If an island is on a subducting plate and close to the area of subduction, it will gradually sink as it moves towards the trench.
If the island is on the plate under which the other plate is subducting, it will experience many earthquakes and volcanic eruptions.
An earthquake. But while this happens the magma fills the gap.
pangea would still be here
Tectonic plates and fault lines created by the movement of tectonic plates.
LOLOLOLOLOLOL hehehe and lol
harry hess named the tectonic plates but I'm not sure why =/
Deep-ocean trenches are formed where seafloor tectonic plates subduct under continental plates.
An Earthquake happens.
they are formed when the tectonic plates are shifted
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.
The Japanese Islands are a part of four tectonic plates. These plates are the North American plate, the Eurasia, the Pacific, and the Philippine sea plates.
Yes they are both above the Tectonic plates therefore follow tectonic movements
An earthquake. But while this happens the magma fills the gap.
Tectonic plates move in various ways, one being through the process of subduction where one plate is forced beneath another. This movement can lead to volcanic activity, creating islands as magma rises to the surface and solidifies. Additionally, plates can also move apart at mid-ocean ridges, allowing magma to rise and form new land.
When two tectonic plates move toward each other and smash together, it can lead to the formation of mountain ranges, earthquakes, and volcanic activity. The collision can cause the plates to crumple, fold, or subduct beneath one another, depending on their density and composition. This process is known as plate convergence and plays a significant role in shaping Earth's geology.
Hot spots are stationary points of volcanic activity within the Earth's mantle, and they do not move with tectonic plates. However, as tectonic plates move over the hot spot, they can create a chain of volcanoes, such as the Hawaiian Islands.
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.
friction