"Stripes" of alternating magnetic field in the basalt rock of the seafloor.
it tugs on the iron pieces in the sand causing ripples.
As mid ocean ridges create new seafloor over extended periods of time, the magnetic poles of the Earth reverse back and forth. The rocks on either side of a mid ocean ridge show the opposite magnetisms and appear striped. From knowing the approximate ages of these magnetic reversals, one can estimate the approximate age of each stripe.
rocks get older as you move away from ocean ridges
diatom shells settle on the ocean floor from the surface
as it spread away from a mid-ocean ridge, the sea floor carries with it a record or magnetic reversals. i hope this answer would be correct :) also, when the magma rises through fractures in the sea floor at the mid-ocean ridge, the magma cools and forms new rocks. this new rock takes place of the old rock and the old rock gets pulled away.
it tugs on the iron pieces in the sand causing ripples.
it tugs on the iron pieces in the sand causing ripples.
it tugs on the iron pieces in the sand causing ripples.
Caused by changes in earth's magnetic field over time, especially reversals of the magnetic poles.
Caused by changes in earth's magnetic field over time, especially reversals of the magnetic poles.
Caused by changes in earth's magnetic field over time, especially reversals of the magnetic poles.
The direction of the Earth's magnetic field has reversed several times during its history. This causes the North magnetic pole to become a South magnetic pole and vice versa. We know this because of the direction of magnetism in the rocks on the ocean floor, which alternates in 'stripes' on either side of the mid-ocean ridges.
A long time since my degree but I believe the orientation of minerals in the rocks either side of the mid ocean ridge, which regularly invert due to polar reversals, are mirrored confirming that the ridge is opening / the sea floor is spreading.
as it spread away from a mid-ocean ridge, the sea floor carries with it a record or magnetic reversals. i hope this answer would be correct :) also, when the magma rises through fractures in the sea floor at the mid-ocean ridge, the magma cools and forms new rocks. this new rock takes place of the old rock and the old rock gets pulled away.
The Earth's magnetic reversals have been recorded in newly forming oceanic seafloor basalt by the orientation of magnetic minerals which become frozen in place as the magma hardens. When the next reversal occurs, it as well becomes part of the ocean floor magnetic record.
I'm assuming you're talking about the ocean floor itself (the earth's crust). The youngestmaterialat the bottom of the ocean is at the riffs between two plates. The mid-Atlantic riff is a good example.
It would indicate that the length of time between reversals is not predictable.