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the claim

Remnants of the Farallon plate have remained stable inside the Earth's mantle

the verdict

SUPPORTED

the evidence backs this

refutedsupported

the weight of evidence

4 sources for · 0 against

Multiple seismic tomography and waveform inversion studies confirm that remnants of the subducted Farallon plate persist deep within the Earth's mantle, including the lower mantle and near the core-mantle boundary.

Evidence for · 4

Understanding seismic heterogeneities in the lower mantle beneath the Americas from seismic tomography and plate tectonic history

2007 · cited by 78

Tomographic and plate motion models associate fast seismic anomalies in the lower mantle with the subducted Farallon plate.

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The analysis

The retrieved papers consistently use seismic tomography and waveform inversions to image subducted Farallon plate material in the lower mantle and deep interior, supporting the claim with multiple independent lines of evidence and no dissenting sources.

More for · 3

Lower Mantle Substructure Embedded in the Farallon Plate: The Hess Conjugate

2017 · cited by 9

Seismic waveform inversions reveal high-velocity slab-like anomalies in the lower mantle beneath the U.S. linked to the Farallon plate.

Seismic evidence for subduction-induced mantle flows underneath Middle America.

2020 · cited by 5

Seismic models identify the Farallon anomaly dominating the transition zone and uppermost lower mantle.

Imaging paleoslabs in the D″ layer beneath Central America and the Caribbean using seismic waveform inversion.

2017 · cited by 2

Seismic waveform inversions image paleoslabs just above the core-mantle boundary beneath Central America and the Caribbean, interpreted as long-subducted Farallon plate remnants.

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first checked04 Aug 2026

judged → SUPPORTED · 8704 Aug 2026

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