Ocean Science for Everyone

Seafloor Mapping

Learn About Seafloor Mapping

A key part of exploration is creating maps to plan efficient and safe expeditions. Multibeam sonars collect high-resolution data using multiple, simultaneous sonar beams (sound waves) at once in a fan-like pattern or “swath.” Multibeam sonar data allow teams to spot previously unseen features such as seamounts, deep-sea sandwaves, faults, ancient coral reefs, shipwrecks, and more.

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Seafloor Mapping

Seamount Mapped
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A point cloud of the seamount mapped during the Seascape Alaska 1: Aleutians Deepwater Mapping expedition, generated from acoustic data collected via multibeam echosounder. The hot colors (red, orange, and yellow) represent the newly mapped peak of the seamount at a depth of 895 meters (2,936 feet), while the cold colors (purple, teal, blue) represent the base of the seamount at a depth of around 4,000 meters (13,123 feet).

Methane Bubble Plumes
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In addition to helping us find features on the seafloor, multibeam sonar allows us to detect things like methane bubbles in the water column. This bathymetric data, collected using the sonars on NOAA Ship Okeanos Explorer, revealed methane bubble plumes at Norfolk Seeps of the Atlantic Coast rising over 900 meters (2,950 feet) above the seafloor in some surveys.

Previously Undiscovered Seamount
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While conducting mapping operations off the coast of California in 2023, Saildrone Surveyor mapped this previously undiscovered seamount that rises nearly 3,500 meters (2.17 miles) off the seafloor. Shaped much like the butte features found in the deserts of the Southwest, researchers do not know why or how the seamount gained its cylindrical shape but do think it was most likely a volcanic formation.

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Mapping watchstander Cameron Kuhle, an Explorer-in-Training on the Seascape Alaska 1: Aleutians Deepwater Mapping expedition, "cleans" multibeam sonar data to ensure consistency and accuracy.

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