These stripes often called zebra stripes, due to the alternating colors of the original magnetometer readings. When the first observations were made, it is directly related to two processes geomagnetic reversals and seafloor spreading.
Symmetrical magnetic patterns in seafloor basalts are formed due to the reversal of Earth's magnetic field over time. As magma solidifies and forms new oceanic crust at a mid-ocean ridge, it locks in the prevailing magnetic orientation. As the crust moves away from the ridge through seafloor spreading, these magnetic patterns create a mirror image on either side of the ridge, providing evidence for the process of seafloor spreading.
As you move away from an ocean ridge, the rocks get older.
A mid-ocean ridge would have magnetic striping on the seafloor. This striping is caused by the alternating polarities of Earth's magnetic field recorded in the basaltic rocks as they cool and solidify at the mid-ocean ridge, providing evidence for seafloor spreading.
They appear to be similar in width because new crust formation is nearly equal on each side of the fault.
Oceanic crust records polarity through the alignment and orientation of magnetic minerals within the rock as it solidifies near mid-ocean ridges. These minerals become magnetized parallel to Earth's magnetic field at the time of their formation and preserve this polarity orientation as the crust moves away from the ridge. By analyzing the magnetic stripes on the ocean floor, scientists can determine the history of magnetic reversals and the movement of tectonic plates.
Mid-Ocean Ridges
The magnetic strips on the sea floor are parallel to the mid-ocean ridge because new oceanic crust is constantly being formed at the ridge due to volcanic activity. As the magma cools and solidifies, it records the Earth's magnetic field orientation at the time. This creates a symmetrical pattern of magnetic strips on either side of the ridge as the Earth's magnetic field reverses over time.
That magnetic minerals spreading from a mid-ocean ridge
That magnetic minerals spreading from a mid-ocean ridge
That magnetic minerals spreading from a mid-ocean ridge
alternating
Linear, magnetic patterns associated with mid-ocean ridges are configured as normal and reversed magnetized strips roughly parallel to the ridge. A very long lived magma source located deep in the mantle is called a hot spot.
Symmetrical magnetic patterns in seafloor basalts are formed due to the reversal of Earth's magnetic field over time. As magma solidifies and forms new oceanic crust at a mid-ocean ridge, it locks in the prevailing magnetic orientation. As the crust moves away from the ridge through seafloor spreading, these magnetic patterns create a mirror image on either side of the ridge, providing evidence for the process of seafloor spreading.
As you move away from an ocean ridge, the rocks get older.
Records of magnetic reversals preserved in rocks on either side of a mid-ocean ridge show parallel patterns of stripes that mirror each other. These stripes indicate that new oceanic crust is continuously forming at mid-ocean ridges and moving away from the ridge as plates separate. The symmetrical pattern of magnetic stripe anomalies provides evidence for seafloor spreading and plate tectonics.
its the same on either side of the mid-ocean ridge
the matching patterns on either side of the mid-ocean ridge could be explained by new ocean crust forming at the ridge and spreading away from it as ocean crust forms it obtains the polarity of the earth's magnetic field at that time over time the strength of the earths magnetic field changes when new ocean crust forms at the center of the spreading it obtains a new kind of magnetic polarity over time a series of magnetic ''stripes'' are formed