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6.2 Layers on Earth: Plate Tectonics Science Matters 1 Grade Six Plate Tectonics Unit Lesson 6.2: Layers of the Earth Lesson Concept The Earth has different layers with different densities and temperatures. Direct and Indirect evidence is used to explain the layers. Link Lesson 6.1 established that relative density of materials are layered from most dense to least dense. This lesson uses direct and indirect evidence to explore properties of different layers of the Earth. Lesson 3 explores the role of convection in moving earth materials between and within layers. Time 2 weeks (approximately 8 class periods). The lesson includes six individual sessions. Each session has an engage, explore and explain. The final extend and evaluation is in session 6. Session 1: (50 min.) The Earth’s interior has many layers Session 2: (50 min) Earth’s layers can be represented using a variety of models. Session 3: (60 min.) Indirect evidence is used to explain Earth layers. Session 4: (50 min.) Direct evidence is used to explain the top layer of the crust. Session 5: (50 min.) Research Project: Earth has different layers with different densities and temperatures. Session 6: (200-250 min) Culminating student product: Earth has different layers with different densities and temperatures. Materials Each session (1-6) has materials and advanced preparation in the following boxes. Session 1: Materials and Advanced Preparation Materials: Whole class Globe Bill Nye video “Earth’s Crust” SBCEO Portal, CA Streaming Chart paper/white board Word Wall

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6.2  Layers  on  Earth:    Plate  Tectonics  Science  Matters       1    

Grade Six Plate Tectonics Unit Lesson 6.2: Layers of the Earth

Lesson Concept The Earth has different layers with different densities and temperatures. Direct and Indirect evidence is used to explain the layers.

Link Lesson 6.1 established that relative density of materials are layered from most dense to least dense. This lesson uses direct and indirect evidence to explore properties of different layers of the Earth. Lesson 3 explores the role of convection in moving earth materials between and within layers.

Time 2 weeks (approximately 8 class periods). The lesson includes six

individual sessions. Each session has an engage, explore and explain. The final extend and evaluation is in session 6. Session 1: (50 min.) The Earth’s interior has many layers Session 2: (50 min) Earth’s layers can be represented using a variety of models. Session 3: (60 min.) Indirect evidence is used to explain Earth layers. Session 4: (50 min.) Direct evidence is used to explain the top layer of the crust. Session 5: (50 min.) Research Project: Earth has different layers with different densities and temperatures. Session 6: (200-250 min) Culminating student product: Earth has different layers with different densities and temperatures.

Materials Each session (1-6) has materials and advanced preparation in the

following boxes. Session 1: Materials and Advanced Preparation Materials: Whole class

• Globe • Bill Nye video “Earth’s Crust” SBCEO Portal, CA Streaming • Chart paper/white board • Word Wall

6.2  Layers  on  Earth:  Plate  Tectonics  Science  Matters     2    

Individual • Student Journals

Advance Preparation:

1. Gather Materials 2. Preview Video 3. Prepare cards for word wall

Session 2: Materials and Advanced Preparation Materials Whole Class

• 1 Meter Wheel (digital preferred available at Garden Centers)

• Journey to Center of the Earth Teacher packet (download from internet http://web.ics.purdue.edu/~braile/edumod/journey/journey.htm

• Location Markers (Teacher Packet) Individual • Student brochure ( Teacher Packet) • Student journal • 4-5 Peanut M&Ms per student

Advance Preparation: 1. Download “Journey to the Center of the Earth” teacher packet.

Read information prior to lesson. http://web.ics.purdue.edu/~braile/edumod/journey/journey.htm 2. Read teacher narrative and highlight important facts to share

with students as you walk the “Journey to the Center of the Earth”

3. Duplicate student brochure from the “Journey to the Center of the Earth” teacher packet for each student.

4. Prepare location markers in label section of the teacher packet.

6.2  Layers  on  Earth:  Plate  Tectonics  Science  Matters     3    

Session 3: Materials and Advanced Preparation Materials Small Group: (groups of 3-4)

• 3 opaque film canisters filled with mystery contents per pair of students (contents may include: cotton balls, sand, rice, marbles, brads, paper clips, rubber-bands, broken crayons, etc). Make sure are sealed shut and students can’t open them

• 3 empty film canisters per pair of students • 1 tub per table group of miscellaneous materials used to fill sealed

canisters plus some extra materials that were not used as detractors.

• Scales available in the room for weighing canisters • 1 rock per pair

Individuals:

• Student lab sheet (H1a & b -Inferring Lab)

Advance Preparation 1. Gather Materials

2. Duplicate Lab sheets (H1a and H1b) 3. Prepare canisters (3 for pair of students) with mystery contents

and number them. Keep a key of number and its contents. 4. Prepare empty canisters (3 per pair of students) and tub of

materials that includes all contents of original canisters. Session 4: Materials and Advanced Preparation Materials Whole Class • Several Road Cut photos (alternative visual) Individual

• One layered cupcake per student • 5 clear straws per student cut in half (10 total) • scissors • paper towel or napkin • Student lab sheet per student (H3)

6.2  Layers  on  Earth:  Plate  Tectonics  Science  Matters     4    

Advanced Preparation 1. Print parent baking guideline sheet (H2) and arrange for parents

to make cupcakes. 2. Gather materials 3. Print Student lab sheet

Session 5: Materials and Advanced Preparation Materials Whole Class

• 7 pages Chart Paper Individual • Textbook section on earth’s layers • 1 Marker per table group (different color for each table)

Advanced Preparation 1. Gather materials

2. Select section of textbook for reading. 3. Prepare charts (7) with labels: Crust, Lithosphere,

Asthenosphere, Mantle, Outer Core, Inner Core, Magnetic Alignment

Session 6: Materials and Advanced Preparation

Materials Whole class Multiple staplers Groups Colored Pencils/Markers Individual

Layer booklet requirement sheets (H4 and H5) Outline sheets (Layers of the Earth: note-taking guide) (H6a-c)

4 (6x18”) construction sheet pages per student Advanced Preparation 1. Cut white construction paper for book pages: need 4 6x18” per

student

6.2  Layers  on  Earth:  Plate  Tectonics  Science  Matters     5    

Procedures for each of the sessions (1-6) for lesson 6.2 follow in order of session: Session 1: The Earth’s interior has many layers. Procedures Engage 1 (10 minutes) The inside of the Earth is not visible. 1. Hold up a globe and remind students the globe is a model for the earth. Ask

students to use notebooks to record what they think the inside of the earth looks like, may draw it. Ask students to include a brief description of how they know.

2. Ask student to share ideas with a partner. Compare how your ideas are the same or different. Underline ideas different from your partner. The underlined activities are ideas we need to gather evidence to prove.

Explore/Explain I (40 minutes) The Earth’s Interior has many layers. 3. Ask students to guess whether anyone has ever been to the center of the Earth?

Explain to students that models are often used to understand what is inside the earth since we have not “journeyed to the center of the earth”.

4. Explain one way to learn about the layers on Earth is to use videos to explain ideas. Review your ideas from step #2 and think about any underlined ideas. The video “Earth’s Crust” might clarify underlined ideas.

5. Ask students to divide a notebook page into four sections or a “4 Square” grid. Explain the grid is used to take notes on four self-selected topics in the video. Ask students to select 4 topics of interest as the video plays.

6. Ask students to watch the Bill Nye “Earth’s Crust” video recording ideas (pictures or words) from the video on the “4 Square” grid in notebooks.

7. Ask students to share ideas recorded with a partner. Discuss notes and how scientists might have found out the information.

8. Display the following words on a word wall: crust, mantle, outer core and inner core. Ask students to share information about each of the layers. Record on a chart under the each word.

9. Ask students to review notebook drawing from steps 1 & 2 and redraw the model of the earth adding labels and any new information gained in the video.

6.2  Layers  on  Earth:  Plate  Tectonics  Science  Matters     6    

Session 2: Earth’s layers can be represented using a variety of models Procedures Engage 2 (10 minutes) Models can be used to label layers.

1. Hold up a peanut M & M and ask students to explain how the “peanut” model of the earth can represent earth’s layers? Chart ideas.      

2. Distribute 3 or 4 peanut M & M’s per student. Ask students to bite one peanut M & M in half. Describe what you see.

3. Ask students to look at one cross section of an M & M. Ask students to talk to a partner and decide what is representing the inner core, out core, mantle, and crust. Draw M & M peanut with earth labels in notebooks.

Teacher Note: Candy coating = crust, White of candy coating = Lithosphere, chocolate = Mantle, Peanut = core, inside part of peanut = inner core. 4. Explain to students that the larger earth layers include two sections where

most of the movement occurs. The crust is rigid like stone. What do you know about the mantle? Chart ideas.

5. Explain the rigid crust meets the liquid mantle and forms two small “transition” layers. One is called lithosphere meaning “stone” sphere. …the bottom of the crust. The other is called asthenosphere (weak sphere) the top of the mantle. This is where most movement takes place.

6. Ask students to bite another M&M and discuss what might represent the lithosphere…stone-sphere bottom of the crust. Is there any part of the M & M model to represent the weak sphere or soft part of the upper mantle called asthenosphere?

7. Discuss model: What is correct/not correct about the M&M model compared to the real earth?

Teacher Note: The upper mantle or asthenosphere is not represented. We need to add that to our mantle diagram.

Explore 2 (30 minutes) Earth layers are very large scale and take a large space to represent.

Teacher Note: Use the procedures from the Teacher Packet to pace off the scale model of the earth (specifically pages 5 and 19). The radius of 1:1,000,000 meters is paced off as the teacher reads pre-highlighted parts of the narrative. Use the meter wheel for marking off the meters.

8. Ask the students to go outside and pace off the scale of the universe. 9. Return to the classroom and debrief using the following questions: How was

the journey to the center of the earth model different or the same as the M & M model? What surprised you? Why would it take 53 days of walking 24 hours a day? How do temperatures change? Can we travel to the center of the earth yet?

6.2  Layers  on  Earth:  Plate  Tectonics  Science  Matters     7    

10. How do models like the M & M or Journey to the Center of the Earth help you understand the layers of the earth or confuse you? Chart responses.

Explain 2 (10 minutes) Earth’s layers can be represented using a variety of models

11. Ask students to review the original drawing of the center of the earth from step 1 and step 9 from Session 1. Edit your original drawing adding information from M & M model and Journey to the Center of the Earth model.

12. Ask students to glue the “brochure” into notebook. Ask students to write reflection about what they know so far about the layers of the Earth. Use the prompts: “I Used to Think… I Now Know”

6.2  Layers  on  Earth:  Plate  Tectonics  Science  Matters     8    

Session 3: Indirect Evidence is used to explain Earth layers. (Inferring Lab) Procedure: Engage 3 (10 minutes) Direct evidence means direct use of five senses to explore.

1. Ask partner students to observe a rock on their desk. Use five senses to make observations. Chart on left side of large paper.

2. Ask students how the center of the rock could be directly observed? Add ideas to chart. Label the chart Direct Evidence since we can use our five senses to make observations.

3. Ask students to think about how scientists know or observe the center of the Earth without direct observations? Chart ideas on the right side of the chart and label it In-Direct Evidence.

Explore 3: (20 minutes) Explore how indirect evidence is used in models. 4. Distribute 3 film canisters to each set of partners. Ask students to make

observations about each canister without opening the canister. Students will use a variety of methods to determine contents (tap, roll, shake, weigh, etc)

Explain 3: (10 minutes) Indirect Evidence is used to explain the Earth Model.

5. Distribute handout for Inferring Lab and record initial observations and prediction of contents. Explain the evidence you have for your prediction.

6. Lead a discussion using the following questions: a. What is different about the canisters? b. What is alike about the canisters? c. How did you obtain your evidence? d. How could you prove your idea without opening the canister?

Extend 3: (20 min. ) Indirect Evidence is used to explain the Earth Model 7. Distribute three empty canisters and content materials to each partner group.

Explain the challenge is to use your senses to create 3 duplicate canisters without opening the canisters.

Teacher Note: Duplicate only one canister if time is an issue.

8. Ask students to record how they know on the handout for Inferring Lab. 9. Ask partner groups to exchange model canisters with a second partner group.

Ask the second group to use senses to determine if they agree with partner groups models. Discuss use of inference or indirect evidence.

10. Lead a discussion using the following questions:

6.2  Layers  on  Earth:  Plate  Tectonics  Science  Matters     9    

a. How did you determine which materials matched your containers? b. How do you know that your new canister matches the sealed canister? c. How is this lab similar to how scientists determine the Earth’s interior

layers? d. What is the evidence scientists use to know about the center of the earth?

Teacher Note: Scientists build models to explain materials that might be in the center of the earth. Seismic waves are used to determine new information based on what we know directly about properties of different materials. (Rocks both molten and hard)

6.2  Layers  on  Earth:  Plate  Tectonics  Science  Matters     10    

Session 4: Direct evidence is used to explain layers of the crust. Procedures: Engage 4 (15 minutes) Models are used to represent the earth’s crust.

1. Distribute cupcakes and clear straws to students and explain the cupcake represents the earth’s crust. Ask students to think, pair, and share how the cupcake might represent the crust of the earth and how it might not represent the crust of the earth.

2. Ask students to predict what is under the top crust of the cupcake without touching the cupcake? What could be done to figure out what is under the crust?

3. Show a road cut photo of layers of rock in the crust of the Earth. Explain one way to find out what is under the crust is to cut away part of a hill. Another way is to drill a hole in the surface. We will show how this is done with the cupcake model.

Explore 4 (15 minutes) Direct evidence exploration of core samples in a model.

4. Ask students how the straw might be used to figure out what the inside of the cupcake looks like?

5. Explain that “miners” used metal tubes (straws in the model) to drill out one section of the earth as direct evidence. The advantage of this method is less of the earth needs to be removed to figure out what is under the crust.

6. Distribute the handout for “Geology Lab” and ask students to select 10 spots in the cupcake crust to drill a core sample with a straw. Drill the ten spots and record on the handout by drawing the layers.

Explain 4 (20 minutes) Core samples are direct evidence to determine types of rock in the crust.

7. Lead a discussion using the following questions: What did you observe from your core samples? Which layer is the oldest? How do you know? Which layer is the youngest? How do you know?

8. Ask students to use the core samples to infer and draw what the interior of the cupcake looks like?

9. Ask students to bite into the cupcake to determine if you were correct on your inference. Discuss accuracy of drawings with a partner.

10. How could scientists use this method (core samples) with rock in the crust to figure out what is under the crust? Why is this method called direct evidence? How is this different from indirect evidence?

6.2  Layers  on  Earth:  Plate  Tectonics  Science  Matters     11    

Session 5: Earth has different layers with different densities and

temperatures. Procedures Engage 5 (10 minutes) Resources can be used to collect information about different layers of the Earth.

1. Ask students to turn to the pages in the textbook on earth’s composition. Predict what information might be presented in this section. Chart.

Explore/Explain 5 (40 minutes) Earth has different layers with different densities

and temperatures

2. Ask students to read the section thinking to find out if predictions are correct. 3. Show the 7 posters with titles of crust, lithosphere, asthenosphere, mantle, outer

core, inner core, magnetic alignment and then distribute a poster to each table group. Explain to students the process for sharing the reading is a carousel.

4. Ask each table group to start at a different poster. The table group brainstorms information about the title from the reading. Chart information directly on the chart. Record as many ideas as possible in 2-3 minutes at the chart.

5. Give a signal to the table groups that it is time to move to the next chart. Ask each group to pass their poster to the next table. Read the previous groups information and add your own.

6. The process is repeated until each group has had all charts. 7. Ask the last group to read the chart aloud. Ask students to listen carefully for any

ideas that need to be expanded or changed for clarity. 8. Explain the charts will provide data for our individual books to be developed

tomorrow about the interior of the earth.

6.2  Layers  on  Earth:  Plate  Tectonics  Science  Matters     12    

Session 6: Earth has different layers with different densities and

temperatures Procedures:

Teacher Note: Layer booklets will be developed based on information of the entire set of sessions. (1-6) Resource page explains how to fold the paper. Optional is whether teacher or students folds the 4 sheets of paper.

Engage 6 (50 minutes) Information can be gathered from a variety of sources.

1. Distribute outline handout to students. Ask students to complete the outline based on the information from the previous lessons.

2. Share outlines with tablemates. Make changes based on feedback from tablemates.

Extend 6 (Multiple Days and/or Homework ) Earth has different layers with different densities and temperatures.

3. Distribute construction paper (4 sheets 6” X 18” folded to make booklet with layers) and ask students to combine sheets into the layer book.

4. Ask students to label each layer of the book on the bottom of each page as follows:

a. Top: Title page b. Crust c. Lithosphere d. Asthenosphere e. Mantle f. Outer Crust g. Inner Core h. Magnetic Field

5. Ask students to develop the information for each page using posters, notes from Sections 1-6 and outline.

Evaluate 6 (20 minutes) Earth has different layers with different densities and temperatures

6. Ask students to use the rubric to analyze the information in the layer book.

Teacher note: Rubric separate file in 6.2 folder.

6.2  Layers  on  Earth:    Plate  Tectonics  Science  Matters       13    

 Inferring Lab

 How  do  scientists  know  what  the  Earth’s  interior  looks  like?    It  is  possible  to  dig  for  direct  evidence.  But,  this  direct  evidence  can  only  be  gathered  for  a  short  distance  through  the  top  of  the  crust.    Going  to  the  center  of  the  Earth  is  only  possible  in  fantasy.    So,  how  have  the  layers  been  determined?    Scientists  are  able  to  determine  and  learn  about  the  Earth’s  interior  through  inferring.    This  is  called  indirect  evidence.    They  use  many  clues  to  learn  about  what  isn’t  possible  to  actually  see.    Today  you  will  use  inferring  to  determine  the  contents  of  sealed  film  canisters.    Objective:  To  investigate  how  scientists  gather  evidence  about  the  Earth’s  interior.    Part I Materials:  3  opaque  sealed  film  canisters  filled  with  a  mystery  substance    Procedures:    

1. Pick  one  of  the  canisters.  2. Gather  evidence  about  what  is  in  the  canister.    You  may  tap,  roll,  shake,  or  weigh  them.    DO  NOT  OPEN  

YOUR  CANISTER!  3. Record  the  number  on  top  of  the  canister  and  your  observations  below.      4. Repeat  with  the  other  two  canisters.  

 Observations:  

     Canister  #____       Canister  #_____     Canister  #____                        

   Based  on  your  observations,  what  do  you  think  is  in  each  canister?     #_____  -­‐       #_____  -­‐       #_____  -­‐    What  differences  were  noticed  between  each  canister?            

H1a  

6.2  Layers  on  Earth:  Plate  Tectonics  Science  Matters     14    

Apart  from  their  outside  appearance,  are  the  canisters  similar  in  any  way?  How  did  you  obtain  your  evidence?  Part II  Procedures:  

1. Get  a  bucket  with  all  the  possible  contents  for  each  sealed  opaque  canister  and  three  empty  canisters  2. With  your  table  partner,  use  your  previous  observations  and  the  original  canister  to  create  your  own  

duplicate  canister.  3. Record  your  content  theories  below.  

 Content  Theory  for  each  canister:  

Canister  #____       Canister  #_____     Canister  #____                        

 How  did  you  determine  which  materials  matched  your  original  containers?        How  do  you  know  that  your  new  canister  matches  the  sealed  canister?        Exchange  your  model  canisters  and  the  original  sealed  canisters  with  your  tablemates.    Do  they  agree  with  your  content  selections?  Why  or  why  not?          Conclusion:  How  is  a  canister  like  Earth?        How  is  this  lab  similar  to  how  scientists  determine  the  Earth’s  interior  layers?            

H1b  

6.2  Layers  on  Earth:    Plate  Tectonics  Science  Matters       15    

 Parent  directions  for  making  

Layered  Cupcakes      

First  of  all…  THANK  YOU!  You  will  be  making  15  or  so  cupcakes.    Use  white  cake  mix.    Once  mixed,  divide  into  5  bowls  or  Ziploc  bags  and  color  each  mix  differently  with  food  coloring.  (ie:  green,  red,  yellow,  blue  and  leave  one  white)    Fill  foil  lined  cupcake  papers  with  the  layers.    The  easiest  way  I  have  found  is  to  use  the  Ziploc  bags  and  cut  the  corner.    Squeeze  into  cups  like  a  pastry  bag.    Mix  up  the  layer  order,  so  each  cupcake  is  different  from  the  rest.    Bake  as  directed.  Frost the top so none of the cupcake can be seen below the frosting.  The  project  idea  is  to  make  core  samples  of  the  cupcakes  (like  geologists  do  with  the  earth)  to  determine  what  the  layers  will  look  like.    Send  all  cupcakes  to  school,  Monday,  January    25th.    Please  have  them  delivered  to  my  classroom  before  school  starts.  Thank  you  again!            

H2  

6.2  Layers  on  Earth:  Plate  Tectonics  Science  Matters     16    

H3  

6.2  Layers  on  Earth:    Plate  Tectonics  Science  Matters       17    

                                                                                         

H4  H4  

6.2  Layers  on  Earth:    Plate  Tectonics  Draft  Aug.  2010       18    

                                                                                         

H5  

6.2  Layers  on  Earth:    Plate  Tectonics  Draft  Aug.  2010       19    

                                                                                         

H6a  

6.2  Layers  on  Earth:    Plate  Tectonics  Draft  Aug.  2010       20    

                                                                                         

H6b  

6.2  Layers  on  Earth:    Plate  Tectonics  Draft  Aug.  2010       21    

         

H6c