The Sun-Earth- Moon System€¦ · Earth continues to rotate steadily, and eventually the Sun comes into view again the next morning. One complete rotation takes about 24 h,or one

The Sun-Earth-Moon System

Full Moon Rising—The Real StoryWhy does the Moon’s appearance change throughout the month?Do the Sun and Moon really rise? You will find the answers tothese questions and also learn why we have summer and winter.

Rotation or revolution—which motion of Earth brings morningand which brings summer? Science Journal

Many common observations,such as seasons, eclipses,and lunar phases, are causedby interactions between theSun, Earth, and the Moon.

SECTION 1EarthMain Idea Earth is asphere that rotates on atilted axis and revolvesaround the Sun.

SECTION 2The Moon—Earth’s SatelliteMain Idea Eclipses andphases of the Moon occur asthe Moon moves in relationto the Sun and Earth.

SECTION 3Exploring Earth’s MoonMain Idea Knowledge of the Moon’s structureand composition has

been increased by manyspacecraft missions to the Moon.

Chad Ehlers/Stone/Getty Images

Earth and the Moon All onEarth can see and feel the move-ments of Earth and the Moon as

they circle the Sun. Make the following Foldableto organize what you learn about these move-ments and their effects.

Fold a sheet of paper in half lengthwise.

Fold paper down2.5 cm from the top.(Hint: From the tip ofyour index finger toyour middle knuckleis about 2.5 cm.)

Open and drawlines along the2.5-cm fold.Label as shown.

Summarize in a Table As you read the chapter,summarize the movements of Earth and theMoon in the left column and the effects of thesemovements in the right column.

STEP 3

STEP 2

STEP 1

Model Rotation and RevolutionThe Sun rises in the morning; at least, itseems to. Instead, it is Earth that moves. Themovements of Earth cause day and night, aswell as the seasons. In this lab, you willexplore Earth’s movements.

1. Hold a basketball with one finger at thetop and one at the bottom. Have a class-mate gently spin the ball.

2. Explain how this models Earth’s rotation.

3. Continue to hold the basketball and walkone complete circle around anotherstudent in your class.

4. How does this model Earth’s revolution?

5. Think Critically Write a paragraph inyour Science Journal describing how thesemovements of the basketball modelEarth’s rotation and revolution.

Start-Up Activities

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Movements Effects

J ◆ 39J ◆ 39Chad Ehlers/Stone/Getty Images

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40 A ◆ J CHAPTER 2 The Sun-Earth-Moon System

Apply It! Practice summarizingas you read this chapter. Stop after each section and write a brief summary.

Learn It! Summarizing helps you organize information,focus on main ideas, and reduce the amount of information to remember.To summarize, restate the important facts in a short sentence or para-graph. Be brief and do not include too many details.

Practice It! Read the text on page 44 labeled Solstices.Then read the summary below and look at the important facts from that passage.

The solstice is the day whenthe Sun reaches its greatestdistance north or south ofthe equator.

Summary

Important Facts

In the northern hemisphere,the summer solstice occurs inJune, and the winter solsticeoccurs in December.

In the southern hemisphere,the winter solstice occurs inJune, and the summer solsticeoccurs in December.

Summer solstice is about thelongest period of daylight ofthe year.

Winter solstice is about theshortest period of daylight ofthe year.

J ◆ 40 B

Before You Read Statement After You ReadA or D A or D

1 Earth’s revolution around the Sun causes dayand night to occur.

2 Earth’s magnetic poles are aligned on Earth’srotational axis.

3 Summer occurs in the northern hemispherewhen Earth is closest to the Sun.

4 During an equinox, the number of daylighthours is nearly equal with the number of night-time hours all over the world.

5 When observing the phases of the Moon, theMoon’s lighted surface area is daylight on the Moonand the dark portion is nighttime on the Moon.

6 The length of one Moon day is about the sameamount of time as the length of one Earth day.

7 A lunar eclipse occurs when the Moon comesbetween Earth and the Sun.

8 Humans first walked on the Moon during theApollo spacecraft missions.

Print out a worksheetof this page at bookj.msscience.com

Reread your su

mmary to mak

e

sure you didn’t c

hange the

author’s origina

l meaning

or ideas.

Use this to focus on the main ideas as you read the chapter.

Before you read the chapter, respond to the statements

below on your worksheet or on a numbered sheet of paper.

• Write an A if you agree with the statement.

• Write a D if you disagree with the statement.

After you read the chapter, look back to this page to see if you’ve

changed your mind about any of the statements.

• If any of your answers changed, explain why.

• Change any false statements into true statements.

• Use your revised statements as a study guide.


Properties of Earth You awaken at daybreak to catch the Sun “rising” from the

dark horizon. Then it begins its daily “journey” from east to westacross the sky. Finally the Sun “sinks” out of view as night falls.Is the Sun moving—or are you?

It wasn’t long ago that people thought Earth was the centerof the universe. It was widely believed that the Sun revolvedaround Earth, which stood still. It is now common knowledgethat the Sun only appears to be moving around Earth. BecauseEarth spins as it revolves around the Sun, it creates the illusionthat the Sun is moving across the sky.

Another mistaken idea about Earth concerned its shape.Even as recently as the days of Christopher Columbus, manypeople believed Earth to be flat. Because of this, they were afraidthat if they sailed far enough out to sea, they would fall off theedge of the world. How do you know this isn’t true? How havescientists determined the true shape of Earth?

Spherical Shape A round, three-dimensional object is calleda sphere (SFIHR). Its surface is the same distance from its cen-ter at all points. Some common examples of spheres are basket-balls and tennis balls.

In the late twentieth century, artificial satellites and spaceprobes sent back pictures showing that Earth is spherical.Much earlier, Aristotle, a Greek astronomer and philosopherwho lived around 350 B.C., suspected that Earth was spherical.He observed that Earth cast a curved shadow on the Moonduring an eclipse.

In addition to Aristotle, otherindividuals made observationsthat indicated Earth’s sphericalshape. Early sailors, for example,noticed that the tops of ap-proaching ships appeared first onthe horizon and the rest appearedgradually, as if they were comingover the crest of a hill, as shownin Figure 1.

■ Examine Earth’s physicalcharacteristics.

■ Differentiate between rotationand revolution.

■ Discuss what causes seasonsto change.

Your life follows the rhythm ofEarth’s movements.

Review Vocabularyorbit: the path taken by an objectrevolving around another

New Vocabulary

• sphere • ellipse• axis • solstice• rotation • equinox• revolution

Earth

Figure 1 For many years, sailorshave observed that the tops ofships coming across the horizonappear first. This suggests thatEarth is spherical, not flat, as wasonce widely believed.

40

Additional Evidence Sailors also noticed changes in how thenight sky looked. As they sailed north or south, the North Starmoved higher or lower in the sky. The best explanation was aspherical Earth.

Today, most people know that Earth is spherical. They alsoknow all objects are attracted by gravity to the center of a spher-ical Earth. Astronauts have clearly seen the spherical shape ofEarth. However, it bulges slightly at the equator and is somewhatflattened at the poles, so it is not a perfect sphere.

Rotation Earth’s axis is the imaginary vertical line aroundwhich Earth spins. This line cuts directly through the center ofEarth, as shown in the illustration accompanying Table 1. Thepoles are located at the north and south ends of Earth’s axis. Thespinning of Earth on its axis, called rotation, causes day and nightto occur. Here is how it works. As Earth rotates, you can see theSun come into view at daybreak. Earth continues to spin, makingit seem as if the Sun moves across the sky until it sets at night.During night, your area of Earth has rotated so that it is facingaway from the Sun. Because of this, the Sun is no longer visible toyou. Earth continues to rotate steadily, and eventually the Suncomes into view again the next morning. One complete rotationtakes about 24 h, or one day. How many rotations does Earth com-plete during one year? As you can infer from Table 1, it completesabout 365 rotations during its one-year journey around the Sun.

Why does the Sun seem to rise and set?

AxisTable 1 Physical Properties of Earth

Diameter (pole to pole) 12,714 km

Diameter (equator) 12,756 km

Circumference (poles) 40,008 km

Circumference (equator) 40,075 km

Mass 5.98 � 1024 kg

Average density 5.52 g/cm3

Average distance to the Sun 149,600,000 km

Period of rotation (1 day) 23 h, 56 min

Period of revolution (1 year) 365 days, 6 h, 9 min

Earth’s RotationSuppose that Earth’srotation took twice aslong as it does now. Inyour Science Journal, pre-dict how conditions suchas global temperatures,work schedules, plantgrowth, and other factorsmight change underthese circumstances.

SECTION 1 Earth J ◆ 41

Rotation

42 ◆ J CHAPTER 2 The Sun-Earth-Moon System

Magnetic FieldScientists hypothesize that the movementof material inside Earth’s core, along with

Earth’s rotation, generates a magnetic field. This magnetic fieldis much like that of a bar magnet. Earth has a north and a southmagnetic pole, just as a bar magnet has opposite magnetic polesat each of its ends. When you sprinkle iron shavings over a barmagnet, the shavings align with the magnetic field of the mag-net. As you can see in Figure 2, Earth’s magnetic field issimilar—almost as if Earth contained a giant bar magnet.Earth’s magnetic field protects you from harmful solar radiationby trapping many charged particles from the Sun.

Magnetic Axis When you observe a compass needle point-ing north, you are seeing evidence of Earth’s magnetic field.Earth’s magnetic axis, the line joining its north and south mag-netic poles, does not align with its rotational axis. The magneticaxis is inclined at an angle of 11.5° to the rotational axis. Ifyou followed a compass needle, you would end up at the mag-netic north pole rather than the rotational north pole.

The location of the magnetic poles has been shown to changeslowly over time. The magnetic poles move around the rotational(geographic) poles in an irregular way. This movement can besignificant over decades. Many maps include information aboutthe position of the magnetic north pole at the time the map wasmade. Why would this information be important?

Figure 2 Earth’s magnetic fieldis similar to that of a bar magnet,almost as if Earth contained a giantmagnet. Earth’s magnetic axisis angled 11.5 degrees from itsrotational axis.

Axis

S

N

North magnetic pole

South magnetic pole

Making Your OwnCompassProcedure

WARNING: Use care whenhandling sharp objects.1. Cut off the bottom of a

plastic foam cup to makea polystyrene disk.

2. Magnetize a sewingneedle by continuouslystroking the needle in thesame direction with amagnet for 1 min.

3. Tape the needle to thecenter of the foam disk.

4. Fill a plate with water andfloat the disk, needle sideup, in the water.

Analysis1. What happened to the

needle and disk when youplaced them in the water?Why did this happen?

2. Infer how ancient sailorsmight have used magnetsto help them navigate onthe open seas.


What causes changing seasons?Flowers bloom as the days get warmer. The Sun appears

higher in the sky, and daylight lasts longer. Spring seems like afresh, new beginning. What causes these wonderful changes?

Orbiting the Sun You learned earlier that Earth’s rotationcauses day and night. Another important motion is revolution,which is Earth’s yearly orbit around the Sun. Just as the Moon isEarth’s satellite, Earth is a satellite of the Sun. If Earth’s orbitwere a circle with the Sun at the center, Earth would maintain aconstant distance from the Sun. However, this is not the case.Earth’s orbit is an ellipse (ee LIHPS)—an elongated, closedcurve. The Sun is not at the center of the ellipse but is a littletoward one end. Because of this, the distance between Earth andthe Sun changes during Earth’s yearlong orbit. Earth gets closestto the Sun—about 147 million km away—around January 3.The farthest Earth gets from the Sun is about 152 million kmaway. This happens around July 4 each year.

What is an ellipse?

Does this elliptical orbit cause seasonal temperatures onEarth? If it did, you would expect the warmest days to be inJanuary. You know this isn’t the case in the northern hemi-sphere, something else must cause the change.

Even though Earth is closest to the Sun in January, thechange in distance is small. Earth is exposed to almost the sameamount of Sun all year. But the amount of solar energy any oneplace on Earth receives varies greatly during the year. Next, youwill learn why.

A Tilted Axis Earth’s axis is tilted23.5° from a line drawn perpendicularto the plane of its orbit. It is this tilt thatcauses seasons. The number of daylighthours is greater for the hemisphere, orhalf of Earth, that is tilted toward theSun. Think of how early it gets dark inthe winter compared to the summer. Asshown in Figure 3, the hemisphere thatis tilted toward the Sun receives morehours of sunlight each day than thehemisphere that is tilted away from theSun. The longer period of sunlight isone reason summer is warmer thanwinter, but it is not the only reason.

North Pole

Figure 3 In summer, the north-ern hemisphere is tilted toward theSun. Notice that the north pole isalways lit during the summer. Observe Why is there a greaternumber of daylight hours in thesummer than in the winter?

Topic: EllipsesVisit for Weblinks to information about orbitsand ellipses.

Activity Scientists compareorbits by how close they come tobeing circular. To do this, they usea measurement called eccentricity.A circle has an eccentricity of zero.Ellipses have eccentricities that aregreater than zero, but less thanone. The closer the eccentricity isto one, the more elliptical theorbit. Compare the orbits of thefour inner planets. List them inorder of increasing eccentricity.

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Radiation from the Sun Earth’s tilt also causes the Sun’sradiation to strike the hemispheres at different angles. Sunlightstrikes the hemisphere tilted towards the Sun at a higher angle,that is, closer to 90 degrees, than the hemisphere tilted away.Thus it receives more total solar radiation than the hemispheretilted away from the Sun, where sunlight strikes at a lower angle.

Summer occurs in the hemisphere tilted toward the Sun,when its radiation strikes Earth at a higher angle and for longerperiods of time. The hemisphere receiving less radiation experi-ences winter.

SolsticesThe solstice is the day when the Sun reaches its greatest dis-

tance north or south of the equator. In the northern hemisphere,the summer solstice occurs on June 21 or 22, and the wintersolstice occurs on December 21 or 22. Both solstices are illus-trated in Figure 4. In the southern hemisphere, the winter sol-stice is in June and the summer solstice is in December. Summersolstice is about the longest period of daylight of the year. Afterthis, the number of daylight hours become less and less, untilthe winter solstice, about the shortest period of daylight of theyear. Then the hours of daylight start to increase again.

Figure 4 During the summersolstice in the northern hemi-sphere, the Sun is directly over thetropic of Cancer, the latitude lineat 23.5° N latitude. During thewinter solstice, the Sun is directlyover the tropic of Capricorn, thelatitude line at 23.5° S latitude. Atfall and spring equinoxes, the Sunis directly over the equator.

Tropic of

Cancer

Equator

Tropic of

Capricor

n

Tropic of

Cancer

Equator

Tropic of

Capricor

n

Tropic of

Cancer

Equator

Tropic of

Capricor

n

Tropic of

Cancer

Equator

Tropic of

Capricor

n

Summer solstice for northern hemisphere

Winter solstice for northern hemisphere

Fall equinox

Spring equinox

Self Check1. Explain why Aristotle thought Earth was spherical.

2. Compare and contrast rotation and revolution.

3. Describe how Earth’s distance from the Sun changesthroughout the year. When is Earth closest to the Sun?

4. Explain why it is summer in Earth’s northern hemisphereat the same time it is winter in the southern hemisphere.

5. Think Critically Table 1 lists Earth’s distance from theSun as an average. Why isn’t an exact measurementavailable for this distance?

SummaryProperties of Earth

• Earth is a slightly flattened sphere that rotatesaround an imaginary line called an axis.

• Earth has a magnetic field, much like a barmagnet.

• The magnetic axis of Earth differs from itsrotational axis.

Seasons

• Earth revolves around the Sun in an ellipticalorbit.

• The tilt of Earth’s axis and its revolution causethe seasons.

• Solstices are days when the Sun reaches itsfarthest points north or south of the equator.

• Equinoxes are the points when the Sun isdirectly over the equator.

6. Classify The terms clockwise and counterclockwise areused to indicate the direction of circular motion. Howwould you classify the motion of the Moon aroundEarth as you view it from above Earth’s north pole?Now try to classify Earth’s movement around the Sun.

EquinoxesAn equinox (EE kwuh nahks) occurs when the Sun is directly

above Earth’s equator. Because of the tilt of Earth’s axis, the Sun’sposition relative to the equator changes constantly. Most of thetime, the Sun is either north or south of the equator, but twotimes each year it is directly over it, resulting in the spring and fallequinoxes. As you can see in Figure 4, at an equinox the Sunstrikes the equator at the highest possible angle, 90°.

During an equinox, the number of daylight hours and night-time hours is nearly equal all over the world. Also at this time,neither the northern hemisphere nor the southern hemisphereis tilted toward the Sun.

In the northern hemisphere, the Sun reaches the spring equinox on March 20 or 21, and the fall equinox occurs onSeptember 22 or 23. In the southern hemisphere, the equinoxesare reversed. Spring occurs in September and fall occurs in March.

Earth Data Review As you have learned, Earth is a spherethat rotates on a tilted axis. This rotation causes day and night.Earth’s tilted axis and its revolution around the Sun cause theseasons. One Earth revolution takes one year. In the next sec-tion, you will read how the Moon rotates on its axis and revolvesaround Earth.


Topic: SeasonsVisit for Weblinks to information about theseasons.

Activity Make a posterdescribing how the seasons differin other parts of the world. Showhow holidays might be celebrateddifferently and how farming mightvary between hemispheres.

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Moon’s orbit

Moon’s rotation

Northpole

46 ◆ J CHAPTER 2 The Earth-Sun-Moon System

Motions of the MoonJust as Earth rotates on its axis and revolves around the Sun,

the Moon rotates on its axis and revolves around Earth. TheMoon’s revolution around Earth is responsible for the changesin its appearance. If the Moon rotates on its axis, why can’t yousee it spin around in space? The reason is that the Moon’s rota-tion takes 27.3 days—the same amount of time it takes torevolve once around Earth. Because these two motions take thesame amount of time, the same side of the Moon always facesEarth, as shown in Figure 5.

You can demonstrate this by having a friend hold a ball infront of you. Direct your friend to move the ball in a circlearound you while keeping the same side of it facing you.Everyone else in the room will see all sides of the ball. You willsee only one side. If the moon didn’t rotate, we would see all ofits surface during one month.

The Moon—Earth’s Satellite

■ Identify phases of the Moon andtheir cause.

■ Explain why solar and lunareclipses occur.

■ Infer what the Moon’s surfacefeatures may reveal about itshistory.

Learning about the Moon can teachyou about Earth.

Review Vocabularymantle: portion of the interior ofa planet or moon lying betweenthe crust and core

New Vocabulary

• moon phase • waning• new moon • solar eclipse• waxing • lunar eclipse• full moon • maria

Figure 5 In about 27.3 days,the Moon orbits Earth. It alsocompletes one rotation on itsaxis during the same period.Think Critically Explain how thisaffects which side of the Moon facesEarth.

SECTION 2 The Moon—Earth’s Satellite J ◆ 47

Reflection of the Sun The Moon seems to shine because itssurface reflects sunlight. Just as half of Earth experiences day asthe other half experiences night, half of the Moon is lightedwhile the other half is dark. As the Moon revolves around Earth,you see different portions of its lighted side, causing the Moon’sappearance to change.

Phases of the Moon Moon phases are the different forms that the Moon takes in

its appearance from Earth. The phase depends on the relativepositions of the Moon, Earth, and the Sun, as seen in Figure 6on the next page. A new moon occurs when the Moon isbetween Earth and the Sun. During a new moon, the lighted halfof the Moon is facing the Sun and the dark side faces Earth. TheMoon is in the sky, but it cannot be seen. The new moon risesand sets with the Sun.

Why can’t you see a new moon?

Waxing Phases After a new moon, the phases begin waxing.Waxing means that more of the illuminated half of the Mooncan be seen each night. About 24 h after a new moon, you cansee a thin slice of the Moon. This phase is called the waxing cres-cent. About a week after a new moon, you can see half of thelighted side of the Moon, or one quarter of the Moon’s surface.This is the first quarter phase.

The phases continue to wax. When more than one quarter isvisible, it is called waxing gibbous after the Latin word for“humpbacked.” A full moon occurs when all of the Moon’s sur-face facing Earth reflects light.

Waning Phases After a full moon, the phases are said tobe waning. When the Moon’s phases are waning, you seeless of its illuminated half each night. Waning gibbous beginsjust after a full moon. When you can see only half of thelighted side, it is the third-quarter phase. The Moon continuesto appear to shrink. Waning crescent occurs just beforeanother new moon. Once again, you can see only a small sliceof the Moon.

It takes about 29.5 days for the Moon to complete its cycle ofphases. Recall that it takes about 27.3 days for the Moon torevolve around Earth. The discrepancy between these two num-bers is due to Earth’s revolution. The roughly two extra days arewhat it takes for the Sun, Earth, and Moon to return to theirsame relative positions.

Comparing the Sunand the MoonProcedure1. Find an area where you

can make a chalk mark onpavement or similarsurface.

2. Tie a piece of chalk to oneend of a 200-cm-longstring.

3. Hold the other end of thestring to the pavement.

4. Have a friend pull thestring tight and walkaround you, drawing acircle (the Sun) on thepavement.

5. Draw a 1-cm-diametercircle in the middle of thelarger circle (the Moon).

Analysis1. How big is the Sun com-

pared to the Moon?2. The diameter of the Sun

is 1.39 million km. Thediameter of Earth is12,756 km. Draw two newcircles modeling the sizesof the Sun and Earth.What scaledid you use?


EclipsesImagine living 10,000 years ago. You are foraging for nuts

and fruit when unexpectedly the Sun disappears from the sky.The darkness lasts only a short time, and the Sun soon returnsto full brightness. You know something strange has happened,but you don’t know why. It will be almost 8,000 years beforeanyone can explain what you just experienced.

The event just described was a total solar eclipse (ih KLIPS),shown in Figure 7. Today, most people know what causes sucheclipses, but without this knowledge, they would have been terrify-ing events. During a solar eclipse, many animals act as if it is night-time. Cows return to their barns and chickens go to sleep. Whatcauses the day to become night and then change back into day?

What happens during a total solar eclipse?

Figure 6 The phases of the Moon change during a cycle that lasts about 29.5 days.

New

1st qtr.

3rd qtr.

Waxinggibbous

Waxingcrescent

Waninggibbous

Waningcrescent

Earth

Full

Sunlight

Figure 7 The outer portion ofthe Sun’s atmosphere is visibleduring a total solar eclipse. It lookslike a halo around the Moon.

Photographs of moon phasesare as seen from Earth.

(bl)Richard J. Wainscoat/Peter Arnold, Inc., (others)Lick Observatory


What causes an eclipse? The revolution of the Mooncauses eclipses. Eclipses occur when Earth or the Moon tem-porarily blocks the sunlight from reaching the other.Sometimes, during a new moon, the Moon’s shadow falls onEarth and causes a solar eclipse. During a full moon, Earth’sshadow can be cast on the Moon, resulting in a lunar eclipse.

An eclipse can occur only when the Sun, the Moon, andEarth are lined up perfectly. Because the Moon’s orbit is not inthe same plane as Earth’s orbit around the Sun, lunar eclipsesoccur only a few times each year.

Eclipses of the Sun A solar eclipse occurs when the Moonmoves directly between the Sun and Earth and casts its shadowover part of Earth, as seen in Figure 8. Depending on where youare on Earth, you may experience a total eclipse or a partialeclipse. The darkest portion of the Moon’s shadow is called theumbra (UM bruh). A person standing within the umbra experi-ences a total solar eclipse. During a total solar eclipse, the onlyvisible portion of the Sun is a pearly white glow around the edgeof the eclipsing Moon.

Surrounding the umbra is a lighter shadow on Earth’s sur-face called the penumbra (puh NUM bruh). Persons standingin the penumbra experience a partial solar eclipse. WARNING:Regardless of which eclipse you view, never look directly at the Sun.The light can permanently damage your eyes.

Area of total eclipse

Umbra

Penumbra

Area of partial eclipse

Distances are not drawn to scale.

Figure 8 Only a small area ofEarth experiences a total solareclipse during the eclipse event.

Topic: EclipsesVisit for Weblinks to information about solarand lunar eclipses.

Activity Make a chart showingthe dates when lunar and solareclipses will be visible in your area.Include whether the eclipses willbe total or partial.

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Eclipses of the Moon When Earth’s shadow falls on theMoon, a lunar eclipse occurs. A lunar eclipse begins when theMoon moves into Earth’s penumbra. As the Moon continues tomove, it enters Earth’s umbra and you see a curved shadow onthe Moon’s surface, as in Figure 9. Upon moving completelyinto Earth’s umbra, as shown in Figure 10, the Moon goes dark,signaling that a total lunar eclipse has occurred. Sometimes sun-light bent through Earth’s atmosphere causes the eclipsed Moonto appear red.

A partial lunar eclipse occurs when only a portion of theMoon moves into Earth’s umbra. The remainder of theMoon is in Earth’s penumbra and, therefore, receives somedirect sunlight. A penumbral lunar eclipse occurs when theMoon is totally within Earth’s penumbra. However, it is dif-

ficult to tell when a penum-bral lunar eclipse occursbecause some sunlight con-tinues to fall on the side ofthe Moon facing Earth.

A total lunar eclipse canbe seen by anyone on thenighttime side of Earth wherethe Moon is not hidden byclouds. In contrast, only alucky few people get towitness a total solar eclipse.Only those people in the smallregion where the Moon’sumbra strikes Earth can wit-ness one.

Figure 9 These photographsshow the Moon moving from rightto left into Earth’s umbra, thenout again.

Figure 10 During a total lunareclipse, Earth’s shadow blocks lightcoming from the Sun.

Umbra

Penumbra

Dr. Fred Espenak/Science Photo Library/Photo Researchers


The Moon’s Surface When you look at the Moon, as shown in Figure 12 on the

next page, you can see many depressions called craters.Meteorites, asteroids, and comets striking the Moon’s surfacecreated most of these craters, which formed early in the Moon’shistory. Upon impact, cracks may have formed in the Moon’scrust, allowing lava to reach the surface and fill up the largecraters. The resulting dark, flat regions are called maria (MAHRee uh). The igneous rocks of the maria are 3 billion to 4 billionyears old. So far, they are the youngest rocks to be found on theMoon. This indicates that craters formed after the Moon’s sur-face originally cooled. The maria formed early enough in theMoon’s history that molten material still remained in theMoon’s interior. The Moon once must have been as geologicallyactive as Earth is today. Before the Moon cooled to the currentcondition, the interior separated into distinct layers.

Inside the Moon Earthquakes allow scientists to learn about Earth’s interior.

In a similar way, scientists use instruments such as the one in Figure 11 to study moonquakes. The data they have receivedhave led to the construction of several models of theMoon’s interior. One such model, shown in Figure 11,suggests that the Moon’s crust is about 60 km thick onthe side facing Earth. On the far side, it is thought to beabout 150 km thick. Under the crust, a solid mantle mayextend to a depth of 1,000 km. A partly molten zone ofthe mantle may extend even farther down. Below thismantle may lie a solid, iron-rich core.

Crust

Upper mantle

Core

Lower mantle

SeismographControl center

Figure 11 Equipment, such asthe seismograph left on the Moonby the Apollo 12 mission, helpsscientists study moonquakes.

Models of the Moon’s interior were created fromdata obtained by scientists studying moonquakes.

Seismology A seismologistis an Earth scientist whostudies the propagation ofseismic waves in geologicalmaterials. Usually thismeans studying earth-quakes, but some seismolo-gists apply their knowledgeto studies of the Moon andplanets. Seismologists usu-ally study geology, physics,and applied mathematics incollege and later specializein seismology for anadvanced degree.

Bettmann/CORBIS

Figure 12

VISUALIZING THE MOON’S SURFACE

52 ◆ J CHAPTER 2

By looking through binoculars, you can see many of the features on the surface of the Moon. These include craters that are hundreds of kilometers wide, light-colored mountains, and darker patches that

early astronomers called maria (Latin for “seas”). However, as the NASA Apollomissions discovered, these so-called seas do not contain water. In fact, maria (singular, mare) are flat, dry areas formed by ancient lava flows. Some of theMoon’s geographic features are shownbelow, along with the landing sitesof Apollo missions sent toinvestigate Earth’sclosest neighborin space.

Sea ofSerenity

(Mare Serenitatis)

Sea of Rains (Mare Imbrium)

Sea of Clouds

(MareNubium)

Sea of Moisture(Mare

Humorum)

Sea of Fertility(Mare

Fecunditatis)

Sea ofNectar

(Mare Nectaris)

Sea ofVapor

(Mare Vaporum)

Sea of Crisis (Mare Crisium)

Sea ofTranquility

(Mare Tranquillitatis)

S e ao f C o l d ( M a r e F r i g

o r i s )

APOLLO 15

APOLLO 17

APOLLO 11

APOLLO 16

APOLLO 12APOLLO 14First major

scientificexperimentsset up onthe Moon

Longestand finalApollomission to the Moon

First landing in thelunar mountains

First astro-naut sets footon the Moon

Crew exploresmountains

Oc

ea

no

fS

to

r ms

(Oce

an

us

Pr

oc

el l a

r um

)

Plato Crater

EndymionCrater

Copernicus CraterKeplerCrater

PythagorasCrater

AristotelesCrater

First wheeled-vehicle excursions

NASAastronaut

NASA


The Moon’s Origin Before the Apollo space missions in the 1960s and 1970s,

there were three leading theories about the Moon’s origin.According to one theory, the Moon was captured by Earth’s grav-ity. Another held that the Moon and Earth condensed from thesame cloud of dust and gas. An alternative theory proposed thatEarth ejected molten material that became the Moon.

The Impact Theory The data gathered by the Apollo mis-sions have led many scientists to support a new theory, knownas the impact theory. It states that the Moon formed billions ofyears ago from condensing gas and debris thrown off whenEarth collided with a Mars-sized object as shown in Figure 13.

Figure 13 According to theimpact theory, a Mars-sized objectcollided with Earth around 4.6 bil-lion years ago. Vaporized materialsejected by the collision beganorbiting Earth and quickly con-solidated into the Moon.

A Mars-sizedobject collidedwith Earth.

The blast ejectedmaterial from bothobjects into space.

A ring of gasand debris formedaround Earth.

Particles in thering joined togetherto form the Moon.

What will you use to survive on the Moon?

You have crash-landed on the Moon. It will take one day to reach a mooncolony on foot. The side of the Moon that you are on will be facing away fromthe Sun during your entire trip. You manage to salvage the following items fromyour wrecked ship: food, rope, solar-powered heating unit, battery-operated heat-ing unit, oxygen tanks, map of the constellations, compass, matches, water, solar-powered radio transmitter, three flashlights, signal mirror, and binoculars.

Identifying the Problem The Moon lacks a magnetic field

and has no atmosphere. How do theMoon’s physical properties and the lackof sunlight affect your decisions?

Solving the Problem 1. Which items will be of no use to you?

Which items will you take with you? 2. Describe why each of the salvaged

items is useful or not useful.


Self Check1. Explain how the Sun, Moon, and Earth are positioned

relative to each other during a new moon and howthis alignment changes to produce a full moon.

2. Describe what phase the Moon must be in to have alunar eclipse. A solar eclipse?

3. Define the terms umbra and penumbra and explainhow they relate to eclipses.

4. Explain why lunar eclipses are more common thansolar eclipses and why so few people ever have achance to view a total solar eclipse.

5. Think Critically What do the surface features andtheir distribution on the Moon’s surface tell you aboutits history?

SummaryMotions of the Moon

• The Moon rotates on its axis about once eachmonth.

• The Moon also revolves around Earth aboutonce every 27.3 days.

• The Moon shines because it reflects sunlight.Phases of the Moon

• During the waxing phases, the illuminatedportion of the Moon grows larger.

• During waning phases, the illuminated por-tion of the Moon grows smaller.

• Earth passing directly between the Sun andthe Moon causes a lunar eclipse.

• The Moon passing between Earth and the Suncauses a solar eclipse.

Structure and Origin of the Moon

• The Moon’s surface is covered with depres-sions called impact craters.

• Flat, dark regions within craters are called maria.• The Moon may have formed as the result of a

collision between Earth and a Mars-sized object.

6. Solve Simple Equations The Moon travels in itsorbit at about 3,400 km/h. Therefore, during a solareclipse, its shadow sweeps at this speed from westto east. However, Earth rotates from west to east atabout 1,670 km/h near the equator. At what speeddoes the shadow really move across this part ofEarth’s surface?

The Moon in History Studyingthe Moon’s phases and eclipses led tothe conclusion that both Earth andthe Moon were in motion around theSun. The curved shadow Earth castson the Moon indicated to early scien-tists that Earth was spherical. WhenGalileo first turned his telescopetoward the Moon, he found a surfacescarred by craters and maria. Beforethat time, many people believed thatall planetary bodies were perfectlysmooth and lacking surface features.Now, actual moon rocks are availablefor scientists to study, as seen inFigure 14. By doing so, they hope tolearn more about Earth.

How has observing the Moon been importantto science?

Figure 14 Moon rocks collectedby astronauts provide scientistswith information about the Moonand Earth.

bookj.msscience.com/self_check_quizRoger Ressmeyer/CORBIS


In this lab, you will demonstrate the positions ofthe Sun, the Moon, and Earth during certainphases and eclipses. You also will see why only asmall portion of the people on Earth witness atotal solar eclipse during a particular eclipse event.

Real-World QuestionCan a model be devised to show the positionsof the Sun, the Moon, and Earth during variousphases and eclipses?

Goals■ Model moon phases.■ Model solar and lunar eclipses.

Materialslight source (unshaded) globepolystyrene ball pencil

Safety Precautions

Procedure1. Review the illustrations of moon phases and

eclipses shown in Section 2.

2. Use the light source as a Sun model and apolystyrene ball on a pencil as a Moonmodel. Move the Moon around the globe toduplicate the exact position that would haveto occur for a lunar eclipse to take place.

3. Move the Moon to the position that wouldcause a solar eclipse.

4. Place the Moon at each of the followingphases: first quarter, full moon, third quar-ter, and new moon. Identify which, if any,type of eclipse could occur during eachphase. Record your data.

5. Place the Moon at the location where a lunareclipse could occur. Move it slightly towardEarth, then away from Earth. Note theamount of change in the size of the shadow.

6. Repeat step 5 with the Moon in a positionwhere a solar eclipse could occur.

Conclude and Apply1. Identify which phase(s) of the Moon

make(s) it possible for an eclipse to occur.

2. Describe the effect of a small change in dis-tance between Earth and the Moon on thesize of the umbra and penumbra.

3. Infer why a lunar and a solar eclipse do notoccur every month.

4. Explain why only a few people have experi-enced a total solar eclipse.

5. Diagram the positions of the Sun, Earth,and the Moon during a first-quarter moon.

6. Infer why it might be better to call a fullmoon a half moon.

Mhhn Phases and E#lipses

Communicate your answers to other students.

LAB J ◆ 55

Moon Phase Observations

Moon Phase Observations

First quarter

Full moon

Third quarter

New moon

Do not write inthis book.

July 20, 1969Apollo 11 lands on the Moon.Neil Armstrong becomes thefirst human to set foot onanother celestial body.

Lunarlander

April 11, 1970Apollo 13 launched.Explosion causes missionto abort. Astronautsbarely make it home.

July 30, 1971Apollo 15 lands on theMoon. Crew deploysfirst lunar roving vehicle.

December 11, 1972Apollo 17 lands on theMoon. The first geologistvisits on the last crewedMoon mission.

August 1966–August 1967Five Lunar Orbiters launched by U.S. photograph virtually the entire Moon.

June 2, 1966Surveyor 1, first ofseven U.S. Surveyormissions, makes aperfect soft landingon the Moon.

July 31, 1964U.S. receives perfectphotos from uncrewedprobe Ranger 7 beforeit crash lands onthe Moon.

October 7, 1959Russian space probeLuna 3 returns firstpictures of the Moon’sfar side.

1959 1964 1965 1967 19681966 1969 1970 1971 1972 1973

December 24, 1968Apollo 8, along withits crew, becomes the first mission to orbit the Moon.

Missions to the MoonThe Moon has always fascinated humanity. People have

made up stories about how it formed. Children’s stories evensuggested it was made of cheese. Of course, for centuriesastronomers also have studied the Moon for clues to its makeupand origin. In 1959, the former Soviet Union launched the firstLuna spacecraft, enabling up-close study of the Moon. Two yearslater, the United States began a similar program with the firstRanger spacecraft and a series of Lunar Orbiters. The spacecraftin these early missions took detailed photographs of the Moon.

The next step was the Surveyor spacecraft designed to takemore detailed photographs and actually land on the Moon. Fiveof these spacecraft successfully touched down on the lunar sur-face and performed the first analysis of lunar soil. The goal ofthe Surveyor program was to prepare for landing astronauts onthe Moon. This goal was achieved in 1969 by the astronauts ofApollo 11. By 1972, when the Apollo missions ended, 12 U.S.astronauts had walked on the Moon. A time line of these impor-tant moon missions can be seen in Figure 15.

■ Describe recent discoveriesabout the Moon.

■ Examine facts about the Moonthat might influence futurespace travel.

Continuing moon missions may resultin discoveries about Earth’s origin.

Review Vocabularycomet: space object orbiting theSun formed from dust and rockparticles mixed with frozenwater, methane, and ammonia

New Vocabulary

• impact basin

Exploring Earth’s Moon


Figure 15 This time line illustrates some of the most important events inthe history of moon exploration.

Surveying the Moon There is still much to learn about theMoon and, for this reason, the United States resumed its studies.In 1994, the Clementine was placed into lunar orbit. Its goal wasto conduct a two-month survey of the Moon’s surface. Animportant aspect of this study was collecting data on the min-eral content of Moon rocks. In fact, this part of its mission wasinstrumental in naming the spacecraft. Clementine was thedaughter of a miner in the ballad My Darlin’ Clementine. Whilein orbit, Clementine also mapped features on the Moon’s sur-face, including huge impact basins.

Why was Clementine placed in lunar orbit?

Impact Basins When meteorites and other objects strike theMoon, they leave behind depressions in the Moon’s surface. Thedepression left behind by an object striking the Moon is knownas an impact basin, or impact crater. The South Pole-AitkenBasin is the oldest identifiable impact feature on the Moon’s sur-face. At 12 km in depth and 2,500 km in diameter, it is also thelargest and deepest impact basin in the solar system.

Impact basins at the poles were of special interest to scien-tists. Because the Sun’s rays never strike directly, the crater bot-toms remain always in shadow. Temperatures in shadowed areas,as shown in Figure 16, would be extremely low, probably nevermore than �173°C. Scientists hypothesize that any ice depositedby comets impacting the Moon throughout its history wouldremain in these shadowed areas. Indeed, early signals fromClementine indicated the presence of water. This was intriguing,because it could be a source of water for future moon colonies.

Figure 16 The South Pole-Aitken Basin is the largest of itskind found anywhere in the solarsystem. The deepest craters in thebasin stay in shadow throughoutthe Moon’s rotation. Ice depositsfrom impacting comets arethought to have collected at thebottom of these craters.

J ◆ 57

Topic: The Far SideVisit for Weblinks to information about the farside of the Moon.

Activity Compare the image ofthe far side of the Moon with thatof the near side shown in Figure 12.Make a list of all the differences younote and then compare them withlists made by other students.

bookj.msscience.com

BMDO/NRL/LLNL/Science Photo Library/Photo Researchers



Mapping the MoonA large part of Clementine’s mission included taking high-

resolution photographs so a detailed map of the Moon’s surfacecould be compiled. Clementine carried cameras and otherinstruments to collect data at wavelengths ranging from infraredto ultraviolet. One camera could resolve features as small as 20 macross. One image resulting from Clementine data is shown inFigure 17. It shows that the crust on the side of the Moon thatfaces Earth is much thinner than the crust on the far side.Additional information shows that the Moon’s crust is thinnestunder impact basins. Based on analysis of the light data receivedfrom Clementine, a global map of the Moon also was createdthat shows its composition, as seen in Figure 18.

What information about the Moon did scientistslearn from Clementine?

The Lunar Prospector The success of Clementine opened thedoor for further moon missions. In 1998, NASA launched the desk-sized Lunar Prospector, shown in Figure 18, into lunar orbit. Thespacecraft spent a year orbiting the Moon from pole to pole, onceevery two hours. The resulting maps confirmed the Clementinedata. Also, data fromLunar Prospector con-firmed that the Moonhas a small, iron-richcore about 600 km indiameter. A small coresupports the impact the-ory of how the Moonformed—only a smallamount of iron could beblasted away from Earth.

Figure 17 This computer-enhanced map based onClementine data indicates thethickness of the Moon’s crust. Thecrust of the side of the Moon facingEarth, shown mostly in red, is thin-ner than the crust on the far side ofthe Moon.

Figure 18 Lunar Prospector per-formed high-resolution mappingof the lunar surface and had instru-ments that detected water ice atthe lunar poles.

(t)Zuber et al/Johns Hopkins University/NASA/Photo Researchers, (b)NASA

SECTION 3 Exploring Earth’s Moon J ◆ 59

Self Check1. Name the first U.S. spacecraft to successfully land

on the Moon. What was the major purpose of thisprogram?

2. Explain why scientists continue to study the Moon longafter the Apollo program ended and list some of thetypes of data that have been collected.

3. Explain how water ice might be preserved in portionsof deep impact craters.

4. Describe how the detection of a small iron-rich coresupports the theory that the Moon was formed from acollision between Earth and a Mars-sized object.

5. Think Critically Why might the discovery of ice inimpact basins at the Moon’s poles be important tofuture space flights?

SummaryMissions to the Moon

• The first lunar surveys were done by Luna,launched by the former Soviet Union, andU.S.-launched Ranger and Lunar Orbiters.

• Five Surveyor probes landed on the Moon.• U.S. Astronauts landed on and explored the

Moon in the Apollo program.

• Clementine, a lunar orbiter, mapped the lunarsurface and collected data on rocks.

• Clementine found that the lunar crust is thin-ner on the side facing Earth.

• Data from Clementine indicated that water icecould exist in shaded areas of impact basins.

Mapping the Moon

• Lunar Prospector orbited the Moon frompole to pole, collecting data that confirmClementine results and that the Moon has asmall iron-rich core.

• Data from Lunar Prospector indicate the pres-ence of large quantities of water ice in cratersat the lunar poles.

6. Infer why it might be better to build a future moonbase on a brightly lit plateau near a lunar pole in thevicinity of a deep crater. Why not build a base in the crater itself?

Icy Poles In addition to photographing thesurface, Lunar Prospector carried instrumentsdesigned to map the Moon’s gravity, magneticfield, and the abundances of 11 elements in thelunar crust. This provided scientists with datafrom the entire lunar surface rather than just theareas around the Moon’s equator, which hadbeen gathered earlier. Also, Lunar Prospectorconfirmed the findings of Clementine that waterice was present in deep craters at both lunarpoles.

Later estimates concluded that as much as3 billion metric tons of water ice was present atthe poles, with a bit more at the north pole.Using data from Lunar Prospector, scientists prepared mapsshowing the location of water ice at each pole. Figure 19 showshow water may be distributed at the Moon’s north pole. At firstit was thought that ice crystals were mixed with lunar soil, butmost recent results suggest that the ice may be in the form ofmore compact deposits.

Figure 19 The Lunar Prospectordata indicates that ice exists incrater shadows at the Moon’s poles.

bookj.msscience.com/self_check_quizNASA


If you walk on blacktop pavement at noon, you can feel the effect ofsolar energy. The Sun’s rays hit at the highest angle at midday. Nowconsider the fact that Earth is tilted on its axis. How does this tilt affectthe angle at which light rays strike an area on Earth? How is the angleof the light rays related to the amount of heat energy and the chang-ing seasons?

Real-World QuestionHow does the angle at which light strikes Earth affect the amountof heat energy received by any area on Earth?

Procedure1. Choose three angles that you will use to aim the light at the paper.

2. Determine how long you will shine the light at each angle beforeyou measure the temperature. You will measure the temperatureat two times for each angle. Use the same time periods for eachangle.

3. Copy the following data table into your Science Journal to recordthe temperature the paper reaches at each angle and time.

4. Form a pocket out of a sheet of black construction paper and tapeit to a desk or the floor.

5. Using the protractor, set the gooseneck lamp so that it will shineon the paper at one of the angles you chose.

Goals■ Measure the tempera-

ture change in a surfaceafter light strikes it atdifferent angles.

■ Describe how theangle of light relates toseasons on Earth.

Materialstapeblack construction paper

(one sheet)gooseneck lamp

with 75-watt bulbCelsius thermometerwatchprotractor

Safety Precautions

WARNING: Do not touchthe lamp without safetygloves. The lightbulb andshade can be hot evenwhen the lamp has beenturned off. Handle thethermometer carefully. If itbreaks, do not touch any-thing. Inform your teacherimmediately.


Temperature Data

Angle of Initial Temperature at Temperature atLamp Temperature ___ Minutes/Seconds ___ Minutes/Seconds

First angle

Second angle

Third angle

AND TEMPERATURETILT

Do not write in this book.

6. Place the thermometer in the paper pocket. Turn on the lamp. Use the ther-mometer to measure the temperature of the paper at the end of the first timeperiod. Continue shining the lamp on the paper until the second time periodhas passed. Measure the temperature again. Record your data in your datatable.

7. Turn off the lamp until the paper cools to room temperature. Repeat steps5 and 6 using your other two angles.

Conclude and Apply1. Describe your experiment. Identify the variables in your experiment. Which

were your independent and dependent variables?

2. Graph your data using a line graph. Describe what your graph tells you aboutthe data.

3. Describe what happened to the temperature of the paper as you changed theangle of light.

4. Predict how your results might have been different if you used white paper. Explain why.

5. Describe how the results of this experiment apply to seasons on Earth.

Compare your results with those of otherstudents in your class. Discuss how thedifferent angles and time periods affectedthe temperatures.

LAB J ◆ 61Matt Meadows

Most people take for granted that aweek is seven days, and that a year is12 months. However there are otherways to divide time into useful units. Roughly1,750 years ago, in what is now south Mexicoand Central America, the Mayan peopleinvented a calendar system based on carefulobservations of sun and moon cycles.

In fact, the Maya had several calendars thatthey used at the same time.

Two calendars were most important—onewas based on 260 days and the other on 365days. The calen-dars were so accu-rate and usefulthat later civiliza-tions, includingthe Aztecs,adopted them.

The 260-Day CalendarThis Mayan calendar, called the Tzolkin

(tz uhl KIN), was used primarily to time planting,harvesting, drying, and storing of corn—their maincrop. Each day of the Tzolkin had one of 20 names,as well as a number from 1 to 13 and a Mayan godassociated with it.

The 365-Day CalendarAnother Mayan calendar, called the Haab

(HAHB), was based on the orbit of Eartharound the Sun. It was divided into 18 monthswith 20 days each, plus five extra days at theend of each year.

These calendars were used together makingthe Maya the most accurate reckoners of timebefore the modern period. In fact, they were onlyone day off every 6,000 years.

Drawing Symbols The Maya created picture symbols for eachday of their week. Historians call these symbols glyphs. Collaboratewith another student to invent seven glyphs—one for each weekday.Compare them with other glyphs at msscience.com/time.

For more information, visitbookj.msscience.com/time

SCIENCEANDHISTORY

SCIENCECAN CHANGE THE COURSE OF HISTORY!

THE

MayanCalendar

Africa

SouthAmerica

NorthAmerica

Australia

Asia

Europe

★

UNITED STATES

GULF OF MEXICO

MEXICO CUBA

S★Chichén Itzá

These glyphs represent four differentdays of the Tzolkin calendar.

The Kukulkan, builtaround the year

1050 A.D., in what isnow Chichén Itzá,Mexico, was usedby the Maya as a

calendar. It had fourstairways, each with

91 steps, a total of365 including the

platform on top.

Cosmo Condina/Stone


Copy and complete the following concept map on the impact theory of the Moon’s formation.

Earth

1. Earth is spherical and bulges slightly atits equator.

2. Earth rotates once per day and orbits theSun in a little more than 365 days.

3. Earth has a magnetic field.

4. Seasons on Earth are caused by the tilt ofEarth’s axis as it orbits the Sun.

The Moon—Earth’s Satellite

1. Earth’s Moon goes through phases thatdepend on the relative positions of the Sun,the Moon, and Earth.

2. Eclipses occur when Earth or the Moontemporarily blocks sunlight from reachingthe other.

3. The Moon’s maria are the result of ancientlava flows. Craters on the Moon’s surfaceformed from impacts with meteorites,asteroids, and comets.

Exploring Earth’s Moon

1. The Clementine spacecraft took detailedphotographs of the Moon’s surface and col-lected data indicating the presence of waterin deep craters.

2. NASA’s Lunar Prospector spacecraft foundadditional evidence of ice.

part of Earth’s crust and mantle to be vaporized and ejected into space,

the Moon when particlesin the ring join together.

causing

which leads to

which forms

bookj.msscience.com/interactive_tutor CHAPTER STUDY GUIDE J ◆ 63


Fill in the blanks with the correct vocabularyword or words.

1. The spinning of Earth around its axis iscalled .

2. The is the point at which theSun reaches its greatest distance north orsouth of the equator.

3. The Moon is said to be whenless and less of the side facing Earth islighted.

4. The depression left behind by an objectstriking the Moon is called a(n) .

5. Earth’s orbit is a(n) .

Choose the word or phrase that best answers thequestion.

6. How long does it take for the Moon torotate once?A) 24 hours C) 27.3 hoursB) 365 days D) 27.3 days

7. Where is Earth’s circumference greatest?A) equator C) polesB) mantle D) axis

8. Earth is closest to the Sun during whichseason in the northern hemisphere?A) spring C) winterB) summer D) fall

9. What causes the Sun to appear to riseand set?A) Earth’s revolutionB) the Sun’s revolutionC) Earth’s rotationD) the Sun’s rotation

Use the photo below to answer question 10.

10. What phase of the Moon is shown in thephoto above?A) waning crescent C) third quarterB) waxing gibbous D) waning gibbous

11. How long does it take for the Moon torevolve once around Earth?A) 24 hours C) 27.3 hoursB) 365 days D) 27.3 days

12. What is it called when the phases of theMoon appear to get larger?A) waning C) rotatingB) waxing D) revolving

13. What kind of eclipse occurs when theMoon blocks sunlight from reaching Earth?A) solar C) fullB) new D) lunar

14. What is the darkest part of the shadowduring an eclipse?A) waxing gibbous C) waning gibbousB) umbra D) penumbra

15. What is the name for a depression onthe Moon caused by an object striking itssurface?A) eclipse C) phaseB) moonquake D) impact basin

64 ◆ J CHAPTER REVIEW

axis p. 41ellipse p. 43equinox p. 45full moon p. 47impact basin p. 57lunar eclipse p. 50maria p. 51moon phase p. 47

new moon p. 47revolution p. 43rotation p. 41solar eclipse p. 49solstice p. 44sphere p. 40waning p. 47waxing p. 47

bookj.msscience.com/vocabulary_puzzlemakerLick Observatory


CHAPTER REVIEW J ◆ 65

16. Predict how the Moon would appear to anobserver in space during its revolution.Would phases be observable? Explain.

17. Predict what the effect would be on Earth’sseasons if the axis were tilted at 28.5°instead of 23.5°.

18. Infer Seasons in the two hemispheres areopposite. Explain how this supports thestatement that seasons are NOT caused byEarth’s changing distance from the Sun.

19. Draw Conclusions How would solar eclipsesbe different if the Moon were twice as farfrom Earth? Explain.

20. Predict how the information gathered bymoon missions could be helpful in thefuture for people wanting to establish acolony on the Moon.

21. Use Variables, Constants, and Controls Describea simple activity to show how the Moon’srotation and revolution work to keep thesame side facing Earth at all times.

22. Draw Conclusions Gravity is weaker on theMoon than it is on Earth. Why mightmore craters be present on the far side ofthe Moon than on the side of the Moonfacing Earth?

23. Recognize Cause and Effect During a newphase of the Moon, we cannot see itbecause no sunlight reaches the side facingEarth. Yet sometimes when there is a thincrescent visible, we do see a faint image ofthe rest of the Moon. Explain what mightcause this to happen.

24. Describe Earth’s magnetic field. Include anexplanation of how scientists believe it isgenerated and two ways in which it helpspeople on Earth.

25. Display Draw a cross section of the Moon.Include the crust, outer and inner mantles,and possible core based on the informationin this chapter. Indicate the presence ofimpact craters and show how the thicknessof the crust varies from one side of theMoon to the other.

26. Poem Write a poem in which you describethe various surface features of the Moon.Be sure to include information on howthese features formed.

27. Orbital Tilt The Moon’s orbit is tilted at an angleof 5° to Earth’s orbit around the sun. Using aprotractor, draw the Moon’s orbit around Earth.What fraction of a full circle (360°) is 5°?

Use the illustration below to answer question 28.

28. Model to Scale You are planning to make ascale model of the Lunar Prospector spacecraft,shown above. Assuming that the three instru-ment masts are of equal length, draw a labeleddiagram of your model using a scale of 1 cmequals 30 cm.

29. Spacecraft Velocity The Lunar Prospector space-craft shown above took 105 hours to reach theMoon. Assuming that the average distance fromEarth to Moon is 384,000 km, calculate its aver-age velocity on the trip.

1.3 m

1.3 m

1.4 m1.4 m

2.5 m

2.5 m

1.3 m

1.4 m

2.5 m

bookj.msscience.com/chapter_reviewNASA


Record your answers on the answer sheetprovided by your teacher or on a sheet of paper.

1. Which of the following terms would youuse to describe the spinning of Earth onits axis?A. revolution C. rotationB. ellipse D. solstice

Use the illustration below to answer questions 2 and 3.

2. Which season is beginning for the southernhemisphere when Earth is in this position?A. spring C. fallB. summer D. winter

3. Which part of Earth receives the greatesttotal amount of solar radiation when Earthis in this position?A. northern hemisphereB. South PoleC. southern hemisphereD. equator

4. Which term describes the dark, flat areason the Moon’s surface which are made ofcooled, hardened lava?A. spheres C. highlandsB. moonquakes D. maria

Use the illustration below to answer questions 5 and 6.

5. Which letter corresponds to the moonphase waning gibbous?A. G C. EB. C D. A

6. The Moon phase cycle lasts about 29.5 days.Given this information, about how longdoes it take the Moon to wax from newmoon to full moon?A. about 3 days C. about 2 weeksB. about 1 week D. about 4 weeks

7. Where have large amounts of water beendetected on the Moon?A. highlands C. mariaB. lunar equator D. lunar poles

8. In what month is Earth closest to the Sun?A. March C. JulyB. September D. January

9. So far, where on the Moon have theyoungest rocks been found?A. lunar highlands C. lunar polesB. maria D. lunar equator

Time

DA B C E F G

North Pole

66 ◆ J STANDARDIZED TEST PRACTICE

Eliminate Choices If you don’t know the answer to amultiple-choice question, eliminate as many incorrect choicesas possible. Mark your best guess from the remaining answersbefore moving to the next question.

Question 5 Eliminate those phases that you know are notgibbous.

STANDARDIZED TEST PRACTICE J ◆ 67

Record your answers on the answer sheetprovided by your teacher or on a sheet of paper.

10. Explain why the North Pole is always insunlight during summer in the northernhemisphere.

11. Describe one positive effect of Earth’smagnetic field.

12. Explain the difference between a solsticeand an equinox. Give the dates of theseevents on Earth.

13. Explain how scientists know that theMoon was once geologically active.

Use the illustration below to answer questions

14 and 15.

14. What type of eclipse is shown above?

15. Describe what a person standing in theMoon’s umbra would see if he or she lookedat the sky wearing protective eyewear.

16. The tilt of Earth on its axis causes seasons.Give two reasons why this tilt causes sum-mer to be warmer than winter.

17. When the Apollo missions ended in 1972,12 astronauts had visited the Moon andbrought back samples of moon soil androck. Explain why we continue to sendorbiting spacecraft to study the Moon.

18. Define the term impact basin, and namethe largest one known in the solar system.

Record your answers on a sheet of paper.

Use the illustrations below to answer questions

19 and 20.

19. As a ship comes into view over the hori-zon, the top appears before the rest of theship. How does this demonstrate thatEarth is spherical?

20. If Earth were flat, how would anapproaching ship appear differently?

21. Explain why eclipses of the Sun occuronly occasionally despite the fact that theMoon’s rotation causes it to pass betweenEarth and the Sun every month.

22. Recent data from the spacecraft LunarProspector indicate the presence of largequantities of water in shadowed areas oflunar impact basins. Describe the hypoth-esis that scientists have developed toexplain how this water reached the moonand how it might be preserved.

23. Compare the impact theory of lunarformation with one of the older theoriesproposed before the Apollo mission.

24. Describe how scientists study the interiorof the Moon and what they have learnedso far.

25. Explain why Earth’s magnetic north polesmust be mapped and why these mapsmust be kept up-to-date.

Umbra

Penumbra

MoonEarth

Sun

bookj.msscience.com/standardized_test


Glencoe Earth Science ModulesModule F: Earth Materials and ProcessesStudent Edition Table of ContentsNature of Science: Monitoring VolcanoesChapter 1: MineralsLaunch Lab: Distinguish Rocks from MineralsFoldablesGet Ready to ReadSection 1: MineralsMiniLAB: Inferring Salt's Crystal SystemVisualizing Crystal SystemsIntegrate Physics Lab: Crystal Formation

Section 2: Mineral IdentificationApplying Science: How can you identify minerals?MiniLAB: Observing Mineral Properties

Section 3: Uses of MineralsScience OnlineIntegrate Social Studies Lab: Mineral IdentificationScience and History: Dr. Dorothy Crowfoot Hodgkin

Chapter 1 Study GuideChapter 1 ReviewChapter 1 Standardized Test Practice

Chapter 2: RocksLaunch Lab: Observe and Describe RocksFoldablesGet Ready to ReadSection 1: The Rock CycleMiniLAB: Modeling RockVisualizing The Rock Cycle

Section 2: Igneous RocksScience OnlineIntegrate Chemistry Lab: Igneous Rock Clues

Section 3: Metamorphic RocksScience Online

Section 4: Sedimentary RocksMiniLAB: Classifying SedimentsIntegrate Career Applying Math: Coal FormationLab: Sedimentary RocksScience and Society: Australia's Controversial Rock Star


Chapter 3: Earth's Energy and Mineral ResourcesLaunch Lab: Finding Energy ReservesFoldablesGet Ready to ReadSection 1: Nonrenewable Energy ResourcesIntegrate Life Science Science OnlineVisualizing Methane HydratesMiniLAB: Practicing Energy Conservation

Section 2: Renewable Energy ResourcesIntegrate Career Science OnlineLab: Soaking up Solar Energy

Section 3: Mineral ResourcesMiniLAB: Observing the Effects of InsulationApplying Science: Why should you recycle?Lab: Model and Invent - Home Sweet HomeOops! Accidents in Science: Black Gold!


Chapter 4: Plate TectonicsLaunch Lab: Reassemble an ImageFoldablesGet Ready to ReadSection 1: Continental DriftScience OnlineMiniLAB: Interpreting Fossil Data

Section 2: Seafloor SpreadingIntegrate Chemistry Lab: Seafloor Spreading Rates

Section 3: Theory of Plate TectonicsScience OnlineApplying Science: How well do the continents fit together?Visualizing Plate BoundariesMiniLAB: Modeling Convection CurrentsIntegrate Career Integrate Physics Lab: Use the Internet - Predicting Tectonic ActivityScience and Language Arts: Listening In


Chapter 5: EarthquakesLaunch Lab: Why do earthquakes occur?FoldablesGet Ready to ReadSection 1: Forces Inside EarthSection 2: Features of EarthquakesIntegrate Physics Visualizing Seismic WavesScience OnlineMiniLAB: Interpreting Seismic Wave DataLab: Epicenter Location

Section 3: People and EarthquakesIntegrate Career Science OnlineApplying Math: Earthquake EnergyMiniLAB: Modeling Seismic-Safe StructuresLab: Earthquake DepthsScience Stats: Moving Earth!


Chapter 6: VolcanoesLaunch Lab: Map a VolcanoFoldablesGet Ready to ReadSection 1: Volcanoes and Earth's Moving PlatesIntegrate Career MiniLAB: Modeling Magma Movement

Section 2: Types of VolcanoesScience OnlineVisualizing LavaIntegrate Health MiniLAB: Modeling Volcanic ConesLab: Identifying Types of Volcanoes

Section 3: Igneous Rock FeaturesApplying Math: Classifying Igneous RocksScience OnlineLab: Design Your Own - How do calderas form?Oops! Accidents in Science: Buried in Ash


Student ResourcesScience Skill HandbookScientific MethodsSafety SymbolsSafety in the Science Laboratory

Extra Try at Home LabsTechnology Skill HandbookComputer SkillsPresentation Skills

Math Skill HandbookMath ReviewScience Applications

Reference HandbooksWeather Map SymbolsRocksMineralsPeriodic Table of the Elements

English/Spanish GlossaryIndexCredits

Feature ContentsCross-Curricular ReadingsNational Geographic VisualizingTIME Science and SocietyOops! Accidents in ScienceScience and Language ArtsScience Stats

LABSLaunch LABMiniLABMiniLAB Try at HomeOne-Page LabsTwo-Page LabsDesign Your Own LabsModel and Invent LabsUse the Internet Labs

ActivitiesApplying MathApplying ScienceIntegrateScience OnlineStandardized Test Practice

Module G: The Changing Surface of EarthStudent Edition Table of ContentsNature of Science: Land Use in FloodplainsChapter 1: Views of EarthLaunch Lab: Describe LandformsFoldablesGet Ready to ReadSection 1: LandformsMiniLAB: Profiling the United StatesScience Online

Section 2: ViewpointsMiniLAB: Interpreting Latitude and LongitudeIntegrate Social Studies

Section 3: MapsIntegrate Physics Visualizing Topographic MapsScience OnlineApplying Science: How can you create a cross section from a geologic map?Lab: Making a Topographic MapLab: Model and Invent - Constructing LandformsScience and History: Location, Location


Chapter 2: Weathering and SoilLaunch Lab: Stalactites and StalagmitesFoldablesGet Ready to ReadSection 1: WeatheringScience OnlineMiniLAB: Observing the Formation of Rust

Section 2: The Nature of SoilVisualizing Soil FormationMiniLAB: Comparing Components of SoilIntegrate Chemistry Applying Math: Soil TextureLab: Soil Texture

Section 3: Soil ErosionIntegrate Career Science OnlineLab: Design Your Own - Weathering ChalkScience and Language Arts: Landscape, History, and the Pueblo Imagination


Chapter 3: Erosional ForcesLaunch Lab: Demonstrate Sediment MovementFoldablesGet Ready to ReadSection 1: Erosion by GravityMiniLAB: Modeling SlumpIntegrate Physics

Section 2: GlaciersScience OnlineLab: Glacial Grooving

Section 3: WindIntegrate History Applying Science: What factors affect wind erosion?MiniLAB: Observing How Soil Is Held in PlaceScience OnlineVisualizing How Dunes Form and MigrateLab: Design Your Own - Blowing in the WindScience Stats: Losing Against Erosion


Chapter 4: Water Erosion and DepositionLaunch Lab: Model How Erosion WorksFoldablesGet Ready to ReadSection 1: Surface WaterIntegrate Career Science OnlineVisualizing Stream DevelopmentScience OnlineMiniLAB: Observing Runoff Collection

Section 2: GroundwaterMiniLAB: Measuring Pore SpaceApplying Math: Groundwater FlowIntegrate Chemistry

Section 3: Ocean ShorelineLab: Classifying Types of SandLab: Water Speed and ErosionScience and Society: Sands in Time


Chapter 5: Clues to Earth's PastLaunch Lab: Clues to Life's PastFoldablesGet Ready to ReadSection 1: FossilsMiniLAB: Predicting Fossil PreservationIntegrate Social Studies Integrate Life Science

Section 2: Relative Ages of RocksScience OnlineVisualizing UnconformitiesScience OnlineLab: Relative Ages

Section 3: Absolute Ages of RocksMiniLAB: Modeling Carbon-14 DatingScience OnlineApplying Science: When did the Iceman die?Lab: Model and Invent - Trace FossilsOops! Accidents in Science: The World's Oldest Fish Story


Chapter 6: Geologic TimeLaunch Lab: Survival Through TimeFoldablesGet Ready to ReadSection 1: Life and Geologic TimeSection 2: Early Earth HistoryIntegrate Chemistry MiniLAB: Dating Rock Layers with FossilsVisualizing Unusual Life FormsScience OnlineLab: Changing Species

Section 3: Middle and Recent Earth HistoryScience OnlineApplying Math: Calculating Extinction by Using PercentagesMiniLAB: Calculating the Age of the Atlantic OceanLab: Use the Internet - Discovering the PastScience Stats: Extinct!





Reference HandbooksWeather Map SymbolsRocksMineralsPeriodic Table of the ElementsTopographic Map Symbols





Module H: The Water PlanetStudent Edition Table of ContentsNature of Science: Exploring the Depths of the Water PlanetChapter 1: WaterLaunch Lab: What is cohesion?FoldablesGet Ready to ReadSection 1: The Nature of WaterScience OnlineIntegrate Life ScienceMiniLAB: Examining Density DifferencesApplying Science: How does water behave in space?Integrate Life ScienceLab: Discovering Latent Heat

Section 2: Why is water necessary?MiniLAB: Predicting Water UseVisualizing Shipping

Section 3: Recycling WaterIntegrate HistoryLab: Design Your Own - Conserving WaterScience and Society: Not a Drop to Drink


Chapter 2: Freshwater at Earth's SurfaceLaunch Lab: How do lake nutrients mix?FoldablesGet Ready to ReadSection 1: StreamsMiniLAB: Modeling Stream FlowScience Online

Section 2: Lakes and ReservoirsScience OnlineIntegrate Life ScienceApplying Math: Bay DepthVisualizing EutrophicationLab: Lake Nutrients

Section 3: WetlandsSection 4: Pollution of FreshwaterMiniLAB: Evaluating DilutionIntegrate HistoryLab: Adopt a StreamScience and History: Great Lakes at a Glance


Chapter 3: Groundwater ResourcesLaunch Lab: Groundwater InfiltrationFoldablesGet Ready to ReadSection 1: GroundwaterMiniLAB: Measuring PorosityScience OnlineIntegrate ChemistryScience OnlineLab: Artesian Wells

Section 2: Groundwater Pollution and OveruseVisualizing Sources of Groundwater PollutionIntegrate CareerMiniLAB: Modeling Groundwater PollutionScience OnlineApplying Science: Can stormwater be cleaned and reused for irrigation?

Section 3: Caves and Other Groundwater FeaturesScience OnlineLab: Pollution in MotionScience Stats: Caves


Chapter 4: Ocean MotionLaunch Lab: Explore How Currents WorkFoldablesGet Ready to ReadSection 1: Ocean WaterSection 2: Ocean CurrentsScience OnlineMiniLAB: Modeling a Density CurrentIntegrate CareerApplying Math: Density of Salt Water

Section 3: Ocean Waves and TidesMiniLAB: Modeling Water Particle MovementVisualizing Wave MovementScience OnlineIntegrate Life ScienceLab: Wave PropertiesLab: Design Your Own - Sink or Float?Science and Language Arts: "The Jungle of Ceylon"


Chapter 5: OceanographyLaunch Lab: How deep is the ocean?FoldablesGet Ready to ReadSection 1: The SeafloorScience OnlineApplying Math: Calculating a Feature's SlopeMiniLAB: Modeling the Mid-Atlantic RidgeLab: Mapping the Ocean Floor

Section 2: Life in the OceanIntegrate CareerIntegrate ChemistryMiniLAB: Observing PlanktonScience OnlineVisualizing The Rocky Shore Habitat

Section 3: Ocean PollutionLab: Use the Internet - Resources from the OceansOops! Accidents in Science: Strange Creatures from the Ocean Floor





Reference HandbooksWeather Map SymbolsRocksMineralsPeriodic Table of the ElementsTopographic Map Symbols



LABSLaunch LABMiniLABMiniLAB Try at HomeOne-Page LabsTwo-Page LabsDesign Your Own LabsUse the Internet Labs


Module I: The Air Around YouStudent Edition Table of ContentsNature of Science: Storm ScientistsChapter 1: AtmosphereLaunch Lab: Observe Air PressureFoldablesGet Ready to ReadSection 1: Earth's AtmosphereScience OnlineApplying Science: How does altitude affect air pressure?MiniLAB: Determining if Air Has MassIntegrate Life ScienceLab: Evaluating Sunscreens

Section 2: Energy Transfer in the AtmosphereIntegrate PhysicsMiniLAB: Modeling Heat Transfer

Section 3: Air MovementScience OnlineVisualizing Global WindsLab: Design Your Own - The Heat is OnScience and Language Arts: Song of the Sky Loom


Chapter 2: WeatherLaunch Lab: What causes rain?FoldablesGet Ready to ReadSection 1: What is weather?Integrate Life ScienceMiniLAB: Determining Dew PointApplying Math: Dew Point

Section 2: Weather PatternsScience OnlineScience OnlineVisualizing TornadoesIntegrate Environment

Section 3: Weather ForecastsMiniLAB: Measuring RainLab: Reading a Weather MapLab: Model and Invent - Measuring Wind SpeedScience and Society: Rainmakers


Chapter 3: ClimateLaunch Lab: Tracking World ClimatesFoldablesGet Ready to ReadSection 1: What is climate?MiniLAB: Observing Solar RadiationIntegrate PhysicsApplying Science: How do cities influence temperature?

Section 2: Climate TypesSection 3: Climatic ChangesMiniLAB: Modeling El NiñoVisualizing El Niño and La NiñaIntegrate CareerScience OnlineScience OnlineLab: The Greenhouse EffectLab: MicroclimatesScience and History: The Year there was No Summer


Chapter 4: Air PollutionLaunch Lab: Acid in AirFoldablesGet Ready to ReadSection 1: Types and Causes of Air PollutionIntegrate Social StudiesMiniLAB: Observing ParticulatesScience OnlineLab: Particulate Pollution

Section 2: Effects of Air PollutionIntegrate HealthMiniLAB: Modeling Ozone Depletion

Section 3: Solutions to Air PollutionScience OnlineVisualizing Emissions ControlApplying Math: Burning CoalLab: Use the Internet - Air Pollution Where You LiveOops! Accidents in Science: Radon: The Invisible Threat





Reference HandbooksWeather Map SymbolsMineralsRocksTopographic Map SymbolsPeriodic Table of the Elements





Module J: AstronomyStudent Edition Table of ContentsNature of Science: Life on MarsChapter 1: Exploring SpaceLaunch Lab: An Astronomer's ViewFoldablesGet Ready to ReadSection 1: Radiation from SpaceIntegrate HealthMiniLAB: Observing Effects of Light PollutionLab: Building a Reflecting Telescope

Section 2: Early Space MissionsApplying Math: Drawing by NumbersIntegrate CareerVisualizing Space ProbesScience OnlineMiniLAB: Modeling a Satellite

Section 3: Current and Future Space MissionsScience OnlineScience OnlineLab: Use the Internet - Star SightingsScience and Society: Cities in Space


Chapter 2: The Sun-Earth-Moon SystemLaunch Lab: Model Rotation and RevolutionFoldablesGet Ready to ReadSection 1: EarthIntegrate Life ScienceMiniLAB: Making Your Own CompassScience OnlineScience Online

Section 2: The Moon—Earth's SatelliteMiniLAB: Comparing the Sun and the MoonScience OnlineIntegrate CareerVisualizing The Moon's SurfaceApplying Science: What will you use to survive on the Moon?Lab: Moon Phases and Eclipses

Section 3: Exploring Earth's MoonScience OnlineLab: Tilt and TemperatureScience and History: The Mayan Calendar


Chapter 3: The Solar SystemLaunch Lab: Model Crater FormationFoldablesGet Ready to ReadSection 1: The Solar SystemScience OnlineIntegrate PhysicsVisualizing The Solar System's FormationLab: Planetary Orbits

Section 2: The Inner PlanetsMiniLAB: Inferring Effects of GravityScience OnlineApplying Math: Diameter of Mars

Section 3: The Outer PlanetsMiniLAB: Modeling PlanetsIntegrate Language Arts

Section 4: Other Objects in the Solar SystemLab: Model and Invent - Solar System Distance ModelOops! Accidents in Science: It Came From Outer Space!


Chapter 4: Stars and GalaxiesLaunch Lab: Why do clusters of galaxies move apart?FoldablesGet Ready to ReadSection 1: StarsMiniLAB: Observing Star PatternsApplying Science: Are distance and brightness related?

Section 2: The SunScience OnlineLab: Sunspots

Section 3: Evolution of StarsScience OnlineIntegrate ChemistryIntegrate History

Section 4: Galaxies and the UniverseMiniLAB: Measuring Distance in SpaceVisualizing The Big Bang TheoryLab: Design Your Own - Measuring ParallaxScience Stats: Stars and Galaxies





Reference HandbooksWeather Map SymbolsMineralsRocksTopographic Map SymbolsPeriodic Table of the Elements





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The Sun-Earth- Moon System€¦ · Earth continues to rotate steadily, and eventually the Sun comes into view again the next morning. One complete rotation takes about 24 h,or one