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© Smithsonian Institution DATE CLASS STUDENT SHEET NAME Lesson 2 Directions Complete Table 1. Then draw a picture of your solar system model and label it. Note any similarities in sizes of or distances between your model planets. Table 1 Model Size and Distance Drawing of Solar System Model: 2.1 OUR SOLAR SYSTEM MODEL Planet Object Representing the Planet Diameter of Object (cm) Distance of Object from the End of the Paper (“Sun”) (cm) STC Unit: Exploring Planetary Systems
Transcript

© S

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DATE CLASS

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NAME

Lesson 2

Directions Complete Table 1. Then draw a picture of your solar system model and label it. Note any similarities in sizes of or distances between your model planets.

Table 1 Model Size and Distance

Drawing of Solar System Model:

2.1 oUr SolAr SyStEM MoDEl

Planetobject

representing the Planet

Diameter of object(cm)

Distance of object from the End of the Paper (“Sun”)

(cm)

STC Unit: Exploring Planetary Systems

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Lesson 2

2.2 USiNg A ScAlE FActor

Directions Use the scale factor (sf ) to complete Table 1 below. The first row is completed as an example for you.

Tabl

e 1

Usi

ng a

Sca

le F

acto

r

Scal

e Fa

ctor

: 1 c

m =

10,

000

km

Plan

etA

ctua

l D

iam

eter

(A

D) (

km)

Scal

ed D

iam

eter

(SD

) (cm

)SD

= A

D ÷

Sca

le F

acto

r (sf

)

Act

ual

Dis

tanc

e fr

om S

un

(AD

s) (k

m)

Scal

ed D

ista

nce

from

Sun

(SD

s) (c

m)

SDs

= A

Ds

÷ sf

Mer

cury

4879

SD =

487

9 km

÷ 1

0,00

0 km

/cm

SD =

0.4

9 cm

≈ 0

.5 c

m

57,9

00,0

00SD

s =

57,9

00,0

00 k

m ÷

10,

000

km/c

m

SDs

= 57

90 c

m ≈

58

m

Venu

s12

,104

108,

200,

000

Eart

h12

,724

149,

600,

000

Mar

s67

7922

7,90

0,00

0

Jupi

ter

139,

822

778,

300,

000

Satu

rn11

6,46

41,

426,

700,

000

Ura

nus

50,7

242,

870,

700,

000

Nep

tune

49,2

444,

498,

400,

000

STC Unit: Exploring Planetary Systems

STC Unit: Exploring Planetary Systems

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Lesson 2

Plan

etA

ctua

l D

iam

eter

(A

D) (

km)

Scal

ed D

iam

eter

(SD

) (cm

)SD

= A

D ÷

Sca

le F

acto

r

Act

ual

Dis

tanc

e fr

om S

un

(AD

s) (k

m)

Scal

ed D

ista

nce

from

Sun

(SD

s) (c

m)

SDs

= A

Ds

÷ sf

Mer

cury

4879

SD =

487

9 km

÷ 1

0,00

0 km

/cm

SD =

0.4

9 cm

≈ 0

.5 c

m

57,9

00,0

00SD

s =

57,9

00,0

00 k

m ÷

10,

000

km/c

m

SDs

= 57

90 c

m ≈

58

m

Venu

s12

,104

SD =

12,

104

km ÷

10,

000

km/c

m

SD =

1.2

1 cm

≈ 1

.2 c

m10

8,20

0,00

0SD

s =

108,

200,

000

km ÷

10,

000

km/c

m

SDs

= 10

,820

cm

≈ 1

08 m

Eart

h12

,742

SD =

12,

742

km ÷

10,

000

km/c

m

SD =

1.2

7 cm

≈ 1

.3 c

m14

9,60

0,00

0SD

s =

149,

600,

000

km ÷

10,

000

km/c

m

SDs

= 14

,960

cm

≈ 1

50 m

Mar

s67

79SD

= 6

779

km ÷

10,

000

km/c

m

SD =

0.6

8 cm

≈ 0

.7 c

m22

7,90

0,00

0SD

s =

227,

900,

000

km ÷

10,

000

km/c

m

SDs

= 22

,790

cm

≈ 2

28 m

Jupi

ter

139,

822

SD =

139,

822

km ÷

10,

000

km/c

m

SD =

13.

98 c

m ≈

14.

0cm

778,

300,

000

SDs

= 77

8,30

0,00

0 km

÷ 1

0,00

0 km

/cm

SDs

= 77

,830

cm

≈ 7

78 m

Satu

rn11

6,46

4 S

D =

116

,464

km

÷ 1

0,00

0 km

/cm

SD =

11.

65 c

m ≈

11.

7 cm

1,42

6,70

0,00

0SD

s =

1,42

6,70

0,00

0 km

÷ 1

0,00

0 km

/cm

SDs

= 14

2,67

0 cm

≈ 1

427

m ≈

1.4

km

Ura

nus

50,7

24SD

= 5

0,72

4 km

÷ 1

0,00

0 km

/cm

SD =

5.0

7 cm

≈ 5

.1 c

m2,

870,

700,

000

SDs

= 2,

870,

000,

000

km ÷

10,

000

km/c

m

SDs

= 28

7,07

0 cm

≈ 2

871

m ≈

2.9

km

Nep

tune

49,2

44SD

= 4

9,24

4 km

÷ 1

0,00

0 km

/cm

SD =

4.9

2 cm

≈ 4

.9 c

m4,

498,

400,

000

SDs

= 4,

498,

400,

000

km ÷

10,

000

km/c

m

SDs

= 44

9,84

0 cm

≈ 4

498

m ≈

4.5

km

Scal

e Fa

ctor

: 1 c

m =

10,

000

kmTa

ble

1 U

sing

a S

cale

Fac

tor (

Ans

wer

Key

)

2.2 USiNg A ScAlE FActor (ANSwEr KEy)

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Lesson 2

2.3a

Table 1 Calculating the Scale Factor

cAlcUlAtiNg thE ScAlE FActor

PlanetActual

Diameter (AD) (km)

Scaled objectScaled

Diameter (SD) (cm)

Scale Factor (sf) (km/cm) sf = AD ÷ SD

Mercury 4879 Small bead 0.2 cmsf = 4879 km ÷ 0.2 cm

sf = 24,395 km/cm

Venus 12,104

Earth 12,742

Mars 6779

Jupiter 139,822

Saturn 116,464

Uranus 50,724

Neptune 49,244

Average Scale Factor (km/cm)

FiNAl AVErAgE Scale Factor: 1 cm = __________________________________km

Directions Complete Table 1 by recording the name and diameter of each of your planetary models in the columns labeled “Scaled Object” and “Scaled Diameter.” Then in the column labeled “Scale Factor,” calculate the scale factor used to create this scale model. Show all work. The first row is completed for you as an example.

STC Unit: Exploring Planetary Systems

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Lesson 2

Table 1 Calculating the Scale Factor (answers may vary)

2.3a cAlcUlAtiNg thE ScAlE FActor (ANticiPAtED rESPoNSES)

PlanetActual

Diameter (AD) (km)

Scaled objectScaled

Diameter (SD) (cm)

Scale Factor (sf) (km/cm) sf = AD ÷ SD

Mercury 4879 Small bead 0.2 cmsf = 4879 km ÷ 0.2 cm

sf = 24,395 km/cm

Venus 12,104 Peppercorn 0.46 cmsf = 12,104 km ÷ 0.46 cm

sf = 26,313 km/cm

Earth 12,742 Peppercorn 0.46 cmsf = 12,742 km ÷ 0.46

sf = 27,700 km/cm

Mars 6779 Small bead 0.2 cmsf = 6779 km ÷ 0.2 cm

sf = 33,895 km/cm

Jupiter 139,822 Rubber ball 5.5 cmsf = 139,822 km ÷ 5.5

sf = 25,422 km/cm

Saturn 116,464 Large bobber 4.6 cmsf = 116,464 km ÷ 4.6

sf = 25,318 km/cm

Uranus 50,724 Acrylic bead 1.7 cmsf = 50,724 km ÷ 1.7 cm

sf = 29,838 km/cm

Neptune 49,244 Acrylic bead 1.7 cmsf = 49,244 km ÷ 1.7 cm

sf = 28,967 km/cm

Average Scale Factor (km/cm)

221,848 km/cm ÷ 8 = 27,731 km = 1 cm

FiNAl AVErAgE Scale Factor: 1 cm = 27,731 km

STC Unit: Exploring Planetary Systems

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Lesson 2

2.3b

Scale Factor: 1 cm = _______________________kmTable 1 Calculating Scaled Distance

cAlcUlAtiNg ScAlED DiStANcE

Planet

Actual Distance from Sun

(ADs) (km)

Scaled Distance (SDs) (cm)SDs = ADs ÷ Scale Factor (sf)

Scaled Distance converted (m) or (km)

Mercury 57,900,000SDs = 57,900,000 ÷ 27,731

SDs = 20882088 cm ≈ 21 m

Mercury (with

your scale factor, if

different)

57,900,000

Venus 108,200,000

Earth 149,600,000

Mars 227,900,000

Jupiter 778,300,000

Saturn 1,426,700,000

Uranus 2,870,700,000

Neptune 4,498,400,000

Directions Record the scale factor (sf ) calculated on Student Sheet 2.3a. Complete Table 1 by calculating the scaled distance for each planetary model. Show all work. The first row is completed for you using the scale factor of 1 cm = 27,731 km. Your scale factor may be different. If so, calculate the scaled distance for Mercury in the second row.

STC Unit: Exploring Planetary Systems

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Lesson 2

Scale Factor: 1 cm = 27,731 km (scale factors may vary)

Table 1 Calculating Scaled Distance (answers may vary)

2.3b cAlcUlAtiNg ScAlED DiStANcE (ANticiPAtED rESPoNSES)

Planet

Actual Distance from Sun

(ADs) (km)

Scaled Distance (SDs) (cm)SDs = ADs ÷ Scale Factor (sf)

Scaled Distance converted (m) or (km)

Mercury 57,900,000SDs = 57,900,000 ÷ 27,731

SDs = 20882088 cm ≈ 21 m

Venus 108,200,000SDs = 108,200,000 ÷ 27,731

SDs = 39023902 cm ≈ 39 m

Earth 149,600,000SDs = 149,600,000 ÷ 27,731

SDs = 53955395 cm ≈ 54 m

Mars 227,900,000SDs = 227,900,000 ÷ 27,731

SDs = 82188218 cm ≈ 82 m

Jupiter 778,300,000SDs = 778,300,000 ÷ 27,731

SDs = 28,06628,066 cm ≈ 281 m

Saturn 1,426,700,000SDs = 1,426,700,000 ÷ 27,731

SDs = 51,44851,448 cm ≈ 514 m

Uranus 2,870,700,000SDs = 2,870,700,000 ÷ 27,731

SDs = 103,520103,520 cm ≈ 1035 m (1.0 km)

Neptune 4,498,400,000SDs = 4,498,400,000 ÷ 27,731

SDs = 162,216162,216 cm ≈ 1622 m (1.6 km)

STC Unit: Exploring Planetary Systems

© S

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Lesson 2

2.3c

Table 1 Solar System Chart

SolAr SyStEM chArto

bjec

t Fe

atur

eD

iam

eter

(k

m)

Dis

tanc

e fr

om

the

Sun

(km

)

Mas

s (k

g)Su

rfac

e g

ravi

ty

(Ear

th =

1)Av

erag

e te

mpe

ratu

re

leng

th

of

Side

real

D

ay

leng

th

of ye

ar

Num

ber

of

obs

erve

d M

oons

Mer

cury

Venu

s

Eart

h

Mar

s

Jupi

ter

Satu

rn

Ura

nus

Nep

tune

Plut

o

Directions Use the “Mission” series in your Student Guide to complete Table 1. You will use the data for your selected solar system object on your travel brochure in the Exploration Activity.

STC Unit: Exploring Planetary Systems

“The History of Space Exploration”

Mission Title

Mission Specifics (date, purpose, other)

Project Mercury

Project Gemini

Apollo Missions

Skylab Project

Apollo-Soyuz Test Project

International Space Station

Scientific Probes

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Lesson 4

Solar System object: ________________________________________________

outline Due Date: ___________________________________________________

history The object’s name, who named it, and what the name means

Discovery When the object was discovered and who discovered it

object structure The interior of the object (what it looks like inside) and its surface features (if it is terrestrial)

Atmosphere The composition and conditions of the object’s atmosphere (for example, does it have storms?), if these are known; if there is no atmosphere, say so

Motion The object’s orbit (how long it takes to get around the Sun) and rotation (how long it takes to turn one time on its axis)

Missions A description of probes or missions to the object, including travel times and dates

Data The information you entered on Student Sheet 2.3c for your object. Include the object’s diameter, average distance from the Sun, mass, surface gravity, average temperature, length of sidereal day, length of year, and number of observed moons.

other Other interesting information (include pictures and drawings)

SolAr SyStEM brochUrE oUtliNE4.1b

STC Unit: Exploring Planetary Systems

The Wetumpka Impact Crater http://www.wetumpkachamber.org/impact_crater.html

The location of the Wetumpka Astrobleme —“star-wound”— originated from a cosmic event that occurred some 80 to 83 million years ago. It was confirmed only recently, after more than two years of extensive investigation and deep earth core drilling conducted on site. It is one of the few above-ground impact crater locations in the United States and one of only about six in the entire World. Even more unusual is the fact that the structure is actually exposed (as you can see from the rim evidence in these photographs). Despite the weathering that has occurred through millions of years, the crater walls are still prominent, so the rim was obviously much higher at one time. The projectile of the meteor impact was probably travelling between 10 and 20 miles per second. So this means the impact would have produced winds in excess of 500 miles per hour, and the meteor most likely struck at a 30-45 degree angle as it came from the northeast. They determined that it came from the northeast by the angle at which the rocks are slanted within the impact area which includes the current flow path of the Coosa River. This can be seen looking from both directions on the Bibb Graves Bridge. Geologists speculate that the shock waves, the damage, and other effects of the impact explosion radiated out from the strike several hundred miles. Debris may have been thrown as far away as the present Gulf of Mexico. Geologists also theorize that the strike area would have been under a shallow sea, perhaps 300 to 400 feet of water that covered most of southern Alabama at the time of the impact. It is estimated that the diameter of the meteorite to be 1,100 feet and could have been as much as three to four times larger. Rock samples were obtained for laboratory analysis for evidence of “shocked quartz.” Quoting from an article in The Wetumpka Herald published on July 1, 1999, “Another piece of evidence confirming meteoritic impact was uncovered …the unusual amounts of iridium, an element relatively common in asteroids and meteorites, but relatively uncommon in the Earth’s crust. Iridium, detected in amounts of approximately 200 parts per trillion within Wetumpka drill-core samples, is considered an anomalously high concentration. This discovery is important proof that an asteroid vaporized upon impact, thus contributing some of its iridium atoms to crater-filling rocks. Discovery of iridium abundance at Wetumpka follows the February 1999 announcement of the discovery of impact-produced shocked quartz in the core samples. Shocked quartz grains are found only in impact craters, and their discovery is considered the most important means of proving meteoritic impacts of the past. One distinctively unique feature is its horseshoe-shaped ridge of rock which is not submerged in water or covered or eroded beyond visibility. In spite of the millions of years of weathering, the crater walls are still prominent with the rim approximately three to four miles wide. A panoramic view of the highest point on the crater rim at Bald Knob Mountain is visible from routes into town. The Coosa River flows across the western edge of the crater. From the Bibb Graves Bridge one can easily see the upturned rock tilting in the direction of the crater. Outcroppings of dramatically upturned rock formations are visible along US Highway 231. There is a Crater Impact Commission consisting of six members—three appointed by the City of Wetumpka and three appointed by the Elmore County Commission. They will be holding public hearings regarding the future development and use of this very rare anomaly in our City, including an interpretative center located on Highway 231 in Wetumpka, AL.

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Lesson 5

Purpose:

How does _____________________________affect _______________________________________?

hypothesis:

Dependent variable:

what i will measure:

Materials i will use:

controlled variable:

independent variable:

Procedures i will follow:

5.2a PlANNiNg ShEEt b

STC Unit: Exploring Planetary Systems

© S

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Lesson 5

ScoriNg rUbric: ASSESSiNg ExPEriMENtAl DESigN

5.2

STC Unit: Exploring Planetary Systems

INQ

UIR

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Directions Use the following rubric, or one you have designed, to assess each student’s experimental design.

Points: 3 = Excellent 2 = good 1 = Fair 0 = Not done

Designs investigation ScoreDid the student include all parts of the experimental design? __________

Follows Experimental DesignDid the student carefully execute all steps in the experimental design? __________

Predicting SkillsDid the student make reasonable predictions, whether they proved right or wrong? __________

Accuracy of records Were all of the student’s observations accurate and easy to read?

If applicable, did the student include all components of the data table, title, and units?

Did the student accurately graph the data?

__________

Understanding of conceptsDid the student prove to others that he or she understands the main idea of this investigation?

__________

Attitude and cooperationDid the student try his or her best at all times?

Did the student work well in a group, if applicable, and fulfill all responsibilities?

__________

Student’s Name: ______________________________________________________________

© S

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Lesson 5

Title: __________________________________________________________________________________

5.2b rEcorDiNg oUr crAtEr DAtA AND coNclUSioNS

independent Variable Data (what i will change)

Dependent Variable Data (what i will measure)trial 1 (cm) trial 2 (cm) trial 3 (cm)

longest ray

Diameter Depth longest ray

Diameter Depth longest ray

Diameter Depth

observations (what happened):

conclusions (why i think it happened):

STC Unit: Exploring Planetary Systems

© S

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Lesson 6

Process: ___________________________________________

Directions Describe the process you used to complete Inquiry 6.1 by filling in each box.

what we did:

what we observed (draw and describe):

why we think this happened:

which photograph from “getting Started” (write the figure number) was most like our results and why:

PlANEtAry ProcESS obSErVAtioNS6.1a

STC Unit: Exploring Planetary Systems

© S

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Lesson 6

6.1b

Table 1 Matching Planetary Processes

MAtchiNg PlANEtAry ProcESSES

Photo card Number

who modeled this in class? (list students’ names.)

what do you see in their plastic box

and photo?

how does this surface feature

form?

which surface feature on Earth

matches this photo card? (Select from

Figures 6.1–6.5.)1

2

3

4

Directions Observe each group’s results. Find the photo card that matches the process modeled in each box. Then complete Table 1 by answering the question in each column.

STC Unit: Exploring Planetary Systems

Help

keep

exc

ess

se

dim

en

t ou

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r cr

eek

s, s

trea

ms

an

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ivers

Wha

t is

a W

ater

shed

?A

wat

ersh

ed is

an

area

of

land

that

dra

ins

to

a co

mm

on p

oint

, su

ch a

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near

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reek

, st

ream

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ry s

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wat

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ows

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Wat

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supp

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Wha

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St

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wat

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wat

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rai

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mel

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snow

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flo

ws

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TAR- Target-Analogy-Reflection Target Describe the concept or phenomenon:

Analogy State the analogy: Describe how the analog and target are alike:

Describe how the analog and target are not alike:

Reflection Describe how the analogy helped you understand the target

2014 Template from Science Formative Assessment- 50 More Practical Strategies for Linking

Assessment, Instruction, and Learning (Page Keeley)

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Lesson 8

8 boDE’S lAw

Table 1 Planetary Distances

background Johann Elert Bode was a German astronomer born in 1747. He observed a mathematical relationship between the distances of the planets from the Sun, which we call Bode’s Law. To learn more about Bode’s mathematical equation, use Table 1 to answer Questions 1–7.

1. Complete this sequence: 0, 3, 6, 12, , , , ,

2. Now add 4 to each number: , , , , , , , ,

3. Divide each number by 10: , , , , , , , ,

4. Record your answers from Question 3 in Table 1 in the columns labeled “Bode’s Numerical Pattern.” Compare your answers with the relative distances of the planets from the Sun on the table.

5. What do you observe about the pattern of numbers?

6. What do you think the irregularity (indicated by ??? in Table 1) between Mars and Jupiter represents? (Bode thought it may have been another planet.)

7. How can you use Bode’s formula to calculate the distances of all of the planets? Which planet(s) cannot be calculated accurately using this formula, and why might that be?

challenge: Scientists do not know if Bode’s Law expresses a coincidence, or if the planets exhibit some systematic order which they cannot yet fully explain. Find out more about Bode’s Law by researching it on your own.

PlanetDistance from the

Sun (km) (rounded)

relative Distance (Earth = 1 AU)

bode’s Numerical Pattern

Mercury 58,000,000 0.4

Venus 108,000,000 0.7

Earth 150,000,000 1.0

Mars 228,000,000 1.5

??? ??? ???

Jupiter 778,000,000 5.2

Saturn 1,400,000,000 9.5

Uranus 2,900,000,000 19.2

Neptune 4,500,000,000 30.1

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Lesson 9

(continued)

9 Exploring planEtary SyStEmS rEViEw

Directions Complete the following questions to prepare for the assessment in Lesson 10. Use the reading selections in your Student Guide, your notes, and your student sheets from Lessons 1–9 to help answer the questions.

How did Copernicus’s view of the solar system differ from Ptolemy’s? (Lesson 1)

List the planets in order according to their distances from the Sun. Tell which planet receives the most light from the Sun and why. (Lesson 2)

Use the scale factor 1 cm = 400 km to estimate how big (in cm) a model of Earth should be. (Lesson 2)

Why is it difficult to create an accurately scaled model of the solar system in the classroom? (Lesson 2)

How are impact craters formed? Draw a crater and label its parts. (Lesson 5)

Why are the craters on Earth’s surface less evident than those on other terrestrial planets’ surfaces? (Lessons 5 and 6)

Other than the eight planets, what objects are in the solar system? (Lessons 1, 5, and 8)

1

2

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Lesson 9

(continued)

9 Exploring planEtary SyStEmS rEViEw (coNtiNUED)

Complete Table 1 Planetary Processes by listing two planetary processes in the first column. Describe the landforms created by each process in the second column. In the last column, name one or more planets on which this process and/or landform can be found. (Lesson 6)

Describe how gravity affects an apple falling from a tree. (Lesson 3)

Describe the difference between mass and weight. (Lesson 3)

Why would a can of soda weigh different amounts on each planet? (Lesson 3)

How does the mass of a planet affect the speed of a moon that orbits it? (Lesson 7)

What happened to your orbiting marble when you lifted up the metal ring? Explain why this happened. (Lesson 7)

Table 1 Planetary Processes

8

9

10

11

12

13

Planetary Process landform created by this Process

Planet where this Process or landform Exists

STC Unit: Exploring Planetary Systems

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Lesson 9

Describe the motion of a planet when it orbits a star. Be specific. How is the motion of a planet near the star different from the motion of a planet far from the star? What is the shape of a planet’s orbit? (Lesson 7)

What did Eugene Shoemaker, his wife, Carolyn Shoemaker, and David Levy witness in 1994? (Lesson 8)

Compare asteroids, comets, meteoroids, and meteors. (Lesson 8)

How have asteroid impacts influenced Earth’s history as a planet? Give one example. (Lesson 8)

Describe what happens to a comet as it nears the Sun. (Lesson 8)

What are fossils, and why are they important to the study of Earth’s history as a planet? (Lesson 9)

Describe Venus’s atmosphere and the gases that make up its atmosphere. Why does Venus have a powerful greenhouse effect? (Lesson 3)

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17

18

19

20

9 Exploring planEtary SyStEmS rEViEw: (coNtiNUED)

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Lesson 10

In this part of the assessment you will evaluate an experiment done by a group of students who used a sphere twirled on the end of a piece of string to investigate how the period of the sphere depended on its length of the string.

On Student Sheet 10a, write a hypothesis about how you think the period of a sphere twirled on the end of a string will change as you change the length of the string.

Below is an equipment list and a description of the procedure that the students used in their investigation. Use the information on this sheet and in the data table provided on your student sheet to complete Student Sheet 10a: Solar System Assessment Experiment Analysis Sheet (Part A). When you have finished, follow your teacher’s directions for turning in the student sheet and inquiry master.

MAtEriAlS USED 1 white sphere 1 piece of string ~ 1.0 meter long 2 stopwatches 1 clear cylinder 1 plastic tube 5 washers 1 meterstick Safety goggles

SolAr SyStEM ASSESSMENtExPEriMENt ShEEt (PArt A)

10a

Figure 1

STC Unit: Exploring Planetary Systems

(continued)

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Lesson 10

Directions Follow each set of directions.

Questions 1–10 Read each question. On your answer sheet, write the correct letter.

A flashlight held close to a wall produces a small, bright circle of light, while a flashlight that is far away from the wall produces a large, dim circle of light. Using this model, what information can you hypothesize about how the Sun’s light affects planets?

A. Planets far away from the Sun receive more of the Sun’s concentrated light.B. Planets close to the Sun receive more of the Sun’s concentrated light.C. Planets far away from the Sun are warmer.D. Planets close to the Sun are colder.

Which best describes the surface of planet Earth over billions of years?A. High mountains and flat plains remain side by side and unchanged for millions of years.B. High mountains gradually wear down until most of Earth’s surface is at sea level.C. High mountains wear down as new mountains are continuously formed.D. A flat surface is pushed up until Earth’s entire surface is covered in mountains.

Comet Shoemaker-Levy 9 impacted Jupiter in 1994. Evidence of the impact was visible on Jupiter for nearly a year. Why are no craters from the impact visible on Jupiter today?

A. Jupiter is a gaseous planet and the comet impacted Jupiter’s upper atmosphere.B. The comet broke up into 21 pieces before it reached Jupiter.C. Wind and water on Jupiter eroded the craters.D. Jupiter trapped the comet in its orbit and it became a moon of Jupiter.

An apple falls from a tree to the ground. When does gravity act on the apple?A. When the apple first drops from the treeB. When the apple is halfway to the groundC. When the apple is closest to the groundD. In all three positions (A, B, and C)

The atmosphere on Venus is made up of many gases. Which of the following gases is found in the greatest amount on Venus and causes a runaway greenhouse effect?

A. NitrogenB. OxygenC. Carbon dioxideD. Hydrogen

You are designing a scale model of the solar system. Mercury is 4,878 km in diameter. Using the following scale factor, how large does your model of Mercury need to be?SCALE: 1 cm = 300 km

A. 160 cm B. 16 cm C. 146 cm D. 30 cm

10b SolAr SyStEM writtEN ASSESSMENt (PArt b)

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Lesson 10

Galileo accepted Copernicus’s model of the solar system and rejected Ptolemy’s model. Select the best reason that Galileo could have had for his decision.

A. Copernicus’s model closely matched Galileo’s observations of the sky.B. Other scientists believed Copernicus’s model.C. Copernicus’s model was more recent than Ptolemy’s was. D. It was common sense to reject Ptolemy’s model.

You are in command of a cannon on a cliff near an ocean. The cannon can only fire straight ahead. You fire on a target. The cannonball curves toward the water and drops just short of the target. Which reason explains why the cannonball moved as it did?

A. The force of the fired cannon caused the ball to move forward, but gravity caused the cannonball to curve toward the water.

B. The cannonball did not have enough forward motion to overcome the gravitational force of Earth.

C. The target was too far away for the force of the cannon.D. All of the above

A scientist finds a fossil along the shore. It is an impression of a mollusk shell in sandstone. What type of fossil did the paleontologist find?

A. A fossil of the actual organism trapped in hardened amberB. A mold of the organismC. A cast of the organismD. A petrified bone

10b SolAr SyStEM writtEN ASSESSMENt (PArt b)(coNtiNUED)

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(continued)

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Lesson 10

Use the illustration below to answer the question. Write the letter of your answer on the answer sheet.

A curved groove is placed on a level table, as shown. A ball is pushed in the groove at P so that it exits the curve at Q. How would the ball move after it leaves the groove at Q?

A. It would curve from Q to P but just miss P.B. It would curve to the left.C. It would go off Q in a straight line.D. It would curve from Q to P exactly.

10b SolAr SyStEM writtEN ASSESSMENt (PArt b)(coNtiNUED)

10

(continued)

P

P

A

c

b

D

P

P

P

Q

Q

Q

Q

Q

STC Unit: Exploring Planetary Systems

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Lesson 10

Questions 11–14 Write your answers in complete sentences on the answer sheet or on a separate sheet of loose-leaf paper.

Consider what it might be like to live on Planet X rather than on Earth. Examine the table. Write at least one reason why it would be difficult to live on Planet X.

Describe two variables that determine the size of a crater that is formed by an asteroid, a comet, or a meteorite. Why does a comet’s tail form when the comet is near the Sun, but not when the comet is farther from the Sun? Examine the photograph of Mars’s surface on the next page. Use the photograph to answer each question.

A. What process do you think formed Apollinaris Patera (A on the photograph)? Explain your answer.

B. What process do you think formed Reuyl crater (B on the photograph)? Can you name any parts of this landform? Explain your answer.

C. Ma’adim Vallis is the channel in the southeast part of the photograph, marked C. Which process do you think formed Ma’adim Vallis? Explain your answer.

D. Gusev is marked D in the photograph. How do you think Gusev formed? Considering the relationship between Ma’adim Vallis and Gusev, what material do you think lines the floor of Gusev?

10b SolAr SyStEM writtEN ASSESSMENt (PArt b)(coNtiNUED)

11

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14

(continued)

Earth Planet xAtmospheric conditions 21% oxygen 10% oxygen

0.03% carbon dioxide 80% carbon dioxide78% nitrogen 5% nitrogenozone layer no ozone layer

Distance from a star like our Sun 149,600,000 km 103,600,000 kmrotation on its axis 1 day 200 Earth daysrevolution around the Sun 3651⁄4 days 200 Earth days

STC Unit: Exploring Planetary Systems

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Lesson 10

boNUS Which formation do you think is the youngest of the four labeled in the photograph? Explain your answer.

10b SolAr SyStEM writtEN ASSESSMENt (PArt b)(coNtiNUED)

AB

D

C

PHOTO: U.S. Geological Survey

STC Unit: Exploring Planetary Systems

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Lesson 10

ProcEDUrE

Students began by tying one end of the string to the white sphere. They then threaded the string through the tube and tied the loose end of the string to the clear plastic tube. Next, they placed five washers in the clear plastic tube.

After putting on safety goggles, students measured off 20 cm as the distance from the center of the sphere to the top of the tube. Then one student began swinging the sphere in a circle around his head. The student made sure that the plastic cylinder stayed the same distance below the tube while the sphere was swinging around the circle. When the sphere had a steady motion, two other students used stopwatches and measured the time it took the sphere to make 10 revolutions around the circle. The fourth member of their group recorded this information in a data table. The students repeated this trial one more time.

The students stopped swinging the sphere and measured off a new distance, 40 cm, from the top of the tube to the center of the white sphere. They repeated the procedure of swinging the sphere around in a circle and measuring the time for the sphere to make 10 revolutions. After recording their data, they repeated this procedure for two more trials, using distances of 60 cm and 80 cm.

When they had finished collecting data, the students put their materials away and began analyzing their data.

SolAr SyStEM ASSESSMENtExPEriMENt ShEEt (PArt A) (coNtiNUED)

10a

STC Unit: Exploring Planetary Systems

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(continued)

Lesson 10

Directions Complete this sheet using the information on Inquiry Master 10a: Solar System Assessment Experiment Sheet (Part A).

Write a hypothesis about how you think the period of a sphere twirled on the end of a string will change as you change the length of the string.

hyPothESiS:

ProcEDUrE:

What is the independent variable in this experiment?

What is the dependent variable in this experiment?

What did the students keep constant during the experiment?

Why did the students keep the cylinder with the washers in it the same distance below the tube while swinging the sphere in a circle?

10a SolAr SyStEM ASSESSMENtExPEriMENt ANAlySiS ShEEt (PArt A)

STC Unit: Exploring Planetary Systems

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Lesson 10

Distance and Time Data

For each trial, compute the average time for 10 revolutions and the period of one revolution and enter it in the table.

Use the grid below to make a graph of period and distance.

coNclUSioNBased on the data table and graph, what can you conclude about the period of the sphere as the distance from the tube increased?

APPlicAtioNExplain how the results of this experiment relate to something you have investigated in this unit.

Distance (cm)

Number of revolutions

time for 10 revolutions

(s)

time for 10 revolutions

Average time for 10 revolutions

Period of revolution*

(s)

20 10 4.3 3.740 10 12.2 11.860 10 19.9 20.180 10 27.6 28.4

10a SolAr SyStEM ExPEriMENt ANAlySiS ShEEt (PArt A) (coNtiNUED)

DAtA ANAlySiS

STC Unit: Exploring Planetary Systems

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