Ocean floor features

Scaling the tallest mountain on earth would take you not to Mt. Everest, but to Mauna Kea on the Big Island of Hawaii. Although this peak reaches only 13,803 feet above sea level, the mountain extends another 19,700 feet below the surface, for a total of 33,500 feet from base to summit. At 29,035 feet, Mt. Everest reaches the highest elevation on Earth, but measured from sea level to summit, it’s nearly a mile shorter than the partially submerged Mauna Kea.

Underwater landforms

Beneath the smooth ocean surface extends an underwater landscape as complex as anything you might find on land. While the ocean has an average depth of 2.3 miles, the shape and depth of the seafloor is complex. Some features, like canyons and seamounts, might look familiar, while others, such as hydrothermal vents and methane seeps, are unique to the deep.

This graphic shows several ocean floor features on a scale from 0-35,000 feet below sea level. The following features are shown at example depths to scale, though each feature has a considerable range at which it may occur: continental shelf (300 feet), continental slope (300-10,000 feet), abyssal plain (>10,000 feet), abyssal hill (3,000 feet up from the abyssal plain), seamount (6,000 feet up from the abyssal plain), ocean trench (36,000 feet), and volcanic island (above sea level).
This graphic shows several ocean floor features on a scale from 0-35,000 feet below sea level. The following features are shown at example depths to scale, though each feature has a considerable range at which it may occur: continental shelf (300 feet), continental slope (300-10,000 feet), abyssal plain (>10,000 feet), abyssal hill (3,000 feet up from the abyssal plain), seamount (6,000 feet up from the abyssal plain), ocean trench (36,000 feet), and volcanic island (above sea level). (NOAA Office of Education)


Continental shelf

Starting from land, a trip across an ocean basin along the seafloor would begin with crossing the continental shelf. The continental shelf is an area of relatively shallow water, usually less than a few hundred feet deep, that surrounds land. It is narrow or nearly nonexistent in some places; in others, it extends for hundreds of miles. The waters along the continental shelf are usually productive, both from light and nutrients from upwelling and runoff.

Abyssal plains

Continuing your journey across the ocean basin, you would descend the steep continental slope to the abyssal plain. At depths of over 10,000 feet and covering 70% of the ocean floor, abyssal plains are the largest habitat on earth. Sunlight does not penetrate to the sea floor, making these deep, dark ecosystems less productive than those along the continental shelf. But despite their name, these “plains” are not uniformly flat. They are interrupted by features like hills, valleys, and seamounts (underwater mountains that are also hotspots for biodiversity).

Mid-ocean ridge

Rising up from the abyssal plain, you would encounter the mid-ocean ridge, an underwater mountain range, over 40,000 miles long, rising to an average depth of 8,000 feet. Tracing their way around the global ocean, this system of underwater volcanoes forms the longest mountain range on Earth.

Ocean trenches

After scaling the mid-ocean ridge and traversing hundreds to thousands of miles of abyssal plains, you might encounter an ocean trench. The Mariana Trench, for example, is the deepest place in the ocean at 36,201 feet.

Finally, you would ascend tens of thousands of feet back up the continental slope and across the continental shelf. Your journey across an ocean basin would end on the shore of another continent.

This image shows the topography of the Okeanos Explorer Seamount, a 4,711 foot feature located south of Midway Islands within the Papahānaumokuākea Marine National Monument. NOAA scientists first mapped the seamount in March 2016 using shipboard mapping sonars and then explored it with OER’s remotely operated vehicle (ROV) Deep Discoverer during the 2016 Hohonu Moana expedition.
Seamounts named to honor NOAA and partners’ role in ocean exploration
Three seamounts in the Pacific Ocean now bear names honoring the contributions to science made by NOAA and its partners in ocean exploration during a campaign led by the NOAA Office of Ocean Exploration and Research (OER).

Plate tectonics and the ocean floor

Bathymetry, the shape of the ocean floor, is largely a result of a process called plate tectonics. The outer rocky layer of the Earth includes about a dozen large sections called tectonic plates that are arranged like a spherical jig-saw puzzle floating on top of the Earth's hot flowing mantle. Convection currents in the molten mantle cause the plates to slowly move about the Earth a few centimeters each year. Many ocean floor features are a result of the interactions that occur at the edges of these plates.

The shifting plates may collide (converge), move away (diverge) or slide past (transform) each other. As plates converge, one plate may move under the other causing earthquakes, forming volcanoes, or creating deep ocean trenches. Where plates diverge from each other, molten magma flows upward between the plates, forming mid-ocean ridges, underwater volcanoes, hydrothermal vents, and new ocean floor crust. Transform boundaries are faults that connect two areas where plates are converging or diverging. The edges of these continental boundaries usually form zig-zag patterns.

New bathymetric map of the western Gulf of Alaska.
New seafloor maps reveal habitat sculpted by ancient glaciers
These maps show for the first time the course of ancient ice masses. They show how they shaped essential habitat for the western Gulf of Alaska’s abundant fish, seabirds, and marine mammals.


Hydrography is the science that measures and describes the physical features of bodies of water and the surrounding land. In 1807, President Thomas Jefferson established the U.S. Coast Survey, the predecessor to NOAA, to conduct hydrographic surveys and create nautical charts of the young nation’s ports and waterways.

Historically, ships would take depth “soundings” by dropping a lead line off of a ship until it reached the bottom and the line went slack. The term “soundings” comes from the Old French “sonder”offsite link (to plumb) or Old English “sund”offsite link for swimming, water, or sea. But coincidentally, this work is now usually done using sound! Today, ships equipped with multibeam echo sounders are the primary method of gathering this information, although hydrographers use many other technologies as well.

By mapping water depth, the shape of the seafloor and coastline, and the location of possible obstructions, hydrography helps to keep our maritime transportation system moving safely and efficiently, both at sea and in the Great Lakes. Hydrography is also used to identify shipwrecks and preserve our maritime heritage.

Very little of the ocean floor has been mapped directly. So how do we make maps of the global ocean floor? It turns out that satellites can “see” below the sea surface. With careful processing, small differences in sea surface heights and gravity can reveal detailed maps of the seafloor.

Photo taken by aerial drone of the Deep Submersible Support Vessel Pressure Drop with its crew on the day explorers Victor Vescovo and Kathy Sullivan dived in a submersible vehicle to the bottom of Challenger Deep, the deepest known part of the world’s ocean. June 7, 2020.
Mapping, listening at the bottom of the sea
Barely had the ink dried on the partnership agreement signed by NOAA and ocean explorer Victor Vescovo, owner of Caladan Oceanic LLC, when his team headed out to the Pacific Ocean to dive and map the Mariana Trench, and answer the questions: How deep and where exactly is the bottom of the ocean.

Marine life and exploration on the ocean floor

New species are discovered in the ocean each year by marine biologists and other ocean scientists. Many of these newly discovered species live deep on the ocean floor in unique habitats that depend on plate movement, underwater volcanoes, and cold water seeps.

Hydrothermal vents

Deep ocean hydrothermal vent ecosystems were discovered in 1977, broadening our understanding of life on Earth. Previously, sunlight was thought to be the energy source that supported the base of every food web on our planet. But organisms in these deep, dark, ecosystems have no access to sunlight, and instead metabolize hydrogen sulfide or other chemicals in a process called chemosynthesis. Since this discovery, sonar, submarines, satellites, and robots have helped find and explore this type of ecosystem and other deep ocean formations around the globe. With only 5% of the ocean explored, many more scientific discoveries await our future generations of explorers in this final unknown frontier of our planet Earth.

3-D image of Brothers Volcano.
Deepest known underwater volcanic eruption
Most of the world’s volcanic activity actually takes place in the ocean, but most of it goes undetected and unseen.


Helping students understand the connections between plate tectonics, ocean floor bathymetry, diversity of life, and adaptations to the environment can help increase their understanding of the interconnectedness of Earth systems. Using examples of current explorations of the unknown and real-time discoveriesoffsite link can increase the relevance of studying the ocean floor and help increase students' excitement for learning. Ocean science is interdisciplinary and includes themes that are relevant in math, geology, biology, geographic information systems, remote sensing, ecology, physics, and more.

Updated May 2020