The site

The shoulder of the great mountain

Mons Mouton is a 130-kilometre massif, the highest mountain of the Moon's south. NASA has listed two Artemis III candidate landing regions on it, targeted its plateau for the VIPER ice rover, and in March 2025 the IM-2 Athena lander touched down on its flank. This site is the plateau's northeastern shoulder: 6,448 metres above the datum, beside the small crater Floss, where the high ground falls away toward the lowlands of Scott. From here the camera looks northwest, far down over the plateau's rim — the visible skyline sits 3.3° below level, and Earth bows into that hollow without ever sinking past its middle.

Property Value
Latitude84.560° S (84° 33′ 36″ S)
Longitude37.650° E (37° 39′ 00″ E)
Height+6,448 m (LOLA laser altimetry)
Distance from the south pole≈ 165 km
Earth's place in the skylow in the northwest, between −3.2° and +11.3°
Skyline under Earth's track−3.3° — looking far down from the heights
Laser-altimetry terrain map of the Mons Mouton massif with the site marked on the northeast plateau shoulder beside Floss crater, a lon/lat grid, and the direction to Earth at the bottom of the map
The mountain, measured by laser: NASA's LOLA elevation model of the Mons Mouton massif with the site marked, oriented so that Earth lies at the bottom of the map — the lon/lat grid shows where you are. Earth stands out over the plateau's rim, down-map. Contours every 500 m.
Close-up LOLA rendering of the southern landing site with lon/lat grid, the 640-metre landing pad and a vector pointing to the exact camera position
The landing site itself: 16 × 16 km on the LOLA 80-m grid, Earth at the bottom, lon/lat grid printed — the 640-metre pad circled and the vector marking the exact camera position, 84.560°S 37.650°E at +6,448 m.

The record

Two centuries, hour by hour

These values come from this project's audit: exact JPL DE440 sky geometry, tested every hour for twenty years against a skyline ray-marched out of NASA's laser elevation maps — and the worst case re-checked across every 18.6-year cycle from 1900 to 2100. Earth is never fully hidden here. Not for an hour. Every number traces to that audit — method, cross-checks and sources on the validation page.

92.5%

Of the time the full disk stands clear of the horizon

7.5%

Of the time the horizon crosses Earth's disk — both worlds in frame

0hours

With Earth fully hidden — in two hundred years of tested sky

+0.24°

Closest the centre ever comes to the skyline — the half-set guarantee

Two hundred years of per-year deepest-bow margins at both featured sites, never approaching the half-set bound
The record, drawn: the deepest bow of every year from 1900 to 2100 at this shoulder (grey; the northern site in white). Earth's centre never comes closer than +0.24° to the skyline — the 2026–2046 window, drawn hour by hour in the gallery below, bottoms out at +0.26° (JPL DE440 + LOLA ray-marched horizons).

The bow

Thirteen bows a year, never past half

From the shoulder Earth circles a small patch of northwestern sky. On nearly every 27.21-day cycle the Moon's nod carries the planet down into the sunken skyline: for about two days the dark plateau rim cuts across the bright disk — ocean, cloud and Moon rock sharing one picture — and then Earth climbs back. At the very deepest bow on record, checked against every year from 1900 to 2100, just over a third of the disk stands below the horizon. The centre never crosses. Because this is a southern site it is the mirror of the north: Earth stands over the opposite horizon, on the opposite phase of the same wobble.

  • 13 bows a year — almost every cycle ends in one; episodes average ~51 hours
  • Deepest bow: 35% of Earth's diameter below the skyline — never half
  • The guarantee survives landing scatter: it holds everywhere within a 640-metre pad
Four months of Earth's elevation at the Mons Mouton northeast shoulder: the white band of Earth's disk bows to the orange laser-measured skyline every 27.2 days, the centre never crossing it
Anatomy of a bow — four months at this site, against its real, laser-measured skyline (orange). The white band is Earth's disk. The lower edge dips behind the horizon on the deep bows; the centre line never touches it. Not every bow is equally deep — the depth breathes over 173 days.

The dial

One mountain carries every picture

Mons Mouton is large enough that where you stand on it chooses the sky. On the central summit plateau, a published JPL full-cycle study found Earth's complete disk clear of the horizon 100% of the time — a portrait that never blinks, and never touches the ground. Down on the south plateau, a European landing study found the opposite: Earth gone entirely between contact windows of roughly 19 days per month. This project's site sits deliberately between those worlds, on the northeast shoulder — the one position found where the horizon takes a real bite of Earth every month, yet can never swallow half of it. Kilometres of plateau, three different skies.

One mountain, three skies: the centre holds Earth forever, the south lets it go — the northeast shoulder makes it bow.
Chart of Earth visibility regimes against lunar latitude, showing the full-disk share falling poleward of 82 degrees, the orange both-worlds band, and the grey hidden region
Why height decides everything here: on level ground, 84.6°S would mean regular full disappearances. This site's 6,448 metres drop the visible skyline 3.3° below level and pull it back into the graze band — every kilometre of height buys about two degrees of latitude.

The southern field

How the south's candidates compare

Every serious southern candidate, tested against one rule: Earth must never sink more than half below the visible horizon — for any epoch, with landing tolerance. Published full-cycle values (JPL, measured terrain) for the classic sites; this project's laser-altimetry audit for the rest. The famous summits fail in opposite directions — one never lets Earth touch the horizon, one lets it sink past the middle. The shoulder between them holds the line.

Site Coordinates Height Full disk Both worlds Hidden Verdict under the half-set rule
Mons Mouton NE shoulder — this site84.56°S, 37.65°E+6,448 m92.5%7.5%0%Selected — margin +0.24°, robust across the pad
Mons Mouton central plateau84.72°S, 39.47°E6,055 m*100%0%0%Passes trivially — Earth never touches the horizon; no bows, no both-worlds frame
Mons Mouton south plateau85.46°S, 31.78°E+6,302 msetsRejected — Earth fully below the skyline between ~19-day monthly windows
Malapert Mons summit86.04°S, 1.70°E4,207 m*94.7%5.3%0%Rejected — never fully lost, but at deep minima the centre crosses the skyline: more than half sinks away
de Gerlache rim88.66°S, ~71°W1,144 m*57.1%13.8%29.0%Rejected — Earth gone ~29% of the time
Connecting Ridge89.39°S, ~138°W1,261 m*51.3%13.8%34.8%Rejected — the Moon's best-lit ground, Earth-poor
Shackleton west rim89.63°S, ~160°W1,072 m*48.4%13.8%37.8%Rejected — iconic, ice-bearing, and Earth-poor

* Published radar-era heights and full-cycle percentages (Bryant 2009, JPL IPN Progress Report 42-176, Table 4; the south plateau row from a 2012 European landing study); the other rows are this project's DE440 + laser-altimetry audit, 2026. The northern half of the field is on the locations page.

Questions

What you need to know about this southern location.

Why this exact position?

Because the mountain's sky changes with every kilometre of position, and this is the one shoulder found where the horizon takes a real bite of Earth nearly every month while the half-set guarantee still holds: the centre stays at least 0.24° above the skyline in every tested year from 1900 to 2100, at every position within a 640-metre landing pad.

Why is height the trick?

At 84.6°S on level ground, Earth would regularly disappear completely. From 6,448 metres the visible horizon drops 3.3° below level — and Earth, riding low, bows into that hollow instead of behind it. Every kilometre of height buys roughly two degrees of latitude; this site spends six and a half kilometres to stand deep in the polar south and still keep more than half of Earth up, always.

How often are both worlds in one frame?

For 7.5% of all hours — about one hour in thirteen, the strongest both-worlds share of any site that passes the half-set rule. Thirteen bows a year on the Moon's 27.21-day nod, each lasting around 51 hours, their depth breathing over 173 days, the full pattern repeating every 18.6 years.

Where does Earth stand in the sky here?

Low in the northwest, drifting through a 17°-wide window between azimuths 314° and 331°, never higher than 11.3° — against a skyline that sits 3.3° below level. The disk is 1.8–2.0° wide. The whole 18.6-year wander fits a fixed lens; nothing ever needs to track.

Is this mountain proven ground?

As proven as the lunar south gets. Mons Mouton carries two Artemis III candidate landing regions; NASA's VIPER rover was targeted at it; the IM-2 Athena lander reached its flank in March 2025. Even its small craters are named — Floss sits 16 km from the site, Masina, Jaci and Dawa on the plateau to the south. The published JPL full-cycle study that mapped its central plateau anchors this page's comparison table.

What is the remaining step before installation?

A metre-class survey of the northwestern skyline. The audit's horizon comes from laser maps at 80–240-metre resolution — good enough to certify the guarantee with margin, but each bow's exact depth still moves by real fractions of a degree with every metre of plateau rim. Extracting a centimetre-grade horizon from orbital stereo imagery is the next phase.

Sources and related pages

The full validation — ephemeris basis, the laser-altimetry horizon method, the pad-robustness test, published-study cross-checks, and the complete source record — is on the validation page and in the downloadable science dossier.