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Not really but sea floor sediments thickness increase with increased distance from spreading centers which is good evidence. Other evidence such as magnetic reversals, temperature, dating methods provide the best evidence of seafloor spreading
seafloor spreading
evidence from molten material evidence from magnetic stripes evidence from drilling samples
The Mid Atlantic Ridge
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.
Not really but sea floor sediments thickness increase with increased distance from spreading centers which is good evidence. Other evidence such as magnetic reversals, temperature, dating methods provide the best evidence of seafloor spreading
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The seafloor rocks vary in different places. Rock samples near ocean ridges are younger than rocks at deep sea trenches
seafloor spreading
Rocks in the seafloor are moving one place to another
because that there are younger rocks found at ocean ridges than the ones found near deep-sea trenches
The ages of the rocks become older the farther the way they are from the ridges. The closer they are the younger it is. This leaves evidence to the seafloor spreading theory.
seafloor spreading
evidence from molten material evidence from magnetic stripes evidence from drilling samples
pole reversals seafloor spreading
The Mid Atlantic Ridge
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.