1) seafloor spreading
2) continental drift
3 i only found 2
Scientists prove seafloor spreading through various methods, including mapping of magnetic stripes on the ocean floor, analysis of seismic activity, and examination of rock samples collected from the ocean crust. These techniques provide evidence of tectonic plate movement and the creation of new oceanic crust at mid-ocean ridges.
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Earthquake patterns were used to provide evidence of seafloor spreading through the discovery of mid-ocean ridges. Scientists observed that earthquakes were concentrated along these ridges, indicating the presence of tectonic activity associated with the movement of tectonic plates. This supported the theory of seafloor spreading, where new oceanic crust is formed at mid-ocean ridges and pushes older crust away from the ridge.
DURR
Scientists found evidence of magnetic stripes on the ocean floor, which indicated periodic reversals in Earth's magnetic field. This discovery helped support the theory of plate tectonics and seafloor spreading.
Magnetic minerals on the ocean floor.
Animal fossils have been found in many places in the ocean.
Scientists have gathered evidence for plate spreading at mid-ocean ridges through various methods. One key piece of evidence is the measurement of magnetic striping on the ocean floor, where symmetrical patterns of magnetic minerals record the Earth's magnetic reversals as new crust forms and pushes older crust away. Additionally, seismic data and direct measurements of seafloor spreading rates using GPS technology confirm that the plates are indeed moving apart. Oceanic rock samples from the ridge also show that younger rocks are found closer to the ridge, supporting the idea of new material being created there.
Convergence supports the theory of seafloor spreading. Samples of the deep ocean floor are evidence of seafloor spreading because the basaltic oceanic crust and overlapping sediment become younger as the mid-ocean ridge is approached. Also, the rock that makes up the floor of the ocean is younger than the continents.
Convergence supports the theory of seafloor spreading. Samples of the deep ocean floor are evidence of seafloor spreading because the basaltic oceanic crust and overlapping sediment become younger as the mid-ocean ridge is approached. Also, the rock that makes up the floor of the ocean is younger than the continents.
Yes, there is evidence supporting seafloor spreading, including magnetic striping patterns on the ocean floor, the age progression of seafloor away from mid-ocean ridges, and the presence of hydrothermal vents along mid-ocean ridges that release magma from the Earth's mantle.
by the plate tectonic and the ocean bridges