The Atlantic Ocean is expanding due to mid-atlantic ridge.
Pangaea broke apart due to the movement of tectonic plates in the Earth's crust. This movement, called plate tectonics, caused the continents to drift apart over millions of years, leading to the formation of the current continents and ocean basins.
Seafloor spreading is caused by two plates moving apart. This is caused by plate tectonics. Continental drift is also caused by plate tectonics. Therefore, we can conclude that continental drift is related to seafloor spreading. When the plates move, it carries the continents with it, and thus the continents drift away from each other.
In continental drift it says that they were drifted apart by the spin of the earth and in seafloor spreading the earths crust is drifted apart by the ridges in the mid-ocean.
Continents are not tecnically moving 'away' from each other, they are just moving. This is due to the sub continent plates and the volcanic activity in the ocean. As new volcanic matter from the earths core comes to the surface it pushes continental plates apart.
The theory that states continents can drift apart from each other is called plate tectonics. It explains how the Earth's lithosphere is divided into large plates that move and interact with each other, leading to processes like continental drift and the formation of mountains, earthquakes, and volcanoes. This theory is supported by evidence such as the matching coastlines of continents, the distribution of fossils, and the presence of deep ocean trenches.
Contienental drift, which is when under the surface magma spreads apart and streches the crust apart.
In the middle of the ocean is a rift where the ocean floor squeezes out lava and pushes the ocean plates apart.
because the continents are drifting further apart due to th oceantal crust separating under water
Pangaea broke apart due to the movement of tectonic plates in the Earth's crust. This movement, called plate tectonics, caused the continents to drift apart over millions of years, leading to the formation of the current continents and ocean basins.
Seafloor spreading is caused by two plates moving apart. This is caused by plate tectonics. Continental drift is also caused by plate tectonics. Therefore, we can conclude that continental drift is related to seafloor spreading. When the plates move, it carries the continents with it, and thus the continents drift away from each other.
In continental drift it says that they were drifted apart by the spin of the earth and in seafloor spreading the earths crust is drifted apart by the ridges in the mid-ocean.
Continents are not tecnically moving 'away' from each other, they are just moving. This is due to the sub continent plates and the volcanic activity in the ocean. As new volcanic matter from the earths core comes to the surface it pushes continental plates apart.
The theory that states continents can drift apart from each other is called plate tectonics. It explains how the Earth's lithosphere is divided into large plates that move and interact with each other, leading to processes like continental drift and the formation of mountains, earthquakes, and volcanoes. This theory is supported by evidence such as the matching coastlines of continents, the distribution of fossils, and the presence of deep ocean trenches.
The discovery of seafloor spreading and magnetic striping on the ocean floor in the 1960s provided compelling evidence for Alfred Wegener's theory of continental drift. This process showed how new oceanic crust is formed at mid-ocean ridges and helps move the continents apart, supporting the idea that continents are not fixed but can drift over time.
Sea floor spreading provides evidence for continental drift by showing that new oceanic crust is created at mid-ocean ridges, pushing the continents apart. As the crust spreads apart, it carries the continents along with it, supporting the idea that the continents were once part of a single landmass that has since drifted apart. This process also explains the distribution of ages of oceanic crust, with the youngest crust found at the mid-ocean ridges and getting progressively older as you move away from the ridges.
A continental shift refers to the movement of continents on the Earth's surface due to plate tectonics. This movement is very slow, occurring over millions of years, and can result in changes to the configuration of the continents and the ocean basins. Examples of continental shifts include the breakup of Pangaea into the continents we see today.
Seafloor spreading refers to the process where new oceanic crust is created at mid-ocean ridges and spreads outward, pushing the continents apart. Continental drift, on the other hand, is the idea that the continents are slowly moving across the Earth's surface. Seafloor spreading is a mechanism that helps explain how continents drift apart as part of the larger theory of plate tectonics.