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Chapter
1313
Origin of Modern
Astronomy
Ancient Greeks
22.1 Early Astronomy
 Astronomy is the science that studies the
universe. It includes the observation and
interpretation of celestial bodies and
phenomena.
 The Greeks used philosophical arguments
to explain natural phenomena.
 The Greeks also used some observational
data.
Astrolabe
Calculating Earth’s Circumference
Ancient Greeks
22.1 Early Astronomy
 Geocentric Model
• In the ancient Greeks’ geocentric model, the
moon, sun, and the known planets—Mercury,
Venus, Mars, and Jupiter—orbit Earth.
 Heliocentric Model
• In the heliocentric model, Earth and the other
planets orbit the sun.
Geocentric and Heliocentric Models
Ancient Greeks
22.1 Early Astronomy
 Ptolemaic System
• Ptolemy created a model of the universe that
accounted for the movement of the planets.
• Retrograde motion is the apparent westward
motion of the planets with respect to the stars.
Retrograde Motion
The Birth of Modern Astronomy
22.1 Early Astronomy
 Nicolaus Copernicus
• Copernicus concluded that Earth is a planet. He
proposed a model of the solar system with the
sun at the center.
The Birth of Modern Astronomy
22.1 Early Astronomy
 Tycho Brahe
• Tycho Brahe designed and built instruments to
measure the locations of the heavenly bodies.
Brahe’s observations, especially of Mars, were
far more precise than any made previously.
The Birth of Modern Astronomy
22.1 Early Astronomy
 Johannes Kepler
• Kepler discovered three laws of planetary motion:
1. Orbits of the planets are elliptical.
2. Planets revolve around the sun at varying
speed.
3. There is a proportional relationship between
a planet’s orbital period and its distance to
the sun.
The Birth of Modern Astronomy
22.1 Early Astronomy
 Johannes Kepler
• An ellipse is an oval-shaped path.
• An astronomical unit (AU) is the average
distance between Earth and the sun; it is about
150 million kilometers.
Planet Revolution
The Birth of Modern Astronomy
22.1 Early Astronomy
 Galileo Galilei
• Galileo’s most important contributions were his
descriptions of the behavior of moving objects.
• He developed his own telescope and made
important discoveries:
1. Four satellites, or moons, orbit Jupiter.
2. Planets are circular disks, not just points of light.
3. Venus has phases just like the moon.
4. The moon’s surface is not smooth.
5. The sun has sunspots, or dark regions.
The Solar System Model Evolves
The Birth of Modern Astronomy
22.1 Early Astronomy
 Sir Isaac Newton
• Although others had theorized the existence of
gravitational force, Newton was the first to
formulate and test the law of universal
gravitation.
 Universal Gravitation
• Gravitational force decreases with distance.
• The greater the mass of an object, the greater is
its gravitational force.
Gravity’s Influence on Orbits
Motions of Earth
22.2 The Earth–Moon–Sun System
 The two main motions of Earth are rotation
and revolution. Precession is a third and
very slow motion of Earth’s axis.
Stonehenge, an Ancient Observatory
Motions of Earth
22.2 The Earth–Moon–Sun System
 Rotation
• Rotation is the turning, or spinning, of a body on
its axis.
• Two measurements for rotation:
1. Mean solar day is the time interval from one
noon to the next, about 24 hours.
2. Sidereal day is the time it takes for Earth to
make one complete rotation (360º) with
respect to a star other than the sun—23 hours,
56 minutes, 4 seconds.
Sidereal Day
Motions of Earth
22.2 The Earth–Moon–Sun System
 Revolution
• Revolution is the motion of a body, such as a
planet or moon, along a path around some point
in space.
• Perihelion is the time in January when Earth is
closest to the sun.
• Aphelion is the time in July when Earth is
farthest from the sun.
Motions of Earth
22.2 The Earth–Moon–Sun System
 Earth’s Axis and Seasons
• Because of the inclination of Earth’s axis to the
plane of the ecliptic, Earth has its yearly cycle of
seasons.
• The plane of the ecliptic is an imaginary plane
that connects Earth’s orbit with the celestial
sphere.
The Ecliptic
Motions of Earth
22.2 The Earth–Moon–Sun System
 Precession
• Precession traces out a cone over a period of
26,000 years.
 Earth–Sun Motion
• The solar system speeds in the direction of the
star Vega.
• The sun revolves around the galaxy.
• Earth is presently approaching one of its
nearest galactic neighbors, the Great Galaxy in
Andromeda.
Precession
Motions of the Earth–Moon System
22.2 The Earth–Moon–Sun System
 Perigee is the point at which the moon is
closest to Earth.
 Apogee is the point at which the moon is
farthest from Earth.
Motions of the Earth–Moon System
22.2 The Earth–Moon–Sun System
 Phases of the Moon
• The phases of the moon are the progression of
changes in the moon’s appearance during the
month.
• Lunar phases are a result of the motion of the
moon and the sunlight that is reflected from its
surface.
Phases of the Moon
Motions of the Earth–Moon System
22.2 The Earth–Moon–Sun System
 Lunar Motions
• The synodic month is based on the cycle of the
moon’s phases. It lasts 29 1/2 days.
• The sidereal month is the true period of the
moon’s revolution around Earth. It lasts 27 1/3
days.
Motions of the Earth–Moon System
22.2 The Earth–Moon–Sun System
• The difference of two days between the synodic
and sidereal cycles is due to the Earth–moon
system also moving in an orbit around the sun.
 Lunar Motions
• The moon’s period of rotation about its axis and
its revolution around Earth are the same, 27 1/3
days. It causes the same lunar hemisphere to
always face Earth.
Lunar Motions
Eclipses
22.2 The Earth–Moon–Sun System
 Solar eclipses occur when the moon
moves in a line directly between Earth and
the sun, casting a shadow on Earth.
 During a new-moon or full-moon phase,
the moon’s orbit must cross the plane of
the ecliptic for an eclipse to take place.
 Lunar eclipses occur when the moon
passes through Earth’s shadow.
Solar Eclipse
Lunar Eclipse
The Lunar Surface
22.3 Earth’s Moon
• A crater is the depression at the summit of a
volcano or a depression produced by a meteorite
impact.
 Craters
• Most craters were produced by the impact of
rapidly moving debris.
• Rays are any of a system of bright, elongated
streaks, sometimes associated with a crater on
the moon.
The Moon’s Surface
Mare Tranquillitatus
(Sea of Tranquility)
Mare Imbrium
(Sea of Rains)
Kepler
Crater
Copernicus
Crater
Formation of a Crater
The Lunar Surface
22.3 Earth’s Moon
• Most of the lunar surface is made up of densely
pitted, light-colored areas known as highlands.
 Highlands
• Maria, ancient beds of basaltic lava, originated
when asteroids punctured the lunar surface,
letting magma bleed out.
 Maria
• A rille is a long channel associated with lunar
maria. A rille looks similar to a valley or a trench.
The Lunar Surface
22.3 Earth’s Moon
• The lunar regolith is a thin, gray layer on the
surface of the moon, consisting of loosely
compacted, fragmented material believed to
have been formed by repeated impacts of
meteorites.
 Regolith
Major Topographic Features of the Moon
Lunar History
22.3 Earth’s Moon
 The most widely accepted model for the
origin of the moon is that when the solar
system was forming, a body the size of
Mars impacted Earth. The resulting debris
was ejected into space, began orbiting
around Earth, and eventually united to form
the moon.
Formation of Earth’s Moon

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Origin of Modern Astronomy

  • 2. Ancient Greeks 22.1 Early Astronomy  Astronomy is the science that studies the universe. It includes the observation and interpretation of celestial bodies and phenomena.  The Greeks used philosophical arguments to explain natural phenomena.  The Greeks also used some observational data.
  • 5. Ancient Greeks 22.1 Early Astronomy  Geocentric Model • In the ancient Greeks’ geocentric model, the moon, sun, and the known planets—Mercury, Venus, Mars, and Jupiter—orbit Earth.  Heliocentric Model • In the heliocentric model, Earth and the other planets orbit the sun.
  • 7. Ancient Greeks 22.1 Early Astronomy  Ptolemaic System • Ptolemy created a model of the universe that accounted for the movement of the planets. • Retrograde motion is the apparent westward motion of the planets with respect to the stars.
  • 9. The Birth of Modern Astronomy 22.1 Early Astronomy  Nicolaus Copernicus • Copernicus concluded that Earth is a planet. He proposed a model of the solar system with the sun at the center.
  • 10. The Birth of Modern Astronomy 22.1 Early Astronomy  Tycho Brahe • Tycho Brahe designed and built instruments to measure the locations of the heavenly bodies. Brahe’s observations, especially of Mars, were far more precise than any made previously.
  • 11. The Birth of Modern Astronomy 22.1 Early Astronomy  Johannes Kepler • Kepler discovered three laws of planetary motion: 1. Orbits of the planets are elliptical. 2. Planets revolve around the sun at varying speed. 3. There is a proportional relationship between a planet’s orbital period and its distance to the sun.
  • 12. The Birth of Modern Astronomy 22.1 Early Astronomy  Johannes Kepler • An ellipse is an oval-shaped path. • An astronomical unit (AU) is the average distance between Earth and the sun; it is about 150 million kilometers.
  • 14. The Birth of Modern Astronomy 22.1 Early Astronomy  Galileo Galilei • Galileo’s most important contributions were his descriptions of the behavior of moving objects. • He developed his own telescope and made important discoveries: 1. Four satellites, or moons, orbit Jupiter. 2. Planets are circular disks, not just points of light. 3. Venus has phases just like the moon. 4. The moon’s surface is not smooth. 5. The sun has sunspots, or dark regions.
  • 15. The Solar System Model Evolves
  • 16. The Birth of Modern Astronomy 22.1 Early Astronomy  Sir Isaac Newton • Although others had theorized the existence of gravitational force, Newton was the first to formulate and test the law of universal gravitation.  Universal Gravitation • Gravitational force decreases with distance. • The greater the mass of an object, the greater is its gravitational force.
  • 18. Motions of Earth 22.2 The Earth–Moon–Sun System  The two main motions of Earth are rotation and revolution. Precession is a third and very slow motion of Earth’s axis.
  • 19. Stonehenge, an Ancient Observatory
  • 20. Motions of Earth 22.2 The Earth–Moon–Sun System  Rotation • Rotation is the turning, or spinning, of a body on its axis. • Two measurements for rotation: 1. Mean solar day is the time interval from one noon to the next, about 24 hours. 2. Sidereal day is the time it takes for Earth to make one complete rotation (360º) with respect to a star other than the sun—23 hours, 56 minutes, 4 seconds.
  • 22. Motions of Earth 22.2 The Earth–Moon–Sun System  Revolution • Revolution is the motion of a body, such as a planet or moon, along a path around some point in space. • Perihelion is the time in January when Earth is closest to the sun. • Aphelion is the time in July when Earth is farthest from the sun.
  • 23. Motions of Earth 22.2 The Earth–Moon–Sun System  Earth’s Axis and Seasons • Because of the inclination of Earth’s axis to the plane of the ecliptic, Earth has its yearly cycle of seasons. • The plane of the ecliptic is an imaginary plane that connects Earth’s orbit with the celestial sphere.
  • 25. Motions of Earth 22.2 The Earth–Moon–Sun System  Precession • Precession traces out a cone over a period of 26,000 years.  Earth–Sun Motion • The solar system speeds in the direction of the star Vega. • The sun revolves around the galaxy. • Earth is presently approaching one of its nearest galactic neighbors, the Great Galaxy in Andromeda.
  • 27. Motions of the Earth–Moon System 22.2 The Earth–Moon–Sun System  Perigee is the point at which the moon is closest to Earth.  Apogee is the point at which the moon is farthest from Earth.
  • 28. Motions of the Earth–Moon System 22.2 The Earth–Moon–Sun System  Phases of the Moon • The phases of the moon are the progression of changes in the moon’s appearance during the month. • Lunar phases are a result of the motion of the moon and the sunlight that is reflected from its surface.
  • 30. Motions of the Earth–Moon System 22.2 The Earth–Moon–Sun System  Lunar Motions • The synodic month is based on the cycle of the moon’s phases. It lasts 29 1/2 days. • The sidereal month is the true period of the moon’s revolution around Earth. It lasts 27 1/3 days.
  • 31. Motions of the Earth–Moon System 22.2 The Earth–Moon–Sun System • The difference of two days between the synodic and sidereal cycles is due to the Earth–moon system also moving in an orbit around the sun.  Lunar Motions • The moon’s period of rotation about its axis and its revolution around Earth are the same, 27 1/3 days. It causes the same lunar hemisphere to always face Earth.
  • 33. Eclipses 22.2 The Earth–Moon–Sun System  Solar eclipses occur when the moon moves in a line directly between Earth and the sun, casting a shadow on Earth.  During a new-moon or full-moon phase, the moon’s orbit must cross the plane of the ecliptic for an eclipse to take place.  Lunar eclipses occur when the moon passes through Earth’s shadow.
  • 36. The Lunar Surface 22.3 Earth’s Moon • A crater is the depression at the summit of a volcano or a depression produced by a meteorite impact.  Craters • Most craters were produced by the impact of rapidly moving debris. • Rays are any of a system of bright, elongated streaks, sometimes associated with a crater on the moon.
  • 37. The Moon’s Surface Mare Tranquillitatus (Sea of Tranquility) Mare Imbrium (Sea of Rains) Kepler Crater Copernicus Crater
  • 38. Formation of a Crater
  • 39. The Lunar Surface 22.3 Earth’s Moon • Most of the lunar surface is made up of densely pitted, light-colored areas known as highlands.  Highlands • Maria, ancient beds of basaltic lava, originated when asteroids punctured the lunar surface, letting magma bleed out.  Maria • A rille is a long channel associated with lunar maria. A rille looks similar to a valley or a trench.
  • 40. The Lunar Surface 22.3 Earth’s Moon • The lunar regolith is a thin, gray layer on the surface of the moon, consisting of loosely compacted, fragmented material believed to have been formed by repeated impacts of meteorites.  Regolith
  • 42. Lunar History 22.3 Earth’s Moon  The most widely accepted model for the origin of the moon is that when the solar system was forming, a body the size of Mars impacted Earth. The resulting debris was ejected into space, began orbiting around Earth, and eventually united to form the moon.

Notas del editor

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