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The Sun-Earth-
Moon System
Notes Sheet
Section One- Earth
• A.Properties of Earth- people used to think that Earth was flat and at
the center of the universe
• 1.Earth is now known to be a round, three-dimensional sphere
• a. Axis- imaginary vertical line around which Earth spins
• b. Rotation- the spinning of Earth around its axis that causes day
and night
• 2.Earth has a magnetic field with north and south poles
• 3.Magnetic axis- imaginary line joining Earth’s magnetic poles
• a. Earth’s magnetic axis does not align with its rotational axis
• b. The location of the magnetic poles slowly changes over time
Section One- Earth
 B.Causes of seasons
1.Revolution- Earth’s yearly orbit around the Sun
• a. Earth’s orbit is an ellipse, or elongated closed curve.
• b. Because the Sun is not centered in the ellipse, the distance
between Earth and the Sun changes during the year
2.Earth’s tilt causes seasons
• a. The hemisphere tilted towards the Sun receives more daylight
hours that the hemisphere tilted away from the Sun
• b. The longer the period of sunlight is one reason summer is
warmer than winter
Section One- Earth
3.Earth’s tilt causes the Sun’s radiation to strike the hemispheres at different angles
• a. The hemisphere tilted toward the Sun receives more total solar
radiation the hemisphere tilted away from the Sun
• b. In the hemisphere tilted toward the Sun, the Sun appears high
in the sky and the radiation strikes Earth more directly
 C.Solstice- the day when the Sun reached its greatest distance
north or south of the equator
1.Summers solstice occurs June 21 or 22 in the northern hemisphere
2.Winter solstice occurs December 21 or 22 in the northern hemisphere
Section One- Earth
 D. Equinox- the day when the Sun is directly over Earth’s equator
1.Daylight and nighttime hours are equal all over the world
2.Vernal (Spring) equinox occurs on March 20 or 21 in the northern
hemisphere
3.Autumnal (Fall) equinox occurs on March 22 or 23 in the northern
hemisphere
Section Two- The Moon- Earth's
Satellites
 A.Motions of the Moon
1.The Moon rotates on its axis
2.The Moon’s rotation takes 27.3 days with the same side always facing the Earth
3.The Moon seems to shine because it reflects sunlight
Section Two- The Moon- Earth's
Satellites
 B.Moon Phases- the different forms the Moon takes in its
appearance from Earth
1.New Moon- when the Moon is between Earth and the Sun and cannot be seen
2.Waxing Phases- more of the illuminated half of the Moon that can be seen each
night after the new moon
• a. First visible thin slice of the moon is a waxing crescent
• b. First quarter phase- half the lighted side of the Moon is visible
• c. Waxing gibbus- more than one quarter is visible
• d. All of the Moon’s lighted side is visible during a full moon
Section Two- The Moon- Earth's
Satellites
3.Waning Phases- less of the illuminated half of the Moon is visible after the full
moon
• a. Waning gibbus- starts after a full moon when more than half of
the lighted side is still visible
• b. Only half of the Moon’s lighted side is visible during the third
quarter phase
• c. The last visible slice before a new moon is called the waning
crescent
4.The Moon completes its cycle of phases in about 29.5 days instead of 27.3 days
because it is keeping up with the Earth’s revolution around the Sun
Section Two- The Moon- Earth's
Satellites
 C.Eclipse- when Earth or the Moon casts a shadow on the other
1.Solar Eclipse- the Moon moved directly between Earth and the Sun, shadowing
part of Earth
• a. Under the umbra, or darkest part of the shadow, a total solar
eclipse occurs
• b. A partial solar eclipse happens in the lighter shadow on Earth’s
surface called the penumbra
• c. A total solar eclipse is visible only on a small area of Earth
Section Two- The Moon- Earth's
Satellites
2.Lunar Eclipse- when Earth’s shadow falls on the Moon
• a. If the Moon is completely in Earth’s umbra, a total lunar eclipse
occurs
• b. Partial lunar eclipse- when only part of the Moon moved into
Earth’s umbra, or the moon is totally in the penumbra
• c. A total lunar eclipse is visible on the night time side of Earth
when the night is clear
Section Two- The Moon- Earth's
Satellites
 D.The Moon’s surface has many depressions, or craters, formed
from meteorites, asteroids, and comets.
1.Cracks in the Moon’s crust caused lava to fill large craters, forming maria, or
dark, flat areas
2.Igneous maria rocks are 3 to 4 billion years old, indicating craters formed after
the surface cooled
 E.Data from moon quakes suggest that under the Moon’s crust
might lie a solid mantle, then a partly molten mantle and solid core.
 F.Impact Theory of the Moon Origin- the Moon formed billions of
years ago from Earth material thrown off when a large object
collided with Earth
Section Three- Exploring Earth's
Moon
 A.Missions to the Moon
1. Early exploration
• a. The first Luna spacecraft, launched by the Soviet Union in
1958,enabled close study of the Moon
• b. The Ranger spacecraft and the Lunar Orbiters of the U.S. took
detailed photographs of the Moon in the 1960s
• c. The seven Surveyor U.S. spacecrafts landed on the Moon
• d. Astronauts of Apollo 11 landed on the Moon in 1969
Section Three- Exploring Earth's
Moon
2.The Clementine spacecraft was placed in lunar orbit in 1994 to survey the
moon’s surface
• a. Collected data on the mineral content of Moon rocks
• b. Mapped features on the Moon’s surface
• c. Impact Basins, or craters, are depressions left by objects striking
the Moon
• d. Identified South Pole-Aitken Basin as possible location for a
moon colony
Section Three- Exploring Earth's
Moon
 B.Mapping the Moon
1.Data from Clementine yielded a map of the Moon showing its composition
• a. Moon’s crust is thinnest under its impact basins
• b. The crust on the side of the Moon facing the Earth is thinner
than on the far side
2.The Lunar Prospector was launched in 1998 to look for clues about the Moon’s
origin and makeup
• a.Showed hydrogen might exist in ice in crates at the Moon’s
poles
• b.Small, iron-rich core of the Moon supports the impact theory of
the Moon’s origin

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The Sun-Earth-Moon System Notes PowerPoint

  • 2. Section One- Earth • A.Properties of Earth- people used to think that Earth was flat and at the center of the universe • 1.Earth is now known to be a round, three-dimensional sphere • a. Axis- imaginary vertical line around which Earth spins • b. Rotation- the spinning of Earth around its axis that causes day and night • 2.Earth has a magnetic field with north and south poles • 3.Magnetic axis- imaginary line joining Earth’s magnetic poles • a. Earth’s magnetic axis does not align with its rotational axis • b. The location of the magnetic poles slowly changes over time
  • 3. Section One- Earth  B.Causes of seasons 1.Revolution- Earth’s yearly orbit around the Sun • a. Earth’s orbit is an ellipse, or elongated closed curve. • b. Because the Sun is not centered in the ellipse, the distance between Earth and the Sun changes during the year 2.Earth’s tilt causes seasons • a. The hemisphere tilted towards the Sun receives more daylight hours that the hemisphere tilted away from the Sun • b. The longer the period of sunlight is one reason summer is warmer than winter
  • 4. Section One- Earth 3.Earth’s tilt causes the Sun’s radiation to strike the hemispheres at different angles • a. The hemisphere tilted toward the Sun receives more total solar radiation the hemisphere tilted away from the Sun • b. In the hemisphere tilted toward the Sun, the Sun appears high in the sky and the radiation strikes Earth more directly  C.Solstice- the day when the Sun reached its greatest distance north or south of the equator 1.Summers solstice occurs June 21 or 22 in the northern hemisphere 2.Winter solstice occurs December 21 or 22 in the northern hemisphere
  • 5. Section One- Earth  D. Equinox- the day when the Sun is directly over Earth’s equator 1.Daylight and nighttime hours are equal all over the world 2.Vernal (Spring) equinox occurs on March 20 or 21 in the northern hemisphere 3.Autumnal (Fall) equinox occurs on March 22 or 23 in the northern hemisphere
  • 6. Section Two- The Moon- Earth's Satellites  A.Motions of the Moon 1.The Moon rotates on its axis 2.The Moon’s rotation takes 27.3 days with the same side always facing the Earth 3.The Moon seems to shine because it reflects sunlight
  • 7. Section Two- The Moon- Earth's Satellites  B.Moon Phases- the different forms the Moon takes in its appearance from Earth 1.New Moon- when the Moon is between Earth and the Sun and cannot be seen 2.Waxing Phases- more of the illuminated half of the Moon that can be seen each night after the new moon • a. First visible thin slice of the moon is a waxing crescent • b. First quarter phase- half the lighted side of the Moon is visible • c. Waxing gibbus- more than one quarter is visible • d. All of the Moon’s lighted side is visible during a full moon
  • 8. Section Two- The Moon- Earth's Satellites 3.Waning Phases- less of the illuminated half of the Moon is visible after the full moon • a. Waning gibbus- starts after a full moon when more than half of the lighted side is still visible • b. Only half of the Moon’s lighted side is visible during the third quarter phase • c. The last visible slice before a new moon is called the waning crescent 4.The Moon completes its cycle of phases in about 29.5 days instead of 27.3 days because it is keeping up with the Earth’s revolution around the Sun
  • 9. Section Two- The Moon- Earth's Satellites  C.Eclipse- when Earth or the Moon casts a shadow on the other 1.Solar Eclipse- the Moon moved directly between Earth and the Sun, shadowing part of Earth • a. Under the umbra, or darkest part of the shadow, a total solar eclipse occurs • b. A partial solar eclipse happens in the lighter shadow on Earth’s surface called the penumbra • c. A total solar eclipse is visible only on a small area of Earth
  • 10. Section Two- The Moon- Earth's Satellites 2.Lunar Eclipse- when Earth’s shadow falls on the Moon • a. If the Moon is completely in Earth’s umbra, a total lunar eclipse occurs • b. Partial lunar eclipse- when only part of the Moon moved into Earth’s umbra, or the moon is totally in the penumbra • c. A total lunar eclipse is visible on the night time side of Earth when the night is clear
  • 11. Section Two- The Moon- Earth's Satellites  D.The Moon’s surface has many depressions, or craters, formed from meteorites, asteroids, and comets. 1.Cracks in the Moon’s crust caused lava to fill large craters, forming maria, or dark, flat areas 2.Igneous maria rocks are 3 to 4 billion years old, indicating craters formed after the surface cooled  E.Data from moon quakes suggest that under the Moon’s crust might lie a solid mantle, then a partly molten mantle and solid core.  F.Impact Theory of the Moon Origin- the Moon formed billions of years ago from Earth material thrown off when a large object collided with Earth
  • 12. Section Three- Exploring Earth's Moon  A.Missions to the Moon 1. Early exploration • a. The first Luna spacecraft, launched by the Soviet Union in 1958,enabled close study of the Moon • b. The Ranger spacecraft and the Lunar Orbiters of the U.S. took detailed photographs of the Moon in the 1960s • c. The seven Surveyor U.S. spacecrafts landed on the Moon • d. Astronauts of Apollo 11 landed on the Moon in 1969
  • 13. Section Three- Exploring Earth's Moon 2.The Clementine spacecraft was placed in lunar orbit in 1994 to survey the moon’s surface • a. Collected data on the mineral content of Moon rocks • b. Mapped features on the Moon’s surface • c. Impact Basins, or craters, are depressions left by objects striking the Moon • d. Identified South Pole-Aitken Basin as possible location for a moon colony
  • 14. Section Three- Exploring Earth's Moon  B.Mapping the Moon 1.Data from Clementine yielded a map of the Moon showing its composition • a. Moon’s crust is thinnest under its impact basins • b. The crust on the side of the Moon facing the Earth is thinner than on the far side 2.The Lunar Prospector was launched in 1998 to look for clues about the Moon’s origin and makeup • a.Showed hydrogen might exist in ice in crates at the Moon’s poles • b.Small, iron-rich core of the Moon supports the impact theory of the Moon’s origin