Sea bed spreading.
When oceanic and continental plates diverge, the oceanic plate moves away from the continental plate, creating a rift. This process can lead to the formation of new oceanic crust as magma rises to fill the gap, resulting in mid-ocean ridges. The continental plate may also experience stretching and thinning, which can create rift valleys. Overall, this divergence contributes to the dynamic nature of plate tectonics and the formation of new geological features.
When oceanic plates diverge an underwater earthquake is the result. Oceanic earthquakes often result in disastrous Tsunamis.
An earth quake. This happens because the vibrations force the plates apart
Oceanic plates are denser and thinner than continental plates, which causes them to be lower in elevation. The denser oceanic plates are effectively pulled downward by gravity, causing them to sink beneath the less dense continental plates. This difference in density and thickness results in oceanic plates being lower than continental plates.
Continental plates are generally thicker than oceanic plates. Continental plates can range from 20-200 km thick, while oceanic plates are typically around 5-10 km thick.
When oceanic and continental plates diverge, the oceanic plate moves away from the continental plate, creating a rift. This process can lead to the formation of new oceanic crust as magma rises to fill the gap, resulting in mid-ocean ridges. The continental plate may also experience stretching and thinning, which can create rift valleys. Overall, this divergence contributes to the dynamic nature of plate tectonics and the formation of new geological features.
When oceanic plates diverge an underwater earthquake is the result. Oceanic earthquakes often result in disastrous Tsunamis.
When two continental plates diverge, a rift valley forms due to the pulling apart of the Earth's crust. Magma rises to fill the gap created by the separating plates, eventually leading to the formation of new oceanic crust. Over time, this process can result in the formation of a new ocean basin.
An earth quake. This happens because the vibrations force the plates apart
Zombie apocalypse.
Oceanic plates are denser and thinner than continental plates, which causes them to be lower in elevation. The denser oceanic plates are effectively pulled downward by gravity, causing them to sink beneath the less dense continental plates. This difference in density and thickness results in oceanic plates being lower than continental plates.
the oceanic plates are denser than continental plates, therefore, when oceanic plates and continental plates converge, the oceanic will go under the continental plates. But when two oceanic converge either both will rise to form moutains, or both will sink and cause a trench.
Continental plates are more buoyant then oceanic plates.
Continental plates are generally thicker than oceanic plates. Continental plates can range from 20-200 km thick, while oceanic plates are typically around 5-10 km thick.
Oceanic plates are denser and thinner, found beneath the oceans, while continental plates are thicker and less dense, making up the Earth's landmasses. These two types of tectonic plates interact at boundaries, influencing processes like earthquakes and volcanic eruptions.
Convergence can occur between oceanic-oceanic, oceanic-continental, and continental-continental plates. This process typically leads to the formation of mountain ranges, deep ocean trenches, and volcanic arcs.
There are two types of lithosphere: the oceanic lithosphere and the continental lithosphere. The oceanic lithosphere exists in the ocean basins while the continental lithosphere exists in the continental crust.