Side-scan sonar, developed by Martin Klein five decades ago, has detected many submerged objects—including mysterious circular stone structures on the bottom of Loch Ness in Scotland. “They were like the stone structures across much of the British Isles, like Stonehenge,” he says. “To this day, I don’t know what the circles are, but they may conceivably be ancient structures.”
Klein’s technology—which uses sound to take pictures of large parts of ocean and lake floors—is renowned for having located the Titanic 12,000 feet deep in the Atlantic 400 miles east of Newfoundland. It also detected the wreckage of the U.S. space shuttle Challenger and downed aircraft including TWA flight 800, Swissair Flight 111, and John F. Kennedy Jr.’s plane. And it can claim pinpointing a Roman shipwreck from 200 BCE off the coast of Turkey, two ships from the War of 1812, and the only existing British Wellington World War II bomber, found in Loch Ness. Today side-scan sonar is widely used by governments, navies, oil companies, and offshore energy companies, and in autonomous underwater vehicles.
The deep sea is an unexpected workplace for Klein. “I had no relationship to the ocean. I grew up in New York City,” he says. At MIT in 1961, the year before he earned a bachelor’s in electrical engineering, Klein visited the lab of Professor Harold “Doc” Edgerton ’27, ScD ’31, to ask about interesting projects. Soon Klein was improving Doc’s mud penetrator and using sonar to explore the bottom of the Charles River.
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