yes but oceanic crust is younger than continental crust because of deep sea trenches
plate tectonics
Deep-oceanic trenches are most abundant around the rim of the Pacific. Deep ocean trenches are surficial evidence for sinking of oceanic lithosphere into the mantle at a subduction zone.
They are called trenches.
Oceanic crust sinks beneath trenches through a process known as subduction. As oceanic plates collide with continental plates, the denser oceanic plate is forced downward into the mantle due to gravitational pull. This creates a subduction zone where the oceanic crust eventually melts and is recycled back into the mantle.
yes but oceanic crust is younger than continental crust because of deep sea trenches
plate tectonics
Deep ocean trenches are made where one plate is submerged under another
Deep-oceanic trenches are most abundant around the rim of the Pacific. Deep ocean trenches are surficial evidence for sinking of oceanic lithosphere into the mantle at a subduction zone.
They are called trenches.
The Pacific Ocean is part of the Ring of Fire. The ring of fire is underwater trenches made my moving plates. The plates pushed on each other and eventually moved downward, creating trenches
rocks
They are called oceanic trenches.
Oceanic crust sinks beneath trenches through a process known as subduction. As oceanic plates collide with continental plates, the denser oceanic plate is forced downward into the mantle due to gravitational pull. This creates a subduction zone where the oceanic crust eventually melts and is recycled back into the mantle.
An oceanic-oceanic convergence occurs when two plates made of oceanic crust collide. This collision can lead to the formation of deep oceanic trenches, volcanic island arcs, and earthquakes. Over time, the denser plate may subduct beneath the other, leading to the recycling of oceanic crust back into the mantle.
oceanic trenches and volcanoes from the rising magma.
Mid-ocean ridges are the birthplace of oceanic crust. Trenches represent the destruction and burial of oceanic crust. They are at opposite ends of the Earth's convection currents that move through the asthenosphere.