Folding paper to the Moon: how many folds is that, really?
Fold a 0.1 mm sheet 42 times and the stack passes the Moon. Drag the thickness across its whole range and that number barely moves. So which slider is doing the work?
Planimeter · Model grade A — arithmetic and probability — this one is either right or wrong · Reviewed 2026-09-26
In January 2002 Britney Gallivan folded a sheet of paper in half twelve times. She was a high-school student in Pomona, California. The standing claim was that no sheet folds more than seven or eight times. She worked out her own equations for the limit first, then went and did it.
A second story about paper runs the other way. Fold a sheet forty-two times, people say, and the stack reaches the Moon. Both stories are about one sheet. Both are arithmetic anyone can check.
They are about two different quantities. One is thickness and the other is length. The chart and the rail below follow the thickness; the length shows up once, as a single readout.
In this model, only the stack of layers is counted — the area halves at every fold, and it is not tracked.
The folds move the answer. The sheet barely does.
There are two sliders. Starting thickness sets how thick the flat sheet is. Folds sets how many times it is folded in half. Three buttons above them jump to preset settings, and one more control, Vertical axis, draws the same numbers two ways.
At 0.10 mm and 42 folds the model puts the stack at 4.398 × 10⁸ m. That is about 439,805 km, which the readout rounds to 439,800 km. The Moon is at 384,400 km, so the stack is past it. Fold 41 falls short, at 2.199 × 10⁸ m.
In this model, one fold is one doubling, so a sheet ten times thicker is worth only about three folds.
Now leave Folds alone and drag Starting thickness from end to end. The whole range is a factor of ten. The crossing moves from fold 43 to fold 40, and no further. For the Moon, ten times the paper buys three folds.
So the model does not make this a fact about paper being thin. In this model the answer is moved mostly by the number of folds; across its whole range, the sheet you start with moves it by three.
Nothing speeds up along the way, either. The doubling rate at fold 3 and at fold 43 is the same. What changes is the axis under the curve, and here is how to read it.
How to read what you are looking at
Almost everything on screen is one number — the height of the stack — drawn three ways. The Length needed card is the one figure from a different formula, explained below. The large number beside the badge gives the height. A badge names the last thing the stack has grown past, or the first one it has yet to pass. Drag Folds and the number doubles at every step. The badge moves far more slowly. It changes only when the stack crosses a marked height, up or down.
Under the readout, the rail puts that same height on a fixed ruler. The ruler is marked in powers of ten and never rescales. A position on it means the same thing at every setting. Each power of ten on it is ten times the one before; on a narrow screen only some of them carry a label. So every fold slides the marker the same distance. The ticks above the rail are the flat sheet and each fold made so far. The dots are the marked heights, filled in once the stack has passed them.
The chart plots that same height against fold count. The Vertical axis toggle is the point of the page. On Linear the axis has to reach the largest value on screen. Once the fold count is high, the early folds are pinned flat against zero. Many of those values are not small: at the default setting, fold 30 is already 107 km. They are small next to the last one. On Logarithmic the same numbers become a straight line with no bend anywhere.
The table at the end lists the first fold that passes each height. One line of arithmetic produces all of it.
Why a tenfold sheet buys at most four folds
A fold doubles the number of layers. That is the whole model.
t=t0·2 to the power of n
t0
thickness of the flat sheet — the Starting thickness slider
n
how many times it is folded — the Folds slider
t
thickness after n folds — the number on the readout
2 to the power of n
how many layers are stacked on each other
The layer count is what doubles. Thickness follows, because the layers sit on one another. Nothing else enters: not the width of the sheet, not the material, not the direction of the folds.
Multiplying t0 by ten is worth log2(10) ≈ 3.32 folds. The whole thickness slider is a factor of ten from end to end. So it moves most answers by three folds. Sometimes four, where that leftover 0.32 crosses one more doubling: a standing adult, a 10-storey building and Mercury's orbit shift by four. The grain of sand shifts by one, because the thickest sheet is already past it.
Each fold adds the same amount to log2(t). The exponent grows in a straight line. The thickness does not. A logarithmic axis is spaced by the exponent, so the model draws a ramp with no bend. A linear axis is spaced by the thickness, so the same numbers look like nothing and then a wall. The exponent is easier to trust once one sheet is counted by hand.
Forty-two folds, counted by hand
Take the default sheet, 0.10 mm, and follow one number.
Seven folds gives 2⁷ = 128 layers. That is 128 × 0.1 mm = 12.8 mm, about a paperback. Fifteen folds is 32,768 layers, or 3.28 m, the first fold past a standing adult. Twenty-seven folds reaches 13.4 km and clears Mount Everest at 8.85 km. Thirty-two folds reaches 429.5 km and passes the model's 400 km mark for the space station.
Each fold is the one before it doubled. Fold 15 and fold 27 differ by a factor of four thousand. On a linear chart that must also fit fold 42, the two sit in the same row of pixels.
Ten more doublings from fold 32 gives fold 42: 429.5 km × 2¹⁰ ≈ 439,805 km.
In this model, counting by hand and raising two to the power of the fold count are separate routes, and they land on the same number.
The exponent gets there in one step and lands on the same number. The readout shows 4.398 × 10⁸ m, and the Layers card shows 4.4 trillion. That is 2⁴² sheets standing on each other. All of it rests on four rules.
Four rules, and eighteen marked heights
Every thickness on this page follows these four. Drop any of the first three and the thicknesses worked out above stop meaning what they say.
Each fold doubles the layer count, and does nothing else.
The layers are perfect: no trapped air, no squashing, no paper lost to the curve at a crease.
The stack is the only thing tracked. Width, material and fold direction do not enter.
The starting thickness is a slider, not a constant. ISO 534 fixes how paper thickness is measured. It does not fix what it is for a given weight.
No simulation. Every thickness is that one line of arithmetic worked out directly. Each multiplication is by a power of two. Only the exponent of the stored number changes, and no rounding error builds up.
The eighteen heights. The marks run from a grain of sand to the Sun. There is one for every power of ten in between. Several are set by a standard, and the model uses the standard's figure as written, among them:
a bank card, 0.76 mm nominal — ISO/IEC 7810
a sheet of A4, 297 mm — ISO 216
the astronomical unit, 149,597,870,700 m — IAU 2012 Resolution B2
Where no body has fixed it, the mark says so on screen. A grain of rice is a round 6 mm and varies by variety. The space station is entered at about 400 km. At the default sheet, a mark entered a little differently can move its fold count by one. A grain of rice longer than 6.4 mm takes a 7th fold, and a station above 429.5 km takes a 33rd. Length is a different matter.
Whether the folding is possible. This is the largest gap on the page. It is not a correction but a different model. The formula Gallivan derived for folding in one direction is
L=π t6×(2 to the power of n + 4)×(2 to the power of n − 1)
L is the length of material needed and t its thickness, in the same units. At 0.10 mm that puts twelve folds at 879 m of paper. Forty-two folds need 1.013 × 10²¹ m. That is around a hundred thousand light years.
The two formulas take the same sheet and the same fold count. Neither one's answer feeds the other. The thickness model has no length term at all. It will report fold 42 for a sheet the size of a postage stamp. Nothing here argues that a sheet can be folded any particular number of times.
Folds that alternate. Folding along alternate sides, rather than always along the same side, is a separate case. Later work has derived lost-length formulas for it, on square and rectangular paper. Only the single-direction case appears here; that extension is not in this model.
The folklore, and the slider. No primary source was found for the seven-fold claim. This page does not attribute it to anyone. The Folds slider stops at 50. Far past that, the stack outgrows what a stored number can hold.
Every computed figure here comes from the two formulas above, worked out directly rather than simulated. How I check things.
Sources.
Ivars Peterson, "Folding Paper in Half—Twelve Times", Science News, 22 January 2004 — the January 2002 fold, and Gallivan's own equations for the limit.
Britney C. Gallivan, How to Fold Paper in Half Twelve Times (Historical Society of Pomona Valley, 2002) is the source of the length formula. No copy could be consulted, so it is reported here rather than verified.
Kabir Srivastav, "Paper Folding: Extensions of Gallivan's Formula", in Proceedings of the 11th IRC Conference on Science, Engineering and Technology (Springer, 2026) — generalizes Gallivan's model and derives lost-length formulas for alternate-side folding, on square and rectangular paper.
The marked heights that come from a document follow ISO 14688-1 (the silt/sand line), ISO/IEC 7810, ISO 216, the R&A rule on the minimum golf ball diameter, the World Athletics rule on track length, the FAI's 100 km Kármán line, the IUGG mean Earth radius, the ITU figure for geostationary orbit, IAU Resolutions B2 (2012) and B3 (2015), and NASA fact sheets for the Moon and Mercury. Each of those figures is used as written, with two changes: the IUGG mean radius, 6,371.0087714 km, is entered as 6,371 km, and the Sun's width is twice the IAU nominal solar radius of 695,700 km. The standing adult, the building, the grain of rice, the airliner and the space station are round figures chosen for this page; the station's 400 km sits inside NASA's 370–460 km range. ISO 534 covers how the starting thickness is measured. ISO/IEC 7810, ISO 216 and ISO 534 are reported from published descriptions rather than checked against a copy, and ISO 14688-1 was read in its free preview.
Mount Everest at 8,848.86 m is the snow height announced jointly by Nepal and China on 8 December 2020, taken from contemporary news reports rather than from a survey document.
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