It is Satelite so it sees when it moves and how fast it moves
Seismic studies show evidence of mid-ocean ridges where new oceanic crust is forming, supporting the theory of seafloor spreading. By analyzing seismic waves, scientists can map the structure of the ocean floor and identify areas of tectonic activity where plates are moving apart. Additionally, seismic data reveals the presence of magnetic striping on the seafloor, further supporting the idea of seafloor spreading.
It just did, you could see it
Like a polyghraph squiggles show the techtonic plates moving.
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.
The age of the sea floor provides evidence for tectonic plate movement through the process of seafloor spreading. As magma rises at mid-ocean ridges, it cools and solidifies to form new oceanic crust, which is youngest at the ridge and gets progressively older as you move away. By dating the rock samples, scientists can map the age of the sea floor and observe how older crust is pushed away from the ridge, demonstrating the movement of tectonic plates. This pattern supports the theory of plate tectonics, illustrating how plates diverge, converge, and interact over geological time.
Seismic studies show evidence of mid-ocean ridges where new oceanic crust is forming, supporting the theory of seafloor spreading. By analyzing seismic waves, scientists can map the structure of the ocean floor and identify areas of tectonic activity where plates are moving apart. Additionally, seismic data reveals the presence of magnetic striping on the seafloor, further supporting the idea of seafloor spreading.
It just did, you could see it
The mid-ocean ridges are the buoyant, hot solidified magma that has formed from the decompressed, melting rock of the upper mantle where the oceanic plates are separating.
example of these is the plates are moving in different ways and when it move the earthquake will occur
Earthquake patterns along mid-ocean ridges show a linear distribution parallel to the ridge axis, indicating that earthquakes occur as the seafloor spreads apart. The earthquakes are caused by the movement of tectonic plates diverging at the ridge, creating tensional stress that results in seismic activity. This pattern of earthquakes along mid-ocean ridges provides direct evidence for sea floor spreading as part of plate tectonics.
Like a polyghraph squiggles show the techtonic plates moving.
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.
Ocean-floor rocks near mid-ocean ridges show a symmetrical pattern of magnetized stripes parallel to the ridge axis. These stripes result from periodic reversals in Earth's magnetic field and provide evidence of seafloor spreading. Sediments on the ocean floor also show younger ages near the ridges, supporting the idea of seafloor spreading.
The age of the sea floor provides evidence for tectonic plate movement through the process of seafloor spreading. As magma rises at mid-ocean ridges, it cools and solidifies to form new oceanic crust, which is youngest at the ridge and gets progressively older as you move away. By dating the rock samples, scientists can map the age of the sea floor and observe how older crust is pushed away from the ridge, demonstrating the movement of tectonic plates. This pattern supports the theory of plate tectonics, illustrating how plates diverge, converge, and interact over geological time.
It's helps to show that the crust of the Earth is moving. That helped to prove the theory that the continents split apart.
The epicenr can be found by location the sound in the waves carried.
Live Floor Show ended in 2003.