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Mantle anomaly mapped beneath Appalachians

Researchers map a hot mantle blob under eastern North America and explain its long term effects on crustal uplift and mountain formation.

August 13, 2025 at 10:37 AM
blur An ancient 250-mile-wide blob is heading towards New York City

Scientists map a deep mantle anomaly that reshapes our view of Earth, moving slowly and far from any immediate danger to NYC.

Ancient 250 mile wide blob nears New York City

Scientists from the University of Southampton map a deep mantle feature called the Northern Appalachian Anomaly. They describe a bulk of hot rock beneath the eastern United States that is spread over roughly 2,249 miles and drifting southwest at about 12 miles per million years. The blob sits about 124 miles below the surface and is classified as a thermal anomaly because it is hotter than surrounding mantle.

The researchers used seismic tomography, an MRI like tool for the planet, to trace the path of the heat. They connect this upwelling to longer term shifts in the planet’s crust, including the breakup of Greenland and North America around 90 to 80 million years ago. This explanation challenges older ideas that the anomaly was simply leftovers from an earlier tectonic split.

As the blob moves away from the Appalachian region, it may help explain why the mountains still stand tall after erosion. It could also influence how the crust responds to future stress. Importantly, the team stresses that the current data do not imply an imminent threat to New York City and place the event on timescales far beyond daily life.

Key Takeaways

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A deep mantle anomaly exists beneath eastern North America
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The feature is mapped using seismic tomography
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The anomaly likely formed during Greenland and North America separation
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It may help explain the persistence of the Appalachian Mountains
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Movement is extremely slow and not a near term hazard for NYC
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The study connects ancient tectonics to present surface geology

"It's not going to be a big, crazy, super volcanic eruption."

Gernon on surface risk

"the millionth of a snail's pace"

Description of change speed

"Maybe in the light of this new idea we can realise what interesting effects they’re having on the surface"

Gernon on implications

"This anomaly is cutting the weight of the crust and lifting the plate"

Mantle wave description

Geology often rewards patience more than drama. This study reminds readers that Earth changes on scales that dwarf human lifetimes. The language is calm and the conclusions conservative, which helps prevent sensational headlines from taking hold. Yet the finding also invites public imagination about a planet that remains active and mysterious beneath our feet. The bigger lesson may be in how scientists map ancient processes to surface features, linking a distant deep future to the mountains we see today.

The piece also highlights a broader trend in science communication: translating complex models into accessible ideas without overselling risk. By framing the anomaly as a long, slow process rather than an alarming threat, the researchers protect public trust while expanding our sense of planetary history.

Highlights

  • It's not going to be a big, crazy, super volcanic eruption.
  • the millionth of a snail's pace
  • Maybe in the light of this new idea we can see the effects on the surface.
  • This anomaly is cutting the weight of the crust and lifting the plate.

Earth keeps long stories beneath our feet.

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