Wonders of Nature Astronomy & Space No background needed About 6 min read

Why Doesn't the Moon Fall to Earth?
― It Really Does Fall, by 1.4 Millimetres Every Second

Let go of an apple and it falls. So why doesn't the Moon, floating in the sky, fall too? The answer is a little surprising. The Moon is falling. It's just that the ground it is falling toward never arrives.

Published: 2026.10.15 Difficulty: ★☆☆ (no background needed) The only maths is in the fold-out section at the end
First, picture this scene

You are walking home at night. A child points at the sky and asks, "Hey, why doesn't the Moon fall down?"

It is tempting to say, "Because there's no gravity in space." But that is wrong. The Moon goes around Earth because Earth's gravity is pulling on it.

It is being pulled, yet it doesn't come down. Let's untangle this apparent contradiction.

There are only two reasons

1
The Moon falls while racing sideways

The Moon moves sideways at about 1 kilometre every second. In that time it falls about 1.4 millimetres toward Earth. Because Earth is round, the ground curves away by just as much as the Moon falls.

2
It is far away, so gravity is very weak

The Moon is about 60 times Earth's radius away. Gravity weakens with distance, and at the Moon it is about 1/3600 of its strength on the ground. This weak pull and the sideways speed are in exact balance.

So the Moon isn't "not falling". It is "falling and missing Earth, again and again". Let's take it step by step.

Is the Moon really falling?

Throw a ball sideways and it traces a curve and drops to the ground. The harder you throw, the farther it lands. So what if you threw it with absurd force?

Earth is round, so the ground curves downward as you go farther. If the ball is fast enough, the ground curves away faster than the ball falls. The ball keeps falling, yet never reaches the ground. It goes all the way around Earth and comes back to where it started.

The Moon is in exactly this state. Look at Figure 1. The slider changes the Moon's sideways speed.

Earth (size exaggerated) Moon Sideways speed The Moon then… Falls to Earth Keeps circling Earth Leaves Earth Slow → curves in too far Just right → a circle Fast → bulges outward Faster → flies away Dotted circle = Moon's real path
Move the slider to change the Moon's path
Figure 1: The paths of Earth and the Moon. Earth is at the centre left, the white circle above it is the Moon, and the arrow pointing right is its sideways speed. The dotted circle is the Moon's real path. Lower the speed with the slider and the path curves inward and hits Earth. Raise it and the path bulges outward, and above about 1.44 kilometres per second the Moon never comes back.

At zero speed, the Moon drops straight onto Earth. A little faster, and it falls at an angle and still hits. At 1.02 kilometres per second, the curve of its fall matches the curve of Earth exactly, and the path becomes a neat circle. The Moon today travels at precisely this speed.

Newton compared the apple and the Moon

The first person to check this idea with numbers is said to be the 17th-century English scientist Isaac Newton. He wondered, "Could the force that makes an apple fall and the force that pulls on the Moon be the same thing?"

Near the ground, an object falls about 4.9 metres in its first second. The Moon is about 60 times Earth's radius away. If gravity weakens in proportion to the square of the distance, then at the Moon it should be 60×60, or 1/3600 as strong. See Figure 2.

Earth Apple 4.9 m in 1 s From Earth's centre: about 60 Earth radii Moon About 1.4 mm in 1 s (1/3600 of the apple) 60× the distance → gravity 1/(60×60) = 1/3600 That weak pull bends the Moon's sideways path a little at a time
Figure 2: How an apple and the Moon fall. The apple near the ground on the left falls 4.9 metres in one second, as the long downward arrow shows. The Moon on the right, at the distance marked by the dotted line, falls only about 1.4 millimetres in one second, as the tiny line just right of the Moon shows. The ratio is almost exactly 1 to 3600, which fits the idea that gravity weakens with the square of the distance.

Next, we work out how far the Moon falls in one second from its own motion. The Moon circles Earth in about 27.3 days. From the size of that circle and the number of days, we find that it bends inward from a straight line by about 1.4 millimetres every second. And 1/3600 of 4.9 metres is also about 1.4 millimetres. The two numbers agree.

The force that drops the apple and the force that keeps the Moon circling were one and the same gravity. This discovery is said to have led to the law of universal gravitation.

💡 What if the Moon suddenly stopped?

If its sideways speed dropped to zero, the Moon would fall straight toward Earth. By calculation, it would hit in about five days. What protects the Moon is not its height but its sideways speed.

💡 The Moon is actually drifting away

Far from falling in, the Moon is moving away from Earth by about 3.8 centimetres a year. This was found by firing laser light at mirrors left on the Moon during the Apollo missions and timing the return. It is thought that, through the ocean tides, Earth's spin is slowly passing some of its momentum to the Moon.

Summary

Earth's gravity pulls the Moon, and it falls about 1.4 millimetres every second. But it also moves sideways at about 1 kilometre per second, so it keeps falling along Earth's curve and never reaches the ground. Too slow, and it would fall in. Too fast, and it would fly away. The Moon today moves at just the right speed in between.

The Moon isn't failing to fall.
It is falling, and missing Earth, again and again.

The reason bodies float inside a space station is the same idea of "continuous falling" (Is it true that people float on the space station because there's no gravity?). For how far away the Moon really is, see How far away is the Moon, really?, and for how the Moon's gravity moves the oceans, see Why are there two tides a day?.

🧪 Feel "sideways speed" with a string and an eraser
  1. Tie an eraser firmly to the end of a string about 50 centimetres long. Do this in a wide space with no people or breakable things nearby.
  2. Hold the other end and swing it slowly over your head. The string pulls the eraser inward, playing the part of gravity for the Moon.
  3. If you slow down, the eraser can't keep its circle and sags inward. The faster you swing it, the harder your hand has to pull on the string.

You can feel with your hand that a steady circle needs sideways speed and an inward pull in balance. Letting go while it is spinning fast is dangerous, so don't.

For those who want more ― terms, formulas and links to your textbooksEach part is labelled by level, from middle-school science to university courses
How to read the labels below
  • Middle schoolCovered in middle-school science
  • High schoolCovered in high-school physics (circular motion, universal gravitation)
  • High school+Advanced high-school material, or textbook sidebars
  • UniversityNot taught in high school; university courses (mechanics, celestial mechanics)
  • ResearchNot yet settled textbook fact; topics researchers are still investigating

Middle schoolTerms: this phenomenon has names

Middle schoolHigh schoolChecking with a formula: how many millimetres does the Moon fall per second?

We work out the inward acceleration the Moon needs to move in a circle, and the value of ground gravity weakened by distance, and compare them. This is the calculation known as Newton's "Moon test".

⓪ The basic formula
In symbolsv² ÷ r = g × ( R ÷ r )²
In words(Moon's speed squared) ÷ (distance to the Moon) = gravitational acceleration on the ground × (Earth's radius ÷ distance to the Moon) squared
Where it comes fromThe left side is the inward acceleration needed to move in a circle (centripetal acceleration). The right side is the law of universal gravitation, where gravity weakens with the square of the distance. When the two are equal, the Moon keeps circling.
vThe Moon's orbital speed (in m/s)
rDistance from Earth's centre to the Moon (in m)
REarth's radius (in m)
gGravitational acceleration on the ground (in m/s²)
① The starting numbers
Average distance from Earth's centre to the Moonabout 384000 km
Earth's radiusabout 6370 km
The Moon's orbital period (one turn relative to the stars)about 27.3 days
Gravitational acceleration on the groundabout 9.8 m/s²
② Working it out
Diameter of the orbit384000 × 2 = 768000 km
Length of one orbit (π = 3.14)768000 × 3.14 ≒ 2411520 km
Seconds in one orbit27.3 × 86400 ≒ 2358720 s
The Moon's speed (per second)2411520 ÷ 2358720 ≒ 1.02 km
Speed squared (taking 1020 m/s)1020 × 1020 = 1040400
Centripetal acceleration (left side)1040400 ÷ 384000000 ≒ 0.00271 m/s²
Distance in Earth radii384000 ÷ 6370 ≒ 60.3
That squared (taking 60)60 × 60 = 3600
Gravity at the Moon (right side)9.8 ÷ 3600 ≒ 0.00272 m/s²
Distance fallen in 1 second (half the acceleration)0.00271 ÷ 2 ≒ 0.00136 m

The left side, 0.00271, and the right side, 0.00272, almost match. The Moon falls toward Earth by about 1.4 millimetres each second. In that same second it moves about 1 kilometre sideways, so the fall is about 1/700,000 of the distance travelled. Add up these tiny bends and you get exactly a circle.

High schoolHigh school+What happens to the path when the speed changes?

High schoolThe speed for a circular orbit is fixed by the condition that centripetal force equals gravitational force. Worked out just above Earth's surface, it gives the first cosmic velocity, about 7.9 kilometres per second. At the Moon's distance, far from Earth, about 1.02 kilometres per second is enough.

High school+If the speed exceeds √2 times (about 1.41 times) the circular-orbit speed, the kinetic energy beats the energy needed to climb out of gravity's pull, and the body never returns. This is the escape velocity. It is why, in Figure 1, the Moon flies away from about 1.44 kilometres per second. At lower speeds the path is an ellipse (Kepler's first law).

UniversityThe two-body problem, and how the Moon drifts away

The motion of two bodies attracting each other, like Earth and the Moon, is called the two-body problem. From the law of universal gravitation and the equations of motion, it follows that the orbit is a circle, an ellipse, a parabola or a hyperbola. The real Moon's orbit wobbles in complicated ways because of perturbations from the Sun's gravity. In addition, the tidal bulge is carried forward by Earth's spin, and its gravity pulls the Moon forward, so angular momentum from Earth's spin passes into the Moon's orbit. The recession of about 3.8 centimetres a year measured by lunar laser ranging is thought to be the result of this tidal acceleration.

📖 Derivations and further reading: Universal gravitation (Wikipedia, in Japanese) / Lunar laser ranging experiment (Wikipedia, in Japanese)

ResearchWhat is still not clear

In other words, this article too is "an explanation within what we know today". How the Moon "falls" was solved over 300 years ago, but the Moon's origin and the nature of gravity remain open questions.

Links to your textbooks (by level)

LevelSubject / unitWhere in this article
Middle schoolScience: "Earth and the Universe" (the Moon's orbit)The Moon circles Earth in about 27.3 days
High schoolPhysics: "Circular motion", "Universal gravitation"Comparing centripetal acceleration with gravity weakening by the inverse square
High school+Physics (advanced): first cosmic velocity, escape velocityThe paths when the speed is changed in Figure 1
UniversityMechanics, celestial mechanics (two-body problem, tidal acceleration)Classifying orbits, and how the Moon drifts away
ResearchPlanetary science, theories of gravityThe Moon's origin, the history of its recession, the nature of gravity
―Links to daily lifeSatellites and space stations also orbit by the same mechanism of continuous falling
References and sources
  1. NASA NSSDCA | Moon Fact Sheet (Moon's distance, orbital period and orbital speed)
  2. Lunar laser ranging experiment (measurement of the Moon receding about 3.8 cm a year)
  3. National Institute of Standards and Technology, Fundamental Physical Constants (recommended value and uncertainty of the gravitational constant)
  4. National Astronomical Observatory of Japan (国立天文台), ed., Rika Nenpyo (理科年表, Chronological Scientific Tables), Maruzen Publishing (Earth and Moon data)
  5. Isaac Newton, Philosophiæ Naturalis Principia Mathematica (自然哲学の数学的諸原理), Book III (the Moon test)

※This article is a general-audience science explainer. The figures given are rough guides to help you understand the mechanism. The Moon's distance and speed vary by a few percent depending on where it is in its orbit.