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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.
Seafloor Spreading
Seafloor spreading at midoceanic ridges.
They proved that the seafloor was spreading.
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.
seafloor spreading
Vine and Matthews
rising molten magma
Tectonic.
Oceanic crust on both sides ofthe ridge shows matching patterns of reversed and normal magnetic polarity
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.
Scientists date sea-floor rocks by looking at patterns in the rocks, including magnetic patterns, and by looking at the geomagnetic reversal time scale.
Geothermal Drift.
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.
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The tide
the primary force that causes the seaffloor to spread and contienents to drift