Question 6 • RMA FL-2001310-Earth/Space Science Semester 2
Harry Hess proposed the theory of seafloor spreading: new oceanic crust forms as magma rises at mid-ocean ridges and moves outward. Therefore, mid-ocean ridges are sites of seafloor spreading. Trenches are generally where older oceanic crust sinks back into the mantle, not where new seafloor spreads.
AI-written and checked against the verified answer.