How do scientists map the ocean floor? Revealexpand_more Flip to revealautorenew
Scientists mainly use sonar, sending sound waves down from a ship and carefully measuring how long each echo takes to bounce back off the seafloor, to calculate the exact depth and shape of the ground far below the surface. By sailing back and forth across an area and combining thousands of these individual depth measurements together, scientists can build an incredibly detailed map showing underwater mountains, deep trenches, and flat plains hidden beneath the waves. Even with modern technology, a surprisingly large portion of the ocean floor remains completely unmapped in fine detail, since mapping the whole ocean thoroughly takes an enormous amount of time, ships, and effort.









