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Field · Emerged 1600s – 1687

Classical Mechanics

What laws govern how things move, from a falling stone to an orbiting planet?

5 chapters4 min read5 turning points1 open problem

Branched from
One of the thread's roots
Branched into
Elasticity and Continuum Mechanics + Fluid Dynamics + General Relativity + Kinetic Theory of Gases + Special Relativity
Figures
Galileo Galilei, Johannes Kepler, Isaac Newton, Robert Hooke, Urbain Le Verrier, Johann Galle, John Couch Adams

In brief

Classical mechanics is the physics of motion and force: why a ball follows a parabola, why the Moon stays in orbit, how bridges carry loads and rockets reach Mars. Newton's three laws and his law of gravity, published in 1687, explained the heavens and the Earth with one set of rules.

For two centuries it looked like the final word, and it still works superbly for everything slower than light and larger than atoms. This thread follows the places where it cracked: the speed of light, and a small wobble in Mercury's orbit.

Key ideas

InertiaEnters c. 1604 – 1638

A body keeps moving in a straight line at constant speed unless a force acts on it. Motion needs no cause; changes in motion do.

Galilean relativityEnters c. 1604 – 1638

The laws of motion are the same in any laboratory moving steadily, like Galileo's ship cabin, where a dropped object falls straight down whether or not the ship is moving. Velocities simply add. This rule is what special relativity would revise.

Force and accelerationEnters 1687

Newton's second law, F=maF = ma: a force changes a body's velocity at a rate inversely proportional to its mass.

Universal gravitationEnters 1687

Every mass attracts every other with a force F=G m1m2/r2F = G\,m_1 m_2 / r^2. The same law makes apples fall and keeps planets in their elliptical orbits.

Conservation laws

Energy, momentum and angular momentum stay constant in an isolated system. They later turned out to be the deepest part of mechanics, since they survive in relativity and in quantum physics.

Draws on other domains

Chapter I

Falling and Orbiting

For two thousand years, motion meant Aristotle. Heavy things fall faster than light ones, moving things stop unless something keeps pushing them, and the heavens obey different rules from the Earth. Galileo Galilei broke the first two rules with experiments. Rolling balls down gentle ramps slowed falling enough to time with a water clock, and the result was simple: every body falls with the same steady acceleration, and distance grows with the square of the time.

He also saw that motion needs no cause. A ball rolling on a perfectly smooth, level surface would roll forever. In his 1632 Dialogue he imagined a closed cabin below decks on a smoothly sailing ship: butterflies fly and water drips exactly as they would in harbour. No experiment inside can tell whether the ship is moving. This principle of relativity would become the seed of Einstein's theory three centuries later.

Meanwhile Johannes Kepler, fitting Tycho Brahe's observations, found that the planets move not in circles but in ellipses, with regular laws linking their speeds and distances. The heavens had their own mathematics. What was missing was a reason.

Chapter II

Newton's Synthesis

Isaac Newton's Principia (1687) supplied it. Three laws of motion (inertia, F=maF = ma, action and reaction) and one law of gravity, an attraction between every pair of masses falling off as the square of the distance, reproduce Kepler's ellipses exactly. The Moon is falling toward the Earth just as an apple does. It simply moves sideways fast enough to keep missing.

The achievement was contested from the start. Robert Hooke insisted he had suggested the inverse-square law to Newton in their correspondence, and Newton answered by striking nearly every mention of Hooke from his book. Others objected to gravity itself: a force acting instantly across empty space, with no mechanism. Newton famously declined to explain it: hypotheses non fingo, "I frame no hypotheses". That unease about how gravity acts at a distance would be answered only by general relativity.

Chapter III

The Clockwork Universe

Over the next century and a half, Euler, Lagrange, Laplace and Hamilton rewrote Newton's mechanics in more powerful mathematical forms. Laplace imagined an intellect that, knowing every position and velocity at one instant, could compute the whole future.

The theory's greatest triumph came in 1846. Uranus was drifting from its predicted path, and Urbain Le Verrier worked backwards to the position of an unseen planet pulling on it. Johann Galle pointed his telescope there and found Neptune on his first night. In England, John Couch Adams's unpublished calculations were later put forward as a rival prediction, and how seriously to take them is still argued.

Chapter IV

A Closer Look: The Moon Is Falling

Newton's key test of universal gravitation, which he said he first tried in the plague years of 1665–66, needs only a few numbers. If the same force that pulls an apple also holds the Moon, and it weakens with the square of distance, then the Moon's acceleration towards the Earth should be the apple's divided by the square of how much farther away it is.

The Moon orbits at about 384,400 km from the Earth's centre, about 60 times the Earth's radius of 6,371 km. So gravity there should be 602=3,60060^2 = 3{,}600 times weaker than at the surface:

9.81 m/s23600≈0.00272 m/s2.\frac{9.81 \text{ m/s}^2}{3600} \approx 0.00272 \text{ m/s}^2 .

Now measure the Moon's actual acceleration, from its orbit alone. A body moving in a circle of radius rr with period TT accelerates towards the centre at 4π2r/T24\pi^2 r / T^2. The Moon's period is 27.32 days, or 2.36×1062.36 \times 10^6 seconds:

4π2×3.844×108 m(2.36×106 s)2≈0.00272 m/s2.\frac{4\pi^2 \times 3.844 \times 10^8 \text{ m}}{(2.36 \times 10^6 \text{ s})^2} \approx 0.00272 \text{ m/s}^2 .

The two agree. The fall of an apple in an orchard and the orbit of the Moon are the same phenomenon, given one rule about how gravity weakens with distance.

Put differently, in one second the Moon falls about 12×0.00272≈1.4\tfrac12 \times 0.00272 \approx 1.4 millimetres towards the Earth, while moving about a kilometre sideways. The curve of its path is exactly that fall. Newton's first attempt did not match as well, partly because the Earth's radius was poorly known. The close agreement, published in the Principia, showed that a law found on Earth governs the heavens.

Chapter V

Cracks at the Edges

The same method failed with Mercury. In 1859 Le Verrier found that its orbit swings around the Sun slightly faster than the other planets' pulls allow: 43 arcseconds per century by modern measurement. He predicted another unseen planet, Vulcan, inside Mercury's orbit. Astronomers looked for decades and never found it. The problem was not a missing planet but Newton's gravity itself.

A second crack was quieter. Galileo's relativity says that velocities simply add, so light should travel at different speeds for observers moving at different speeds. But electromagnetism was about to predict a single, fixed speed of light. The two theories could not both be right, and their collision produced special relativity.

Classical mechanics was not overthrown so much as bounded. Within its domain it remains exact enough to fly spacecraft and forecast weather, and even there it holds open problems. Whether the equations of fluid flow always have smooth solutions is still unknown.

Applications

Where it is used

  • Spaceflight

    Orbits, transfers and gravity assists

    Every spacecraft trajectory is Newtonian mechanics. A close pass by a planet can steal some of its orbital momentum. Michael Minovitch and Gary Flandro's work in the 1960s on such gravity assists made the Voyager "Grand Tour" of the outer planets possible.

    › Sources (1)
    • Flandro, G. A. (1966). Fast reconnaissance missions to the outer solar system utilizing energy derived from the gravitational field of Jupiter. Astronautica Acta 12: 329–337.
  • Planetary defence

    Nudging an asteroid

    In 2022 NASA's DART spacecraft deliberately struck the small asteroid Dimorphos and shortened its nearly 12-hour orbit around its companion by about 33 minutes. It was the first test of changing a celestial body's motion on purpose, planned and measured with classical mechanics.

    › Sources (1)
    • Thomas, C. A. et al. (2023). Orbital period change of Dimorphos due to the DART kinetic impact. Nature 616: 448–451.
  • Weather and climate

    Forecasting as fluid mechanics

    Numerical weather prediction solves the equations of fluid motion on a grid covering the planet. Lewis Fry Richardson attempted it by hand during the First World War and published the method in 1922. Modern forecasts and climate models are the same idea at vastly larger scale.

    › Sources (1)
    • Richardson, L. F. (1922). Weather Prediction by Numerical Process. Cambridge University Press.
  • Engineering

    Structures and machines

    Bridges, buildings, engines and vehicles are designed with Newton's laws extended to solid and fluid bodies. At everyday speeds and sizes, the corrections from relativity and quantum mechanics are far too small to matter.

Open problems

Where the map runs out

Open

Navier–Stokes existence and smoothness

Open as of 2026; a Clay Millennium Prize Problem.

The Navier–Stokes equations describe how fluids like water and air flow: they are Newton's second law applied to every parcel of a fluid. Do smooth starting flows in three dimensions always stay smooth, or can the equations develop infinite velocities in finite time?

Why it is hard

Turbulence moves energy across a huge range of scales, and the known conserved quantities are too weak to control the smallest ones. Estimates that close the argument in two dimensions fail in three. Computers can suggest behaviour but cannot prove it.

What resolving it unlocks

A proof of smoothness would put the equations behind weather forecasting, aircraft design and blood-flow modelling on a secure mathematical footing. A blow-up would show that the equations themselves break down, a sign that new physics is needed at small scales.

› Sources (1)
  • Fefferman, C. L. (2006). Existence and smoothness of the Navier–Stokes equation. In J. Carlson, A. Jaffe & A. Wiles (eds.), The Millennium Prize Problems: 57–67. Clay Mathematics Institute / AMS.

Further reading

  1. Feynman, R. P., Leighton, R. B. & Sands, M. (1963). The Feynman Lectures on Physics, Vol. I. Addison-Wesley.

    Mechanics taught for insight rather than drill. The full text is free online.

  2. Westfall, R. S. (1980). Never at Rest: A Biography of Isaac Newton. Cambridge University Press.

    The standard scholarly biography, including the Principia and its disputes.

  3. Taylor, J. R. (2005). Classical Mechanics. University Science Books.

    A clear undergraduate textbook, from Newton's laws through Lagrangian mechanics and chaos.