82°30′00″ N · 0°00′00″ E

The geometric solution — on the sub-Earth meridian in the north-polar highlands just south of Gioja crater, where Earth hangs permanently at the lowest point it can reach above the horizon while never setting.

The site

On the prime meridian, just south of Gioja crater

This site sits on the prime meridian in the north-polar highlands, just south of Gioja crater, in the worn highland terrain that forms the south-west approaches to Byrd crater. Gioja — about 25 km north-northeast — is the nearest sizeable named feature, with Main and Scoresby to the south-southeast and Byrd and Peary toward the pole.

Coordinate Decimal degrees Degrees-minutes-seconds
Latitude82.50° N82° 30′ 00″ N
Longitude0.00° E0° 00′ 00″ E
This site sits just inside the geometric always-visible zone — only about a third of a degree from its edge — which is exactly why Earth here sinks lower than at any other confirmed location while still never setting, and it works because the ground falls gently away toward Earth, dropping the Earthward skyline below the horizontal so the grazing planet still clears it.
Plot of Earth's full 18.6-year track across the northern site's sky — compass direction against height above the horizon — with the lowest and highest points marked and Earth's disk drawn to scale at its nearest and farthest distances
Earth's complete path across the sky from this site over the Moon's full 18.6-year wobble, shown as compass direction (left–right) against height above the horizon (up–down). Each dot is a moment in the roughly month-long cycle; colour marks where in that monthly cycle it falls. Earth never rises or sets — it drifts within this compact patch low in the sky. Its lowest point (the binding moment) and highest point are marked, and Earth's disk is drawn to scale at its nearest and farthest distances.

Where it is

The northern site on the map

North-pole selenographic projection locating the northern site near Gioja crater, with the always-visible zone edge drawn in green and nearby named craters shown to scale
A north-pole polar projection with the site marked, the always-visible zone edge drawn in green, the named craters shown to scale, and the terrain-clearance margin called out.

Other passing candidates

Other northern locations

The other northern locations that keep the entire Earth disk permanently visible (full-disk passers). The clearance margin shown is the full-disk margin (the stricter test); a dagger marks sites whose margin is not yet robust and still needs high-resolution confirmation.

Coordinates Earth elevation range Clearance margin (full-disk) Binding terrain feature
81.00°N, 0.0°E+1.84° … +15.65°+0.41°ridge +72 m at 6.8 km (az 187°)
80.50°N, 5.0°W+2.19° … +16.14°+0.83°ridge +126 m at 9.2 km (az 181°)
80.50°N, 0.0°E †+2.33° … +16.15°+1.03°local pad rise at <1 km (az 187°)
80.50°N, 15.0°E+1.70° … +16.04°+0.43°ridge +103 m at 11.3 km (az 203°)
80.00°N, 25.0°W+1.34° … +16.15°+1.92°depressed horizon −150 m at 87.5 km (az 147°)
80.00°N, 10.0°W+2.45° … +16.62°+1.63°near-level horizon −5 m at 4.2 km (az 162°)
80.00°N, 5.0°W †+2.67° … +16.64°+2.10°near-level horizon −2 m at 1.1 km (az 183°)
80.00°N, 0.0°E+2.83° … +16.65°+1.58°ridge +14 m at 2.4 km (az 187°)
80.00°N, 5.0°E+2.68° … +16.65°+1.62°ridge +367 m at 26.8 km (az 177°)
79.50°N, 30.0°W+1.24° … +16.30°+1.99°depressed horizon −751 m at 59.5 km (az 142°)
79.50°N, 25.0°E+1.79° … +16.63°+1.00°ridge +41 m at 17.6 km (az 212°)
79.00°N, 15.0°W+3.07° … +17.53°+1.32°ridge +213 m at 9.2 km (az 163°)
79.00°N, 5.0°W †+3.65° … +17.64°+1.74°near-pad rise at 0.3 km (az 182°)
79.00°N, 0.0°E+3.82° … +17.65°+1.54°ridge +74 m at 3.1 km (az 172°)
79.00°N, 5.0°E †+3.66° … +17.65°+2.76°near-pad rise at 0.3 km (az 177°)

† Margin not yet robust — sits at or near the camera pad and still needs a high-resolution (LROC NAC) elevation check before it can be trusted.

Closest to this site's latitude band: 81.00°N, 0.0°E is the nearest neighbour (1.5° of latitude away), followed by the three sites at 80.50°N. Most robust margins: the sturdiest clear full-disk margins belong to sites roughly three degrees nearer the equator — 79.00°N/5.0°E (+2.76°), 80.00°N/5.0°W (+2.10°), 79.50°N/30.0°W (+1.99°) and 80.00°N/25.0°W (+1.92°) — but at all of those, Earth never drops as low as it does here. The selected site deliberately carries the thinnest full-disk margin of the whole group (+0.26°), because it is the geometric-edge site where Earth reaches its lowest possible point: lowest Earth and slimmest margin are the same trade.

Curve showing how tall a ridge at a given distance must be to hide a low Earth, rising with distance as the Moon's surface curves away
How tall a hill or ridge at a given distance would have to be to hide a low Earth. The threshold rises with distance because the Moon's surface curves away; this site's binding feature is in fact a stretch of horizon that sits below the camera (the ground drops away toward Earth), so it falls far under the curve and Earth stays clear by 1.21°.
Map of every candidate tested in the final phase, coloured by terrain-clearance margin from green (comfortable) to red (marginal), with the selected northern site starred
Every candidate tested in the final phase, coloured by how much clear sky stands between the full Earth and the local terrain — green is comfortable, red is marginal. The selected site is starred; ringed points keep the entire Earth disk permanently visible. The northern site sits in the marginal band by design, because that is where Earth rides lowest.

In plain language

What this site actually is

The EXAX project aims to place a single camera on the surface of the Moon and point it permanently at Earth. Not a spacecraft that orbits and looks away every hour, but a fixed eye on solid ground that keeps the whole planet in frame for years on end — a continuous, uninterrupted portrait of Earth as one object in space.

Choosing where to put it is less obvious than it sounds. The Moon always keeps very nearly the same face turned toward Earth, so it is tempting to assume Earth simply hangs motionless in the lunar sky and almost any near-side spot would do. It does not work that way. The Moon does not hold perfectly still as it travels its orbit: it nods and rocks slightly, a slow wobble that swings Earth's apparent position back and forth over a rhythm that takes about 18.6 years to complete. Near the edges of the face we can see, that wobble is enough to drag Earth down to the horizon and, in the wrong spot, briefly behind a hill or crater rim and out of sight. Keeping Earth permanently visible therefore means finding a place where, across the entire 18.6-year cycle and from behind every nearby ridge, the planet never once drops below the local skyline. Settling that took a four-stage investigation: first working out exactly where Earth appears in the sky from each candidate point at every moment, then checking that the real lunar landscape — measured from laser-altimeter maps made from orbit — never rises up to block it.

This particular location lies in the Moon's far north, on the line that points most directly at Earth, in old, worn highland country just south of a crater named Gioja. The ground here is smooth and rounded rather than jagged, and it slopes very gently away in the direction of Earth.

From here Earth never rises and never sets. It hangs low in one corner of the sky and stays there — a large, brilliant ball, roughly three to four times as wide as the full Moon looks from a back garden, and far brighter. Day to day and month to month it drifts slowly within a small patch, tracing a slow loop rather than marching across the heavens; over the years the loop shifts, but Earth always keeps to the same low corner. The camera would catch the planet turning once a day, continents and oceans and weather rolling past, the line between day and night sweeping across its face. And Earth runs through phases, just as the Moon does for us — a slim crescent, a half, a full bright disk — completing the cycle about once a month, always opposite to the Moon's phase in our own sky.

To turn this candidate into a real camera site, the one remaining step is a close-up survey of the ground in the few tens of kilometres toward Earth, mapped finely enough to confirm the exact shape of the horizon down to the last hand's-breadth, so the camera can be set with its view guaranteed clear.

More

The full positional-astronomy and terrain-clearance analysis — ephemeris basis, terrain models, and the complete source record behind this site — is documented in the downloadable science dossier.

Download the dossier (PDF)

Back to both confirmed sites · See the southern site