Empirical Earth · We Went to the Moon — the Landings Were Real

382 kilograms of Moon you can hold in your hand

The claim

“There’s no proof anyone went — just pictures.”

What is measured

382 kg of Moon rock (2,196 samples, 110,000+ subsamples) has been studied worldwide for 50 years: dry, vacuum-formed, 3.1–4.5 Gyr old, isotopically Earth-matched. Soviet robotic samples agree. You cannot fake that much alien geology.

What would show this is wrong

a credible demonstration that the Apollo samples are terrestrial or synthetic, or that independent (including Soviet) analyzes disagree on their lunar origin.

Sources

  1. Apollo & Soviet lunar samples. Six Apollo missions returned 382 kg (2,196 samples; 110,000+ subsamples) with radiometric ages of 3.1–4.5 Gyr; three Soviet Luna probes returned ~301 g robotic link
  2. China’s Chang’e-5 and far-side Chang’e-6 lunar samples. Chang’e-5 returned 1,731 g of soil in December 2020, and Chang’e-6 brought 1,935.3 g from the lunar far side (South Pole–Aitken basin) link
  3. The ages of the Apollo lunar samples. Apollo basalts date to ~3.1–3.8 Gyr and highland rocks to ~4.4–4.5 Gyr; a zircon in Apollo 17 sample 72255 places the Moon’s formation at ~4.46 Gyr. The link
  4. The three new lunar minerals. Apollo 11 rocks yielded three minerals new to science — armalcolite (named for Armstrong, Aldrin and Collins), pyroxferroite and tranquillityite; terrestrial oc link
  5. Solar-wind & cosmic-ray signatures in lunar samples. Lunar grains carry implanted solar-wind gases and a solar nitrogen-isotope signature, plus cosmic-ray spallation products and surface-exp link
  6. Lunar oxygen isotopes & the giant-impact origin. Lunar samples share Earth’s oxygen-isotope composition to high precision yet are volatile-depleted — a key constraint behind the giant-impact link
  7. Chang’e-5: the youngest dated lunar basalts. A lead–lead age of 2,030 ± 4 Myr for Chang’e-5 basalts (Li et al., Nature 2021) is the youngest radiometric age for lunar lava, extending lunar v link
  8. Lunar meteorites corroborate the returned samples. Hundreds of meteorites independently identified as lunar — e.g. ferroan anorthosites matching Apollo 16 highlands and mare basalts of 3.1–3 link
The full entry, with the working →

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