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the claim

Earth loses rotational velocity in the vacuum of space primarily due to tidal friction and gravitational interaction with the Moon

the verdict
SUPPORTED
the evidence backs this
Recorded sources
3 sources for · 0 against

Counts group repeated records of the same source within each side. They do not measure evidence strength or source independence.

Is it true that Earth loses rotational velocity in the vacuum of space primarily due to tidal friction and gravitational interaction with the Moon?

Yes. Multiple independent lines of evidence, including lunar laser ranging and geological tidal records, confirm that Earth is losing rotational velocity primarily due to tidal friction and gravitational interactions with the Moon.

Verdict: SUPPORTED · 3 sources for, 0 against · Last checked

The analysis

The retrieved papers provide robust, direct evidence that Earth's rotational deceleration is caused by tidal friction and angular momentum transfer to the Moon (papers 3, 7, and 9). There are no papers contradicting this established geophysical consensus.

Evidence for · 3
The past and present Earth-Moon system: the speed of light stays steady as tides evolve
2014
Analysis of lunar laser ranging data shows Earth rotation slowing due to tidal dissipation driven by the Earth-Moon system.
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Williams, J. G., Turyshev, S., & Boggs, D. (2014). The past and present Earth-Moon system: the speed of light stays steady as tides evolve. doi.org. https://doi.org/10.1186/s13535-014-0002-5

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More for · 2
Constraints on Moon's Orbit 3.2 Billion Years Ago From Tidal Bundle Data
2022
Geologic tidal deposits demonstrate that angular momentum was transferred from Earth's rotation to the Moon's orbit via tidal friction over billions of years.
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Eulenfeld, T. & Heubeck, C. (2022). Constraints on Moon's Orbit 3.2 Billion Years Ago From Tidal Bundle Data. doi.org. https://doi.org/10.1029/2022JE007466

Scaling in global tidal dissipation of the Earth-Moon system
2016
Global tidal dissipation modeling confirms that gravitational and tidal interactions between Earth and the Moon account for the slowing of Earth's rotation over geological time.
Get citation
Putten, M. (2016). Scaling in global tidal dissipation of the Earth-Moon system. doi.org. https://doi.org/10.1016/j.newast.2017.01.012

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Receipt History
first checked05 Aug 2026
judged → SUPPORTED · 8505 Aug 2026
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