The process is called "subduction." It occurs when one tectonic plate moves beneath another at a convergent boundary, where the oceanic plate is forced down into the mantle at a subduction zone. This process leads to the recycling of old oceanic crust back into the mantle.
Mountains are created by the physical process of pushing the Earth's crust up, while valleys and canyons are formed by the process of wearing down the crust through erosion.
The process by which oceanic crust sinks beneath a deep-ocean trench and back into the mantle at a convergent plate boundary is called subduction. This occurs because oceanic crust is denser than the underlying asthenosphere, causing it to be pulled down into the mantle. Subduction zones are associated with the formation of volcanic arcs and deep-sea trenches.
Isostatic rebound. This is a slow process where the Earth's crust adjusts after being weighed down by glaciers or ice sheets, causing it to rise back up over time.
The movement of material down slope along a curved surface is called creep. It is a slow, continuous process of particle-by-particle movement typically caused by gravity and can occur on various slope angles.
The process is called "subduction." It occurs when one tectonic plate moves beneath another at a convergent boundary, where the oceanic plate is forced down into the mantle at a subduction zone. This process leads to the recycling of old oceanic crust back into the mantle.
The earths crust is moved rather than pulled by things called convection currents. This is when heated rock from the earths core rises up and reaches the crust where it cools. It then sinks down again and carries on in a circle which moves the crust
Infiltration is the process of water moving vertically down through the soil.
Longshore Drift
Mountains are created by the physical process of pushing the Earth's crust up, while valleys and canyons are formed by the process of wearing down the crust through erosion.
erosion
The breakdown of the Earth's crust into sediment is called weathering. This process includes physical and chemical processes that break down rocks into smaller particles, creating sediment over time.
The process of breaking down the Earth's crust is known as weathering. Weathering can occur through physical processes such as frost action and abrasion, as well as chemical processes such as hydration and oxidation. Over time, these processes break down rocks into smaller particles and ultimately contribute to the formation of soil.
percolation
The process by which oceanic crust sinks beneath a deep-ocean trench and back into the mantle at a convergent plate boundary is called subduction. This occurs because oceanic crust is denser than the underlying asthenosphere, causing it to be pulled down into the mantle. Subduction zones are associated with the formation of volcanic arcs and deep-sea trenches.
The plate boundary where oceanic crust is destroyed is a subduction zone. In this process, one tectonic plate is forced beneath another into the Earth's mantle. As the descending plate moves deeper into the mantle, it is eventually melted down and destroyed.
Peristalsis is the process that involuntarily makes it is possible to swallow water while standing on your head and moves food from your mouth down to your stomach. Peristalsis affects the muscles in the intestines also.