Fun With Science  /  Globe Deconstruction  /  Claim #3 · pages 166, 169

The Selenelion, and the Photograph at p. 169

A lunar eclipse with the Sun already up — what the word actually means, and a photograph whose geometry the model got right before anyone measured it.

How precise the picture measurements are, and why. The photograph has been measured twice: once off a 300 dpi render of the book page, and once off the image the book actually embeds, pulled straight out of the file at its own resolution. The two disagree by about a fifth on the two circle-fit quantities — and by only two to four per cent on the coverage and the arc span — because the Moon in that image is only about sixty-six pixels across, so the bright rim’s bloom is a large fraction of it. Both readings are given below and neither is close to a phase. Everything else on this page is computed from JPL’s DE421 and is reproducible from the scripts named in each caption.

The Moon list at p. 166 reads: “A partial lunar eclipse and the Sun can be seen in the sky at the same time. This is called the selenelion eclipse and is conveniently explained away with, you guessed it, REFRACTION.” The emphasis is ours, and it is worth keeping, because “partial” is exactly what Santa Fe got: the deep partial, with totality arriving after the Moon had set. It is worked on the facing page: p. 169 is a photograph captioned “taken at sunrise in the Santa Fe area, looking toward Los Alamos,” with the verdict: “The heliocentric model dictates that the ball’s shadow would be on the bottom of the Moon. Here we see the opposite.”

Everything on this page is about Earth’s shadow falling on the Moon. The same entry at p. 166 carries a second Moon complaint — that “the moon-tilt illusion explanation is not satisfactory” — and the spread at p. 168 works that one. It is a different mechanism entirely: the lit side of an ordinary Moon and which way it appears to point, the Moon’s own shadow on itself rather than ours on it. Running the two together is what makes the spread hard to answer, so they are answered separately. That one is at The Moon-Tilt Illusion, which is still in draft and has not been through the review pass this page has — so read it as work in progress rather than as an answer.

The observation: accurately reportedp. 169: its premise about the heliocentric model is wrongAs a discriminator: decides nothing
Where this lands

The photograph is not a photograph: it is a frame from moon observations, an unlisted upload on the book’s own Shape Debate channel, carrying Steve Matthews’ footage of the eclipse of 10 December 2011. Its description of the scene is accurate throughout. We computed the eclipse from JPL’s DE421 and then measured the frame: the dark edge cutting the disc fits a circle of 2.52 Moon-radii centred 1.86 radii away, against 2.65 and 1.99 computed for 06:47 MST, with 83% of the diameter covered either way. That is Earth’s umbra, where the ephemeris puts it. What fails is not the photograph but what the book says the model predicts: the heliocentric model does not dictate a side at all. It computes one per eclipse, from where the Moon crosses the shadow — the top for 10 December 2011, the bottom on other dates from that same spot. There is no favourite side to catch it contradicting. As for the p. 166 entry itself — that a selenelion is “conveniently explained away” with refraction — the eclipse owes refraction nothing. It ran identically for everyone who could see the Moon at all. What refraction buys is only the seam: a thin band along the day/night line, present at almost every umbral eclipse, where both bodies clear opposite horizons at once. Standing in this thin band at the day/night terminator is all a selenelion is, and the bending that opens it is the same ordinary half-degree that ends every sunset at that spot on any day of the year — about 25′ per body needed here, against a textbook 34.5′ — roughly three-quarters of it. Less bending than every sunset already supplies, not more.

And it settles nothing either way. Where a shadow falls on a disc is a projection effect, present in identical form under any model of the Earth’s shape. It cannot count for or against one, whichever way it comes out.

One thing at the outset, because it shapes everything below: that eclipse did have a selenelion, but neither the p. 169 frame nor the video it comes from caught it. The eclipse ran three and a half hours; the selenelion at Santa Fe was under two minutes at the very end of that, and the camera was elsewhere for all of it. What the book prints is an eclipsed Moon in a twilight sky — which is what an umbral eclipse looks like from almost everywhere, and is not the thing the word names.

Before any of the arithmetic, here is what the video actually shows.

A still from the Santa Fe segment of the video: a thin bright crescent, lit along its lower edge and dark across the top, hanging in a grey-blue twilight sky above a long snow-streaked mountain ridge, with the lights of a town on the plain at lower right.
The scene at p. 169, from the footage it was taken from. The Moon is lit along the bottom and dark across the top, above the ridge toward Los Alamos. Cropped from a frame of moon observations on the Shape Debate channel, carrying Steve Matthews’ footage. The crop excludes an on-screen ring and cursor the video adds to the left of the Moon; nothing else is altered.

And here is the whole descent that frame came from. Every moon in this strip is our own capture from the same segment — not a photograph of anyone else’s — and every one of them is an ordinary lunar eclipse in a twilight sky.

Nine frames of the Moon captured from the Santa Fe segment of the video, composited on one background plate at their real positions in the fixed camera frame, descending toward the mountain ridge. Each is labelled with its time and the Sun's depth below the horizon, and each is captioned as a regular eclipse. An arrow low and to the right marks where the selenelion happened, after the last exposure.
Santa Fe: nine moons, all of them ordinary. The camera was locked off for the whole sequence, so these are the Moon’s real positions in the frame rather than a designed layout. The selenelion ran 07:02:23–07:04:22, after the last of them — and from this camera it was behind the ridge before that. Frames extracted from the Santa Fe segment; times matched to each frame’s eclipse phase against the JPL DE421 table, good to a few minutes rather than to the second. Built by the local agent; method and caveats in notes/REPORT-descent-figure-video-build-2026-08-31.md.

A selenelion is not a kind of eclipse

With that in mind, it is worth being plain about something the word hides, because the p. 166 entry treats a selenelion as an exotic event the model has to explain away, and it is nothing of the sort.

There is no special kind of eclipse behind the word. A lunar eclipse is the Moon passing through Earth’s shadow, 380,000 km away, and it runs identically for everyone who can see the Moon at all. Nothing about 10 December 2011 was unusual. What was mildly unusual was where one edge of its audience fell.

Start with who sees a lunar eclipse, because the answer is simpler than intuition expects. In a solar eclipse the Moon’s shadow falls on the Earth, in a strip barely a hundred kilometres wide, and you have to be standing in it. In a lunar eclipse the shadow falls on the Moon, and you need nothing but line of sight — and since a full Moon stands opposite the Sun, “line of sight to the Moon” means “standing in the night.” A lunar eclipse visibility map is a map of night.

Now the word itself, which is simpler than it sounds. To be in Earth’s shadow at all, the Moon has to be very nearly opposite the Sun — that is what an eclipse is. So if the Sun is coming up on your eastern horizon, the eclipsed Moon is going down on your western one, at the same moment. If “opposite” were exact, and if the two were points, and if there were no air, you would miss it by a hair: the Moon would set at the very instant the Sun rose, so you would see one or the other with no overlap at all — never both at once.

Three things give you slack, and none of them has anything to do with the eclipse. The Moon is not exactly opposite — it runs a degree or so off. Both discs have width, half a degree each. And near the horizon the air lifts every image by about another half-degree, so both are still showing after the bare geometry has parted them. Add those together and there is a thin strip of the planet, a degree or two wide, running along the day/night line, where the two just overlap. What that buys you in practice is a couple of per cent of wiggle room at the very fringe of an otherwise ordinary eclipse — a few minutes out of three and a half hours, in which you just might catch the Sun and the Moon on opposite horizons at once. Standing in that strip is a selenelion. It is not a property of the eclipse; it is a property of where you stood.

Counted properly, on that day:

QuantityValue on 10 December 2011
Where the Sun’s upper limb is up — cap radius90.843° from the sub-solar point
Where the Moon’s upper limb is up — cap radius89.906° from the sub-lunar point
How far apart those two centres were178.4° to 179.6°
So the overlap was1.1° to 2.3° wide — never zero, and narrower than most, because a total eclipse is a central one
across the whole run, first penumbral contact to last; the widest figure is at the ends and the narrowest at greatest eclipse

The Moon’s cap is the smaller of the two because of parallax: standing on the surface rather than at the centre of the Earth costs the Moon 0.92° of altitude, more than its semidiameter and refraction together give back. The Sun, four hundred times further off, loses nothing worth counting.

Two things follow, and between them they are the whole content of the word.

Every umbral eclipse has one. The overlap in that table never goes to zero. It is narrowest at greatest eclipse, when the Moon is closest to the anti-solar point, and on 10 December 2011 even there it was 1.1°. The floor is lower for a more central eclipse than this one — a perfectly central pass, with the Moon dead on the anti-solar point, leaves the two cap radii less 180°, about three quarters of a degree at this lunar distance and two thirds at perigee. Lower, but never zero, which is the part that matters. There is nothing to arrange and nothing rare about it: the band is simply the seam where the night side ends.

And the Earth turns underneath it. At any single minute the band is a hairline. Over the three and a half hours between first and last umbral contact the planet rotates 53°, and the hairline sweeps.

Two places are marked on the map below, because the rest of this page turns on them: Santa Fe, where the frame at p. 169 was shot, and Cahokia in Illinois, where the same video’s second observer set up his camera 1,443 km east. The band’s eastern edge runs between them.

A world map shaded by how many minutes each place had the risen Sun and the eclipsed Moon above opposite horizons on 10 December 2011. A broad S-shaped swath runs from the north-west Pacific down across the Americas and the South Atlantic, palest at its eastern edge and deepening westward, covering 27 per cent of the planet by area. A single dark line inside it marks the band at one minute, 14:03 UT. An inset of North America shows Santa Fe well inside the swath and Cahokia just outside its eastern edge.
The shading counts minutes with both bodies up. Twenty-seven per cent of the planet, by area, got some overlap that morning — a median of five minutes where it happened at all, and a longest anywhere of 153 minutes, out on the polar rim, where the Moon rode far enough north of the Sun to hang about for hours. Sun and Moon upper limbs, 34.5′ horizon refraction, lunar parallax removed, sea-level horizon, no terrain. Computed on a quarter-degree grid at ten-second steps from JPL DE421 by scripts/selenelion_band_map.py, reading the sub-solar point, the sub-lunar point and both cap radii from docs/selenelion/data/eclipse-2011-12-10-3d.json.

And it is worth seeing what kind of object that band is, because it is not an exotic one. Measure longitude from the Sun instead of from Greenwich — hold the Sun still and let the Earth turn underneath — and the band takes its place in a family the reader already knows.

The same morning drawn in a Sun-fixed frame, so the Sun sits at the centre of the map and the twilight zones become fixed bands. Working outward from the daylit region there is a pale civil-twilight band, then nautical, then astronomical, then night. A thin dark line, the selenelion band, hugs the sunrise edge of the daylight, far narrower than any of them. Both observers appear as horizontal dashed lines crossing the bands from night into day, with their narrated times marked; a magnified inset of the dawn side shows both men inside the wide civil-twilight band, Santa Fe's 07:02 mark reaching the dark line and Cahokia's 07:04 mark stopping just short of it.
A twilight band and a selenelion band are the same kind of thing. A twilight band is where the Sun is a given distance below the horizon; the selenelion band is where the Sun has cleared one horizon and the eclipsed Moon has not yet left the other. Both are strips along the day/night line, both sweep west at fifteen degrees an hour, and the selenelion one is the narrower: civil twilight is a ring 6° of arc wide, and the band that morning ran 1.1° to 1.7° through the umbral phase — the hours this page is about — tucked against the sunrise edge. Counted from first penumbral contact instead it reaches 2.3°, since the band is at its widest when the Moon is furthest from the shadow’s centre. Which settles what the two men were filming. In the magnified panel both spend the whole of their footage inside the wide grey band, walking toward the narrow dark one — Santa Fe reaching it at 07:02, Cahokia stopping short at 07:04. “The sky is getting brighter” is civil twilight arriving; the Sun is below the horizon for every frame either of them shot, which is why neither ever films it. The seam on the dusk side is the same band with the roles swapped, the Moon rising as the Sun sets. Drawn by scripts/twilight_band_map.py.

So a selenelion is the Moon sitting a degree or so off the shadow’s dead centre, plus the half-degree of lift the air gives every image at every horizon — the same half-degree that makes every sunrise arrive a couple of minutes early. There is no “dramatic bending” anywhere in it — only that half-degree, which anyone with a horizon and a clock measures daily. The rest is not merely possible. It is required: a spinning globe with an atmosphere has to lay this band down at every umbral eclipse, and the model would be in trouble if it did not. All that is uncommon is where the band happens to fall.

Where the photograph comes from

It is not a photograph. It is a frame from a video — and the footage is not Miller’s, though the upload the book links is.

Put the book’s crop beside a frame from the upload its p. 167 QR code reaches and it is plainly the same footage: the same snow-streaked peak with the same shoulder, the same secondary summit to its right, the same pattern of snow on the left flank, the same strung-out town lights below. The book uses a tighter, brighter crop, which is also why the image is soft. The upload’s own title card credits Steve Matthews; Sources has the channel, the date and the rest of the paperwork.

What matters here is not the paperwork but where that upload sits: on Shape Debate, the book’s own channel. Its description is where the p. 169 claim is written out:

“Forgot to include the biggest debunk of all, the impossible ‘selenelion’ eclipse. Sun is rising in the east, looking at moon towards the west, the ‘shadow’ is on the top instead of the bottom! How?????”

So the credit needs running in both directions. The observation is Matthews’, and so is the conclusion he draws from it in the narration — at 19:34 he says the footage “definitely proves this is not caused by the so-called ball.” But that description is not something the book inherited. It was written on the book’s own channel, over footage collected there, and its escalation — the biggest debunk of all, impossible, How????? — is this side of the argument in its own voice. p. 169 then prints the same claim with a premise attached: that the heliocentric model requires the shadow on the bottom.

None of which takes anything away from what the observation gets right, and we would rather say that plainly than leave it implied. The shadow really was on the top. The eastern sky really was brightening. The p. 169 caption locates the scene correctly, and this page will confirm each of those in turn. Nothing here is a case of anybody seeing badly. The error is in the sentence about what the model requires — and that sentence is the book’s own.

On our side it changes one thing: credit for the observation belongs to Steve Matthews, and we would rather say so than let a frame of his work sit here unattributed.

What a lunar eclipse looks like from the ground, and from anywhere else

Before measuring anything, it is worth being clear about what the photograph is a picture of, because the honest difficulty in this claim is not arithmetic.

From the ground you cannot see that the Moon is entering a shadow. You see a dark edge creeping across a disc. The cone is invisible, the alignment is invisible, and the diagrams meant to help are drawn from a viewpoint nobody has ever occupied. That is a real complaint and it deserves better than a wave. So here are both at once, from the same numbers.

From the side
His sky, as refraction delivered it
The same sky, with refraction switched off
04:00
Moon Sun umbra centre covered

10 December 2011 over Santa Fe, every frame computed from JPL’s DE421 — three views of one instant, not an illustration of one. From the side is the textbook diagram, with the stick figure standing where the camera was and the dashed line from his feet marking his “up”. The angle marked at his feet is the Moon’s altitude — the same number the sky panels plot and the readout prints — and it closes to nothing as the Moon sets (the view is distance-compressed, so the arc points rather than measures). The camera sits well south of the Sun–Earth–Moon line and looks at it almost edge-on; the Earth is drawn as a plain ball, so its tilt is not something to read off this picture. Notice what this view cannot tell you on its own: which side of the Moon goes dark. His sky is that same instant as he saw it, and there the bite on top stops being a claim. The same sky, refraction off is the same sum with one term removed. The altitude axis is stretched near the horizon because all of this is a fraction of a degree; the hollow markers show where each body would have been without the air.

Run it once and watch the first panel. The Moon slides into the cone, and nothing in that view tells you which side goes dark — which is the challenge with a good many of the common diagrams, all of them flattening a three-dimensional arrangement onto a page. Then look across to the third. The geometry has not changed by a hair. Only the direction you are looking from and which way is up — and now the answer is in front of you, and it matches the sky panel underneath.

The one-line rule that settles which side

Earth’s shadow points directly away from the Sun. So the centre of that shadow, projected on the sky, is the point exactly opposite the Sun. If the Sun is a degree below your horizon, the centre of Earth’s shadow is a degree above it, in the opposite direction. There is no more to the calculation than that. Strictly that rule is written from Earth’s centre, and the page has just docked the Moon 0.92° for standing on the surface rather than at the centre — so from your spot the shadow’s centre is about that much lower than the rule says. It does not matter here, because the shadow’s centre sits at the Moon’s distance and is displaced by the same 0.92° as the Moon itself. The two move together, the offset between them is untouched, and the table below computes both in one consistent frame rather than applying the rule by hand.

The standard lunar-eclipse diagram, drawn in the observer's frame. Earth's penumbra and umbra are concentric circles with the anti-solar point at the centre. The Moon's disc is drawn at five moments along a track that climbs from lower right up into the umbra. In every position the Moon sits below the shadow's centre, so the dark part of each disc is at its top and the lit part at its bottom; by the last position, at moonset, only a thin rim along the bottom is still lit.
The Moon came up into the shadow from below, so the bite is on top. This is the ordinary eclipse diagram — shadow fixed, Moon moving across it — with one change: up is the observer’s zenith, not the plane of the orbits. That is the only frame in which the p. 169 question can even be asked, and it is the frame the textbook version throws away. The Moon’s distance from the shadow’s centre and its position angle are both measured in it; nothing is rotated by hand. The shadow’s centre is the anti-solar point, and it stood above the Moon all morning and sank faster — 12.2° an hour against the Moon’s 11.7° — so the umbra’s edge reached the top of the disc at first contact, 05:46 MST, and worked down. That centre is a direction anyone can check without a telescope: it is the same anti-solar point as the dark band that rises in the east at every sunset. The track stops at the horizon — the Sun rose at 07:02, the Moon set at 07:04 with a rim still lit, and totality began two minutes later out of sight. Drawn by scripts/shadow_track_figure.py.

The whole eclipse, as it stood over Santa Fe

The umbral phase began at 05:46 MST. The Sun’s upper limb cleared the horizon at 07:02:23, and the Moon’s upper limb dropped below it at 07:04:22 — one minute fifty-nine seconds with both bodies in the sky at once, on a level horizon with standard refraction. That overlap is the selenelion. The Moon was 98% swallowed when the Sun came up and all but entirely inside the umbra as it went down; totality itself began at 07:06, after the Moon had set, and then ran its course below the horizon — so northern New Mexico saw the deep partial and missed the red phase.

Each limb is refracted at its own altitude here, and positions are apparent — light-time and aberration included — because the question is where each body was seen. Refracting the disc’s centre and then adding the semidiameter, which treats the disc as rigid, puts each upper limb about 2.2′ too high near the horizon: refraction is weaker up there than at the centre. That is the same error that used to sit in the shadow-edge figure above, and correcting it shortens this window by about forty seconds. Dropping aberration would shorten it by a further two.

MSTMoon alt / az
apparent
Sun alt / az
geometric
Shadow centre, from the Moon’s centreTilt from straight upDiameter covered
04:4026.00° / 279.6°−28.15° / 99.2°1.414°15.4° left
05:4613.41° / 287.8°−15.13° / 107.6°0.913°10.3° left1% — first contact
06:158.08° / 291.5°−9.58° / 111.4°0.706°5.0° left42%
06:403.66° / 294.8°−4.92° / 114.8°0.544°3.6° right74%
06:541.34° / 296.7°−2.36° / 116.8°0.466°11.3° right90%
07:02:230.08° / 297.8°−0.85° / 117.9°0.426°17.4° right98% — the Sun rises
07:04:22−0.20° / 298.1°−0.49° / 118.2°0.418°19.0° right99% — the Moon sets

Altitudes are of the disc centres, and the two columns are on deliberately different conventions. The Moon’s are apparent — refraction included — because it was in the sky and the question is where it was seen; in the last row its centre is just under the horizon while its upper half is still showing. The Sun’s are geometric, because for most of the morning it was below the horizon, and a body below the horizon has no apparent altitude to quote: no ray from it reaches the eye, and the standard refraction formula is not defined down there. That is also why the Sun is still 0.85° below the horizon in the row where it rises — 34.5′ of refraction lifts the disc and its own 16′ radius does the rest, which is the budget the refraction section below works through in full. Position angles are measured in the observer’s own frame: straight up in the photograph is straight up in the table.

The umbra crosses the Moon from the top throughout. Its centre never departs from the vertical by more than 20° while the Moon is up, so at no point in the eclipse, from that place, could the shadow have been on the bottom.

The photograph at p. 169, reduced

The photograph is a lunar eclipse — the selenelion of 10 December 2011, which the book’s own list raises two lines above the moon-tilt entry. So the claim is testable in the strongest sense available: the geometry was fixed by the date, we can compute it, and then we can measure the picture and see whether the two agree.

Everything above was computed without reference to the picture: the umbra covered the Moon from the top all morning, leaving a thin bright rim along the bottom. Now the picture. We fitted circles to the two edges of that rim — twice, off two different renderings of the same photograph, so that the measurement carries its own error bar rather than a single figure with an implied precision it does not have.

QuantityMeasured — 300 dpi page renderMeasured — the book’s own embedded imageComputed for 06:47 MST
±3 min — see the bloom note
A phase would give
Radius of the dark edge cutting the disc2.52 × the Moon’s radius2.132.6511.00 — a half-ellipse on the disc itself
Its centre, from the Moon’s centre1.86 Moon-radii1.441.9910 — the Moon’s own centre
Its position angle from straight up+4.6°+5.3°+7.6°
How much of the diameter is covered83%85%83%
How far the lit rim runs around the edge105.5°101.2°117.6°exactly 180° — the horns of a phase are a diameter

Two measurements of the same photograph, by the same script, differing only in what was fed to it. The page render is what a reader looking at the printed book is looking at; the embedded image is the 799 × 470 raster the file actually contains, which the render upsamples about three-fold. Upsampling adds no information, so the gap between the two columns is not resolution — it is where each run puts the edge of a bloomed rim on a disc sixty-six pixels wide. That spread — about a fifth on the first two rows, two to four per cent on the coverage and the arc — is the honest error bar on this measurement, and it is wider than we would like. It is also nowhere near wide enough to matter: every reading in both columns is a large circle centred well outside the disc, and the thing being ruled out sits at 1.00 and 0 and 180°.

The Moon is about 213 px across in that render, upsampled from sixty-six in the file itself, and the image is soft, so the bright rim blooms outward. The circle fits themselves are tight — 0.50 px rms on the Moon’s outer edge and 0.68 px on the dark one, against a 107 px radius — but that tightness is a fit statistic, not an accuracy. Re-run on the embedded raster the two circle quantities move by about a fifth, which is the number to trust: a rim that blooms shifts where the edge is, and no amount of tight fitting to the wrong edge fixes that. The coverage and the arc span are far steadier, at two and four per cent.

Four quantities, computed before they were measured, agreeing to within a few per cent. The dark edge in the photograph is a circle two and a half times the size of the Moon, centred just under two Moon-widths away, almost exactly above it. That is Earth’s umbra, at the size and in the place the ephemeris puts it — the round shadow of the Earth falling across the Moon, which is not a shape any phase of the Moon produces.

And round is doing more work here than it looks, because a circular shadow is only automatic when the thing casting it is a ball. On 10 December 2011 the anti-solar point — the direction Earth’s shadow points — stood 67° from the celestial pole. A flat Earth turning about that pole was therefore being lit from well off to one side, and would have laid down an ellipse roughly two-fifths as tall as it is wide. The edge in this frame fits a circle to better than one per cent. That is a measurement of the Earth’s shape, taken from a photograph the book prints itself, on a date the book chose.

Nor can something else be standing in for the Earth. The alignment does not merely permit Earth’s shadow to be there — it requires it. At an umbral eclipse the line from the Sun to the Moon passes through the Earth: that morning it missed Earth’s centre by 0.39 of an Earth radius. Sunlight heading for the Moon therefore runs into the Earth, and the shadow lands whether anything else is present or not. A rival occulter would have to sit where the Earth already is and intercept that sunlight before it arrived — which is to say, stand between us and the Sun and cause a solar eclipse instead.

And the cosmology this project has endorsed does not offer a rival occulter anyway. The book itself declines to advance a positive model — but its launch video carries a geocentric introduction by another presenter, which the author endorses as representing his own thinking, and that one commits to a self-luminous Moon. Under a Moon that makes its own light, an eclipse is not a shadow at all. It is the Moon dimming. That has to be said out loud, because it is a much harder thing to defend than an occulter. The dimming would have to be circular; sized to Earth’s cross-section at the Moon’s distance and not some other size; entered from the edge that faces away from the Sun and left by the other; timed to the exact instants of syzygy; and — this is the part the survey table below supplies — landing on the top of the disc in December 2011 and the bottom in June 2012, from the same back garden in New Mexico, for no reason available to a lamp. Every one of those is a free parameter under a self-luminous Moon and a consequence under a shadow. The table is the same table that answers p. 169; it happens to answer this too. We are quoting no wording from that introduction here, because this site’s rule is to cite it by timestamp only once each quotation has been checked against the audio rather than an automatic transcript. What is described above is its position, not its phrasing.

The model does not merely accommodate this photograph. It predicted its geometry — including the part the caption calls impossible.

The same video contains a second observer location, and the model predicts that too

Later in the video a second observer’s footage is shown from the same morning, and it provides an extremely useful correlation — a second, independent test of what the globe model predicts.

He is standing on top of Monks Mound at Cahokia, just east of St Louis — 1,443 km east of Santa Fe — and he narrates the clock as he films. His segment runs from 20:03 in the video, where the presenter introduces him, to 21:56. Everything he says is checkable, and it checks:

AtWhat he saysWhat the ephemeris gives for that spot
20:2206:30 — “a full moon which will soon be going into a… eclipse as it sets”the umbra has not touched it; first contact 06:46 CST
20:31“at the same time behind us, the sun is already [rising]”Sun 7.3° below the horizon — nautical twilight. The glow is rising; the Sun is not
20:4006:55 — “a little bit brighter out here… you can see the shadow right across the moon”13% of the diameter covered; Sun 2.9° down, civil twilight
21:2007:04 — “you can hardly see anything, but… we can just barely make out a little bit of the moon”Sun’s upper limb 0.4° below the horizon; Moon’s 0.4° above
21:34“it’s about two-thirds the way covered with earth’s shadow, and it’s turning a pale orange, pinkish colour”26% covered — his one overestimate
21:40“with the bright morning sun coming up, there’s not enough contrast to be able to see the moon there”

Two of those are quantities rather than impressions — not yet touched at 6:30, a bite at 6:55 — and both land. The third does not: at 7:04 he calls the Moon two-thirds covered when the umbra had taken a quarter of it. That miss is worth keeping rather than smoothing away, because it points the same way as everything else here. Overshooting by that much is what happens when you are trying to read a disc that has become a bright smudge in a brightening sky — which is what he says he is doing, in the very next breath.

Set against that, he is a careful reporter, working in the dark with a hand-held camera and calling what he sees, and it is worth saying so before anything is said about the conclusion he draws from it.

And here is the part worth keeping. The shadow is on the top for him too — he says so, and reports the same surprise. But it is tilted the other way. At any moment when both men could see the Moon, the umbra’s centre sits to the left of Cahokia’s vertical and to the right of Santa Fe’s: same Moon, same shadow, same minute, and about eight degrees of difference in how it is tilted, purely because the two men stand in different places and their verticals point in different directions. On a flat plane that difference would be zero — not small, but exactly zero, because on a plane every vertical is parallel to every other and a distant object shows the same tilt from everywhere on it. Each man’s own footage differs by more than that — nearer thirty degrees — but the two clips are three quarters of an hour apart, so most of that gap is the eclipse advancing rather than the distance between them. Eight degrees is the part that is purely about where you stand, and it is the part that matters here.

The same eclipse diagram as the Santa Fe figure, drawn for Cahokia, Illinois: Earth's umbra as a fixed circle with the Moon crossing below it. The line from the Moon to the shadow's centre leans 15 degrees to the left of the observer's vertical, where the Santa Fe version leans 7 degrees to the right.
The same shadow, the same minutes, tilted the other way. Drawn to exactly the same scale as the Santa Fe figure above, from the same ephemeris, in the second observer’s own horizontal frame. Nothing about the eclipse has changed between the two pictures — only which way “up” points for the man holding the camera. His track is also much shorter, because his Moon set at 07:07 with only a third of it covered, where Santa Fe’s reached 99%. Same source and conventions as the figure above; scripts/shadow_track_figure.py.

That is the whole of the moon-tilt idea, arriving unbidden inside the exhibit meant to refute it: how a thing in the sky is tilted depends on where you are standing.

Be careful about what has and has not been measured here. The qualitative prediction is tested at two stations at once and passes at both: the shadow is on top for each man, and each says so. The eight degrees is a different kind of statement — it is what the geometry predicts, not something read off the footage. Cahokia’s camera is hand-held and pans between the presenter and the sky, and a hand-held frame cannot fix which way is up; that is why discs 5 and 6 in the strip below are drawn from the ephemeris rather than captured. A tripod at Cahokia would have let us check it. What the pairing is still worth: the two men filmed independently and had no knowledge of each other, and putting their clips side by side was the video’s own editorial choice, made to argue something else. A model that merely accommodated the first clip would have nothing to say about why the second should be rotated at all. This one says eight degrees, before you look.

Moving a hundred kilometres either way changes the tilt by under two degrees, so nothing here is sensitive to the exact spot. Monks Mound is the largest earthwork north of Mexico and about thirty metres high, which is what “standing on top of” refers to.

Neither camera, and neither observer, caught the Sun and the Moon above opposite horizons at once

Which brings back the band from the top of this page, and the edge of it that runs between these two men. It settles something the video never thinks to ask.

The window at Santa Fe opened at 07:02:23. The frame the book prints at p. 169 is fixed at 06:47 by its own eclipse phase — a quarter of an hour earlier, with the Sun still 3.6° below the horizon. At Cahokia the Sun’s upper limb cleared the horizon at 07:06:58 and the Moon’s dropped below it at 07:07:04: an overlap of under six seconds, which is to say none at all. He was standing on the seam and fell on the wrong side of it.

Santa FeCahokia
Sun’s upper limb clears the horizon07:02:23 MST07:06:58 CST
Moon’s upper limb drops below it07:04:22 MST07:07:04 CST
Simultaneous view1 min 59 sunder six seconds — in practice none
The footage we are actually shown06:47, Sun 3.6° below06:30 to 07:04, Sun 7.3° to 1.4° below
So the sky in it iscivil twilightnautical twilight, then civil
And the camera’s own skylinemountains — Moon gone from 06:54flat floodplain west, bluffs east — see the note below
Where the umbra sat, from his own vertical8° right of straight up19° to 15° left of straight up

At Santa Fe the window was behind a mountain. The frame is a long-lens shot of the skyline toward Los Alamos, and the Moon in it is its own ruler: its angular diameter that morning is known to four decimals, so a circle fitted to the lit outer arc calibrates the picture in degrees per pixel with nothing else assumed — no focal length, no sensor size, no claim about exactly where the tripod stood. The fitted disc is 183 pixels across; the skyline directly beneath it is 323 pixels lower. That is a different image at a different scale from the p. 169 measurement above, where the Moon came out about 213 px across on the 300 dpi book render — which is why the two sections quote different pixel counts for the same Moon. That is 0.885°, and the Moon has to fall all of it plus its own radius before the disc is gone. There are about seven minutes of Moon left in the shot. Dating the frame at 06:47 from its eclipse phase, it was behind the ridge by 06:54 — and the Sun did not clear even a flat horizon until 07:02:23. He stood inside the band and could not have seen it from where he stood.

The Santa Fe video frame with measurements drawn on it: a red circle fitted to the eclipsed Moon's lit outer arc, a cyan line along the mountain skyline directly beneath it, and a white bar between them labelled 323 pixels or 0.885 degrees.
The Moon is its own ruler. Fitting a circle to the Moon’s own outer edge calibrates the frame; the drop to the skyline then gives the ridge’s apparent height without any camera data at all. Earth’s shadow is drawn on the same picture, and it is not fitted to anything: its size and position come from the ephemeris at 06:47, scaled only by that ruler. Its lower edge lands on the crescent’s inner boundary to within eight pixels on a 183-pixel disc, and its centre sits 7° right of the observer’s vertical — which is why the bite is on the top. The seven-minute figure needs no timestamp — it is a distance to fall divided by a known rate of falling — and holds across every plausible dating of the frame, which put the Moon behind the ridge between 06:52 and 06:59. Two things deliberately not claimed: the crescent’s thickness would date the frame independently, but the umbra’s edge is diffuse enough that the answer swings five minutes on the choice of threshold; and the ridge’s height in metres needs a range the frame cannot supply, so no summit is named. Neither affects the result. scripts/santafe_ridge.py; frame from moon observations on the Shape Debate channel.

His whole descent is above. Here is the second man’s, built the same way from the same video — and it ends even further from the event than the first.

Six moons for the Cahokia segment: four real frame captures showing a small round unbitten disc, and two drawn from the ephemeris with dashed outlines because no clean frame of the Moon survives at those times. Labelled with times, and an arrow marking the six-second window he never reached.
Cahokia: the first ones are not even an eclipse yet. The umbra reached his disc at about 06:45, which is exactly what he says on the footage. His own window was 07:06:58–07:07:04 — six seconds, and never on camera. This camera is handheld and pans between the presenter and the sky, so the layout is designed rather than positional, unlike the Santa Fe strip. Discs 5 and 6 are drawn from the ephemeris with dashed outlines because at both of those on-screen times the presenter is facing the camera, not the sky, and no clean frame of the Moon survives.

Both men describe the eastern sky getting brighter, and both are right about that. But a brightening eastern sky is dawn, and dawn is available to anyone facing east on any clear morning; it is not the Sun. The second observer says so himself, at 21:40: “with the bright morning sun coming up, there’s not enough contrast to be able to see the moon there.” By the time his sky was bright enough to argue about, his Moon had gone.

This does not weaken the claim under examination. It sharpens it. The shadow really was on top in both clips, and that is the thing worth explaining, which is what the rest of this page does. But the selenelion is not what either camera recorded: the footage offered as proof of it stops a quarter of an hour short at one station — with a mountain range in the way of the rest — and six seconds short at the other.

Both figures are for a level, sea-level horizon, and at Cahokia the real one is not level — but it leans the other way from the way that would help. Monks Mound does not stand on a bluff: it stands on the American Bottom, the Mississippi floodplain, and the bluffs — the Collinsville escarpment — are four or five kilometres to the east, in the direction he needed the Sun to come from. On published elevations rather than a survey, they put the skyline in the sunrise direction something like a quarter of a degree above level, which delays his sunrise by a minute and a half. His western horizon really is flat bottomland, so the mound’s own thirty metres depress it by 0.16° and hold the Moon up about a minute longer. Run together: sunrise 07:08:27, moonset 07:08:15 — the six seconds do not widen, they close. Anything above a fifth of a degree of bluff does that, so the conclusion does not hang on the exact figure. And in any case, by then his Moon was four tenths of a degree up, a quarter covered, and on his own account invisible.

One more thing the word does badly. The photograph people most often reach for when “selenelion” comes up — Michael Zeiler’s multiple-exposure chain of ten moons dropping toward a ridge, published here — is of this same eclipse, from this same corner of New Mexico. We have not reproduced it, because the point does not need it. The caption printed directly under it says the Sun had not yet come up: “the moon was setting in Los Alamos, N.M., the sun was just about to rise.” So none of its exposures caught the selenelion either — the same answer as the two clips examined above, on the same morning, for the same reason. The photographer and the publication reported it accurately. What does not survive being shared is the caption.

The same morning as a guided 3-D reconstruction: the shadow cone, the terminator, the gold selenelion band, and both observers, driven entirely by the ephemeris dataset behind this section — four short acts, then free exploration. Every window readout above is computed live from the same file. If the interactive version cannot run here, four still posters captured from it stand in.

What the caption gets right, and what it does not

“The ball’s shadow” means Earth’s shadow, which is the reading the book’s usage supports and the correct one here. “Taken at sunrise in the Santa Fe area, looking toward Los Alamos” is right too: Los Alamos bears 303.5° from Santa Fe, the Moon was at azimuth 296°, and at 06:47 the Sun stood 3.6° below the eastern horizon in bright civil twilight — which is the sky in the frame, blue with the snow on the Jemez lit. Nor is the location the book’s inference: the footage carries its own on-screen caption, “View is towards Los Alamos, New Mexico — Vantage point is just north of Santa Fe”, near enough word for word. And the frame can be checked without taking anyone’s word for it, because it carries its own longitude. How deeply the Moon is eclipsed depends only on the clock and is the same everywhere; how far the Sun has climbed depends on where you stand. At 83% covered the Sun is 3.6° down at Santa Fe and 12.3° down at Los Angeles — near darkness, not this. The west coast is excluded twice over: by the time Los Angeles had the Sun up, the Moon there was totally eclipsed, so there was no bright rim left to photograph. Everything in the caption checks out.

The single thing that does not is “the heliocentric model dictates that the ball’s shadow would be on the bottom of the Moon.” It dictates nothing of the kind. It computes which side from where the Moon crosses the shadow, and for 10 December 2011 it says the top — which is what the photograph shows, to within a few degrees. The observation is accurate, carefully described, and correctly located. It is the premise about what the model requires that does not hold, and that is a claim about the model rather than about the sky.

The model has no favourite side

It is worth answering the p. 169 claim on its own terms even though its photograph does not support it, because the underlying idea — that the model commits to one side and can be caught out — is testable and false. Which side goes dark is set by where the Moon crosses the shadow, and it changes from eclipse to eclipse. Here is every morning selenelion visible from Santa Fe between 1995 and 2030, and where the shadow sat on the disc in each.

The list is swept, not assembled by hand: scripts/selenelion_survey.py walks every full Moon in the window, keeps the ones where Earth’s umbra actually touches the disc, and asks of each whether Santa Fe ever had the Sun’s upper limb and the eclipsed Moon’s above opposite horizons at the same instant. Nothing is filtered by judgement, so nothing can be quietly left out. It finds twelve events; the four not shown here are evening ones, with the Moon rising as the Sun set, which is the same seam with the roles swapped. The tilt is measured at the middle of each window — the sequence table above gives 19.0° for 10 December 2011 because it is quoting the very last instant, at moonset, by which time the shadow has rotated a further degree. One near-miss is worth naming, because it shows how fine the edge is. On 15 April 1995 the Sun’s upper limb cleared Santa Fe’s eastern horizon and the eclipsed Moon’s dropped below the western one in the same second — a computed overlap of about a tenth of a second the wrong way — which is the script’s raw output and far inside any real uncertainty, since the limb convention and the morning’s refraction are each worth thousands of times that — with a tenth of the Moon in shadow. On a standard atmosphere it is out by a hair; on a slightly kinder morning it would have been in. Which is the whole point about the band: it is a fact about where you stood and what the air was doing, not about the eclipse.

DateMoon azimuthHow long both were up at onceHow much of the Moon was covered in that timeWhere the shadow sat
28 Jul 1999246.8°7 min 30 s30% of its widthlower left
16 Jul 2000243.4°18 seconds6%upper left
26 Jun 2010239.7°2 min 45 s53%upper right
10 Dec 2011298.0°1 min 59 s99% — a rim still litthe top — 18.2° from vertical
4 Jun 2012242.2°9 min 01 s18%the bottom
4 Apr 2015262.9°6 min 33 s73%the bottom
31 Jan 2018290.7°3 min 42 sall of it — totalthe right side — but total, so no bite
26 May 2021243.4°7 min 08 s84%the bottom

Look down the time column first. Twenty-two years of eclipses, and this spot’s entire lifetime allowance of simultaneous Sun and eclipsed Moon comes to about thirty-nine minutes — the longest a single event ever managed was nine, and one of them lasted eighteen seconds. That is the width of the band, felt as a clock rather than as a number of degrees.

Three of the eight put the shadow squarely on the bottom, which is the appearance p. 169 says the model requires. The model produces that too — on other dates, from the same spot, with the same arithmetic. It also produces the top, the sides and both diagonals. There is no preferred side to be caught contradicting; there is only a date, and an answer.

Yes, it is refraction — and this much of it

That leaves the other half of the p. 166 entry: that the selenelion is “conveniently explained away” with refraction. It is right that refraction is doing real work, and it deserves a straight answer. At Santa Fe, without refraction there would have been no simultaneous view. At the moment their true altitudes crossed, the Sun and Moon were both 0.675° below the horizontal. Neither was up. So how much bending does the explanation need?

That is a fact about that spot, not about the eclipse. Both discs are about half a degree wide, and their width alone opens a band without any refraction at all — up to 1.18° of it, over roughly seven eighths of the morning. It closes only for about three quarters of an hour either side of greatest eclipse, when the Moon sits closest to the shadow’s centre. So refraction widens the seam, roughly doubling it; it does not create it. What refraction did at Santa Fe was decide whether that particular hillside fell inside the band or just outside it.

QuantityValueAs a share of the ordinary horizon lift
What the air actually gives a body at the horizon, standard atmosphere34.5′ — a little over half a degree, 0.58°100% — the everyday amount, and the yardstick for every row below
Lift the two disc centres would have needed40.5′ each — 0.68°117% — more than the air gives, so at this site the two centres never both cleared
Lift the two upper limbs needed — which is what an eye actually sees25.5′ Moon, 24.3′ Sun — 0.42° and 0.41°74% and 70% — about three-quarters of it
So the margin, on the limbs that matterabout 9′ to spare — 0.15°26% left over

That second row is about Santa Fe, not about the eclipse, and it is worth being careful here. Centre-to-centre was perfectly possible that morning — just not there. Because the discs bring their own half-degree to the sum, a centre-to-centre band existed at every moment of the eclipse somewhere on Earth: 0.6° to 1.8° wide, narrower than the limb band above it but never closed. So the reason to work in upper limbs is not that centres are impossible. It is that a limb is what an eye sees — the Sun “rises” when its top edge clears the horizon, not when its middle does, and the same goes for the Moon still setting behind you.

Two panels at the same angular scale. Left: an ordinary sunset, with the Sun's true position drawn as a dashed circle wholly below the horizon and the visibly flattened disc you actually see resting on the horizon line, 34.5 arcminutes higher. Right: Santa Fe at 07:03 MST on 10 December 2011, with the Sun low in the east and the eclipsed Moon low in the west, each shown dashed where it really is and solid where it is seen, lifted 36 and 35 arcminutes respectively.
The same air, and you have already watched it work. Refraction is a horizon effect: it is 34.5′ for a body on the horizon, 5′ at ten degrees up, and 1.5′ where the Moon sits at the start of the animation. That is why nothing visible happens to the Moon for most of that run and everything happens in the last few minutes. Left panel: the lift at the horizon, 34.5′, is larger than the Sun’s own diameter of 32′ — 108% of its own width — so the Sun you watch touch the horizon has already set, entirely, and the 6.1′ by which its lower limb is lifted more than its upper is the flattening in everyone’s sunset photographs. Right panel: both bodies are lifted, 36′ and 35′, not one of them specially. Drawn by scripts/refraction_figure.py.

The shadow is lifted too, and by nearly the same amount. The Moon is raised by refraction as it falls — and so is Earth’s shadow, because the shadow’s place in the sky is fixed by the Sun, so the shadow’s lift is the solar half of the same story. The two run together all the way down: 5′ and 5′ at ten degrees up, 12′ and 13′ at four degrees, 30′ and 32′ near the horizon. Near the horizon the shadow’s edge is lifted slightly more than the Moon — by 2.3′ — because that edge hangs below it and sits in thicker air. That difference is the entire effect of refraction on the eclipse itself: two arcminutes on a 30′ disc, or under 8% of its width, at the very end. It is why the bite looks the same whether you plot the true positions or the seen ones, and why refraction cannot move a shadow from one side of the Moon to the other. Computed by scripts/refraction_tracks.py.

Refraction turns up twice in this event, and it is worth naming the second one because it is the same physics doing a much smaller job. Earth’s shadow is not a clean geometric cone: the air around the planet bends and absorbs light at the edge, so the umbra arrives at the Moon about 2% wider than pure geometry gives — Danjon’s rule, in every eclipse prediction since the 1950s, and drawn as the outer of the two rings in the animation above. It changes how much of the disc is covered by a couple of per cent. It changes which side by nothing at all.

So the ordinary, everyday, textbook number does it comfortably, with room left over. It does not need to be stretched, and no special atmosphere has to be invoked. That is the whole of the “dramatic bending of sunlight” the spread asks about: about half a degree, the same half a degree that makes every sunrise arrive a couple of minutes early and every sunset leave a couple of minutes late, and which has been in navigational tables since long before anyone had a camera.

The observing site is also 2,130 m up, which on a level horizon would depress it a further 1.35° and widen the window considerably. We have deliberately not counted that, because northern New Mexico’s horizons are mountains rather than sea, and the terrain correction could go either way. The numbers above stand without it.

A selenelion photograph measures the refraction it disputes

This is the part we would most like a reader to take away, because it turns the objection into an experiment rather than a stand-off.

Refraction is not uniform. It is strongest right at the horizon and falls off fast with altitude, so it lifts the bottom of a low disc more than the top. That squashes the disc — vertically only, never horizontally. The amount is not adjustable; it follows from the same standard-atmosphere curve used above.

What you photographPredicted shape
The Sun sitting on the horizon32.0′ wide, about 25.9′ tall — flattened by a fifth
A typical 31′ Moon at 0.5° altitudesquashed by 5.0′, 16%
A typical 31′ Moon at 1° altitudesquashed by 3.9′, 12.5%
A typical 31′ Moon at 5° altitudesquashed by 0.8′, 2.6%

Any selenelion photograph shows a Moon within a degree or two of the horizon, so its disc should be visibly oval, and by a stated amount. Measure it and you have measured the refraction the objection says is being invented to cover a gap. Anyone can run the same check on any sunset, in an afternoon. If the setting Sun is a circle, the standard refraction curve is wrong and so are we — and a good deal of surveying and navigation goes with us.

If you do run it on the Sun, use a proper solar filter, and do not look at the Sun through any lens without one. That is first a matter of your eyes, and second a matter of the measurement: an unfiltered image of the Sun is mostly bloom, and bloom is round. Glare spreads the disc symmetrically and will hide the very flattening you are trying to measure, or invent an edge where there is none — so an unfiltered phone shot is not a null result, it is no result. A certified solar film or eclipse-viewing filter over the lens turns the Sun into a clean measurable disc. The Moon needs no filter, and a low full Moon is flattened by the same air in the same way — 16% at half a degree up, per the table above. If you want to do this safely with no equipment at all, do it on the Moon.

What would change our mind

Where this page could be wrong

How to check this yourself

The script that produced every eclipse number on this page, and the frame table the animation is driven from, is in the repository at scripts/selenelion_2011.py. It needs skyfield and downloads JPL’s DE421 ephemeris on first run. It prints the sequence table, the refraction budget, the disc-flattening predictions, the survey of morning selenelions, and four cross-checks against published eclipse elements it did not use:

QuantityOurs, from DE421Published
Greatest eclipse14:32 UT14:33 TD (EclipseWise)
Gamma0.3875−0.3882 (EclipseWise)
Umbral magnitude at greatest1.11591.1061 (EclipseWise)
Magnitude visible at 06:54 MST0.8960.890 (timeanddate)

The sign of gamma is a convention — negative means the Moon passed south of the shadow’s axis, which is what our computation also finds. The small residual in umbral magnitude is the umbra-enlargement rule, where different sources use slightly different conventions.

The picture measurements are checkable too, and both routes are two commands. scripts/measure_p169_moon.py fits the two edges of the rim in whatever image you hand it, so the only difference between the columns above is what you feed it:

# the page as printed, rasterised
pdftoppm -f 196 -l 196 -r 300 -png book.pdf page
python3 scripts/measure_p169_moon.py page-196.png

# the raster the file actually embeds, at its own resolution
pdfimages -f 196 -l 196 -png book.pdf p169
python3 scripts/measure_p169_moon.py p169-000.png

Mind the page number. Book folio 169 is page 196 to pdftoppm and pdfimages — an offset of 27, constant through this chapter and checked at four landmarks — in the copy these commands were run against: the 500-page Canva export of 3 August 2026, MD5 0182065c1fc8cddb431dcaa67d64c8f1. Two cautions. The prerelease circulates in renders whose leading pages differ, so anyone working from another copy should find folio 169 by eye rather than trust 196. And our own text dump of this same file numbers its pages one lower than poppler does, which is where the landing page’s offset of 26 comes from — same copy, two counting tools, one page apart. The folio is the citation; the index is a command-line argument. The second command writes a single 799 × 470 image, which is the whole of what the book has. We are not reproducing that file here — it is the book’s, and anyone with the prerelease can pull it in a second.

Sources & further reading