The Mariana Trench formed from a convergent boundary between the Pacific Plate and the Philippine Plate in a subduction zone. The older, denser Pacific Plate subducted beneath the younger, less dense, Philippine Plate. Because the Pacific Plate density is so high, and is the largest tectonic plate, it caused this ocean trench to become the deepest. The crust gets its high density because it faces pressure from the water and sediments above it which compacts the crust. Also as the crust ages it loses heat energy in the molecules, which makes those molecules compact and move slower.