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Scientists have discovered new deep-sea ecosystems, hydrothermal vents, underwater volcanoes, sunken ships, and hidden species using state-of-the-art technology such as deep-sea submersibles, remotely operated vehicles (ROVs), and autonomous underwater vehicles (AUVs). These advancements have allowed for the mapping of underwater topography, exploration of marine biodiversity, and understanding of geological processes on the ocean floor.

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What two topographic features of the ocean floor were discovered only with the use of sonar?

Two topographic features of the ocean floor discovered with sonar are underwater mountain ranges known as mid-ocean ridges and deep ocean trenches. Sonar technology allowed scientists to map these submarine structures and gain insights into plate tectonics and the Earth's geology.


What did scientist find at the ocean floor?

Scientists have discovered a variety of things at the ocean floor, including new species of marine life, underwater volcanoes, hydrothermal vents, and deep-sea trenches. They have also found evidence of ancient civilizations, shipwrecks, and valuable resources like oil and minerals. Exploration of the ocean floor continues to reveal new and exciting discoveries about our planet's underwater world.


Which of thee following is not a technology that helps us know what the ocean floor is like?

A bicycle is not a technology that helps us know what the ocean floor is like. Sonar, bathymetry, and remote-operated vehicles are technologies commonly used for mapping the ocean floor.


During world war 2 what did scientist discover on the ocean floor?

During World War II, scientists discovered new deep-sea regions and features on the ocean floor, such as underwater mountain ranges and deep-sea trenches. These discoveries helped advance our understanding of the ocean's geology and biology, providing valuable information for future research and exploration.


What technology did Harry Hess use to map the ocean floor?

Harry Hess used echo sounding technology to map the ocean floor. This technology involved sending sound waves from a ship and measuring the time it took for the sound waves to bounce back, allowing scientists to determine the depth of the ocean floor and create detailed maps.