How Marie Tharp Pioneered Mapping the Bottom of the Ocean
Despite all the deep-sea expeditions and samples taken from the seabed over the past 100 years, humans still know very little about the ocean’s deepest reaches. And there are good reasons to learn more.
Most tsunamis start with earthquakes under or near the ocean floor. The seafloor provides habitat for fish, corals and complex communities of microbes, crustaceans and other organisms. Its topography controls currents that distribute heat, helping to regulate Earth’s climate.
Hand-painted rendition of Heezen-Tharp 1977 ‘World ocean floor’ map, by Heinrich Berann. Library of Congress, Geography and Map Division, CC BY-ND
July 30 marks the 100th anniversary of the birth of Marie Tharp, a geologist and oceanographer who created maps that changed the way people imagine two-thirds of the world. Beginning in 1957, Tharp and her research partner, Bruce Heezen, began publishing the first comprehensive maps that showed the main features of the ocean bottom – mountains, valleys and trenches.
As a geoscientist, I believe Tharp should be as famous as Jane Goodall or Neil Armstrong. Here’s why.
Traversing the Atlantic
Well into the 1950s, many scientists assumed the seabed was featureless. Tharp showed that it contained rugged terrain, and that much of it was laid out in a systematic way.
Her images were critical to the development of plate tectonic theory – the idea that plates, or large sections of Earth’s crust, interact to generate the planet’s seismic and volcanic activity. Earlier researchers – particularly Alfred Wegener – noticed how well the coastlines of Africa and South America fit together and proposed the continents had once been connected; Tharp identified mountains and a rift valley in the center of the Atlantic Ocean where the two continents could have been ripped apart.
Tharp’s East-West profiles across the North Atlantic. The Floors of the Ocean, 1959
Thanks to Tharp’s hand-drawn renditions of the ocean floor, I can imagine a walk across the Atlantic Ocean bottom from New York City to Lisbon. The journey would take me out along the continental shelf. Then downward towards the Sohm Abyssal Plain. I’d need to detour around underwater mountains, called seamounts. Then I’d start a slow climb up the Mid-Atlantic Ridge, a submerged north-south mountain range.
After ascending to 8,200 feet (2,500 meters) below sea level to the ridge’s peak, I would descend several hundred feet, cross the ridge’s central rift valley and proceed up over the ridge’s eastern edge. Then back down to the ocean floor, until I began trekking up the European continental slope to Lisbon. The total walk would be about 3,800 miles (6,000 kilometers) – almost twice the length of the Appalachian Trail.
Mapping the unseen
Born in Ypsilanti, Michigan, Tharp studied English and music in college. But then in 1943 she enrolled in a University of Michigan master’s degree program designed to train women to be petroleum geologists during World War II. “Girls were needed to fill the jobs left open because the guys were off fighting,” Tharp later recalled.
After working for an oil company in Oklahoma, Tharp sought a geology job at Columbia University in 1948. Women couldn’t go on research ships, but Tharp could draft, and was hired to assist male graduate students.
Tharp worked with Bruce Heezen, a grad student who gave her seafloor profiles to draft. These are long paper rolls that show the depth of the seafloor along a linear path, measured from a ship using sonar.
Starting with a large blank sheet of paper, Tharp marked lines of latitude and longitude. Then she’d carefully mark where the ship had traveled. Next she’d read the depth at each location off the sonar profile, mark it on the ship’s track and create her own condensed profile, showing the depth to the ocean floor versus the distance the ship had traveled.
One of her important innovations was creating sketches depicting what the seafloor would look like. These views made it easier to visualize the ocean floor’s topography and create a physiographic map.
Tharp’s careful plotting of six east-to-west profiles across the North Atlantic revealed something no one had ever described before: a cleft in the center of the ocean, miles wide and hundreds of feet deep. Tharp suggested that it was a rift valley – a type of long trough that was known to exist on land.
Heezen called this idea “girl talk” and told Tharp to recalculate and redraft. When she did, the rift valley was still there.
Another research assistant was plotting locations of earthquake epicenters on a map of the same size and scale. Comparing the two maps, Heezen and Tharp realized that the earthquake epicenters fell inside the rift valley. This discovery was critical to the development of plate tectonic theory: It suggested that movement was occurring in the rift valley, and that the continents might actually be drifting apart.
This insight was revolutionary. When Heezen, as a newly-minted Ph.D., gave a talk at Princeton in 1957 and showed the rift valley and epicenters, geology department chair Harry Hess replied, “You have shaken the foundations of geology.”
Exploring mid-ocean ridges provides vast amounts of information about life on Earth.
In 1959 the Geological Society of America published “The Floors of the Oceans: I. The North Atlantic” by Heezen, Tharp and “Doc” Ewing, director of the Lamont Observatory, where they worked. It contained Tharp’s ocean profiles, ideas and access to Tharp’s physiographic maps.
Some scientists thought the work was brilliant, but most didn’t believe it. French undersea explorer Jacques Cousteau was determined to prove Tharp wrong. Sailing aboard his research vessel, the Calypso, he purposely crossed the mid-Atlantic Ridge and lowered an underwater movie camera. To Cousteau’s surprise, the film showed that a rift valley existed.
“There’s truth to the old cliché that a picture is worth a thousand words and that seeing is believing,” Tharp observed in a 1999 retrospective essay.
What could have created the rift? Princeton’s Hess proposed some ideas in a 1962 paper. It postulated that hot magma rose from inside the Earth at the rift, expanded as it cooled and pushed two adjoining plates further apart. This idea was a key contribution to plate tectonic theory, but Hess failed to reference the critical work presented in “The Floors of the Oceans” – one of the few publications that included Tharp as a co-author.
Marie Tharp in July 2001. Bruce Gilbert, Lamont-Doherty Earth Observatory
Tharp continued working with Heezen to bring the ocean floor to life. Their collaboration included an Indian Ocean map, published by National Geographic in 1967, and a 1977 World Ocean Floor map that is now held at the Library of Congress.
After Heezen died in 1977, Tharp continued her work until her death in 2006. In October 1978, Heezen (posthumously) and Tharp were awarded the Hubbard Medal, the National Geographic Society’s highest honor, joining the ranks of explorers and discoverers such as Ernest Shackleton, Louis and Mary Leakey and Jane Goodall.
Today ships use a method called swath mapping, which measures depth over a ribbon-like path rather than along a single line. The ribbons can be stitched together to create an accurate seafloor map.
Left. Detail of Canary Islands from Marie Tharp’s physiographic map of the North Atlantic. Right. Modern swath mapping depiction of the same area. Colors indicate depth. Vicki Ferrini, Lamont-Doherty Earth Observatory.
But because ships move slowly, it would take one ship 200 years to completely map the seafloor. An international effort to map the entire ocean floor in detail by 2030 is under way, using multiple ships, led by the Nippon Foundation and the General Bathymetric Chart of the Oceans.
This information is critical to beginning to understand what the seafloor looks like on a neighborhood scale. Marie Tharp was the first person to show the rich topography of the ocean floor and its different neighborhoods.
Suzanne O'Connell is a professor of earth & environmental sciences at Wesleyan University. This article appears courtesy of The Conversation and may be found in its original form here.
The opinions expressed herein are the author's and not necessarily those of The Maritime Executive.