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.
Midocean ridges are areas where continents broke apart. Midocean ridges are closest to the landmasses in younger oceans. One example where a midocean ridge intersected a landmass is the Arabian sea, which was formed by the pulling apart of the Arabian Peninsula and Africa.
parallel to and symmetric about ocean ridges
Mid-Ocean Ridges
Magnetic fields are recorded by rocks in strips parallel to ridges on Earth's surface. This phenomenon is known as magnetic striping, and it provides evidence of seafloor spreading and the movement of tectonic plates over time.
At transform faults or transform zones.
One of the midocean ridges is, but others are in other oceans, seas, and bays.
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.
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.
Older, as it moves away from the mid-ocean ridge the sediment gets thicker and older
(1)midocean spreading ridges, (2) subduction zones, and (3) transform faults.Normal fault, Reverse fault, and strike-slip fault
Magnetic stripes can be seen as you move away from ocean ridges.
Magnetic symmetry refers to the pattern of magnetic anomalies found on either side of mid-ocean ridges, where the Earth's magnetic field has reversed over geological time. As magma rises and solidifies at these ridges, it records the Earth's magnetic orientation, creating symmetrical patterns of magnetic stripes on the seafloor. This symmetry indicates that new oceanic crust is continuously being created and pushed outward, supporting the theory of seafloor spreading. The parallel arrangement of these magnetic anomalies on either side of the ridge provides evidence of the age and movement of tectonic plates.