Scientists discover mountains 100x taller than Everest hidden deep in Earth's mantle

Nobody knows what they are, or if they're permanent
Lead researcher Dr. Arwen Deuss on the fundamental mystery surrounding these deep-Earth formations.
Mark

So these mountains are real, then? They're not theoretical?

Mimi

They're real in the sense that seismic data shows them. Scientists detected them by noticing how earthquakes behave at the core-mantle boundary. But we haven't seen them directly—we can't, given where they are.

Luke

That's the key distinction. We're reading the signature of their presence in seismic waves, not observing the mountains themselves. It's inference from data, not direct evidence.

Mark

How confident are scientists that they've interpreted the data correctly?

Mimi

Confident enough that it's being published and discussed seriously, but Deuss herself admits uncertainty about what they are. The interpretation seems solid, but the nature of the structures—what they're made of, exactly how they formed—that's still open.

Luke

And the age estimates are particularly soft. Half a billion years is a floor, not a ceiling. They could be much older, or the dating method itself could be refined as we learn more.

Mark

Why does this matter beyond the novelty of finding tall mountains?

Mimi

It changes how we think about Earth's interior. If there are mountains this large hidden in the mantle, what else are we missing? It also tells us something about how ocean floor gets recycled into the planet's depths.

Luke

Though we should note: the mechanism of formation is understood in broad strokes—ancient seafloor sinking—but the specifics of why these particular formations grew so tall, and whether they're stable or transient, those are still open questions.

Mark

Could they disappear?

Mimi

Possibly. Deuss said they might be temporary. Over geological time, the mantle moves and changes. These could be eroded away or absorbed back into the rock over millions of years.

Luke

But we don't have a timeline for that, or even confirmation that they are temporary. It's an honest acknowledgment of uncertainty, not a prediction.

  • Two mountains dwarfing Everest by a factor of 100 have been confirmed deep inside Earth, shattering assumptions about the scale of geological features hidden within the planet.
  • The only reason they remained unknown for so long is that seismic technology could not detect them — they were invisible to science until earthquake data revealed an inexplicable slowdown at the core-mantle boundary in 1996.
  • Scientists still cannot agree on whether these formations are permanent fixtures of Earth's interior or transient structures that will eventually dissolve back into the mantle.
  • The discovery opens an unsettling possibility: if mountains this massive went undetected until recently, other large-scale structures may still be lurking undiscovered in the deep Earth.
  • Further progress hinges on developing more precise seismic imaging tools, as the extreme heat and pressure at those depths make any form of direct observation physically impossible.

Beneath the familiar surface of the Earth, where no climber will ever set foot, scientists have confirmed the existence of two mountains 620 miles tall — roughly 100 times the height of Everest — buried 1,200 miles deep at the boundary between Earth's mantle and core. First detected in 1996 through the subtle slowing of seismic waves, these ancient formations may be as old as the planet itself, quietly reshaping what we thought we knew about the world beneath our feet. Their discovery is a reminder that the most profound unknowns are not always found in distant galaxies, but in the depths we have always stood upon.

Mount Everest has long defined the outer limit of earthly scale — 29,032 feet of rock and ice that has claimed hundreds of lives in pursuit of its summit. But scientists have now confirmed the existence of two mountains that make Everest look modest: 620-mile-tall formations buried approximately 1,200 miles beneath the surface, sitting at the boundary between Earth's mantle and core. No one will ever climb them. They exist in a realm permanently beyond human reach.

The mantle, Earth's thickest layer, is composed of magnesium-rich rock that slowly absorbs ancient ocean floor over geological time — the same process that built Hawaii. These deep mountains appear to be made of exactly that fossilized seafloor material. Their existence went undetected for most of human history, until 1996, when researchers at Utrecht University noticed that seismic waves from earthquakes were inexplicably slowing at certain points along the core-mantle boundary beneath the central Pacific. That anomaly eventually resolved into the outline of two colossal peaks.

How old they are remains one of geology's open questions. Estimates suggest at least half a billion years, but they could date back to Earth's formation itself. Lead researcher Dr. Arwen Deuss has been candid about the limits of current knowledge: nobody knows whether these are permanent features of the planet's interior or temporary structures that will eventually vanish.

The implications reach beyond the mountains themselves. For decades, geologists believed seismic mapping had given them a reasonably complete picture of Earth's interior. These formations represent a significant gap in that picture — and suggest others may still exist. What comes next depends on whether scientists can build better tools to probe the core-mantle boundary, a region where pressure and temperature make direct observation impossible. For now, these peaks remain the most inaccessible mountains on Earth — not because of altitude or danger, but because they exist in a world humans can never physically enter.

Mount Everest has long held the title of Earth's tallest mountain—a 29,032-foot peak in the Himalayas that demands 42 days of climbing and has claimed at least 340 lives in pursuit of its summit. But that record may need rewriting. Scientists have discovered two mountains on the boundary between Africa and the Pacific Ocean that dwarf Everest entirely. These peaks stretch 620 miles into the sky, making them roughly 100 times taller than the world's most famous mountain. The catch: no one will ever climb them, because they exist entirely beneath the planet's surface, buried approximately 1,200 miles down in Earth's mantle.

The mantle is the thickest layer of the planet, composed of magnesium-rich rock that acts as a kind of graveyard for ancient ocean floor. These deep-Earth mountains are made from those fossilized pieces of seafloor, the same geological process that created mountains like Hawaii. For most of human history, their existence went unnoticed simply because they were too far down to detect. It wasn't until 1996 that scientists working at Utrecht University began investigating the core-mantle boundary beneath the central Pacific Ocean and noticed something odd: earthquakes were slowing down at certain points along that boundary. That anomaly eventually led to the discovery of these colossal formations.

The age of these mountains remains one of the great unknowns. Researchers estimate they are at least half a billion years old, but they could be far older—potentially dating back to Earth's formation itself, billions of years in the past. Dr. Arwen Deuss, the lead researcher on the project, captured the uncertainty plainly: nobody knows what they truly are, or whether they represent a permanent feature of the planet's interior or merely a temporary phenomenon that will eventually disappear. The scientific community has no consensus on how long these structures have existed or how long they will remain.

The discovery raises fundamental questions about how we understand planetary structure. For decades, geologists mapped Earth's interior using seismic data from earthquakes, gradually building a picture of the layers beneath our feet. These mountains represent a significant gap in that picture—massive geological features that went undetected until very recently. Their existence suggests there may be other large-scale structures hidden in the mantle that remain unknown. The research also hints at how dynamic Earth's interior truly is, with ancient ocean floor continuously sinking into the depths and accumulating over geological time.

What happens next depends on whether scientists can develop better tools to study the core-mantle boundary in greater detail. Current seismic imaging has limits, and the extreme pressure and temperature at those depths make direct observation impossible. Researchers will likely continue analyzing earthquake data and refining their models of how these mountains formed and what role they play in Earth's internal dynamics. For now, these 620-mile peaks remain among the most inaccessible mountains on the planet—not because they are remote or dangerous, but because they exist in a realm humans can never physically reach.

Nobody knows what they are, and whether they are only a temporary phenomenon, or if they have been sitting there for millions or perhaps even billions of years.
— Dr. Arwen Deuss, lead researcher, Utrecht University
Envie de l'histoire complète ? Lire l'original sur indy100 ↗
Nous contacter FAQ