetic field reverses, newly formed iron bearing minerals will record the magnetic reversal. magnetic reversals show new rock being formed at mid-ocean ridges. This helped explain how the crust could move
mid ocean ridges
the wind ;)