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molten material, magnetic stripes, and the ages of the rock.
It helps them determine the frequency of shifts in the magnetic orientation of the Earth, and initially led to the confirmation of seafloor spreading at the mid-ocean ridges.
They proved that the seafloor was spreading.
Magnetic reversals and sea floor spreading.
Magnetic Reversal
Vine and Matthews
Lawrence W. Morley, Frederick John Vine, and Drummond Hoyle Matthews were the first to tie magnetic stripe anomalies to seafloor spreading. The magnetic anomalies was the first evidence that supported the theory of seafloor spreading.
The magnetic properties of rocks along the mid-oceanic ridges change alignment in a symmetrical manner.
Scientists indicated that the seafloor was spreading, so the poles "reverse"
Scientists indicated that the seafloor was spreading, so the poles "reverse"
molten material, magnetic stripes, and the ages of the rock.
Scientists found Alternating bands of magnetism.
It helps them determine the frequency of shifts in the magnetic orientation of the Earth, and initially led to the confirmation of seafloor spreading at the mid-ocean ridges.
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
They proved that the seafloor was spreading.