the heavier plate gets subsided as it is weighed down, causing the lighter plate to fold up, as the heavier plate goes down it gets heated to exsteme temperature and creates magma which causes volcanos.
When two plates subduct, the overriding plate may develop volcanic arcs due to melting of the subducting plate, often forming chains of volcanoes. Additionally, deep ocean trenches can form at the boundary where the two plates converge and subduct. Collision zones and fold mountain ranges can also develop as a result of the intense tectonic forces between the plates.
Oceanic plates are denser than continental plates due to their composition and age. When two plates collide and one is denser, the denser plate will subduct beneath the less dense plate. This is why oceanic plates subduct beneath continental plates in a process known as subduction.
oceanic convergence is when two oceanic plates subduct beneath one another.
oceanic convergence is when two oceanic plates subduct beneath one another.
Density plays a key role in convergent boundaries. When two plates collide at a convergent plate boundary, it is the denser plate that will subduct.
When two plates subduct, the overriding plate may develop volcanic arcs due to melting of the subducting plate, often forming chains of volcanoes. Additionally, deep ocean trenches can form at the boundary where the two plates converge and subduct. Collision zones and fold mountain ranges can also develop as a result of the intense tectonic forces between the plates.
Oceanic plates are denser than continental plates due to their composition and age. When two plates collide and one is denser, the denser plate will subduct beneath the less dense plate. This is why oceanic plates subduct beneath continental plates in a process known as subduction.
Deep-ocean trenches are formed where seafloor tectonic plates subduct under continental plates.
oceanic convergence is when two oceanic plates subduct beneath one another.
oceanic convergence is when two oceanic plates subduct beneath one another.
oceanic convergence is when two oceanic plates subduct beneath one another.
Some plates subduct under others mainly due to difference in their densities. Relatively lighter plate tends to be more buoyant than heavier ones, so in such situations when two such plates meet, the lighter one rises while the denser plate is been subducted.
Continents generally do not subduct beneath oceanic plates because continents are less dense and thicker than oceanic plates. This makes them more buoyant and resistant to being forced downward into the Earth's mantle. Additionally, the composition and structure of continents make them less likely to be pulled into subduction zones.
Density plays a key role in convergent boundaries. When two plates collide at a convergent plate boundary, it is the denser plate that will subduct.
At convergent boundaries, the amount of mass in a given volume, known as density, determines which tectonic plate will subduct. Typically, oceanic plates are denser than continental plates, so when they converge, the denser oceanic plate sinks beneath the lighter continental plate. This process is influenced by factors such as temperature, composition, and the age of the plates, with older oceanic crust generally being denser and more likely to subduct.
The oceanic plate would subduct beneath the continental plate. This is because oceanic plates are denser than continental plates due to their composition, so they are more likely to be forced beneath the less dense continental plate.
Oceanic crust is denser than continental crust, dense enough to sink into the mantle. Continental crust is not dense enough to do this.