Web24 sep. 2024 · Where seafloor sinks back into the Earth’s mantle or is being subducted? Subduction zones. Subduction zones are where the cold oceanic lithosphere sinks back into the mantle and is recycled. They are found at convergent plate boundaries, where the oceanic lithosphere of one plate converges with the less dense lithosphere of another … Web31 dec. 2002 · 1. INTRODUCTION [2] Subduction zones are descending limbs of mantle convection cells and are the dominant physical and chemical system of Earth's interior. The sinking of lithosphere in subduction zones provides most of the force needed to drive the plates and cause mid-ocean ridges to spread, with the result that plate tectonics and …
ESC CH 5 Flashcards Quizlet
WebSinking of oceanic lithosphere into the mantle at a subduction zone. A very long-lived magma source located deep in the mantle is called a (n) __________. hot spot. A … Web19 sep. 2024 · Explanation: It is a low lying area found on both land and seas of oceanic ridges subduction zones along the convergent plate boundaries which are sited … phoenix inn bangor maine
That Move Above The Mantle - QnA
Web1 mrt. 2024 · A subducted slab of lithosphere may slowly slip into the upper mantle and fall to the transition zone due to its relative density and coolness. Over millions of years, it may sink further into the lower mantle. Convection currents may then transport the hot, buoyant material in D’’ back through the other layers of the mantle. Web1 dag geleden · An oceanic plate will sink back into the mantle. Remember, oceanic plates are formed from mantle material at midocean ridges. Young oceanic lithosphere is hot and buoyant (low density) … Web30 jan. 2004 · The rigid outer layer of our planet, called the lithosphere, is the cold, top boundary of convection cells in the mantle. Two features of the ocean floor are the results of this active process. At ocean trenches, old, cold, and dense lithosphere sinks back into the hotter mantle below, dragging surface plates along with it. ttms logo