Physics II. Attachments
|
|
- Evelyn Wright
- 6 years ago
- Views:
Transcription
1 Physics II Attachments
2 Attachment A CLE: 1.1.D.a Page 1 Particle Theory of Matter Objectives Students will understand the particulate (kinetic) theory of matter; differentiate the behavior of particles in the solid, liquid, and gas phases; use the following skills: observing and inferring from observations. Motivation for Learning Materials Approximately ml of margarine Hot mitts Approximately 100 ml of popcorn kernels Hot air corn popper (optional) Two 250 ml beakers Additional popcorn for snacking (optional) One 1500 ml or 2000 ml beaker Salt (optional) Hot plate Paper napkins (optional) Preparation 1. Melt ml of margarine in a 250 ml beaker. It is a good idea to measure the melted margarine in a graduated cylinder. Too much or too little margarine will ruin the experiment. 2. Add 100 ml of popcorn kernels to the margarine in the beaker. 3. Place the beaker with the popcorn-margarine mixture in a freezer to harden. 4. After the popcorn-margarine mixture has hardened, warm the outside of the beaker in a hot water bath to loosen the solid and remove it from the beaker. 5. Put your popcorn margarine mixture on a piece of wax paper. Replace any stray kernels. At this point, sometimes the popcorn-margarine mixture falls apart. Just put it all back together the same way that you would make hamburger patties from ground beef. Wrap the popcorn-margarine mix in the wax paper. 6. Place the popcorn-margarine mixture back in the freezer. 356
3 Attachment A CLE: 1.1.D.a Page 2 Procedure 1. Discuss with students the states of matter and relate it to the particulate or kinetic theory of matter. 2. When you are finished, show the students the popcorn-margarine solid mixture and explain that the corn kernels are the molecules in a solid being held by the forces that are represented by the margarine. 3. Review the properties of a solid using the popcorn-margarine solid mixture as an example. 4. Place the solid in a 250 ml beaker on a hot plate and warm it until the margarine melts. 5. Pour the "liquid" back and forth between two 250 ml beakers. 6. Talk about the properties of a liquid, etc. 7. Heat the "liquid" in a 1500 ml or 2000 ml beaker over the hot plate until the "molecules" (popcorn kernels) begin to pop. The large beaker allows the popcorn to spread out for better popping. It also minimizes the spattering of hot margarine, unpopped popcorn, and popped popcorn. Watch splattering hot margarine, but don't cover the beaker. 8. As the popcorn leaves the beaker, talk about the properties of a gas. 9. The kids will want to eat the popcorn. As they write up what they saw and explain it, make another batch in the hot air popper and pass around. Background Information The object of this demonstration is to use popcorn kernels to represent molecules and the margarine to represent the bonding forces between molecules. Heating results in physical changes in the popcorn-margarine mixture that are analogous to the melting and boiling of matter. Extensions Have students develop their own analogous models that describe the particulate theory of matter and the phases of matter. This is a great "writing to learn" activity for science! 357
4 Attachment B CLE: 1.1.D.a Name Assessment 1. What was added to the solid to cause it to melt? What would you take away from the system to make it re-solidify? 2. How is a liquid transformed into a gas? 3. How is a gas transformed into a liquid? 4. In the popcorn and margarine model, what does the margarine represent? What do the popcorn kernels represent? 5. What do you consider to be the strengths of this popcorn and margarine model? The weaknesses? 358
5 Attachment B CLE: 1.1.D.a Answers to Assessment 1. Heat (thermal energy) was added to the solid to cause it to melt, and if the heat were taken away then the liquid would re-solidify 2. Thermal energy (heat) is transferred to the particles of the liquid causing them to bombard one another and recoil to larger and larger distances, thus phase changing into a gas. 3. As a gas loses the high amounts of energy causing the individual particles of the gas to collide and ricochet at relatively large distances, the particles calm down so-to-speak and the intra-atomic or intramolecular forces of attraction overcome the forces of repulsion so that the particles are able to come in very close proximity and slide against one another in liquid form. 4. The margarine represents the intra-molecular forces that hold the molecules of a solid in vibrating stasis. The individual kernels represent the particles, or in this case molecules within a sample of a compound. 5. Strengths might include: Macro examples of particles and forces otherwise invisible to the human eye (both naked and with most microscopic equipment; ability to show more than one phase using the same materials; ability to eat model. Weaknesses might include: The force is represented by something tangible when in reality it is not; the kernels in the solid are not vibrating; the popping of the kernels relates more to sublimation than evaporation, and sublimation is a topic not covered. 359
6 Attachment C CLE: 1.2.A.a Energy from Chemical Fuels 360
7 361 Attachment C CLE: 1.2.A.
8 362 Attachment C CLE: 1.2.A
9 NAME Attachment C CLE: 1.2.A 363
10 NAME: Attachment C CLE: 1.2.A 364
11 Attachment D CLE: 1.2.A.g Experiments with States of Matter: Mpemba Effect - Freezing Hot Water Faster than Cold Water The Mpemba Effect states that hot water changes its state from liquid to solid--or freezes--faster than cold water. This does not seem to make sense, but it has been discovered to be true. Goal of experiment The goal is to compare the time is takes to freeze a container of water at various starting temperatures of the water, under the same conditions. Conditions In any good experiment, you want to change only one variable and keep everything else to the same. You must also be able to determine when you achieved the outcome of the experiment. Factors Factors that must remain the same are: The temperature of the freezer The amount of water in the container The size, shape and material of the container Any type of air motion over the water The only thing you vary is the initial temperature of the water. When frozen Possible ways to determine when the water is frozen include: Use a thermometer or temperature probe in the water to see when the temperature near the bottom levels off at the freezing point. Visibly check to determine when the water in the container is frozen; perhaps a clear container would help. 365
12 Attachment D CLE: 1.2.A.g Experiment You can do the experiment using one or even several containers that you place in a freezer compartment. One container in freezer If you use one container, fill it with hot water, put it in a freezer and measure the time it takes the water to freeze. Then repeat the experiment with exactly the same amount of water in the same container at a cooler temperature. Do this a number of times, reducing the initial temperature of the water. Two or more containers in freezer Or, you could take two or more containers of the same size, shape and material and put exactly the same amount of water--but different temperatures-- into each. Then you put them both in the freezer and see which freezes first. The reason the containers must be exactly the same is because the shape and material of the container affects the rate of heat loss. Outside in winter In either of the above cases, you would have to periodically open the freezer to see if the water is freezing. An alternative would be to place the containers outside during the winter when the temperature was below freezing. You could then easily watch the freezing process from a window in your house. Data By comparing the time it takes to freeze for the various starting water temperatures, you should be able to find a situation where warmer water freezes faster than water at a colder temperature. 366
13 367 Attachment E CLE: 5.2.B.a-b
14 368 Attachment F CLE: 5.2.B.a-b
15 369 Attachment F CLE: 5.2.B.a-b
16 Attachment G CLE: 5.2.B.d-e Earthquakes and Plate Tectonics Introduction The tectonic plates of the world are constantly moving in relation to each other. The boundaries between plates are zones of active faulting and earthquakes. There are 3 types of plate boundaries and 3 types of faults. Remember, there are two types of crust which can be involved in this faulting, oceanic crust and continental crust. Review questions about type of crust. Which type of crust floats higher? Which type of crust subducts? What happens when dense crust runs into buoyant crust? PUSH and PULL 1) Where plates push together we call it a convergent boundary. Convergent boundaries are where subduction zones and collision zones are located. The type of faults that form along convergent boundaries are reverse faults, also called thrust faults. Convergence involving oceanic crust results in a subduction zone, where the oceanic crust dives back into the mantle. Along subduction zones, a trench forms on the ocean floor adjacent to a strato-volcano mountain range which is built on the overriding plate. When a convergent boundary involves 2 pieces of continental crust, a collision zone develops as the plates push mountains up into the sky. Task 1 On a world map, identify the convergent boundaries or the zones of thrust faults. (Color the subduction zones blue and the collision zones green. Remember that you must first determine if oceanic crust is involved) Questions 1a Can you name 5 countries located along 5 different convergent boundaries? 1b. Can you locate any convergent boundaries in your space shuttle photographs? 1c. Is the direction of motion of the portion of the convection cell in the mantle below a convergent zone UP? or DOWN? 2) Where plates pull apart we call it a divergent boundary. Along divergent boundaries we see rifting or fracture along normal faults. Spreading centers form along ocean ridges as oceanic crust is pulled or torn apart. Under all the worlds oceans new volcanic material erupts in rift valleys in the form of pillow basalt. A shield volcano can form as the lava builds up the ocean floor above sea level. Divergent boundaries can occur under continental crust and pull pieces apart to form parallel basins and ranges. (When you pull apart a "Fig Newton" which way to the little faults form? Draw a picture). 370
17 Task 2 Attachment G CLE: 5.2.B.d-e On a world map, identify the divergent boundaries or the zones of rifting and normal faults. (Color the ocean spreading centers red and rift zones orange.) Questions 2a Can you name 5 places that spreading or rifting is taking place? 2b. Can you locate any divergent boundaries on your shuttle photographs? 2c. Is the direction of motion of the portion of the convection cell in the mantle below a divergent zone UP? or DOWN? 3) Transform faults are associated with convergent and divergent boundaries. A transform fault moves pieces of crust past each other forming a strike-slip fault. This lateral motion can be described as either leftlateral or right-lateral. The way to determine whether a transform fault is left-lateral or right-lateral is to picture yourself standing and looking across the fault. If the land on the other side of the fault moves to your left, it's a left-lateral fault. If the land on the other side of the fault moves to your right, it's a right-lateral fault. Transform faults in continental crust can commonly involve aspects of divergence and convergence, when the fault is not straight. Where there is divergence, the land pulls apart forming a basin. Where there is convergence, the land collides, forming mountains. 371
18 Task 3 Circle the correct answer (You are now looking down on the Earth.) Attachment G CLE: 5.2.B.d-e 3a. Left-lateral or right-lateral? 3b. Left-lateral or right-lateral? 3c. Left-lateral or right-lateral? 3d. Left-lateral or right-lateral? Draw where you would expect mountains and valleys 3e. Left-lateral. 3f. 372
19 Attachment H CLE: 5.2.B.d-e Teaching Plate Tectonics with Easy-to-Draw Illustrations Next time you teach plate tectonics, consider a draw-with-me presentation that will engage your students and help them understand the spatial and movement aspects of plate boundary environments. The process of drawing a picture involves students much more deeply than reading or discussion. This is because drawings give students an opportunity to visualize sizes, shapes, motions, and spatial relationships. Important facts can be added through annotations and captions. Many students find a draw-with-me presentation an enjoyable experience. Drawing enhances their learning, understanding, and retention processes. And, at the end of the class session, they have a set of illustrations that can be used for study, reference, and communication purposes. I have used the illustrations in this booklet, with only minor modifications, to lead students from primary grades through graduate school in lessons about plate movements, volcanoes, earthquakes, and the rock cycle. When time allows, I always opt to draw these illustrations step-by-step with my students. It s fun that way! When time is short, presenting the illustrations on an overhead projector can be a good alternative, especially if your students have photocopies of the illustrations to which they can add important details and annotations. Please feel free to use the illustrations here in any way that will enhance your teaching. And, if you have time, draw them once for me. Hobart M. King hobart@geology.com 373
20 374 Attachment H CLE: 5.2.B.d-e
21 375 Attachment H CLE: 5.2.B.d-e
22 376 Attachment H CLE: 5.2.B.d-e
23 377 Attachment H CLE: 5.2.B.d-e
24 378 Attachment H CLE: 5.2.B.d-e
25 Attachment I CLE: 7.1.A Page 1 Scoring Rubric: Student Laboratory Reports Problem Statement The student is to clearly identify the problem under investigation as accurately and completely as possible from background information. The students explanation should strive to be precise and thorough. Experimental Hypothesis The student should predict what will happen based on proper use and interpretation of background information, not merely on what he or she thinks will happen. Experimental Design The explanation of the design should include: 1. A listing of all materials to be used, relating the materials to the dependent and independent variables as appropriate and noting controls to be placed on the study as needed. 2. A description of the design of the study, including: a. What data will be collected? b. How many trials will be completed? c. How will variables be controlled? d. How will the data be interpreted? e. What graphs or charts will be based on the data collected? 3. A description of all safety concerns and how each will be addressed. Data Collection, Display, and Analysis The student conducts the experiment, carefully and systematically making measurements and entering data. Graphic presentation(s) of data is produced appropriate to the analysis. 379
26 Attachment I CLE: 7.1.A Page 2 Conclusion This includes a statement of what data results indicate (data analysis) and whether data supports or does not support the hypothesis. In addition, experimental errors should be identified and their possible effect on the reported results. Students are to discuss possible applications and extensions of research findings, indicate other studies which have been or may be conducted to support the conclusion of the experiment. Statement of problem is irrelevant or erroneous Limited or no relevant explanation Problem Statement Problem partially identified with partial validity Limited relevant explanation Problem sufficiently identified with some validity Experimental Hypothesis Basic relevant explanation Problem is appropriately identified Precise, clear and relevant explanation Unreasonable association between problem and predicted results Results are not operationalized Defends or challenges established knowledge Scant use of scientific concepts and vocabulary Association between problem and predicted results Made attempt to operationalize key variables Hypothesis has some relationship to established knowledge but is not supported Scientific concepts and vocabulary used, but contains errors Reasonable association between the problem and the predicted results Key variables are operationalized Hypothesis has a reasonable relationship with established knowledge; this relationship is generally supported Scientific concepts and vocabulary used without significant error Association between the problem and the predicted results is direct and relevant All variables are clearly operationalized Hypothesis clearly refutes or defends established knowledge and is fully supported Student demonstrates facility in the use of scientific concepts and vocabulary 380
27 Attachment I CLE: 7.1.A Page 3 Design is not relevant to the hypothesis List of materials and controls incomplete Experimental Design Some procedural components generally described but are not replicable Safety concerns are not specified, are irrelevant or are not appropriate to the experiment Data are inaccurate Data are haphazardly recorded Data table missing Design has general relevance to the hypothesis List of materials and controls is nearly complete, missing at least one important item Description makes it possible to replicate the experiment if researcher makes some inferences Safety concerns miss at least one important consideration; procedures will result in some risk to student safety if not revised Design is adequate to test the hypothesis List of materials and controls is complete and some description provided Description makes it likely that the experiment can be reliably replicated All major safety concerns are adequately addressed; procedures adopted are likely to produce a safe experiment some further refinement could minimize possible discomfort to the student Data Collection & Analysis Design is a wellconstructed test of the stated hypothesis List of materials and controls is complete and thoroughly described The description of the experiment is complete, insuring that it can be replicated Safety concerns are fully addressed and procedures for conducting the experiment insure that there is little or no risk of safety or discomfort to the student Most data are collected but checks are not placed on measurement to insure accuracy Data are recorded in a manner that threatens reliability Data table incomplete or contain inconsistencies All significant data measured with some checks placed on measurement for accuracy Data recorded effectively The data table is relevant to the task requirements All significant data measured, checks are placed on measurements for accuracy Data recorded effectively and efficiently The data table well-designed to the task requirements 381
28 Attachment I CLE: 7.1.A Page 4 Graph form inappropriate Data Display Data points missing or incorrect Inappropriate labeling Intervals inappropriate Inconclusive, or conclusion not warranted by data analysis Graph form is appropriate All data points included, some inaccurately plotted Labeling lacks clarity Intervals are appropriate Graph form is appropriate, multiple graphs used as warranted All data points included and accurately plotted Labeling clear Intervals appropriate Graph visually designed to assist reader Conclusion All graph forms are appropriate, multiple graphs used as warranted All data points accurately plotted Labeling clear Intervals appropriate Graph visually compelling, highlights conclusions of the study Conclusion too general or over- reaches the data analysis Conclusion uses the language of the experiment but does not translate conclusion to its relevance to the original problem Conclusion precise, related to the hypothesis Conclusion uses operational terms of the experiment and attempts to translate the conclusion to make it relevant to the original problem The conclusion related to general interest and other studies Conclusion precisely stated, relates directly to support or non-support of the hypothesis Conclusion uses operational terms and suggests how the conclusion has relevancy in resolution of the original problem Conclusion relates the study to general interest, other studies that have been or could be conducted 382
29 Attachment J CLE: 8.2.A.a-b Research Paper CATEGORY Organization Information is very organized with wellconstructed paragraphs and subheadings. Information is organized with wellconstructed paragraphs. Information is organized, but paragraphs are not well-constructed. The information appears to be disorganized. 8) Amount of Information There is a clear introduction and conclusion, and the scientist's life is extensively detailed and connected to his/her work. There is a good introduction and conclusion, and the scientist's life is well detailed and connected to his/her work. There is an introduction and conclusion, and the scientist's life is adequately detailed and connected to his/her work. Introduction or Conclusion missing, poor account of scientist's life and poorly connected to his/her work. Sources All sources (information and graphics) are accurately documented in the desired format. All sources (information and graphics) are accurately documented, but a few are not in the desired format. All sources (information and graphics) are accurately documented, but many are not in the desired format. Some sources are not accurately documented. Mechanics No grammatical, spelling or punctuation errors. Almost no grammatical, spelling or punctuation errors A few grammatical spelling, or punctuation errors. Many grammatical, spelling, or punctuation errors. Diagrams & Illustrations (optional) Citations At least three illustrations are included that add to the reader's understanding of the topic. At least three citations from research sources are included and are correctly punctuated. Two illustrations are included that add to the reader's understanding of the topic. Two citations from research sources are included and are correctly punctuated. One illustration is included that adds to the reader's understanding of the topic. Only one citation from research sources are included and are correctly punctuated Diagrams and illustrations are not included OR do not add to the reader's understanding of the topic. No citations are included, or the ones that are included are incorrectly punctuated. Sources At least three different kinds of sources are used (book, magazine, website) Two different kinds of sources are used (from the following: book, magazine, website) Only one kind of source is used (from the following: book magazine, website) No research sources are used 383
Unit 10 ~ Learning Guide
Unit 10 ~ Learning Guide Name: INSTRUCTIONS Using a pencil, complete the following practice questions as you work through the related lessons. You are required to have this package completed BEFORE you
More informationWrite It! Station Directions
Write It! Station Directions It is recommended that you have completed at least two of the following stations before working at this station. -Read It! -Explore It! -Watch It! -Research It! Answer each
More informationWhat is the theory of plate tectonics? Lesson 1 Lesson 2 Lesson 3
Name Plate Tectonics What is the theory of plate tectonics? Date Before You Read Before you read the chapter, think about what you know about plate tectonics Record your thoughts in the first column Pair
More information1. In your own words, what is the Earth s crust?
The Structure of Earth Classwork Classwork #1 Name: 1. In your own words, what is the Earth s crust? 2. The Earth s surface became the way it is: A. only very recently. B. because of one event in history.
More informationSea Floor Spreading Lab ES2 # 1 Purpose: Show rock age and magnetism patterns in spreading sea floor with a paper model.
Names & B Date your name (first and last) partner Sea Floor Spreading Lab ES2 # 1 Purpose: Show rock age and magnetism patterns in spreading sea floor with a paper model. Background: In the last few decades,
More informationThanks. You Might Also Like. I look forward helping you focus your instruction and save time prepping.
Thanks Connect Thank you for downloading my product. I truly appreciate your support and look forward to hearing your feedback. You can connect with me and find many free activities and strategies over
More informationThe Theory of Plate Tectonics
Plate Tectonics Objectives Describe how plates move. Explain the features of plate tectonics. Describe the types of plate boundaries and the features that can form and events that can occur at each. The
More informationSea Floor Spreading Lab ES2 # 2!
Names & Bl Date your name (first and last) partner Sea Floor Spreading Lab ES2 # 2 Purpose: Show rock age and magnetism patterns in spreading sea floor with a paper model. Background: In the last few decades,
More informationSeptember 14, SWBAT explain how divergent boundaries shape Earth s surface.
September 14, 2016 Aims: SWBAT explain how divergent boundaries shape Earth s surface. Agenda 1. Do Now 2. Class Notes 3. Guided Practice 4. Independent Practice 5. Practicing our AIMS: Homework: EI.11
More informationSnack Tectonics or Modeling Plate Movement
Snack Tectonics or Modeling Plate Movement Objective: Use models to describe how tectonic plates cause major geological events such as; ocean basins, earthquakes, volcanoes, and mountain building. Questions:
More information4 Deforming the Earth s Crust
CHAPTER 7 4 Deforming the Earth s Crust SECTION Plate Tectonics BEFORE YOU READ After you read this section, you should be able to answer these questions: What happens when rock is placed under stress?
More informationFinding Fault with Food or Modeling Plate Movement
Finding Fault with Food or Modeling Plate Movement Objective: Use models to describe how tectonic plates cause major geological events such as; ocean basins, earthquakes, volcanoes, and mountain building.
More information1. What is Wegener s theory of continental drift? 2. What were the 4 evidences supporting his theory? 3. Why wasn t Wegener s theory excepted?
Notebook 7a and 7b Objective (left-side): Students will be able to explain the theory of plate tectonics and be able to make predictions about plate interactions. Mapping Reflection 1. What is Wegener
More information4 th Grade PSI. Slide 1 / 107 Slide 2 / 107. Slide 3 / 107. Slide 4 / 107. Slide 5 / 107. Slide 6 / 107. The History of Planet Earth
Slide 1 / 107 Slide 2 / 107 4 th Grade PSI The History of Planet Earth 2015-11-10 www.njctl.org Slide 3 / 107 Slide 4 / 107 The History of Planet Earth The Structure of Earth Rock Layers Fossils and Relative
More informationCONTINENTAL DRIFT THEORY
CONTINENTAL DRIFT THEORY Proof or crazy idea? CONTINENTAL DRIFT THEORY What is Continental Drift Theory? Continental drift theory (CDT): Alfred Wegener found all the continents were once together called
More informationPlate Tectonics Practice Test
Plate Tectonics Practice Test 1. What is the main idea Alfred Wegner proposed in the Theory of Continental Drift that he published in 1915? a. The continents float on a liquid layer that allows them to
More information10/29/13. Plate Boundaries. 3 types of plate boundaries: Divergent (divide) Convergent (collide) Transform (slide past)
Plate Boundaries 3 types of plate boundaries: Divergent (divide) Convergent (collide) Transform (slide past) 1 Remember the plates are in motion. When plates move, they can either: A) converge (collide)
More informationPlate Tectonics Comic Book Pg s 9-13
Plate Tectonics Comic Book Pg s 9-13 Your Comic Book should include the following on each page: Your CHARACTER thoroughly explaining the concept for the page DRAWINGS for each of the topics A brief EXPLANATION
More informationTECTONIC PLATES. reflect
reflect Has anyone ever told you to sit still? You may do as you re told, but in truth, you can never really sit still. You have probably already learned that Earth is constantly moving through space,
More informationName Date Class. How have geologists learned about Earth s inner structure? What are the characteristics of Earth s crust, mantle, and core?
Chapter 4 Plate Tectonics Section 1 Summary Earth s Interior How have geologists learned about Earth s inner structure? What are the characteristics of Earth s crust, mantle, and core? Earth s surface
More informationEarth s Dynamic Surface
Earth s Dynamic Surface Shaping Earth s Surface What do you think? Read the two statements below and decide whether you agree or disagree with them. Place an A in the Before column if you agree with the
More informationGrade 7 Science Curriculum Map - Norwell Middle School SUBJECT: Science Grade Level: 7
Grade 7 Science Curriculum Map - Norwell Middle School SUBJECT: Science Grade Level: 7 Unit: Physical Science (Chemistry) ~ 10 Weeks Ending Near Thanksgiving Science Standard 2: Differentiate between volume
More informationWhy Does the Mantle Move the Way it Does?
Why Does the Mantle Move the Way it Does? In the demonstration, you observed warm water rising through cool water. You also observed cool water sinking to replace the warm water. The movement of a fluid
More informationSAC Geography Form 2 Chapter 3: Plate Tectonics Topic 3: Plate Movement
What causes an earthquake? Plate movement causes pressure to build up along faults, or breaks, in the earth's crust. When the rocks cannot take any more pressure, the rock layers shift and an earthquake
More informationName: Block: Date: Student Notes. OBJECTIVE Students will investigate the relationship between temperature and the change of the state of matter.
Name: Block: Date: LCPS Core Experience Heat Transfer Student Notes OBJECTIVE Students will investigate the relationship between temperature and the change of the state of matter. LINK 1. Particles in
More informationPlate Tectonics Notes
Plate Tectonics Notes Last 30 Days Earthquakes Physical Features Last 30 Days Earthquakes with Plate Boundaries Earth s Structure Earth s Layers Core: Inner Core: Center of the earth, solid ball of metal
More informationEarth s Changing Surface
Earth s Changing Surface Tectonics What do you think? Read the two statements below and decide whether you agree or disagree with them. Place an A in the Before column if you agree with the statement or
More informationCh. 9 Review. Pgs #1-31 Write Questions and Answers
Ch. 9 Review Pgs. 356-357 #1-31 Write Questions and Answers 356-357 #1-5 Answers 1. The layer of the upper mantle that can flow is the: A - Asthenosphere 2. Most scientists rejected Wegener s theory of
More informationScience 10 PROVINCIAL EXAM STUDY BOOKLET. Unit 4. Earth Science
Science 10 PROVNCAL EXAM STUDY BOOKLET Unit 4 Earth Science Student nstructions 1. Ensure that you have blank paper and a Data Booklet. 2. Record all answers on a separate piece of paper. 3. Answer keys
More informationPLATE TECTONICS Chapter 4 Notes
PLATE TECTONICS Chapter 4 Notes Review Earth s Interior Ch 1. Geologists have used two main types of evidence to learn about Earth s interior: Direct evidence from rocks drilled from deep inside Earth
More informationDynamic Planet. Student Name. Teacher
Dynamic Planet Student Name Teacher The Dynamic Planet 1. What makes our planet dynamic? 2. Draw the Earth and its systems: 3. What makes up the four systems of our Earth? Geosphere: Hydrosphere: Atmosphere:
More informationPLATE TECTONICS REVIEW GAME!!!!
PLATE TECTONICS REVIEW GAME!!!! Name the four layers of the earth - crust - mantle - outer core - inner core Which part of Earth s structure contains tectonic plates? LITHOSPHERE Name one reason why the
More informationSection 3. What Drives the Plates? What Do You See? Think About It. Investigate. Learning Outcomes
Section 3 What Drives the Plates? What Do You See? Learning Outcomes In this section, you will Calculate the density of liquids and compare their densities with their position in a column of liquid. Observe
More informationThe continents are in constant! movement! Earth Science!
The continents are in constant movement Earth Science Transitional Science 10 Note and Activity Package for Chapter 12 Note: If you lose this package it is your responsibility to print out a new copy from
More informationUse a highlighter to mark the most important parts, or the parts. you want to remember in the background information.
P a g e 1 Name A Fault Model Purpose: To explore the types of faults and how they affect the geosphere Background Information: A fault is an area of stress in the earth where broken rocks slide past each
More informationCore. Crust. Mesosphere. Asthenosphere. Mantle. Inner core. Lithosphere. Outer core
Potter Name: Date: Hour: Score: /21 Learning Check 4.1 LT 4.1 Earth s Interior: I can draw and interpret models of the interior of the earth. Draw the following models (put the words in the right order)
More informationSURFACE FEATURES AND PLATE TECTONICS (MODIFIED FOR ADEED)
(MODIFIED FOR ADEED) Science Concept: There are three types of movements related to the motion of Earth s plates. Mountain Building, faults (which can generate earthquakes), and volcanoes are all surface
More informationEarth s Changing Surface
Earth s Changing Surface Earthquakes and Volcanoes Key Concepts What causes earthquakes? What causes volcanoes to form? How do earthquakes and volcanoes change Earth s surface? What do you think? Read
More informationContinental Drift to Plate Tectonics: From Hypothesis to Theory
Continental Drift to Plate Tectonics: From Hypothesis to Theory 1 Key Understandings Internal structure of the earth/structure of the crust. Difference between continental drift & plate tectonics. Evidence
More information1. I can describe evidence for continental drift theory (e.g., fossil evidence, mountain belts, paleoglaciation)
Science 10 Review Earth Science Vocabulary asthenosphere continental drift theory converging plates diverging plates earthquakes epicentre fault hot spot inner core lithosphere mantle mantle convection
More informationBoundaries, Stresses, and Faults OH MY! How do geologic events change and shape Earth s surface?
Boundaries, Stresses, and Faults OH MY! How do geologic events change and shape Earth s surface? Remember The Lithosphere is made of The CRUST + The Upper Rigid Mantle Plates may be called by different
More informationTO GO TO ANY OF THE PAGES LISTED BELOW, CLICK ON ITS TITLE
TO GO TO ANY OF THE PAGES LISTED BELOW, CLICK ON ITS TITLE CHAPTER 6 Plate Tectonics 1 6-1 What is continental drift? 2 6-2 Why is the seafloor spreading? 3 6-3 What evidence supports seafloor spreading?
More informationEarth is over 1200 km thick and has four distinct layers.
1 2.2 F e a ture s o f P la te T e c to nic s Earth is over 1200 km thick and has four distinct layers. These layers are the crust, mantle (upper and lower), outer core, and inner core. Crust outer solid
More informationEarth s Interior. Use Target Reading Skills. Exploring Inside Earth
Plate Tectonics Name Date Class Earth s Interior This section explains how scientists learn about Earth s interior. The section also describes the layers that make up Earth and explains why Earth acts
More informationPlate Tectonics. Continental Drift Sea Floor Spreading Plate Boundaries
Plate Tectonics Continental Drift Sea Floor Spreading Plate Boundaries Continental Drift 1915, Alfred Wegener - Pangea hypothesis: suggested Earth s continents were part of a large super-continent 200
More informationThis nonfiction book
This nonfiction book explains how islands are born from underwater volcanoes. The challenging content is made accessible with simple text, captions, photographs, labels, and diagrams. 16 pages, 231 words
More information12.2 Plate Tectonics
12.2 Plate Tectonics LAYERS OF THE EARTH Earth is over 1200 km thick and has four distinct layers. These layers are the crust, mantle (upper and lower), outer core, and inner core. Crust outer solid rock
More informationOutcome C&D Study Guide
Name: Class: Outcome C&D Study Guide Identify the layers of Earth s interior Lithosphere the upper most layer of the earth that includes the crust and the hard outer mantle. It is fractured into tectonic
More informationPlate Boundaries. Presented by Kesler Science
Presented by Kesler Science Essential Questions: 1. What is plate tectonics? 2. What are the three types of plate boundaries? 3. What crustal features are formed at plate boundaries? Quick Action INB Template
More information5. Convergent boundaries produce a relatively low number of earthquakes compared to other boundaries. a. True
1. Earth s crust is thinner than its mantle. ANSWER: True 2. The concept of isostacy states that high-density rock will stand higher than low-density rock, which explains the formation of subduction zones.
More informationTopic 12 Review Book Earth s Dynamic Crust and Interior
Topic 12 Review Book Earth s Dynamic Crust and Interior Define the Vocabulary 1. asthenosphere 2. continental crust 3. Convection current 4. Convergent plate boundary 5. Divergent plate boundary 6. earthquake
More informationForces that Shape the Land. Plate Tectonics
Forces that Shape the Land Plate Tectonics Directions: This packet goes along with my plate tectonics powerpoint. After viewing the powerpoint, students are to complete this activity sheet. 1. Start by
More informationPlate Tectonics. The Theory of Plate Tectonics. The Plate Tectonics Theory. 62 Plate Tectonics Reading Essentials
CHAPTER 4 LESSON 3 Tectonics The Theory of Tectonics Key Concepts What is the theory of plate tectonics? What are the three types of plate boundaries? Why do tectonic plates move? What do you think? Read
More informationThe Four Layers The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and
Earth s Structure The Four Layers The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and
More informationUnit 4 Lesson 6 Plate Tectonics
Unit 4 Lesson 6 Plate Tectonics Indiana Standards 7.2.1 Describe how the earth is a layered structure composed of lithospheric plates, a mantle and a dense core. 7.2.4 Explain how convection currents in
More informationPlate Tectonics Investigation
Plate Tectonics Investigation Exploration A Look at a watch or clock with a second hand in the classroom. 1. What evidence of movement do you see on the clock face? 2. What other movement do you know takes
More informationRefer to the map on page 173 to answer the following questions.
Chapter 8-1 Plate Tectonics 1. Brainstorm the type of evidence that would indicate a climate change and how this evidence supports the theory of continental drift. Tropical fossils in cold regions Evidence
More informationsonar seismic wave basalt granite
geologist sonar crust geology seismic wave mantle constructive force basalt inner core destructive force granite outer core The solid, rocky, surface layer of the earth. an instrument that can find objects
More informationUnit: 4 Plate Tectonics LT 4.1 Earth s Interior: I can draw and interpret models of the interior of the earth.
Unit: 4 Plate Tectonics LT 4.1 Earth s Interior: I can draw and interpret models of the interior of the earth. 1. Can you draw the 3-layer model and the 5-layer model of the Earth? #1 Yes I can: 2. Can
More informationPlate Tectonics. By Destiny, Jarrek, Kaidence, and Autumn
Plate Tectonics By Destiny, Jarrek, Kaidence, and Autumn .The Denali Fault and San Andreas Fault - The San Andreas Fault is a continental transform fault that extends roughly 1300 km (810 miles) through
More informationPlates & Boundaries The earth's continents are constantly moving due to the motions of the tectonic plates.
Plates & Boundaries The earth's continents are constantly moving due to the motions of the tectonic plates. As you can see, some of the plates contain continents and others are mostly under the ocean.
More informationMAR110 Lecture #4 Fundamentals of Plate Tectonics
1 MAR110 Lecture #4 Fundamentals of Plate Tectonics The Ocean Sea Floor is formed Along the Mid-Ocean Ridge Spreading Centers The Ocean Sea Floor is destroyed in the Subduction Zones Figure 4.2 Convection
More information4 Deforming the Earth s Crust
CHAPTER 7 4 Deforming the Earth s Crust SECTION Plate Tectonics BEFORE YOU READ After you read this section, you should be able to answer these questions: What happens when rock is placed under stress?
More informationOBJECTIVE: For each boundary type, give an example of where they occur on Earth.
OBJECTIVE: Explain the theory of Plate Tectonics. COMPARE AND CONTRAST DIVERGENT, CONVERGENT AND TRANSFORM BOUNDARIES. ***very important. Describe what geologic features form at each of the three CONVERGENT
More informationGraham Cracker Plate Tectonics
Graham Cracker Plate Tectonics Purpose 1. To identify and demonstrate the forces that shape the features of the Earth 2. To understand how plate boundaries interact with each other and the features created
More information8 th Grade Campus Assessment- NSMS Plate Tectonics
1. A group of students were discussing plate tectonics in their science class. All of the following statements about the tectonic plates are incorrect EXCEPT: A. The Eurasian Plate consists of the Asian
More informationMission to Mars! IS EARTH THE ONLY PLANET TO EXPERIENCE PLATE TECTONICS?
Mission to Mars! IS EARTH THE ONLY PLANET TO EXPERIENCE PLATE TECTONICS? PLATE TECTONICS Earth s crust is split up into several tectonic plates which are constantly moving around (about the same speed
More informationShown is the supercontinent Pangaea before it broke up and the continents drifted.
Has anyone ever told you to sit still? Did you know you can never really sit still? You have probably already learned that Earth is constantly moving through space, but did you know that the ground beneath
More informationUnit 4 Lesson 2 Plate Tectonics. Copyright Houghton Mifflin Harcourt Publishing Company
Puzzling Evidence What evidence suggests that continents move? In the late 1800s, Alfred Wegener proposed his hypothesis of continental drift. According to this hypothesis, the continents once formed a
More informationPlate Tectonics and fun Earth Stuff
Plate Tectonics and fun Earth Stuff Set Up - 1 large graham cracker - 2 3-in squares of fruit roll up - 1 cup of water - Frosting/cool whip - Wax paper or plate - Plastic spoon http://learningplatetectonics.weebly.com/activity.html
More informationFORCES ON EARTH. An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth.
FORCES ON EARTH An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth. GEOLOGY Geologists scientists who study the forces that make and shape the Earth Geologists
More information8 th Grade Science Plate Tectonics and Topography Review
8 th Grade Science Plate Tectonics and Topography Review #1 Scientists believe that the land masses of Earth were once joined together as one supercontinent called. A: Australia B: Wegner C: Pangaea D:
More informationEarth s Plates, Part 1: What Are They, Where Are They and What Do They Do?
Earth s Plates, Part 1: What Are They, Where Are They and What Do They Do? A scientist named Alfred Wegener believed that, at one time, all of the continents were one landmass. Although he had no real
More information7th Grade. Science. September. Scientific Inquiry- Scientific Method
7th Grade Science September Scientific Inquiry- Scientific Method 1. Develop a problem or question 2. Produce a hypothesis 3. Identify and organize controls and variable in an experiment 4. Perform the
More informationAsteroids and comets.
Asteroids and comets. Question 1 Can Asteroids and comets cause the earth to change? Asteroids do change the earth because when the earth was first starting out Asteroids and comets would come to the earth
More informationPlate Tectonics Scavenger Hunt
Plate Tectonics Scavenger Hunt Directions: GO TO TEACHER WEBPAGE FOR LINKS TO WEBSITES! Read each page from the websites very carefully and use the information given to complete the scavenger hunt. SITE:
More informationTopics. Nuclear waste storage, risk analysis, evidence and tradeoffs, Groundwater, aquifer, aquitard. literacy
UNIT OVERVIEW GEOLOGICAL PROCESSES Listed below is a summary of the activities in this unit. Note that the total teaching time is listed as 26 32 periods of approximately 45 50 minutes (approximately 6
More informationName: Date: Per. Plate Tectonics Study Guide (Ch. 5)
Name: Date: Per. Plate Tectonics Study Guide (Ch. 5) 1. Fill in the Chart about heat Transfer Types Description Examples Where it takes place Radiation Sun s rays reaching earth Heat Transfer between objects
More informationSea-Floor Spreading. Use Target Reading Skills. Mid-Ocean Ridges. What Is Sea-Floor Spreading?
Name Date Class Plate Tectonics Guided Reading and Study Sea-Floor Spreading This section explains sea-floor spreading and describes evidence that it happens. The section also explains subduction and describes
More informationName Date Class. Plate Tectonics
Chapter Review Plate Tectonics Part A. Vocabulary Review Directions: Write the term that matches each description below in the spaces provided. Then unscramble the letters in the boxes to reveal the mystery
More informationPlate Tectonic Theory
Have you ever looked at a world map and noticed the shapes of the continents? Have you ever noticed how some continents appear to fit together like the pieces of a jigsaw puzzle? Why do you think this
More informationNotepack # 9 AIM: Why are the continents drifting apart? Do Now: Watch the video clip and write down what you observe.
Notepack # 9 AIM: Why are the continents drifting apart? Do Now: Watch the video clip and write down what you observe. http://www.youtube.com/watch?v=ci 5P5yy0xlg&feature=related What do we know as a class,
More informationINTRODUCTION TO LESSON CLUSTER 7
INTRODUCTION TO LESSON CLUSTER 7 EXPLAINING MELTING AND SOLIDIFYING A. Lesson Cluster Goals and Lesson Objectives Goals Students should be able to explain melting and solidifying, by reference to the molecular
More informationGeneral Oceanography Geology 105 Expedition 8 Plate Boundaries Beneath the Sea
General Oceanography Geology 105 Expedition 8 Plate Boundaries Beneath the Sea Name Not attempting to answer questions on expeditions will result in point deductions on course workbook (two or more blank
More informationPlate Tectonics Introduction
Name Block Plate Tectonics Introduction Go to the following site: http://www.learner.org/interactives/dynamicearth/index.html On the top of the screen are different tabs, click on each section as listed
More informationWhat is a natural hazard?
What is a natural hazard? Give me a definition not examples These words might help you A natural hazard is a naturally occurring event that might have a negative effect on people or the environment. Location
More informationFORCES ON EARTH UNIT 3.2. An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth.
FORCES ON EARTH UNIT 3.2 An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth. USE THESE NOTES: OUR HOME PLANET EARTH: What do you know about our planet? SO.HOW
More informationWarm-Up. Explain why the Earth is like a chocolate chip cookie that was recently taken out of the oven. Mmm Earth Cookie
Warm-Up Explain why the Earth is like a chocolate chip cookie that was recently taken out of the oven Mmm Earth Cookie New Area of Focus: Layers of the Earth Learning about the earth s interior. The force
More informationLesson Plan: Plate Tectonics
Lesson Plan: Plate Tectonics Lesson Plan: Plate Tectonics Lesson Plan Content: This lesson plan and slide presentation is to be used in conjunction with: 1 x plate tectonics teacher briefing 1 x plate
More informationSnackin Plate Tectonics
Name of group members: Date: Period: Snackin Plate Tectonics Purpose of Activity: To model the interactions of Earth s lithosphere (tectonic plates) as they slowly move on the Earth s upper mantle (asthenosphere),
More information5th Grade Science Syllabus and Classroom Expectations
5th Grade Science Syllabus and Classroom Expectations Class Description: The organization of this class will include topics from the physical sciences, Biology, and earth Science. This year you will be
More informationTectonic Forces Simulation: Earthquakes Activity One
Tectonic Forces Simulation: Earthquakes Activity One Introduction If you marked all the earthquakes from the past century on a world map, you'd notice that most tend to occur along certain lines around
More informationMAR110 Lecture #3 Ocean Bathymetry / Plate Tectonics
1 MAR110 Lecture #3 Ocean Bathymetry / Plate Tectonics Ocean Basin Geographic Zones The geographic zones of the North Atlantic are identified in the bird s eye view of the sea floor above. Below is shown
More informationTheory of Continental Drift
Plate Tectonics Theory of Continental Drift Alfred Wegener suggested that continents had once been part of a supercontinent named Pangaea, that later broke up. The pieces moved apart over millions of years
More informationName Test Date Hour. the interior of the Earth to the surface. younger less dense plate.
Name Test Date Hour Earth Processes#2 - Notebook Plate Tectonics LEARNING TARGETS I can identify and describe the three main layers of Earth. I can explain the difference between an oceanic and a continental
More informationPlate Tectonics. Theory of Plate Tectonics. What is Plate Tectonics. Plate Tectonics Plate Boundaries Causes of Plate Tectonics
Theory of Plate Tectonics Plate Tectonics Plate Boundaries Causes of Plate Tectonics Plate Tectonics What is Plate Tectonics The Earth s crust and upper mantle are broken into sections called plates Plates
More informationEarth s Ocean Waters
Earth s Ocean Waters BigIdeas Nearly three-quarters of Earth is covered by water, the majority of which is saltwater found in the ocean. Water has many unique properties that shape our planet and life
More informationLesson 2 Changes in State
Lesson 2 Changes in State Student Labs and Activities Page Launch Lab 25 Content Vocabulary 26 Lesson Outline 27 MiniLab 29 Content Practice A 30 Content Practice B 31 Language Arts Support 32 School to
More informationThe Crust How does the crust move?
Lesson Plan 3 The Crust Introduction Discuss with the aid of a world map Have the Earth s land areas always looked the same? Can you show any evidence if you think the position of continents has changed?
More informationPlate Boundaries & Resulting Landforms
Plate Boundaries & Resulting Landforms Divergent Plate Boundaries (plates being pulled apart) Type: oceanic plates Description: rising magma gently lifts the crust creating a ridge. The flow of convection
More information