Lieutenant Matthew Maury of the U.S. Navy released a bathymetric chart in 1855 that contained the first real evidence of mountains underwater in the central Atlantic ocean. After World War I was over, echo-sounding devices were invented. These “primitive sonar systems” began to measure the depth of the ocean by noting how long it took for a sound generated from a ship to bounce off the ocean floor and come back. These signals showed scientists that the floor of the ocean was much more rough than they had imagined before. These sonar measurements showed us the ruggedness of the underwater chain of mountains that became known later as the Mid-Atlantic
Lieutenant Matthew Maury of the U.S. Navy released a bathymetric chart in 1855 that contained the first real evidence of mountains underwater in the central Atlantic ocean. After World War I was over, echo-sounding devices were invented. These “primitive sonar systems” began to measure the depth of the ocean by noting how long it took for a sound generated from a ship to bounce off the ocean floor and come back. These signals showed scientists that the floor of the ocean was much more rough than they had imagined before. These sonar measurements showed us the ruggedness of the underwater chain of mountains that became known later as the Mid-Atlantic