Chapter 3: The Copernican Revolution

Chapter 1
How Science Works

  • The Scientific Method
  • Evidence
  • Measurements
  • Units and the Metric System
  • Measurement Errors
  • Estimation
  • Dimensions
  • Mass, Length, and Time
  • Observations and Uncertainty
  • Precision and Significant Figures
  • Errors and Statistics
  • Scientific Notation
  • Ways of Representing Data
  • Logic
  • Mathematics
  • Geometry
  • Algebra
  • Logarithms
  • Testing a Hypothesis
  • Case Study of Life on Mars
  • Theories
  • Systems of Knowledge
  • The Culture of Science
  • Computer Simulations
  • Modern Scientific Research
  • The Scope of Astronomy
  • Astronomy as a Science
  • A Scale Model of Space
  • A Scale Model of Time
  • Questions

Chapter 2
Early Astronomy

  • The Night Sky
  • Motions in the Sky
  • Navigation
  • Constellations and Seasons
  • Cause of the Seasons
  • The Magnitude System
  • Angular Size and Linear Size
  • Phases of the Moon
  • Eclipses
  • Auroras
  • Dividing Time
  • Solar and Lunar Calendars
  • History of Astronomy
  • Stonehenge
  • Ancient Observatories
  • Counting and Measurement
  • Astrology
  • Greek Astronomy
  • Aristotle and Geocentric Cosmology
  • Aristarchus and Heliocentric Cosmology
  • The Dark Ages
  • Arab Astronomy
  • Indian Astronomy
  • Chinese Astronomy
  • Mayan Astronomy
  • Questions

Chapter 3
The Copernican Revolution

  • Ptolemy and the Geocentric Model
  • The Renaissance
  • Copernicus and the Heliocentric Model
  • Tycho Brahe
  • Johannes Kepler
  • Elliptical Orbits
  • Kepler's Laws
  • Galileo Galilei
  • The Trial of Galileo
  • Isaac Newton
  • Newton's Law of Gravity
  • The Plurality of Worlds
  • The Birth of Modern Science
  • Layout of the Solar System
  • Scale of the Solar System
  • The Idea of Space Exploration
  • Orbits
  • History of Space Exploration
  • Moon Landings
  • International Space Station
  • Manned versus Robotic Missions
  • Commercial Space Flight
  • Future of Space Exploration
  • Living in Space
  • Moon, Mars, and Beyond
  • Societies in Space
  • Questions

Chapter 4
Matter and Energy in the Universe

  • Matter and Energy
  • Rutherford and Atomic Structure
  • Early Greek Physics
  • Dalton and Atoms
  • The Periodic Table
  • Structure of the Atom
  • Energy
  • Heat and Temperature
  • Potential and Kinetic Energy
  • Conservation of Energy
  • Velocity of Gas Particles
  • States of Matter
  • Thermodynamics
  • Entropy
  • Laws of Thermodynamics
  • Heat Transfer
  • Thermal Radiation
  • Wien's Law
  • Radiation from Planets and Stars
  • Internal Heat in Planets and Stars
  • Periodic Processes
  • Random Processes
  • Questions

Chapter 5
The Earth-Moon System

  • Earth and Moon
  • Early Estimates of Earth's Age
  • How the Earth Cooled
  • Ages Using Radioactivity
  • Radioactive Half-Life
  • Ages of the Earth and Moon
  • Geological Activity
  • Internal Structure of the Earth and Moon
  • Basic Rock Types
  • Layers of the Earth and Moon
  • Origin of Water on Earth
  • The Evolving Earth
  • Plate Tectonics
  • Volcanoes
  • Geological Processes
  • Impact Craters
  • The Geological Timescale
  • Mass Extinctions
  • Evolution and the Cosmic Environment
  • Earth's Atmosphere and Oceans
  • Weather Circulation
  • Environmental Change on Earth
  • The Earth-Moon System
  • Geological History of the Moon
  • Tidal Forces
  • Effects of Tidal Forces
  • Historical Studies of the Moon
  • Lunar Surface
  • Ice on the Moon
  • Origin of the Moon
  • Humans on the Moon
  • Questions

Chapter 6
The Terrestrial Planets

  • Studying Other Planets
  • The Planets
  • The Terrestrial Planets
  • Mercury
  • Mercury's Orbit
  • Mercury's Surface
  • Venus
  • Volcanism on Venus
  • Venus and the Greenhouse Effect
  • Tectonics on Venus
  • Exploring Venus
  • Mars in Myth and Legend
  • Early Studies of Mars
  • Mars Close-Up
  • Modern Views of Mars
  • Missions to Mars
  • Geology of Mars
  • Water on Mars
  • Polar Caps of Mars
  • Climate Change on Mars
  • Terraforming Mars
  • Life on Mars
  • The Moons of Mars
  • Martian Meteorites
  • Comparative Planetology
  • Incidence of Craters
  • Counting Craters
  • Counting Statistics
  • Internal Heat and Geological Activity
  • Magnetic Fields of the Terrestrial Planets
  • Mountains and Rifts
  • Radar Studies of Planetary Surfaces
  • Laser Ranging and Altimetry
  • Gravity and Atmospheres
  • Normal Atmospheric Composition
  • The Significance of Oxygen
  • Questions

Chapter 7
The Giant Planets and Their Moons

  • The Gas Giant Planets
  • Atmospheres of the Gas Giant Planets
  • Clouds and Weather on Gas Giant Planets
  • Internal Structure of the Gas Giant Planets
  • Thermal Radiation from Gas Giant Planets
  • Life on Gas Giant Planets?
  • Why Giant Planets are Giant
  • Gas Laws
  • Ring Systems of the Giant Planets
  • Structure Within Ring Systems
  • The Origin of Ring Particles
  • The Roche Limit
  • Resonance and Harmonics
  • Tidal Forces in the Solar System
  • Moons of Gas Giant Planets
  • Geology of Large Moons
  • The Voyager Missions
  • Jupiter
  • Jupiter's Galilean Moons
  • Jupiter's Ganymede
  • Jupiter's Europa
  • Jupiter's Callisto
  • Jupiter's Io
  • Volcanoes on Io
  • Saturn
  • Cassini Mission to Saturn
  • Saturn's Titan
  • Saturn's Enceladus
  • Discovery of Uranus and Neptune
  • Uranus
  • Uranus' Miranda
  • Neptune
  • Neptune's Triton
  • Pluto
  • The Discovery of Pluto
  • Pluto as a Dwarf Planet
  • Dwarf Planets
  • Questions

Chapter 8
Interplanetary Bodies

  • Interplanetary Bodies
  • Comets
  • Early Observations of Comets
  • Structure of the Comet Nucleus
  • Comet Chemistry
  • Oort Cloud and Kuiper Belt
  • Kuiper Belt
  • Comet Orbits
  • Life Story of Comets
  • The Largest Kuiper Belt Objects
  • Meteors and Meteor Showers
  • Gravitational Perturbations
  • Asteroids
  • Surveys for Earth Crossing Asteroids
  • Asteroid Shapes
  • Composition of Asteroids
  • Introduction to Meteorites
  • Origin of Meteorites
  • Types of Meteorites
  • The Tunguska Event
  • The Threat from Space
  • Probability and Impacts
  • Impact on Jupiter
  • Interplanetary Opportunity
  • Questions

Chapter 9
Planet Formation and Exoplanets

  • Formation of the Solar System
  • Early History of the Solar System
  • Conservation of Angular Momentum
  • Angular Momentum in a Collapsing Cloud
  • Helmholtz Contraction
  • Safronov and Planet Formation
  • Collapse of the Solar Nebula
  • Why the Solar System Collapsed
  • From Planetesimals to Planets
  • Accretion and Solar System Bodies
  • Differentiation
  • Planetary Magnetic Fields
  • The Origin of Satellites
  • Solar System Debris and Formation
  • Gradual Evolution and a Few Catastrophies
  • Chaos and Determinism
  • Extrasolar Planets
  • Discoveries of Exoplanets
  • Doppler Detection of Exoplanets
  • Transit Detection of Exoplanets
  • The Kepler Mission
  • Direct Detection of Exoplanets
  • Properties of Exoplanets
  • Implications of Exoplanet Surveys
  • Future Detection of Exoplanets
  • Questions

Chapter 10
Detecting Radiation from Space

  • Observing the Universe
  • Radiation and the Universe
  • The Nature of Light
  • The Electromagnetic Spectrum
  • Properties of Waves
  • Waves and Particles
  • How Radiation Travels
  • Properties of Electromagnetic Radiation
  • The Doppler Effect
  • Invisible Radiation
  • Thermal Spectra
  • The Quantum Theory
  • The Uncertainty Principle
  • Spectral Lines
  • Emission Lines and Bands
  • Absorption and Emission Spectra
  • Kirchoff's Laws
  • Astronomical Detection of Radiation
  • The Telescope
  • Optical Telescopes
  • Optical Detectors
  • Adaptive Optics
  • Image Processing
  • Digital Information
  • Radio Telescopes
  • Telescopes in Space
  • Hubble Space Telescope
  • Interferometry
  • Collecting Area and Resolution
  • Frontier Observatories
  • Questions

Chapter 11
Our Sun: The Nearest Star

  • The Sun
  • The Nearest Star
  • Properties of the Sun
  • Kelvin and the Sun's Age
  • The Sun's Composition
  • Energy From Atomic Nuclei
  • Mass-Energy Conversion
  • Examples of Mass-Energy Conversion
  • Energy From Nuclear Fission
  • Energy From Nuclear Fusion
  • Nuclear Reactions in the Sun
  • The Sun's Interior
  • Energy Flow in the Sun
  • Collisions and Opacity
  • Solar Neutrinos
  • Solar Oscillations
  • The Sun's Atmosphere
  • Solar Chromosphere and Corona
  • Sunspots
  • The Solar Cycle
  • The Solar Wind
  • Effects of the Sun on the Earth
  • Cosmic Energy Sources
  • Questions

Chapter 12
Properties of Stars

  • Stars
  • Star Names
  • Star Properties
  • The Distance to Stars
  • Apparent Brightness
  • Absolute Brightness
  • Measuring Star Distances
  • Stellar Parallax
  • Spectra of Stars
  • Spectral Classification
  • Temperature and Spectral Class
  • Stellar Composition
  • Stellar Motion
  • Stellar Luminosity
  • The Size of Stars
  • Stefan-Boltzmann Law
  • Stellar Mass
  • Hydrostatic Equilibrium
  • Stellar Classification
  • The Hertzsprung-Russell Diagram
  • Volume and Brightness Selected Samples
  • Stars of Different Sizes
  • Understanding the Main Sequence
  • Stellar Structure
  • Stellar Evolution
  • Questions

Chapter 13
Star Birth and Death

  • Star Birth and Death
  • Understanding Star Birth and Death
  • Cosmic Abundance of Elements
  • Star Formation
  • Molecular Clouds
  • Young Stars
  • T Tauri Stars
  • Mass Limits for Stars
  • Brown Dwarfs
  • Young Star Clusters
  • Cauldron of the Elements
  • Main Sequence Stars
  • Nuclear Reactions in Main Sequence Stars
  • Main Sequence Lifetimes
  • Evolved Stars
  • Cycles of Star Life and Death
  • The Creation of Heavy Elements
  • Red Giants
  • Horizontal Branch and Asymptotic Giant Branch Stars
  • Variable Stars
  • Magnetic Stars
  • Stellar Mass Loss
  • White Dwarfs
  • Supernovae
  • Seeing the Death of a Star
  • Supernova 1987A
  • Neutron Stars and Pulsars
  • Special Theory of Relativity
  • General Theory of Relativity
  • Black Holes
  • Properties of Black Holes
  • Questions

Chapter 14
The Milky Way

  • The Distribution of Stars in Space
  • Stellar Companions
  • Binary Star Systems
  • Binary and Multiple Stars
  • Mass Transfer in Binaries
  • Binaries and Stellar Mass
  • Nova and Supernova
  • Exotic Binary Systems
  • Gamma Ray Bursts
  • How Multiple Stars Form
  • Environments of Stars
  • The Interstellar Medium
  • Effects of Interstellar Material on Starlight
  • Structure of the Interstellar Medium
  • Dust Extinction and Reddening
  • Groups of Stars
  • Open Star Clusters
  • Globular Star Clusters
  • Distances to Groups of Stars
  • Ages of Groups of Stars
  • Layout of the Milky Way
  • William Herschel
  • Isotropy and Anisotropy
  • Mapping the Milky Way
  • Questions

Chapter 15
Galaxies

  • The Milky Way Galaxy
  • Mapping the Galaxy Disk
  • Spiral Structure in Galaxies
  • Mass of the Milky Way
  • Dark Matter in the Milky Way
  • Galaxy Mass
  • The Galactic Center
  • Black Hole in the Galactic Center
  • Stellar Populations
  • Formation of the Milky Way
  • Galaxies
  • The Shapley-Curtis Debate
  • Edwin Hubble
  • Distances to Galaxies
  • Classifying Galaxies
  • Spiral Galaxies
  • Elliptical Galaxies
  • Lenticular Galaxies
  • Dwarf and Irregular Galaxies
  • Overview of Galaxy Structures
  • The Local Group
  • Light Travel Time
  • Galaxy Size and Luminosity
  • Mass to Light Ratios
  • Dark Matter in Galaxies
  • Gravity of Many Bodies
  • Galaxy Evolution
  • Galaxy Interactions
  • Galaxy Formation
  • Questions

Chapter 16
The Expanding Universe

  • Galaxy Redshifts
  • The Expanding Universe
  • Cosmological Redshifts
  • The Hubble Relation
  • Relating Redshift and Distance
  • Galaxy Distance Indicators
  • Size and Age of the Universe
  • The Hubble Constant
  • Large Scale Structure
  • Galaxy Clustering
  • Clusters of Galaxies
  • Overview of Large Scale Structure
  • Dark Matter on the Largest Scales
  • The Most Distant Galaxies
  • Black Holes in Nearby Galaxies
  • Active Galaxies
  • Radio Galaxies
  • The Discovery of Quasars
  • Quasars
  • Types of Gravitational Lensing
  • Properties of Quasars
  • The Quasar Power Source
  • Quasars as Probes of the Universe
  • Star Formation History of the Universe
  • Expansion History of the Universe
  • Questions

Chapter 17
Cosmology

  • Cosmology
  • Early Cosmologies
  • Relativity and Cosmology
  • The Big Bang Model
  • The Cosmological Principle
  • Universal Expansion
  • Cosmic Nucleosynthesis
  • Cosmic Microwave Background Radiation
  • Discovery of the Microwave Background Radiation
  • Measuring Space Curvature
  • Cosmic Evolution
  • Evolution of Structure
  • Mean Cosmic Density
  • Critical Density
  • Dark Matter and Dark Energy
  • Age of the Universe
  • Precision Cosmology
  • The Future of the Contents of the Universe
  • Fate of the Universe
  • Alternatives to the Big Bang Model
  • Space-Time
  • Particles and Radiation
  • The Very Early Universe
  • Mass and Energy in the Early Universe
  • Matter and Antimatter
  • The Forces of Nature
  • Fine-Tuning in Cosmology
  • The Anthropic Principle in Cosmology
  • String Theory and Cosmology
  • The Multiverse
  • The Limits of Knowledge
  • Questions

Chapter 18
Life On Earth

  • Nature of Life
  • Chemistry of Life
  • Molecules of Life
  • The Origin of Life on Earth
  • Origin of Complex Molecules
  • Miller-Urey Experiment
  • Pre-RNA World
  • RNA World
  • From Molecules to Cells
  • Metabolism
  • Anaerobes
  • Extremophiles
  • Thermophiles
  • Psychrophiles
  • Xerophiles
  • Halophiles
  • Barophiles
  • Acidophiles
  • Alkaliphiles
  • Radiation Resistant Biology
  • Importance of Water for Life
  • Hydrothermal Systems
  • Silicon Versus Carbon
  • DNA and Heredity
  • Life as Digital Information
  • Synthetic Biology
  • Life in a Computer
  • Natural Selection
  • Tree Of Life
  • Evolution and Intelligence
  • Culture and Technology
  • The Gaia Hypothesis
  • Life and the Cosmic Environment

Chapter 19
Life in the Universe

  • Life in the Universe
  • Astrobiology
  • Life Beyond Earth
  • Sites for Life
  • Complex Molecules in Space
  • Life in the Solar System
  • Lowell and Canals on Mars
  • Implications of Life on Mars
  • Extreme Environments in the Solar System
  • Rare Earth Hypothesis
  • Are We Alone?
  • Unidentified Flying Objects or UFOs
  • The Search for Extraterrestrial Intelligence
  • The Drake Equation
  • The History of SETI
  • Recent SETI Projects
  • Recognizing a Message
  • The Best Way to Communicate
  • The Fermi Question
  • The Anthropic Principle
  • Where Are They?

Newton's Law of Gravity


Newton's most brilliant step was to unite motions on Earth and in the sky. He knew that a force must cause an object like an apple to fall to the Earth. He also knew that the Moon must have a force acting on it to make it travel in a curved path as it orbits the Earth. Could these be the same force? (It is not known if the story of Newton getting his insight from watching a falling apple is true, but there is an apple orchard outside his childhood home in England!) Newton's universal law of gravitation is one of the most important discoveries in the history of science.


A portrait of Isaac Newton.

Newton expressed his law mathematically. In words, we can write: every particle in the universe attracts every other particle with a force proportional to the product of their masses and inversely proportional to the square of the distance between them. We, therefore, define gravity as a universal attractive force; it is a property of every object in the universe. This expression of gravity means that if you could double the mass of the Sun, the Sun's gravitational attraction to the Earth would double; but if you doubled the distance between them, the force on the Earth would decrease by a factor of four (the square of two). Similarly, if you tripled the Sun's mass, the force would triple, but if you tripled the distance, the force would decrease by a factor of nine.


A photograph of Halley's comet taken in 1986.

Gravity is a force that follows an inverse square law. That is, the strength diminishes with the square of the distance from the object. Newton was able to show that if gravity followed an inverse square law, then the planet orbits that are predicted must be ellipses with the Sun at one focus. Here, at last, was the elegant explanation for Kepler's work. Newton's gravity was used to successfully predict the return of Halley's comet on its highly elliptical orbit of the Sun — a stunning confirmation of the theory.

Newton's law of gravity applies to two single particles. How then can we calculate the force of gravity on a person, when the attraction due to all the different parts of the Earth must be added together? Newton invented the calculus to solve this problem - with the result that a spherical object like a planet behaves as if it had all its mass concentrated at the center. Newton did many of these important calculations and then buried them on his desk, as his voracious mind found new problems to study. Spurred on by Edmund Halley, the famous astronomer, he finally published his work in a masterful book called "Principia," in 1687.


A diagram illustrating the Inverse Square Law. S represents an ideal source of electromagnetic radiation and A represents an arbitrary segment of the surface of a sphere of radius r.

Newton's universal law of gravitation is a common type of law called an inverse square law. The force of gravity due to some object depends on the inverse square of the distance. This dependence is typical of many forces that emanate from a point — in fact, it is a property of the three-dimensional space we inhabit. We can imagine lines of gravity force emerging from an object in all directions. The concentration of the lines of force is then a measure of the strength of the gravity. The surface area of any sphere surrounding the object is 4πD2, where D is the distance from the object. The lines of force spread out more and more as we move away from the object. This decreasing concentration corresponds to the decreasing force of gravity. The total number of lines of force does not move away from the object, but they are spread over an area that increases proportionally to D2. Therefore the concentration or number of lines of force in any particular area decreases with the inverse square of the distance, i.e. proportional to 1 / D2.

Electric and magnetic forces obey the same relationship with distance as gravity. You can also understand how the inverse square law would apply to the radiation from a light bulb, reaching surfaces at different distances. Imagine rays of light moving out from a light source. If at a certain distance, the light emitted in a certain direction is spread over one unit, then at twice that distance it is spread over four units. The intensity of the light at twice the distance is thus ¼ as much. In the same way, the intensity at three times the initial distance is only 1/9 as much. So light, like gravity, obeys an inverse square law.

Here is Isaac Newton's reasoning as he used the inverse square law of gravity to connect the falling apple with the orbit of the Moon. We will use simple geometry to get the answer roughly — calculus is required for a more accurate result. The distance from the Moon to the center of the Earth is 60 times the radius of the Earth. So by the inverse square law, the Earth's gravity at the distance of the Moon should be 602 times less than at the Earth's surface. The acceleration of the Moon that causes it to deviate from a straight path and curve around the Earth is 9.8 / 602 = 0.0027 meters per second per second. In each second of its orbit, the moon falls 0.0027 / 2 = 0.0014 meters or only 1.4 millimeters toward the Earth.

How far does the Moon travel in its orbit in one second? This is just the circumference of the orbit divided by the orbital time in seconds. The orbit time is 27.3 days or 27.3 x 24 x 3600 = 2.36 x 106 seconds (Note that the time for the Moon to complete a cycle of phases — 29.5 days — is longer than the orbit time because the Earth moves in its own orbit in a month). So in one second the Moon travels (2 π 384,000) / 2.36 × 106 = 1.02 kilometers. For such a small piece of the orbit, we can approximate the curved path as a straight line and use the small angle equation, which gives a / 206,265 = d / D, so a = 206,265 (0.0014 / 1020) = 0.3 arc seconds. This is the angle by which the Moon deviates in its orbit each second due to the gravity of the Earth. The angle by which it rotates in its orbit is a / 206,265 = d / D, so a = 206,265 (1.02 / 384,000) = 0.5 arc seconds, a similar number. So we can see that an inverse square law of gravity describes the Moon's orbit.

It is actually easier to write the law of gravitation in mathematical terms than to spell it out in words. If we have two masses MA and MB, separated by a distance R, then Newton's law of gravity gives the force between mass A and mass B of

F = G MA MB / R2

The number G is the gravitational constant, a fundamental constant of nature. If we measure mass in kilograms, distance in meters, and force in the normal units of Newtons (N), G = 6.67 × 10-11 N m2 kg2. The constant G is a tiny number - gravity is actually a very weak force. It is only the presence of enormous amounts of matter that gives gravity a sizable force.

The mass of the Earth, 6 × 1024 kg, gives us a downward acceleration of 9.8 meters/sec2. But everything with mass attracts everything else with mass, so what about other objects? Suppose two ocean liners of mass 10,000 tons (107 kg) were sitting in the water separated by 100 meters. The force between them would be (6.67 × 10-11 x 107 x 107) / (100)2 = 0.67 Newtons. Using Newton's second law of motion, acceleration = force / mass, the acceleration on each ship would be 6.7 × 10-8 meters/sec2. This is clearly too tiny to measure — the gravity of astronomical objects clearly overwhelms the gravity of everyday objects!

If we want to compare the gravity due to two different objects, we can take ratios and not need to use the gravitational constant. To compare the relative gravitational force of objects B and C on object A, we divide

FB on A / FC on A = (MB / MC) x (RC to A / RB to A)2

The gravitational constant and the mass of A cancel out. We are pinned to the Earth by its gravity. Let's see how the gravity of other objects compares. Using the equation above where B is the Sun and C is the Earth, the relative force is (2 × 1030 / 6 × 1024) x (6400 / 1.5 × 108)2 = 6 × 10-4. So the Sun exerts less than a tenth of a percent as much gravity on you as the Earth. What about two people sitting in a room? If they weigh 50 kg and are 1 meter apart, the relative force is (50 / 6 × 1024) × (6400 / 0.001)2 = 2 × 10-9. This is a billionth of the force that keeps us down to Earth. Whatever else might attract two people, gravity has very little part in it!

Newton's gravity incorporates his laws of motion. Gravity is the force that keeps the Moon in its curving motion around the Earth, or the Earth in its curving motion around the Sun. In the absence of gravity, the Earth would just fly off straight into space, just as a stone whirled overhead on a string would fly if the string broke. In the vacuum of space, there is no friction or air resistance, so the solar system can maintain its motions for a very long time. Also, gravity is a mutual force that illustrates Newton's third law of motion. The Earth exerts a gravitational force on you, but you exert an equal gravitational force on the Earth! Gravity has a long reach. It declines in strength as the distance increases but never becomes zero. Using this logic Newton was sure that gravity was a universal force.

It is important to keep in mind the difference between mass and weight. Mass is a fundamental property of an object or particle. It is the amount of "stuff" or the number of atoms in something, measured in units of kilograms. This measure determines the force of gravity. Weight depends on your location in space. On the Earth's surface, the acceleration due to gravity is 9.8 meters/sec2 — usually given the symbol g (to distinguish it from the universal constant G). This is an increase in speed of 9.8 meters per second for every second of falling. On the smaller and less massive Moon, the acceleration due to gravity is only 1.6 meters/sec2. If you weighed 60 kg on Earth you would weigh 10 kg on the Moon. In orbit around the Earth, you would be weightless. This is because you and the spacecraft experience the same gravity force, and there is no net force between you and the spacecraft. You would also be weightless in deep space, far from the gravity of any star or planet. In all of these situations, your mass is the same. But your weight depends on the local gravity force.

Newton the man was a bundle of contradictions. He could be humble when thinking of his predecessors. He said, "If I have seen any further than others, it is because I have stood on the shoulders of giants." Yet he could be brutal with colleagues and rivals. The man who gave birth to the rational and mechanistic view of a "clockwork" universe spent much of his effort on alchemy. After he died his estate was found to contain thousands of pages of detailed analysis of the Bible. Newton the scientist is easier to judge. He used one simple law to understand a huge variety of seemingly unrelated effects: your weight, an apple falling from a tree, the Moon moving around the Earth, the arcing path of a comet, or the planets moving around the Sun. The English writer, Alexander Pope, got it right when he penned this clever verse upon Newton's death:

"Nature and Nature's laws lay hid in night;
God said "Let Newton be! and all was light."


Author: Chris Impey