Have you ever searched for something that you felt like you would never find? Maybe you lost your cellphone or you swear that your favorite t-shirt is hiding from you. You search every corner of your home, tear open drawers, and look under the bed, but you still can’t find it. When you eventually find the item, you realize it was right in front of you the whole time.

For centuries, humans have wondered what generates Earth’s internal energy and how it affects the planet’s surface. Scientists have been formally investigating Earth’s interior and volcanic activity around the world for decades. They constantly look for anomalies and unique features that no one has ever discovered. Sometimes it feels like parts of Earth are hiding from scientists, just like your lost cellphone hides from you.

A detailed map shows the topography throughout the Pacific Ocean, where Tamu Massif is located.
(Will Sager/Schmidt Ocean Institute)

The world’s largest volcano has been hiding from us for millions of years underneath the depths of the ocean. How did one of the largest geological features in our solar system go unnoticed for so long?

This volcano, named Tamu Massif, was discovered and researched by a scientist named William Sager. “Tamu” is an abbreviation of Texas A&M University, where Sager worked for 29 years, and “Massif” comes from the French word for massive.

Tamu Massif is located about 1,000 miles east of Japan. The 145 million year old volcano lies about 1,981 meters (6,500 feet) under the ocean’s surface. Though Hawaii’s Mauna Loa volcano stands taller than Tamu Massif, Tamu spans an area nearly 50 times larger.

Scientists developed a detailed 3D map of the seafloor shape, revealing features of the world's largest single volcano.
(Will Sager/Schmidt Ocean Institute)

Tamu Massif has a very gentle slope, meaning that it is not tall, but extremely wide. It is categorized as a shield volcano because the gentle slope and dome-shape make it look like a giant shield protruding from the ground.

Studying this volcano, and many of Earth’s underwater features, is challenging because it lies in the dark depths of the ocean. Sager and his research team have delved these depths, discovering more about the formation of seafloor structures.

To study Tamu Massif, the team used sonar and magnetic fields to create maps of the ocean floor with considerable detail. Using this data, the scientists create 3D maps that allow us to look at what was once hidden underneath the ocean.

This information reveals that Tamu Massif formed when an enormous amount of magma rose up from Earth’s mantle. Tamu Massif sits at a unique boundary of three tectonic plates. Magma rose up through the particularly thin crust at this intersection, cooled, and created new rock to form this extraordinary volcanic mass.

A segment of the detailed mapping of Tamu Massif shows a basal escarpment, or long cliff, on the volcano.
(Will Sager/Schmidt Ocean Institute)
Sometimes scientists encounter unexpected obstacles while conducting research. In this case sharks interfered! It turns out the magnetometers, a tool that the scientists used to map the volcano, emitted magnetic fields that attracted sharks. The sharks bumped, moved, and damaged many of the devices. But, the researchers worked around the sharks in order to show the world something new and exciting.
Uncovering Tamu Massif as one of Earth’s hidden wonders opens many doors. Continued studies of Tamu Massif and similar ocean floor features will help to support scientists’ knowledge of plate tectonics and potentially reveal even more mysteries.
A 3D map reveals the tremendous size of Tamu Massif and the geological features surrounding the volcano.
(Will Sager/Schmidt Ocean Institute)

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  • anomaly

    noun

    Something that is unexpected, abnormal, or differing from what is common.

  • crater

    noun

    A bowl-shaped hole in Earth's surface.

  • earthquake

    noun

    A sudden shaking of the ground producing seismic waves or vibrations, which may result in destruction. An earthquake occurs when slabs of rock suddenly slip past each other at a break in Earth's crust, called a fault.

  • geyser

    noun

    A type of hot spring that sends heated water and steam up into the air.

  • lava

    noun

    Hot, molten rock that has reached Earth's surface through volcanic eruption or a crack in the crust.

  • mid-ocean ridge

    noun

    A long line of mountains on the seafloor, formed by divergent plate boundaries and the upwelling of magma. Seismic and volcanic activity are common along these regions.

  • seismometer (or seismograph)

    noun

    A tool to measure the movement of the ground. This instrument can measure seismic activity, such as the force and duration of an earthquake.

  • tectonic plate

    noun

    Large, slowly moving, slab of solid rock that make up Earth's crust.

  • convergent boundary

    noun

    A location where tectonic plates collide with each other. When two continental plates push toward each other, they fold together and form mountain ranges.

  • crust

    noun

    The outermost layer of Earth. The crust is the coolest and thinnest layer of Earth, ranging from about 5 to 70 km thick. The crust is divided into large slabs of rock, called tectonic plates.

  • eruption

    noun

    Molten rock, ash, and steam ejected from a volcano or geyser.

  • horizontal

    adjective

    At a right angle to the vertical or parallel to the ground level.

  • maar

    noun

    A broad volcanic crater typically filled with water. Maars are created from the explosion that occurs when groundwater meets hot magma.

  • p-wave

    noun

    A type of seismic wave, called primary waves, because they are the first waves from an earthquake to reach a seismograph. P-waves are compressional waves, shaking the ground back and forth, towards and away from the direction the wave is traveling.

  • steam

    noun

    Water in the gas phase.

  • transform boundary

    noun

    A location where tectonic plates slide horizontally past one another. The plates grind together causing frequent earthquakes.

  • convergent with subduction boundary

    noun

    At convergent plate boundaries with subduction, plates push together, and one plate moves underneath the other. This type of boundary may result in the formation of trenches, volcanoes, islands, and earthquakes, which can trigger tsunamis.

  • divergent boundary

    noun

    A location where tectonic plates move away from one another. When plates move apart, lava and magma rise to the surface and make new rock. This type of boundary may result in the formation of small volcanoes, shield volcanoes and rift valleys.

  • fault

    noun

    A fracture or crack in the rocks that make up Earth's crust.

  • hydrothermal vent

    noun

    An opening in the sea floor where magma meets water. This interaction causes heated water, filled with minerals, to rise up from the opening.

  • magma

    noun

    Hot liquid or molten rock located beneath the surface of Earth.

  • seismic wave

    noun

    The vibration from an earthquake that travels within Earth or along Earth's surface.

  • s-wave

    noun

    A type of seismic wave, called shear waves or secondary waves, because they reach a seismograph and shake the ground second, after an earthquake occurs. S-waves shake the ground perpendicularly to the direction the waves are traveling.

  • volcano

    noun

    An opening in Earth's crust which releases hot gases and molten rock.