Evidence record
Where did the Moon come from?
Every sentence on the exploration belongs to at least one claim below. Each says what kind of statement it is, what it rests on, what the evidence does not establish, and how far it was checked. Nothing here is a score, and none of it is a verdict on a belief or a theory.
Last checked 24 September 2026.
- A judgement, not a fact: 9
- Source checked: 45
- Presented as open: 3
- Partly checked: 5
If something here is wrong, misquoted, out of date or unfair, write to support@unknownoceans.com and give the claim number, which does not change.
What the question takes for granted
A question about a past event, answered from samples and simulations. The impact itself is the field’s leading account; which impact, and how the Moon came to match Earth, is not settled.
The Moon formed in a giant impact
Established
The leading account since 1984 and the frame for every model on the page; established as the field’s account, not as an observed event.
The Moon is isotopically like Earth
Established
Measured in oxygen, titanium and other elements; the 2024 oxygen result finds no difference at all.
The impactor was isotopically unlike Earth
Contested
The canonical puzzle depends on it. Some researchers think an Earth-like impactor improbable, others that bodies from the same region would match.
How the question is labelled
Claim: Made of us
- Kind
- This page’s reading. A judgement the page makes from the evidence. Others read it differently.
- Review
- A judgement, not a fact. Reviewed for whether it is fairly put and follows from the checked claims. No source can confirm it.
The title names the isotopic match the page is about.
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Measurement
The source reads: the Earth and Moon are within ... 0.2 ± 1.6 ppm isotopically identical
What this does not establish
The Moon matching Earth in its isotopes is measured; whether it is mostly made of Earth material is the open question the page describes.
Claim 1 · checked 24 September 2026 · AI-assisted audit
Claim: The Moon
- Kind
- Framing. Signposting. It asserts nothing a source could check.
The question
Claim: The rocks brought back are isotopically almost identical to Earth
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Measurement
The source reads: the Earth and Moon are within ... 0.2 ± 1.6 ppm isotopically identical
Context
The proto-Earth as a significant source of lunar materialabstract
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026
The source reads: Oxygen isotopic compositions have been found to be identical between terrestrial and lunar samples
Read as an abstract only; the claim is carried by the full-text sources.
What this does not establish
Apollo samples come from the lunar surface; the comparison is of those rocks and Earth’s mantle.
Later work looked for
Crossref, 2021 on, "oxygen isotope Earth Moon": Fischer and others (PNAS, December 2024) find no Earth-Moon difference at 0.2 ± 1.6 ppm and no heterogeneity among lunar rock types, against Cano and others (2020); page now reports the 2024 result.
Claim 3 · checked 24 September 2026 · AI-assisted audit
Claim: which is a problem for the theory that explains nearly everything else
- Kind
- What scholars argue. A report of what specialists argue, or where they disagree.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.2, Canonical impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: The key difficul ty for a canoni cal impact is accounting for Earth -Moon isotopic similarities.
Supports
Origin of the Moonsection 3.2, Canonical impact, and section 1
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Review of the field
The source reads: can produce an iron-depleted Moon and a planet-disk system whose angular momentum is ... account for the Earth -Moon system angular momentum and the Moon's mass
Qualifies
Origin of the Moonsection 6, Conclusions and open issues
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: has been a longstanding issue for a giant impact origin
The Moon’s orbital tilt is not explained by a single impact on its own.
Corrected
24 September 2026. Previously: “The rocks brought back are isotopically almost identical to Earth, which is a problem for the theory that explains everything else.” The review lists things the impact does not by itself explain, such as the Moon’s orbital tilt.
Claim 4 · checked 24 September 2026 · AI-assisted audit
Claim: A giant impact early in the solar system explains the Moon’s size, the spin of the Earth-Moon pair and the Moon’s lack of iron.
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 1 and section 3.2, Canonical impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Review of the field
The source reads: the impact of a Mars -sized body at the end of Earth's accretion could account for the main physical properties of the Earth -Moon system ... can produce an iron-depleted Moon and a planet-disk system whose angular momentum is ... account for the Earth -Moon system angular momentum and the Moon's mass
Supports
Origin of the Moonsection 1, Introduction
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Review of the field
The source reads: The Moon has a tiny core, perhaps with only ~ 1% of its mass, in contrast to Earth whose core contains nearly 30% of its mass
Supports
Moon FactsFormation
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Reference work
The source reads: The Moon likely formed after a Mars-sized body collided with Earth several billion years ago.
Qualifies
Origin of the Moonsection 6, Conclusions and open issues
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: has been a longstanding issue for a giant impact origin
The Moon’s orbital tilt is not explained by a single impact on its own.
What this does not establish
A model that reproduces these properties in simulation; the Moon’s orbital tilt is a separate, unresolved problem for it.
Corrected
24 September 2026. Previously: “A giant impact early in the solar system explains the Moon’s size, its orbit and its lack of iron.” “Its orbit” overstated: the impact accounts for the system’s angular momentum, while the orbit’s tilt is a longstanding problem for it (review, section 6).
Claim 5 · checked 24 September 2026 · AI-assisted audit
Claim: Its standard version also predicts that most of the Moon should be made of the impactor, and the samples say otherwise.
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 1, Introduction
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: this so -called “canonical impact” left a conundrum: it predicted the Moon formed primarily from material from the impactor, whereas the similarity in isotopic composition of the Earth and Moon
Supports
Origin of the Moonsection 3.2, Canonical impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Review of the field
The source reads: In canonical impacts, most of the disk, typically ... 70 to 80%, originates from the impactor's mantle
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Measurement
The source reads: the Earth and Moon are within ... 0.2 ± 1.6 ppm isotopically identical
What this does not establish
The prediction is from simulations of the canonical impact; one modified code (Hosono and others, 2019, reported in the review) gets an Earth-dominated disc.
Corrected
24 September 2026. Previously: “It also predicts that most of the Moon should be made of the impactor, and the samples say otherwise.” The prediction belongs to the canonical impact, not to every impact model, as the page itself goes on to say.
Claim 6 · checked 24 September 2026 · AI-assisted audit
Claim: Several fixes exist and none is agreed.
- Kind
- Open question. Something the page says is not known.
- Review
- Presented as open. The page says this is unresolved, and the review found that it is.
The review surveys several impact scenarios and concludes none is established.
Supports
Origin of the Moonsection 6, Conclusions and open issues
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: Current models provide an array of possible solutions, but all involve conditions whose likelihood appears small or remains highly uncertain.
Claim 7 · checked 24 September 2026 · AI-assisted audit
Claim: The Moon is absurdly large for a planet this size
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 1, Introduction
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Review of the field
The source reads: The Moon is roughly ¼ the radius of the Earth ... than all known satellites other than Pluto’s Charon
Later work looked for
A ratio of sizes, not a finding later work revises.
Claim 8 · checked 24 September 2026 · AI-assisted audit
Claim: its iron core is tiny
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 1, Introduction
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Review of the field
The source reads: The Moon has a tiny core, perhaps with only ~ 1% of its mass, in contrast to Earth whose core contains nearly 30% of its mass
Supports
Moon FactsStructure
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Reference work
The source reads: The Moon’s core is proportionally smaller than other terrestrial bodies' cores. The solid, iron-rich inner core is 149 miles (240 kilometers) in radius. It is surrounded by a liquid iron shell 56 miles (90 kilometers) thick.
Later work looked for
Crossref, 2022 on, "lunar inner core radius": Briaud and others (Nature, 2023, abstract) give an inner core radius of 258 ± 40 km, consistent with NASA’s 240 within its uncertainty; page unchanged.
Corrected
24 September 2026. Previously: “it has almost no iron core” The core is small, about 1 per cent of the Moon’s mass by the review’s estimate, but it is there: NASA gives it a radius of about 330 kilometres.
Claim 9 · checked 24 September 2026 · AI-assisted audit
Claim: and it is drifting away from us by a few centimetres a year.
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Moon FactsSize and Distance
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Reference work
The source reads: The Moon is slowly moving away from Earth, getting about an inch farther away each year.
What this does not establish
NASA rounds the rate to about an inch a year; the page does not give a more precise figure.
Later work looked for
Crossref, 2016 on, "lunar recession rate laser ranging": nothing that changes a rate of a few centimetres a year.
Corrected
24 September 2026. Previously: “and it is receding from us at about the speed a fingernail grows.” The comparison with a fingernail had no source; the rate is now NASA’s.
Claim 10 · checked 24 September 2026 · AI-assisted audit
Claim: One collision accounts for the first two
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.2, Canonical impact, and section 1
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Review of the field
The source reads: can produce an iron-depleted Moon and a planet-disk system whose angular momentum is ... account for the Earth -Moon system angular momentum and the Moon's mass
Supports
Origin of the Moonsection 1, Introduction
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Review of the field
The source reads: The Moon is roughly ¼ the radius of the Earth ... than all known satellites other than Pluto’s Charon
What this does not establish
In simulation; which version of the collision is right is the open question.
Corrected
24 September 2026. Previously: “One event accounts for all three.” The Moon’s drift is caused by tides, not by the impact; the impact explains where it started (review, section 3.1.1).
Claim 11 · checked 24 September 2026 · AI-assisted audit
Claim: and would have left the Moon close to Earth, from where tides have been pushing it outward ever since.
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.1.1, Constraints
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: has caused the Earth’s spin to slow and the Moon’s orbit to expand while conserving angular momentum. A newly-formed Moon orbiting just outside the Roche limit
What this does not establish
A newly formed Moon just outside the Roche limit is the review’s working assumption for impact models.
Claim 12 · checked 24 September 2026 · AI-assisted audit
Claim: The difficulty is in the isotopes.
- Kind
- What scholars argue. A report of what specialists argue, or where they disagree.
- Review
- Source checked. The cited passage was read, and it says this.
The review names the isotopic similarity as the key difficulty for the canonical impact.
Supports
Origin of the Moonsection 3.2, Canonical impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: The key difficul ty for a canoni cal impact is accounting for Earth -Moon isotopic similarities.
Claim 13 · checked 24 September 2026 · AI-assisted audit
What the rocks say
Claim: What the rocks say
- Kind
- Framing. Signposting. It asserts nothing a source could check.
What the samples show
Claim: What the samples show
- Kind
- Framing. Signposting. It asserts nothing a source could check.
Claim: The Moon as a whole holds less than a tenth of its mass in iron, although its mantle is relatively rich in it
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.1.1, Constraints
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Review of the field
The source reads: The mantle of the Moon is relatively iron ... but overall, the Moon contains less than ... 10% of its mass in the element iron due to its small core
Later work looked for
A bulk property stated by the review; the 2023 inner-core study (Briaud and others, abstract) is consistent with a small core. No further search.
Corrected
24 September 2026. Previously: “Lunar rock is depleted in iron and in volatile elements relative to Earth, consistent with material that was once vaporised and had already lost its metal.” Lunar rock is not iron-depleted: the review says the Moon’s mantle is relatively iron-rich and that the whole Moon is iron-poor because its core is small. The cause of the volatile loss is given as Day and Moynier give it.
Claim 16 · checked 24 September 2026 · AI-assisted audit
Claim: what is missing is the metal.
- Kind
- This page’s reading. A judgement the page makes from the evidence. Others read it differently.
- Review
- A judgement, not a fact. Reviewed for whether it is fairly put and follows from the checked claims. No source can confirm it.
Follows from the review’s statement that the mantle is iron-rich and the bulk Moon iron-poor because of its small core.
Supports
Origin of the Moonsection 3.1.1, Constraints
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Review of the field
The source reads: The mantle of the Moon is relatively iron ... but overall, the Moon contains less than ... 10% of its mass in the element iron due to its small core
Claim 17 · checked 24 September 2026 · AI-assisted audit
Claim: Its rocks are also depleted in volatile elements relative to Earth
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 2.1
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Review of the field
The source reads: The depletion in the abundances of volatile elements in the Moon relative to Earth’s mantle was documented starting in the 1970s
Context
Evaporative fractionation of volatile stable isotopes and their bearing on the origin of the Moonabstract
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026
The source reads: The Moon is depleted in volatile elements relative to the Earth and Mars.
Read as an abstract only.
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: The depletion of the Moon in volatile elements has two sources: i) the volatile element depletion of the building blocks of the Moon (proto-Earth, Theia) by nebular fractional condensation and ii) volatile loss during the formation of the Moon.
Later work looked for
Fischer and others (2024, read in full) restate the depletion and its two candidate sources; no further search.
Claim 18 · checked 24 September 2026 · AI-assisted audit
Claim: most probably by evaporation, during the impact or in a later ocean of magma.
- Kind
- What scholars argue. A report of what specialists argue, or where they disagree.
- Review
- Partly checked. Only part of the source could be read. What was not read is listed.
Supports
Evaporative fractionation of volatile stable isotopes and their bearing on the origin of the Moonabstract
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026 · Artefacts and sites · Review of the field
The source reads: The most probable cause of volatile depletion is global-scale evaporation resulting from a giant impact or a magma ocean phase
Qualifies
Evaporative fractionation of volatile stable isotopes and their bearing on the origin of the Moonabstract
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026
The source reads: Problems exist for models of planetary volatile depletion following giant impact.
What this does not establish
Only the abstract was read. The authors say problems exist for the impact route and that a magma-ocean phase may explain the loss better.
Claim 19 · checked 24 September 2026 · AI-assisted audit
Claim: The iron core reaches only about 330 kilometres out, a solid inner core of 240 inside a liquid shell 90 thick, in a body whose radius is about 1,740.
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Moon FactsStructure
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Reference work
The source reads: The Moon’s core is proportionally smaller than other terrestrial bodies' cores. The solid, iron-rich inner core is 149 miles (240 kilometers) in radius. It is surrounded by a liquid iron shell 56 miles (90 kilometers) thick.
Supports
Moon FactsSize and Distance
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Reference work
The source reads: With a radius of about 1,080 miles (1,740 kilometers)
What this does not establish
The core’s size is inferred from seismic and tidal data, not measured directly; a 2023 study gives an inner core of 258 ± 40 kilometres.
Later work looked for
Crossref, 2022 on, "lunar inner core radius": Briaud and others (Nature, 2023, abstract) give an inner core radius of 258 ± 40 km, consistent with NASA’s 240 within its uncertainty; page unchanged.
Corrected
24 September 2026. Previously: “in a body whose radius is 1,737” Matched to the cited source, which gives about 1,740 kilometres.
Claim 20 · checked 24 September 2026 · AI-assisted audit
Claim: Proportionally it is smaller than any other rocky world’s
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Moon FactsStructure
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Reference work
The source reads: The Moon’s core is proportionally smaller than other terrestrial bodies' cores. The solid, iron-rich inner core is 149 miles (240 kilometers) in radius. It is surrounded by a liquid iron shell 56 miles (90 kilometers) thick.
Later work looked for
Crossref, 2022 on, "lunar inner core radius": Briaud and others (Nature, 2023, abstract) give an inner core radius of 258 ± 40 km, consistent with NASA’s 240 within its uncertainty; page unchanged.
Corrected
24 September 2026. Previously: “Proportionally it is far smaller than any other rocky world’s.” NASA says “proportionally smaller”; “far smaller” is carried only for Earth, whose core holds nearly 30 per cent of its mass (review).
Claim 21 · checked 24 September 2026 · AI-assisted audit
Claim: and far smaller than Earth’s, which holds nearly a third of the planet’s mass.
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 1, Introduction
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Review of the field
The source reads: The Moon has a tiny core, perhaps with only ~ 1% of its mass, in contrast to Earth whose core contains nearly 30% of its mass
Later work looked for
Standard figures stated by the review; not something later work revises.
Claim 22 · checked 24 September 2026 · AI-assisted audit
Claim: Its oxygen and titanium isotope ratios, though, match Earth’s to high precision.
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Measurement
The source reads: the Earth and Moon are within ... 0.2 ± 1.6 ppm isotopically identical
Supports
Origin of the Moonsection 2.3
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Review of the field
The source reads: a robust conclusion is that the Earth and shallow Moon have ... 17O values within ~0.01‰ (10 ppm) of each other, whereas samples derived from the deeper lunar interior exhibit differences up to about 20 ppm
Context
The proto-Earth as a significant source of lunar materialabstract
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026 · Artefacts and sites · Measurement
The source reads: we find that the 50Ti/47Ti ratio of the Moon is identical to that of the Earth within about four parts per million, which is only 1/150 of the isotopic range documented in meteorites
Read as an abstract only; the claim is carried by the full-text sources.
What this does not establish
Earlier studies disagreed at the level of a few parts per million, and one argued that deep-sourced samples differ by about 20; the 2024 study found no such difference.
Later work looked for
Crossref, 2021 on, "oxygen isotope Earth Moon": Fischer and others (PNAS, December 2024) find no Earth-Moon difference at 0.2 ± 1.6 ppm and no heterogeneity among lunar rock types, against Cano and others (2020); page now reports the 2024 result.
Claim 23 · checked 24 September 2026 · AI-assisted audit
Claim: The Moon’s 50Ti/47Ti sits within about four parts per million of Earth’s, a hundred and fiftieth of the range meteorites cover
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Partly checked. Only part of the source could be read. What was not read is listed.
Supports
The proto-Earth as a significant source of lunar materialabstract
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026 · Artefacts and sites · Measurement
The source reads: we find that the 50Ti/47Ti ratio of the Moon is identical to that of the Earth within about four parts per million, which is only 1/150 of the isotopic range documented in meteorites
What this does not establish
Only the abstract of Zhang and others was read; the figures are the abstract’s own.
Later work looked for
Crossref, 2013 on, "titanium isotope Moon Earth lunar samples": nothing that revises it; the 2021 review still cites it as the titanium constraint.
Claim 24 · checked 24 September 2026 · AI-assisted audit
Claim: and a 2024 oxygen study, working at a precision earlier ones could not reach, found no difference down to a part or two per million.
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Oxygen isotope identity of the Earth and Moon with implications for the formation of the Moon and source of volatilesabstract and Results
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Measurement
The source reads: We conducted precise measurements of oxygen isotope ratios of lunar and terrestrial rocks. ... the Earth and Moon are within ... 0.2 ± 1.6 ppm isotopically identical
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Measurement
The source reads: The isotope identity of the Earth and Moon had earlier been suggested (23–26) but is now observed on the previously unresolved <1 ppm scale
What this does not establish
One laboratory’s measurement of 14 lunar samples; earlier studies reported small differences, and whether any remains is argued.
Later work looked for
Crossref, 2021 on, "oxygen isotope Earth Moon": Fischer and others (PNAS, December 2024) find no Earth-Moon difference at 0.2 ± 1.6 ppm and no heterogeneity among lunar rock types, against Cano and others (2020); page now reports the 2024 result.
Corrected
24 September 2026. Previously: “” Added: the most recent high-precision oxygen result, which the page did not report.
Claim 25 · checked 24 September 2026 · AI-assisted audit
Claim: Mars and most meteorites carry isotopic fingerprints of their own, and the Moon carries ours.
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.1.1, Constraints
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Review of the field
The source reads: while meteorites from Mars and the asteroid belt differ substantially
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Review of the field
The source reads: Many elements (O, Si, S, Ti, Cr, and W) show distinct, partly mass-independent isotope heterogeneity among solar system bodies (planets and asteroids) but show no (O, Si, S, Ti, and Cr) or only very small (O and W) differences between the Earth and Moon
Later work looked for
Crossref, 2021 on, "isotopic dichotomy meteorites Earth Moon nucleosynthetic": nothing that changes it; Fischer and others (2024) restate it.
Corrected
24 September 2026. Previously: “Each body in the solar system has its own isotopic fingerprint, and the Moon has ours.” Not every body differs: enstatite meteorites are close to Earth in oxygen (review, section 2.3). The sentence now names what the sources compare.
Claim 26 · checked 24 September 2026 · AI-assisted audit
The giant impact explains almost everything
Claim: The giant impact explains almost everything
- Kind
- This page’s reading. A judgement the page makes from the evidence. Others read it differently.
- Review
- A judgement, not a fact. Reviewed for whether it is fairly put and follows from the checked claims. No source can confirm it.
A heading; the passage below lists what the impact accounts for.
Supports
Origin of the Moonsection 3.2, Canonical impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Review of the field
The source reads: can produce an iron-depleted Moon and a planet-disk system whose angular momentum is
Qualifies
Origin of the Moonsection 6, Conclusions and open issues
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: has been a longstanding issue for a giant impact origin
The Moon’s orbital tilt is not explained by a single impact on its own.
What this does not establish
The Moon’s orbital tilt and its isotopes are not explained by the standard impact on its own.
Claim 27 · checked 24 September 2026 · AI-assisted audit
Claim: In the standard version a body about the size of Mars struck the young Earth obliquely.
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.2, Canonical impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Review of the field
The source reads: can produce an iron-depleted Moon and a planet-disk system whose angular momentum is
Supports
Moon FactsFormation
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Reference work
The source reads: The Moon likely formed after a Mars-sized body collided with Earth several billion years ago.
Supports
Origin of the Moonsection 3.1.1, Constraints
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: An oblique collision(s) is a natural source of Earth’s early rapid spin
What this does not establish
The canonical impact in simulation; the size and angle are what the model needs, not something observed.
Claim 28 · checked 24 September 2026 · AI-assisted audit
Claim: The collision threw mantle material into orbit, most of it the impactor’s, where it gathered into the Moon, and left Earth spinning fast.
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.2, Canonical impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Review of the field
The source reads: In canonical impacts, most of the disk, typically ... 70 to 80%, originates from the impactor's mantle
Supports
Origin of the Moonsection 3.1.1, Constraints
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: An oblique collision(s) is a natural source of Earth’s early rapid spin
Supports
Origin of the Moonsection 1, Introduction
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Review of the field
The source reads: The Earth-Moon system has a high total angular momentum, implying a rapidly spinning Earth when the Moon formed
What this does not establish
In simulation. Most of the disc being the impactor’s is exactly what the isotopes contradict.
Corrected
24 September 2026. Previously: “The collision stripped mantle material into orbit, where it condensed into the Moon, and left Earth spinning fast.” In the canonical model the orbiting material is mostly the impactor’s mantle (review, section 3.2); the old wording left that out, which is the point of the next section.
Claim 29 · checked 24 September 2026 · AI-assisted audit
Claim: That accounts for the Moon’s mass, the angular momentum of the pair and the missing iron
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.2, Canonical impact, and section 1
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Review of the field
The source reads: can produce an iron-depleted Moon and a planet-disk system whose angular momentum is ... account for the Earth -Moon system angular momentum and the Moon's mass
What this does not establish
In simulation, for a narrow range of impact angles and speeds.
Corrected
24 September 2026. Previously: “That accounts for the Moon’s mass, the angular momentum of the pair, the missing iron and the missing volatiles.” Day and Moynier give the impact and a later magma ocean as the two candidates for the volatile loss, and name problems for the impact route.
Claim 30 · checked 24 September 2026 · AI-assisted audit
Claim: and offers one route to the missing volatiles.
- Kind
- What scholars argue. A report of what specialists argue, or where they disagree.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: The depletion of the Moon in volatile elements has two sources: i) the volatile element depletion of the building blocks of the Moon (proto-Earth, Theia) by nebular fractional condensation and ii) volatile loss during the formation of the Moon.
Context
Evaporative fractionation of volatile stable isotopes and their bearing on the origin of the Moonabstract
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026 · Artefacts and sites · Review of the field
The source reads: The most probable cause of volatile depletion is global-scale evaporation resulting from a giant impact or a magma ocean phase
Read as an abstract only.
Qualifies
Evaporative fractionation of volatile stable isotopes and their bearing on the origin of the Moonabstract
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026
The source reads: Problems exist for models of planetary volatile depletion following giant impact.
What this does not establish
The cause of the volatile loss is argued; a magma-ocean phase is the other candidate.
Claim 31 · checked 24 September 2026 · AI-assisted audit
Claim: It is not a fringe idea
- Kind
- What the field holds. The settled view of a field, as a review, a consensus statement or a reference work gives it. Not one study.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 1, Introduction
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: Origin via a giant impact with the Earth emerged from the 1984 “Origin of the Moon” conference as the leading hypothesis
Supports
Origin of the Moonsection 5.5, Discussion
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: large impacts are efficient producers of moons
Supports
Moon FactsFormation
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Reference work
The source reads: The Moon likely formed after a Mars-sized body collided with Earth several billion years ago.
Later work looked for
Crossref, 2021 on, "Moon-forming giant impact": work since (Kegerreis 2022, Fischer 2024, Hopp 2025) all works within the impact framework.
Claim 32 · checked 24 September 2026 · AI-assisted audit
Claim: and it is not in trouble as a class of explanation.
- Kind
- This page’s reading. A judgement the page makes from the evidence. Others read it differently.
- Review
- A judgement, not a fact. Reviewed for whether it is fairly put and follows from the checked claims. No source can confirm it.
The review’s authors work within the impact framework; what the isotopes challenge is a particular impact.
Supports
Origin of the Moonsection 5.5, Discussion
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: large impacts are efficient producers of moons
Supports
Origin of the Moonsection 6, Conclusions and open issues
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: Current models provide an array of possible solutions, but all involve conditions whose likelihood appears small or remains highly uncertain.
Other readings
Melosh (2014), quoted in the review, called the isotopic problem an “isotopic crisis” for the giant impact model.
Claim 33 · checked 24 September 2026 · AI-assisted audit
Where the theory strains
Claim: Where the theory strains
- Kind
- Framing. Signposting. It asserts nothing a source could check.
Claim: Mars and most meteorites have signatures of their own.
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.1.1, Constraints
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Review of the field
The source reads: while meteorites from Mars and the asteroid belt differ substantially
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Review of the field
The source reads: Many elements (O, Si, S, Ti, Cr, and W) show distinct, partly mass-independent isotope heterogeneity among solar system bodies (planets and asteroids) but show no (O, Si, S, Ti, and Cr) or only very small (O and W) differences between the Earth and Moon
Later work looked for
Crossref, 2021 on, "isotopic dichotomy meteorites Earth Moon nucleosynthetic": nothing that changes it; Fischer and others (2024) restate it.
Corrected
24 September 2026. Previously: “Every other body in the solar system has its own signature.” Enstatite meteorites are close to Earth in oxygen; the line now names what the sources compare.
Claim 35 · checked 24 September 2026 · AI-assisted audit
Claim: The Moon has ours.
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Measurement
The source reads: the Earth and Moon are within ... 0.2 ± 1.6 ppm isotopically identical
Later work looked for
Crossref, 2021 on, "oxygen isotope Earth Moon": Fischer and others (PNAS, December 2024) find no Earth-Moon difference at 0.2 ± 1.6 ppm and no heterogeneity among lunar rock types, against Cano and others (2020); page now reports the 2024 result.
Claim 36 · checked 24 September 2026 · AI-assisted audit
Why the Moon is not made of the impactor
Claim: Why the Moon is not made of the impactor
- Kind
- This page’s reading. A judgement the page makes from the evidence. Others read it differently.
- Review
- A judgement, not a fact. Reviewed for whether it is fairly put and follows from the checked claims. No source can confirm it.
A heading stating the puzzle the section describes.
Supports
Origin of the Moonsection 1, Introduction
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: this so -called “canonical impact” left a conundrum: it predicted the Moon formed primarily from material from the impactor, whereas the similarity in isotopic composition of the Earth and Moon
What this does not establish
Whether the Moon is mostly Earth material, or a thorough mix, is what the section says is unsettled.
Claim 37 · checked 24 September 2026 · AI-assisted audit
Claim: Simulations of the classic version put most of the Moon’s material from the impactor rather than from Earth.
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.2, Canonical impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Review of the field
The source reads: In canonical impacts, most of the disk, typically ... 70 to 80%, originates from the impactor's mantle
Context
Making the Moon from a Fast-Spinning Earth: A Giant Impact Followed by Resonant Despinningabstract
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026
The source reads: simulations of the current giant impact hypothesis for Moon formation find that most lunar material originated from the impactor, which should have had a different isotopic signature
Read as an abstract only.
Context
Forming a Moon with an Earth-like Composition via a Giant Impactabstract (PMC author manuscript)
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026
The source reads: Prior impact simulations predict that much of the disk material originates from the impacting planet.
Read as an abstract only.
What this does not establish
One modified code reported in the review gives an Earth-dominated disc for the same impact.
Claim 38 · checked 24 September 2026 · AI-assisted audit
Claim: Unless that body happened to be isotopically almost identical to Earth, or the two were mixed thoroughly afterwards, the samples should show it.
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.2, Canonical impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: In general, a canonical Moon-forming impact requires either an impactor with an Earth ... or that the compositional signature of the impactor in the disk was erased by vapor mixing
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Argument
The source reads: The isotope identity of Moon and Earth, as illustrated in diagram Fig. 3 requires either Theia and proto-Earth having the same composition (16), vigorous mixing of Theia and Earth after the Moon-forming impact (37–39), or a combination of both.
What this does not establish
Whether vapour mixing after the impact could do this is itself unresolved.
Corrected
24 September 2026. Previously: “Unless that body happened to have an isotopic composition identical to Earth’s, which is not what the rest of the solar system looks like, the samples should show it.” The old sentence left out mixing after the impact and stated as settled that an Earth-like impactor is implausible, which the review reports as argued both ways.
Claim 39 · checked 24 September 2026 · AI-assisted audit
Claim: Some researchers think such a twin unlikely; others argue that neighbours built from the same material would match.
- Kind
- What scholars argue. A report of what specialists argue, or where they disagree.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.1.1, Constraints
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: The case has been made that an isotopically Mars-like impactor is most likely (Pahlevan & Stevenson 2007), although counter arguments for an Earth ... composition impactor have also been advanced
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: Such a mode of accretion of Theia and proto-Earth in the same feeding zone may also explain the similarity of the Earth and Moon in oxygen, titanium, and chromium.
Supports
Immediate origin of the Moon as a post-impact satellitesection 1, Introduction
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Argument
The source reads: it seems unlikely, though perhaps possible, that the impactor would already match the proto-Earth target’s composition
Later work looked for
Crossref, 2023 on, "Theia Moon-forming impactor origin isotopes": Hopp and others (Science, 2025, abstract) find Theia and proto-Earth both inner Solar System material; it does not settle whether Theia was isotopically identical, so the page reports the disagreement.
Claim 40 · checked 24 September 2026 · AI-assisted audit
Claim: Two fixes were published together in 2012.
- Kind
- Historical claim. A statement about the past that historical evidence can test.
- Review
- Partly checked. Only part of the source could be read. What was not read is listed.
Supports
Forming a Moon with an Earth-like Composition via a Giant ImpactCrossref record
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026
Science 338(6110), 1052-1055, issue of 23 November 2012.
Supports
Making the Moon from a Fast-Spinning Earth: A Giant Impact Followed by Resonant DespinningCrossref record
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026
Science 338(6110), 1047-1052, issue of 23 November 2012.
Context
Forming a Moon with an Earth-like Composition via a Giant Impactabstract (PMC author manuscript)
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026
The source reads: Here we simulate impacts involving larger impactors than previously considered. We show these can produce a disk with the same composition as the planet’s mantle
Read as an abstract only.
Context
Making the Moon from a Fast-Spinning Earth: A Giant Impact Followed by Resonant Despinningabstract
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026
The source reads: typical last giant impacts onto a fast-spinning proto-Earth can produce a Moon-forming disk derived primarily from Earth's mantle
Read as an abstract only.
What this does not establish
Established from the publication records and abstracts; the papers themselves were not read.
Claim 41 · checked 24 September 2026 · AI-assisted audit
Claim: In one the impactor is much larger than the canonical Mars-sized body, comparable in mass to the proto-Earth, and the collision leaves a disc with the composition of Earth’s mantle.
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.5, Half-Earth impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Review of the field
The source reads: Somewhat asymmetric collisions with an impactor whose mass is > 40% of the Earth’s mass can produce disk-planet compositional differences as small as
Context
Forming a Moon with an Earth-like Composition via a Giant Impactabstract (PMC author manuscript)
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026
The source reads: Here we simulate impacts involving larger impactors than previously considered. We show these can produce a disk with the same composition as the planet’s mantle
Read as an abstract only.
What this does not establish
In simulation; the impactor holds more than 40 per cent of Earth’s mass in the successful cases.
Claim 42 · checked 24 September 2026 · AI-assisted audit
Claim: In the other the Earth is spinning very fast before a smaller body strikes it, and the Moon forms largely from Earth’s own mantle.
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.4, Fast-spinning Earth impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Review of the field
The source reads: Relatively small, fast impactors ... produced potential Moon-forming disks with ... with the disk material originating overwhelmingly from the target’s mantle
Context
Making the Moon from a Fast-Spinning Earth: A Giant Impact Followed by Resonant Despinningabstract
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026
The source reads: typical last giant impacts onto a fast-spinning proto-Earth can produce a Moon-forming disk derived primarily from Earth's mantle
Read as an abstract only.
What this does not establish
In simulation; it assumes an Earth spinning near its breakup limit before the impact.
Claim 43 · checked 24 September 2026 · AI-assisted audit
Claim: Both leave the pair turning too fast, and both rely on a later resonance between the Moon and the Sun to shed the excess.
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.4, Fast-spinning Earth impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: Both require a subsequent dynamical mechanism to bring the system to the present-day angular momentum
Context
Forming a Moon with an Earth-like Composition via a Giant Impactabstract (PMC author manuscript)
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026
The source reads: Such impacts require subsequent removal of angular momentum from the Earth-Moon system through a resonance with the Sun as recently proposed.
Read as an abstract only.
Context
Making the Moon from a Fast-Spinning Earth: A Giant Impact Followed by Resonant Despinningabstract
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026
The source reads: a faster-spinning early Earth-Moon system can lose angular momentum and reach the present state through an orbital resonance between the Sun and Moon
Read as an abstract only.
What this does not establish
The later reduction of spin is a separate calculation from the impact itself.
Claim 44 · checked 24 September 2026 · AI-assisted audit
Claim: Later work finds the resonance can do that only in a limited range of conditions, and a 2026 study that follows the young Earth as it cools finds it unlikely to manage alone.
- Kind
- What scholars argue. A report of what specialists argue, or where they disagree.
- Review
- Source checked. The cited passage was read, and it says this.
Canup, an author of the 2026 study, proposed one of the two 2012 models.
Supports
Origin of the Moonsection 6, Conclusions and open issues
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: Interaction of the Moon with the evection resonance can enable the needed angular momentum extraction for limited parameter regimes ... but whether this is likely for realistic models of the post
Supports
Earth’s Rapid Rotation and Magma Ocean Solidification Drastically Limit Angular Momentum Removal by the Evection Resonance After a High-angular-momentum Moon-forming Giant Impacttitle, publication line and abstract
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Model
The source reads: Earth’s Rapid Rotation and Magma Ocean Solidification Drastically Limit Angular Momentum Removal by the Evection Resonance ... published 2026 September 2 ... in all cases the Moon exits evection before enough AM is removed from the system
Context
Earth’s Rapid Rotation and Magma Ocean Solidification Drastically Limit Angular Momentum Removal by the Evection Resonance After a High-angular-momentum Moon-forming Giant Impactsection 4, Conclusions
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026
The source reads: The evection resonance between the Earth, Moon, and Sun is one of only two mechanisms (the other is discussed below) shown to be potentially capable of the required AM extraction.
What this does not establish
One modelling study; its authors list caveats about the atmosphere and the Moon’s tidal properties, and a second mechanism (an orbital instability) is not tested by it.
Later work looked for
Crossref, 2021 on, "evection resonance Moon angular momentum": Rufu, Canup and Korenaga (2026) find the Moon leaves the resonance too early in every case they model; page updated.
Corrected
24 September 2026. Previously: “” Added: the review finds the resonance works only for limited parameters, and Rufu, Canup and Korenaga (2026) find it unlikely to remove enough spin on its own.
Claim 45 · checked 24 September 2026 · AI-assisted audit
Claim: Other routes exist: vapour mixing the disc with Earth after the impact, a Moon built from many smaller impacts, and a hot, vaporised, fast-spinning body called a synestia.
- Kind
- Hypothesis. A proposed explanation, not an established one.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 2.3
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: it has been argued that the Earth–Moon similarity in O isotopes could reflect isotopic equilibration between the terrestrial magma ocean and protolunar disk via the vapor phase
Supports
Origin of the Moonsection 3.7, Multiple impacts
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: In the Rufu et al. (2017) multiple impact model, the Moon forms from a sequence of medium- to large-size collisions
Supports
Origin of the Moonsection 3.6
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: Lock and Stewart (2017) and Lock et al. (2018) found that a wide range of giant impacts produce a so-called synestia – a partially vaporized, rapidly rotating and distended planetary body
What this does not establish
Each is proposed, not established; the review calls the likelihood of mixing highly uncertain.
Later work looked for
Crossref, 2021 on, "Moon-forming giant impact" and "immediate origin of the Moon": Kegerreis and others (2022) and Fischer and others (2024) add routes; nothing found that selects one model. The 2021 review by the models’ own authors is the most recent field-level account read.
Corrected
24 September 2026. Previously: “A third option arrived in 2022, from simulations run with far more particles than the earlier ones: on some impacts a satellite of the right mass and iron content is placed into orbit within hours, rather than accreting from a disc, and its outer layers come out around sixty per cent proto-Earth material.” The 2022 result was not the third option: mixing (2007), multiple impacts (2017) and synestias (2017) were already proposed. And only the outer layers reach 60 per cent proto-Earth; the whole satellite is 30 to 40 per cent (Kegerreis and others, section 3.3).
Claim 46 · checked 24 September 2026 · AI-assisted audit
Claim: In 2022 simulations run with far more particles than the earlier ones found that some impacts place a satellite of about the right mass and iron content into orbit almost at once, rather than accreting it from a disc.
- Kind
- Experimental result. What an experiment or trial found, under its own conditions. A result in animals, cells or a simulation is not a result in people.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Immediate origin of the Moon as a post-impact satelliteabstract
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Model
The source reads: Above a high resolution threshold for simulations, we find that giant impacts can immediately place a satellite with similar mass and iron content to the Moon into orbit far outside the Earth’s Roche limit.
Supports
Immediate origin of the Moon as a post-impact satellitesection 1, Introduction
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Model
The source reads: here with orders of magnitude more particles, we find that stable satellites are produced
What this does not establish
A simulation result, above a resolution threshold; the authors say later evolution needs bespoke study.
Later work looked for
Crossref, 2021 on, "Moon-forming giant impact" and "immediate origin of the Moon": Kegerreis and others (2022) and Fischer and others (2024) add routes; nothing found that selects one model. The 2021 review by the models’ own authors is the most recent field-level account read.
Claim 47 · checked 24 September 2026 · AI-assisted audit
Claim: Its outer layers come out around sixty per cent proto-Earth material, though the satellite as a whole is still mostly impactor.
- Kind
- Experimental result. What an experiment or trial found, under its own conditions. A result in animals, cells or a simulation is not a result in people.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Immediate origin of the Moon as a post-impact satelliteabstract
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Model
The source reads: the outer layers of these directly formed satellites are molten over cooler interiors and are composed of around 60% proto-Earth material
Supports
Immediate origin of the Moon as a post-impact satellitesection 3.3, Satellite compositions and interiors
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Model
The source reads: Here, the immediate satellites typically have moderately higher bulk compositions of around 30–40% proto-Earth material.
What this does not establish
In simulation. If the layers later mixed, the authors estimate the Moon would be little better matched than in the canonical model.
Later work looked for
Crossref, 2021 on, "Moon-forming giant impact" and "immediate origin of the Moon": Kegerreis and others (2022) and Fischer and others (2024) add routes; nothing found that selects one model. The 2021 review by the models’ own authors is the most recent field-level account read.
Claim 48 · checked 24 September 2026 · AI-assisted audit
Claim: Each works under some set of conditions.
- Kind
- This page’s reading. A judgement the page makes from the evidence. Others read it differently.
- Review
- A judgement, not a fact. Reviewed for whether it is fairly put and follows from the checked claims. No source can confirm it.
Follows from the review’s account of each scenario and its requirements.
Supports
Origin of the Moonsection 6, Conclusions and open issues
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: Current models provide an array of possible solutions, but all involve conditions whose likelihood appears small or remains highly uncertain.
Corrected
24 September 2026. Previously: “All three work in simulation. None has been singled out by the samples, and each requires conditions that have to be assumed rather than derived.” The judgement is now the review’s, in its words, rather than the page’s.
Claim 49 · checked 24 September 2026 · AI-assisted audit
Claim: None has been singled out by the samples
- Kind
- Open question. Something the page says is not known.
- Review
- Presented as open. The page says this is unresolved, and the review found that it is.
Supports
Origin of the Moonsection 6, Conclusions and open issues
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: Current models provide an array of possible solutions, but all involve conditions whose likelihood appears small or remains highly uncertain.
Claim 50 · checked 24 September 2026 · AI-assisted audit
Claim: and a review written by several of the models’ own authors says all of them involve “conditions whose likelihood appears small or remains highly uncertain”.
- Kind
- Quotes a source. The words of a named text, checked against the source.
- Review
- Source checked. The cited passage was read, and it says this.
Canup, Ćuk, Stewart, Lock and Rufu, among the review’s authors, proposed several of the models described.
Supports
Origin of the Moonsection 6, Conclusions and open issues
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: Current models provide an array of possible solutions, but all involve conditions whose likelihood appears small or remains highly uncertain.
Claim 51 · checked 24 September 2026 · AI-assisted audit
Claim: The evidence and the awkwardness
- Kind
- Framing. Signposting. It asserts nothing a source could check.
Claim: The Moon has a tiny iron core.
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 1, Introduction
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Review of the field
The source reads: The Moon has a tiny core, perhaps with only ~ 1% of its mass, in contrast to Earth whose core contains nearly 30% of its mass
Supports
Moon FactsStructure
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Reference work
The source reads: The Moon’s core is proportionally smaller than other terrestrial bodies' cores. The solid, iron-rich inner core is 149 miles (240 kilometers) in radius. It is surrounded by a liquid iron shell 56 miles (90 kilometers) thick.
Later work looked for
Crossref, 2022 on, "lunar inner core radius": Briaud and others (Nature, 2023, abstract) give an inner core radius of 258 ± 40 km, consistent with NASA’s 240 within its uncertainty; page unchanged.
Corrected
24 September 2026. Previously: “The Moon has almost no iron core.” The core is small but real (review; NASA).
Claim 53 · checked 24 September 2026 · AI-assisted audit
Claim: It formed from mantle material, after a body had already separated its metal into a core.
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.1.1, Constraints
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: It is typically assumed that a successful impact must produce an iron -depleted disk, although alternatively the disk could evolve into an iron-depleted state via post-impact vapor mixing with the Earth’s mantle
Other readings
The review notes the disc could instead have become iron-poor by vapour mixing with Earth’s mantle after the impact.
Claim 54 · checked 24 September 2026 · AI-assisted audit
Claim: Earth and Moon share isotopic ratios to high precision.
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Measurement
The source reads: the Earth and Moon are within ... 0.2 ± 1.6 ppm isotopically identical
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Review of the field
The source reads: Many elements (O, Si, S, Ti, Cr, and W) show distinct, partly mass-independent isotope heterogeneity among solar system bodies (planets and asteroids) but show no (O, Si, S, Ti, and Cr) or only very small (O and W) differences between the Earth and Moon
Later work looked for
Crossref, 2021 on, "oxygen isotope Earth Moon": Fischer and others (PNAS, December 2024) find no Earth-Moon difference at 0.2 ± 1.6 ppm and no heterogeneity among lunar rock types, against Cano and others (2020); page now reports the 2024 result.
Claim 55 · checked 24 September 2026 · AI-assisted audit
Claim: Either the Moon is mostly Earth, or the impactor was a twin, or the collision mixed both thoroughly.
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Argument
The source reads: The isotope identity of Moon and Earth, as illustrated in diagram Fig. 3 requires either Theia and proto-Earth having the same composition (16), vigorous mixing of Theia and Earth after the Moon-forming impact (37–39), or a combination of both.
Supports
Origin of the Moonsection 3.2, Canonical impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: In general, a canonical Moon-forming impact requires either an impactor with an Earth ... or that the compositional signature of the impactor in the disk was erased by vapor mixing
What this does not establish
These are the routes the sources list; they can also combine.
Claim 56 · checked 24 September 2026 · AI-assisted audit
Claim: The pair carries a large amount of angular momentum.
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 1, Introduction
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Astronomical observation · Review of the field
The source reads: The Earth-Moon system has a high total angular momentum, implying a rapidly spinning Earth when the Moon formed
Later work looked for
A measured property of the system; not something later work revises.
Claim 57 · checked 24 September 2026 · AI-assisted audit
Claim: An oblique collision.
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.1.1, Constraints
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: An oblique collision(s) is a natural source of Earth’s early rapid spin
What this does not establish
An inference from the spin, not an observation of the impact.
Corrected
24 September 2026. Previously: “A grazing collision.” The canonical impact is at 40 to 50 degrees (review, section 3.2), oblique rather than grazing.
Claim 58 · checked 24 September 2026 · AI-assisted audit
Claim: The difficulty is that the versions which fit the isotopes leave extra spin that something must later remove.
- Kind
- What a model says. What a theory or model predicts or describes, which is not the same as what has been observed.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.4, Fast-spinning Earth impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: which could satisfy the oxygen isotopic data even in the limit of a Mars -like composition impactor ... Both require a subsequent dynamical mechanism to bring the system to the present-day angular momentum
What this does not establish
Whether the extra spin could be removed is unresolved; see the passage above.
Corrected
24 September 2026. Previously: “The difficulty is that the versions which fit the isotopes leave too much spin to shed.” “Too much to shed” said it could not be removed; the review says it must be, and that whether it could is unclear.
Claim 59 · checked 24 September 2026 · AI-assisted audit
What would settle it
Claim: What would settle it
- Kind
- Framing. Signposting. It asserts nothing a source could check.
Claim: The models differ in how much impactor they leave in the Moon, so measuring the isotopes more precisely in more elements is one lever.
- Kind
- What scholars argue. A report of what specialists argue, or where they disagree.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 3.2, Canonical impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Review of the field
The source reads: In canonical impacts, most of the disk, typically ... 70 to 80%, originates from the impactor's mantle
Supports
Origin of the Moonsection 3.5, Half-Earth impact
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · A simulation · Review of the field
The source reads: Somewhat asymmetric collisions with an impactor whose mass is > 40% of the Earth’s mass can produce disk-planet compositional differences as small as
Supports
Origin of the Moonsection 2.3
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: Future data may better constrain the relative Earth -Moon oxygen isotopic compositions.
Corrected
24 September 2026. Previously: “The isotopic difference the theories predict is small, and measuring it more precisely in more elements is the main lever.” The canonical model predicts a large difference, not a small one; and the review lists Venus, and the physics of mixing and spin loss, alongside better measurements.
Claim 61 · checked 24 September 2026 · AI-assisted audit
Claim: Another is Venus: if a planet that size proved isotopically Earth-like, an Earth-like impactor would look less like luck.
- Kind
- What scholars argue. A report of what specialists argue, or where they disagree.
- Review
- Source checked. The cited passage was read, and it says this.
Supports
Origin of the Moonsection 6, Conclusions and open issues
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: If Venus proved Earth-like, the likelihood of an Earth-like impactor would be increased
Claim 62 · checked 24 September 2026 · AI-assisted audit
Claim: So is sampling the parts of the Moon the Apollo and Luna collections do not cover.
- Kind
- This page’s reading. A judgement the page makes from the evidence. Others read it differently.
- Review
- A judgement, not a fact. Reviewed for whether it is fairly put and follows from the checked claims. No source can confirm it.
Follows from the argument, reported in the review, that samples from deeper in the Moon may differ from the surface.
Supports
Origin of the Moonsection 2.3
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Review of the field
The source reads: a robust conclusion is that the Earth and shallow Moon have ... 17O values within ~0.01‰ (10 ppm) of each other, whereas samples derived from the deeper lunar interior exhibit differences up to about 20 ppm
Supports
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Measurement
The source reads: The rocks that were brought back by the Apollo astronauts were all collected from the lunar surface.
Claim 63 · checked 24 September 2026 · AI-assisted audit
Claim: The far side has now been sampled.
- Kind
- Historical claim. A statement about the past that historical evidence can test.
- Review
- Partly checked. Only part of the source could be read. What was not read is listed.
Supports
A sample of the Moon’s far side retrieved by Chang’e-6 contains 2.83-billion-year-old basaltabstract
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026 · Artefacts and sites · Measurement
The source reads: The Chang'e-6 (CE-6) spacecraft collected samples from the South Pole-Aitken (SPA) basin on the farside and brought them to Earth.
What this does not establish
Only the abstract was read. One site, in the South Pole-Aitken basin.
Corrected
24 September 2026. Previously: “The far side is no longer one of them.” One far-side site has been sampled; the far side is not covered.
24 September 2026. Previously: “The far side has now been sampled once.” The Chang’e-6 abstract says samples were collected from the far side; it does not say this is the only time, so "once" is gone.
Claim 64 · checked 24 September 2026 · AI-assisted audit
Claim: Chang’e-6 returned material from the South Pole-Aitken basin, and a 2024 study dated basalt from it at 2,830 million years, give or take five.
- Kind
- Observation. Something measured or seen, as the named source reports it.
- Review
- Partly checked. Only part of the source could be read. What was not read is listed.
Supports
A sample of the Moon’s far side retrieved by Chang’e-6 contains 2.83-billion-year-old basaltabstract
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026 · Artefacts and sites · Measurement
The source reads: The Chang'e-6 (CE-6) spacecraft collected samples from the South Pole-Aitken (SPA) basin on the farside and brought them to Earth.
Supports
A sample of the Moon’s far side retrieved by Chang’e-6 contains 2.83-billion-year-old basaltabstract
Cited · Link answered, 19 October 2026 · Abstract only, 24 September 2026 · Artefacts and sites · Measurement
The source reads: We used lead-lead and rubidium-strontium isotope systems to date low-titanium basalt in a CE-6 sample, finding a consistent age of 2830 (±5) million years.
What this does not establish
Only the abstract was read; the date is for one basalt sample.
Later work looked for
Crossref, 2024 on, "Chang’e-6 farside basalt age": a separate team (Zhang and others, Nature, November 2024) dated Chang’e-6 basalt at about 2.8 billion years in the same weeks, so the page no longer calls this the first date; a 2025 Science abstract gives a U-Pb age of 2823.0 ± 5.9 million years, consistent.
Corrected
24 September 2026. Previously: “Chang’e-6 returned material from the South Pole-Aitken basin in 2024, and the first basalt dated from it came out at 2,830 million years, give or take five.” Another team published a date in the same weeks, so “first” is not supportable; and the year is the study’s, which the sources read carry.
Claim 65 · checked 24 September 2026 · AI-assisted audit
Claim: The deep interior is still out of reach.
- Kind
- This page’s reading. A judgement the page makes from the evidence. Others read it differently.
- Review
- A judgement, not a fact. Reviewed for whether it is fairly put and follows from the checked claims. No source can confirm it.
No returned sample comes from the deep interior; what is known of it is inferred from volcanic rocks with deep sources.
Supports
Origin of the Moonsection 2.3
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Artefacts and sites · Review of the field
The source reads: a robust conclusion is that the Earth and shallow Moon have ... 17O values within ~0.01‰ (10 ppm) of each other, whereas samples derived from the deeper lunar interior exhibit differences up to about 20 ppm
Claim 66 · checked 24 September 2026 · AI-assisted audit
Claim: It is waiting on ideas as much as on rocks.
- Kind
- This page’s reading. A judgement the page makes from the evidence. Others read it differently.
- Review
- A judgement, not a fact. Reviewed for whether it is fairly put and follows from the checked claims. No source can confirm it.
Follows from the review’s list of open issues, which includes theory as well as samples.
Supports
Origin of the Moonsection 6, Conclusions and open issues
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: The potential for planet-disk equilibration and theoretical, numerical and/or observational tests for or against equilibration.
Supports
Origin of the Moonsection 6, Conclusions and open issues
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: Interaction of the Moon with the evection resonance can enable the needed angular momentum extraction for limited parameter regimes ... but whether this is likely for realistic models of the post
Corrected
24 September 2026. Previously: “This is a question waiting on rocks rather than on ideas, which is an unusual and comfortable position for a planetary science problem.” The review’s open issues include the physics of mixing and of spin loss, not only new samples.
Claim 67 · checked 24 September 2026 · AI-assisted audit
Claim: Whether vapour could really have mixed the Moon and Earth, and whether the resonance could shed as much spin as the models ask of it, are both still open.
- Kind
- Open question. Something the page says is not known.
- Review
- Presented as open. The page says this is unresolved, and the review found that it is.
Supports
Origin of the Moonsection 6, Conclusions and open issues
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: The potential for planet-disk equilibration and theoretical, numerical and/or observational tests for or against equilibration.
Supports
Origin of the Moonsection 6, Conclusions and open issues
Cited · Link answered, 19 October 2026 · Read in full, 24 September 2026 · Review of the field
The source reads: Interaction of the Moon with the evection resonance can enable the needed angular momentum extraction for limited parameter regimes ... but whether this is likely for realistic models of the post
Claim 68 · checked 24 September 2026 · AI-assisted audit
What was read
- Forming a Moon with an Earth-like Composition via a Giant ImpactCanup, Science · PMC6476314 author manuscript via NCBI efetch, which carries only the abstract; Crossref record for issue and dateAbstract only, 24 September 2026 · Copyright; quoted briefly
- The proto-Earth as a significant source of lunar materialZhang and others, Nature Geoscience · Abstract from the nature.com dc.description tagAbstract only, 24 September 2026 · Copyright; quoted briefly
- Moon FactsNASA Science · science.nasa.gov/moon/facts, as served on the access dateRead in full, 24 September 2026 · Public domain (NASA)
- Making the Moon from a Fast-Spinning Earth: A Giant Impact Followed by Resonant DespinningĆuk and Stewart, Science · Europe PMC record abstract; Crossref record for issue and dateAbstract only, 24 September 2026 · Copyright; quoted briefly
- Evaporative fractionation of volatile stable isotopes and their bearing on the origin of the MoonDay and Moynier, Philosophical Transactions of the Royal Society A · PMC4128272 author manuscript via NCBI efetch, which carries only the abstractAbstract only, 24 September 2026 · Copyright; quoted briefly
- A sample of the Moon’s far side retrieved by Chang’e-6 contains 2.83-billion-year-old basaltCui and others, Science · Europe PMC record abstractAbstract only, 24 September 2026 · Copyright; quoted briefly
- Immediate origin of the Moon as a post-impact satelliteKegerreis and others, The Astrophysical Journal Letters · arXiv:2210.01814, draft of 6 October 2022 (accepted version)Read in full, 24 September 2026 · CC BY 4.0 (published version)
- Origin of the MoonCanup and others, New Views of the Moon II (Reviews in Mineralogy and Geochemistry), accepted version · arXiv:2103.02045v1 (2 March 2021), accepted version; published as chapter 2 of New Views of the Moon 2 (De Gruyter, 2024), doi 10.1515/9781501519895-005. Read sections 1, 2.1, 2.3, 3, 4.7, 5.5 and 6.Read in full, 24 September 2026 · Copyright; quoted brieflyThe PDF text layer splits some words ("Ea rth"); excerpts keep the text as served.
- Oxygen isotope identity of the Earth and Moon with implications for the formation of the Moon and source of volatilesFischer and others, Proceedings of the National Academy of Sciences · PNAS 121(52), e2321070121; Europe PMC full text PMC11670184Read in full, 24 September 2026 · CC BY-NC-ND 4.0
- Earth’s Rapid Rotation and Magma Ocean Solidification Drastically Limit Angular Momentum Removal by the Evection Resonance After a High-angular-momentum Moon-forming Giant ImpactRufu, Canup and Korenaga, The Astrophysical Journal · The Astrophysical Journal 1008:175 (2026), published PDF from iopscienceRead in full, 24 September 2026 · CC BY 4.0The PDF text layer runs some words together; excerpts are taken from clean passages.