Asteroids and comets.
|
|
- Todd Dickerson
- 5 years ago
- Views:
Transcription
1 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 and helped create the earth's crust with the molten lava hardening. Crust Crust is the outer layer of the earth. Molten lava Molten lava is melted rock that explodes out of a volcano.
2 Crust Forming 2. Crust is made by heaviest elements sinking to the core and lighter elements including oxygen and silicon rising to the surface where they erupt in volcanoes of molten rock. Earth's surface cools and molten lava solidifies to form crust. Erupt: (of a volcano) to become active and throw forth lava, ash, and gases. Lava: hot molten or semifluid rock erupted from a volcano or fissure, or solid rock resulting from cooling of this.
3 (Meteorites): Space rock made up of dibri from space Earth's water Question 3 Where Earth got its water from as been a mystery, but most believe the meteorites had a lot of water and it landed on Earth. (Water) A liquid that covers 75% of Earth's surface By: Emma Bowadt
4 (Continental Crust): The thick part of the Earth s crust that forms the large landmasses we live on today. It is older and more complex than ocean crust. Continental Crust (Question #4) How is the continental crust not destroyed? (Buoyant): Something that is buoyant has little density. The continental crust is not destroyed because it is made out of granite. It is buoyant enough to stay on the top of the crust, and not fall into the ocean, but strong enough to hold together.
5 Mantle: 5- Plate Tectonics Moving The heat and pressure in the mantel make the rock flexible enough to allow what? The plate tectonics that sit on the mantle, move when the heat and pressure makes the mantle flexible enough to allow the plates above to move. The mantle is the part of the Earth between the Earth s crust and core. Plate Tectonics: Plate Tectonics are the layers in the Earth s crust that move and float. They sometimes fracture/collide causing, drift, earthquakes, volcanoes, mountains etc.
6 Identical fossils in different continents Question 6: The distribution of ancient fossils shows that the continents moved because there were identical fossils on separate continents. This shows that the continents were once together. Fossil: The remains of an organism preserved in a rock. Continents: Earth s main large pieces of land sometimes separated by ocean.
7 Flow of Energy Question 7- Earth gets its heat from radioactive decay, but most come from leftover from collisions and massive bombardment during early years of of earth. Radioactive: emitting or relating to the emission of ionizing radiation or particles Decay: the state or process of rotting or decomposition
8 (ONE PICTURE) (Molten Rock) (Question #8) When the molten rock reaches the surface, it creates rock. Molten Rock: A solid that becomes liquid caused by heat. Lava: Molten rock that comes out of a volcano when erupted.
9 (ONE PICTURE) Rising Rock (Academic Vocabulary Word): Molten Rock (or Magma): It is an object that's reduced to liquid form by heating. (Academic Vocabulary Word): Mantel: #8 Answer: Earth's center is hotter than the surface and causes molten rock from the mantel to rise. When it reaches the surface, new rock is created and pushes the plates apart. The Mantel is made up of magma and rock is the part of the earth between the core and the the crust is the mantel.
10 E PICTURE) Mid Atlantic ridge 9. The ridge that is causing the plates to move apart is the Mid Atlantic ridge. It is also a mid-ocean ridge, a divergent tectonic plate or constructive plate boundary located along the floor of the Atlantic Ocean, and part of the longest mountain range in the world. Ridge - a long narrow hilltop, mountain range, or watershed. Plate - the two sub-layers of the earth's crust (lithosphere) that move, float, and sometimes fracture and whose interaction causes continental drift, earthquakes, volcanoes, mountains, and oceanic trenches.
11 Atlantic Catching up to the Pacific (10)The Atlantic Ocean will eventually catch to Pacific Ocean due to tectonic plate movement. At the meeting point of the the North American plate and the Eurasian plate, a rift creates new crust at its center which pushes the two plates apart, expanding the Atlantic Ocean. Tectonic Plate Movement: A small number of plates that independently float along the Earth's mantel. Rift: A long underwater zone of faulting resulting from tensional stress in the Earth s crust. A underwater valley formed from stress in the Earth's crust.
12 ANSWER The oceanic crust is constantly being created at the mid ocean ridge. It moves away, cools, and eventually sinks back into the Earth causing destruction. Destruction of the Oceanic Crust (Question 11: How is the oceanic crust destroyed?) (Academic Vocabulary Word): Oceanic Crust: The oceanic crust is the uppermost layer on the tectonic plates. (Academic Vocabulary Word): Mid Ocean Ridge: The mid ocean ridge is an underwater mountain range that is formed by plate tectonics.
13 plates: Plates are chunks of earth that constantly move around. rift: A Rift s Split 12. What happens at rifts? At rifts, magma rises from the mantle and forms new land which pushes back the old land from the plates. Rifts are in between two plates that has lava that comes out, forms new land, and pushes old land backward. Evidence: Magma from the rifts rise and push the plates backward and form new land. Reasoning: This evidence shows how the earth s always changing because when the plates get pushed back by magma, movement is happening, and at the same time, subduction zones take in the land that gets too old and sinks into the mantle.
14 Rifts- what happens at them? (Question #13) (Reword question in your answer. Use details.) Answer: At rifts, the molten rock comes up and it cannot be contained. Volcanoes show where some rock has risen to the surface Rifts: a crack of something or where something splits. They can come up on the land or on the ocean. Volcanoes : a mountain that holds magma and it sometimes erupts. Volcanoes mark spots where molten rock have risen to the surface in the past
15 Subduction Zone : A region of land on the Crust where two tectonic plates meet. Mantle: part of the earth between the core and the the crust Subduction Zones! (Question #14) What subduction zones? By: Casey Lin. ANSWER: When a large continent splits apart, the separate pieces move apart from each other. New land is created in between the two. Since Earth has a constant surface area, the same amount of land created must be absorbed and then melted in the mantle at the subduction zone.
16 (ONE PICTURE) Last Supercontinent Question #15 What Was The Last Supercontinent? The last supercontinent was called Pangaea. Pangaea looked like a combination of all major continents. Pangaea was formed when the previous supercontinent, Gondwana formed together with the landmass in the Northern Hemisphere. (Pangaea was located in the Southern Hemisphere.) (Plate Tectonics): Plate tectonics is the theory that earth s outer shell is divided into plates that glide over the mantle. (Supercontinent): A super continent is when 2 or more landmasses form together to create one large landmass, which is called a supercontinent. Supercontinent
17 Same fossils but different place? 16) What evidence is there that the United States and North Africa were once next to each other?: The evidence that the United States were once next to each other was that the same fossils were found but were far away from each other. The fossils were so closely related and similar that it couldn t have been that they were different specimens. This also shows the continental drift because they were once next to each other and then they drift apart from each other. ACADEMIC VOCABULARY: Continental Drift: Movement of continents across earth s surface over a long period of time Fossil: the remain of a prehistoric organism; an ancient artifact that scientists can use
18 Continental Plates: Colliding Plates 17. When two continental plates collide and neither are pushed back into the mantel, there is a battle for supremacy. The plates grind and smash into each other, and sometimes create mountains. Tectonic plates that lie under the earth s surface land masses. Mantel The part of the earth between the core and the crust.
19 Ocean rocks on top of the mountain (18#) Rocks that were once at the bottom of the ocean end up at the top of the Alps because when the plates tectonics bumped to each other then it created the mountain and picked up the rock that were on the bottom of the ocean (ONE PICTURE) (Academic Vocabulary Word): plates tectonics- a theory explaining the structure of the earth's crust and many associated phenomena as resulting from the interaction of rigid lithospheric plates that move slowly over the underlying mantle. (Academic Vocabulary Word): mountain-a large natural elevation of the earth's surface rising abruptly from the surrounding level
20 19 Missing
21 The Grand Canyon s Canyon. 20) The Grand Canyon came to be by first the formation of a great plateau very far above sea level. After millions of years, it was transformed by water erosion from the Rocky Mountains. The runoff streams joined to be what is now the Colorado River. Plateau: An area much like a mountain but with relatively vertical and straight sides and with a flat top. Erosion: The decay of materials by natural forces over a long period of time. By: Catherine Miller
22 (ONE PICTURE) Tectonic plates (Volcanoes) 21.Some volcanoes are created when a tectonic plate starts to slide under another plates, and when the pressure is so strong that it causes these underwater volcanoes to form. If the pressure is super strong it will start making a lot of small islands Two sub layers that are under the earth's crust that move Pressure A continuous physical force exerted on or against an object by something in contact with it
23 (ONE PICTURE) Volcanoes, Earthquakes, and tsunami Question 22: Earthquakes, Volcanoes, and tsunamis are all caused by tectonic plates moving and shoving each other. Volcanoes: mountains that shoot up lava when they erupt. Dormant: volcano that does not erupt anymore. The volcano is asleep.
Continental Drift. & Plate Tectonics
Continental Drift & Plate Tectonics Alfred Wegener, a German scientist, proposed the hypothesis of CONTINENTAL DRIFT, in 1912. Hypothesis stated: All Earth s continents were once a single landmass (Pangaea)
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 information22.4 Plate Tectonics. Africa
The Red Sea between Africa and the Arabian peninsula in Asia marks a region where two pieces of the lithosphere are slowly moving apart. Over the next 100 million years, the Red Sea could become an ocean.
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 informationGeologists are scientists who study Earth. They want to
What Is Inside Earth? Figure 1 Over time, the Grand Canyon in Arizona was carved out by the flowing water of the Colorado River. We can see that Earth s surface is constantly changing. But what is happening
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 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 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 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 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 informationContinental Drift and Plate Tectonics
Continental Drift and Plate Tectonics Continental Drift Wegener s continental drift hypothesis stated that the continents had once been joined to form a single supercontinent. Wegener proposed that the
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 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 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 informationI. Earth s Layers a. Crust: Earth s outside layer. Made of mostly rock. i. Continental: er; made of mostly granite, forms the continents and shallow
I. Earth s Layers a. Crust: Earth s outside layer. Made of mostly rock. i. Continental: er; made of mostly granite, forms the continents and shallow sea beds, floats! ii. Oceanic: er; dense rock such as
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 informationUNIT 11 PLATE TECTONICS
UNIT 11 PLATE TECTONICS A. ALFRED WEGENER 1. Continental drift hypothesis Single supercontinent called Pangaea 200 million years ago Pangaea (all land) began to break up and started drifting to their present
More informationEarth Movement and Resultant Landforms
Earth Movement and Resultant Landforms Structure of the Earth Lithosphere : earth s crust Asthenosphere : upper mantle zone where material is near its melting point & acts almost like liquid (appprox.
More informationEARTH S INTERIOR, EVIDENCE FOR PLATE TECTONICS AND PLATE BOUNDARIES
EARTH S INTERIOR, EVIDENCE FOR PLATE TECTONICS AND PLATE BOUNDARIES LAYERS OF THE EARTH Crust Inner Core Most Dense Solid Iron & Nickel Mantle Thickest layer Outer Core Liquid Iron & Nickel ANOTHER LOOK
More informationPrentice Hall EARTH SCIENCE
Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 9 Plate Tectonics 9.1 Continental Drift An Idea Before Its Time Wegener s continental drift hypothesis stated that the continents had once been joined
More informationPrentice Hall EARTH SCIENCE
Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 9 Plate Tectonics 9.1 Continental Drift An Idea Before Its Time Wegener s continental drift hypothesis stated that the continents had once been joined
More informationUnit 11: Plate Tectonics
Unit 11: Plate Tectonics A. Alfred Wegner 1. Continental drift hypothesis a. single supercontinent called Pangaea b. 200 million years ago Pangaea (all land) began to break up and started drifting to their
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. Chapter 8
Plate Tectonics Chapter 8 Vocabulary Crust Mantle Core Lithosphere Continental Drift Plate Tectonics Plate Boundary Fault What Are The Earth s Layers Made Of? Atmosphere: Contains nitrogen, oxygen, carbon
More informationExploring Inside the Earth
Plate Tectonics Exploring Inside the Earth Geologists have used evidence from rock samples and evidence from seismic waves to learn about Earth s interior. Geologists are scientists who study the forces
More informationPlate Tectonic Vocabulary Chapter 10 Pages
Name: Period: Plate Tectonic Vocabulary Chapter 10 Pages 239-260 Vocabulary Word What is this? What are some examples? What does it look like? (draw a picture or diagram) Continental drift Mid-ocean ridge
More informationCh 9.1 Notes. Objective: Be able to explain the theory of plate tectonics and be able to explain evidence that supports it.
Ch 9.1 Notes Objective: Be able to explain the theory of plate tectonics and be able to explain evidence that supports it. Pangaea Alfred Wegener proposed that land on Earth formed a single, huge landmass.
More informationIn 1912 Alfred Wegener proposed Continental Drift the continents have moved over time the continents were part of one giant landmass named Pangaea.
Plate Tectonics In 1912 Alfred Wegener proposed Continental Drift the continents have moved over time the continents were part of one giant landmass named Pangaea. Pangaea Landmass movements over millions
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 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 informationIn order to study Plate Tectonics, we must first
TB Chapter 13 In order to study Plate Tectonics, we must first reorganize our layering system for the Earth: Old System 4 layers Crust (rigid) id) (rigid) Mantle (putty like) (semi rigid) Outer core (liquid)
More informationTHE INTERNAL STRUCTURE OF THE EARTH
UNIT 1 THE INTERNAL STRUCTURE OF THE EARTH 1.1.Earth s interior layers The interior of the Earth can be divided into layers according to: -Composition layers ( organized in order of increasing density
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 information1. occurs when the oceanic crust slides under the continental crust.
1. occurs when the oceanic crust slides under the continental crust. 2. What type of stress is shown? 3. Where two plates slide past one another is called a boundary. 4. What type of stress is shown? 5.
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 informationChapter 7 Plate Tectonics. Plate tectonics accounts for important features of Earth s surface and major geologic events.
Chapter 7 Plate Tectonics Plate tectonics accounts for important features of Earth s surface and major geologic events. 7-2 Alfred Wegener s Hypothesis of Continental Drift (1915) He noticed that the continents
More informationUNIT 6 PLATE TECTONICS
UNIT 6 PLATE TECTONICS CONTINENTAL DRIFT Alfred Wegner proposed the theory that the crustal plates are moving over the mantle. He argued that today s continents once formed a single landmass, called Pangaea
More informationPlate Tectonics. These icons indicate that teacher s notes or useful web addresses are available in the Notes Page.
Plate Tectonics These icons indicate that teacher s notes or useful web addresses are available in the Notes Page. This icon indicates the slide contains activities created in Flash. These activities are
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 informationDirected Reading. Section: Continental Drift. years ago? WEGENER S HYPOTHESIS
Skills Worksheet Directed Reading Section: Continental Drift 1. Who obtained new information about the continents and their coastlines 400 years ago? 2. What did people notice when they studied new world
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 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 informationDirected Reading. Section: The Theory of Plate Tectonics. to the development of plate tectonics, developed? HOW CONTINENTS MOVE
Skills Worksheet Directed Reading Section: The Theory of Plate Tectonics 1. The theory that explains why and how continents move is called. 2. By what time period was evidence supporting continental drift,
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 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 information05/22/15. Tectonic plate (Noun) Plate tectonics (Noun) Oceanic crust/plate (Noun) Continental crust/plate (Noun) Continental drift (Noun)
Tectonic plate (Noun) The pieces of the Earth s crust that float on the mantle, causing continental drift and earthquakes and creating volcanoes, trenches, and mountains. The Earth s crust is divided into
More informationIn the space provided, write the letter of the definition that best matches the term or phrase.
Skills Worksheet Directed Reading Section: The Changing Continents 1. What is the result of slow movements of tectonic plates? RESHAPING EARTH S CRUST In the space provided, write the letter of the definition
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 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 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 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 information1.4 Notes: Plates Converge or Scrape Past Each Other Think About Tectonic Plates Push Together at Convergent Boundaries
1.4 Notes: Plates Converge or Scrape Past Each Other Think About If new crust is created at divergent boundaries, why does the total amount of crust on Earth stay the same? Tectonic Plates Push Together
More informationCHAPTER 9. Basics Of geology: earthquakes & volcanoes
161 CHAPTER 9 Basics Of geology: earthquakes & volcanoes CHAPTER s Objectives To introduce the theory of one supercontinent To discuss the clues and proofs that support the theory of one supercontinent
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 informationMoving Plates: Restless Earth
Name Date Moving Plates: Restless Earth 1-9 Read the paragraphs and write the word that completes the sentence correctly. fossils mantle continent supercontinent plates motion ontinental Drift Plate Tectonics
More informationChapter 7 Plate Tectonics. Plate tectonics accounts for important features of Earth s surface and major geologic events.
Chapter 7 Plate Tectonics Plate tectonics accounts for important features of Earth s surface and major geologic events. 7-2 Alfred Wegener s Hypothesis of Continental Drift (1915) ONE single landmass
More informationSUBSURFACE CHANGES TO EARTH. Ms. Winkle
SUBSURFACE CHANGES TO EARTH Ms. Winkle OVERVIEW Subsurface events: occurring inside the crust and mantle Moving the lithosphere due to the convection currents in the asthenosphere Main Theories: 1912 Wegener,
More informationUnit 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 informationPLATE TECTONICS. SECTION 17.1 Drifting Continents
Date Period Name PLATE TECTONICS SECTION.1 Drifting Continents In your textbook, read about continental drift. Circle the letter of the choice that best completes each statement. 1. Early mapmakers thought
More informationChapter 5 Notes: Plate Tectonics
Chapter 5 Notes: Plate Tectonics Earth s Interior Scientists learn about the interior of Earth in 2 ways o Direct Method Rock Samples Drilling Caves o Indirect Method Seismic Waves Speed of waves and paths
More information4 Layers of the earth 7 main plates of the earth 3 main plate boundaries 2 types of crust 3 main features of plate tectonics 3 main theorists and
4 Layers of the earth 7 main plates of the earth 3 main plate boundaries 2 types of crust 3 main features of plate tectonics 3 main theorists and theories Human interaction The Earth is made up of 3 main
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 informationSection 1: Continental Drift
Plate Tectonics Section 1 Section 1: Continental Drift Preview Key Ideas Wegener s Hypothesis Sea-Floor Spreading Paleomagnetism Wegener Redeemed Continental Drift (Pangaea) Plate Tectonics Section 1 Key
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 informationEarth Systems, Structures and Processes
Earth Systems, Structures and Processes Date: 6.E.2 Understand the structure of the earth and how interactions of constructive and destructive forces have resulted in changes in the surface of the Earth
More informationPlate Tectonics Unit II: Plate Boundaries (3.5 pts)
T. James Noyes, El Camino College Plate Tectonics Unit II: The Plate Boundaries (Topic 11A-2) page 1 Name: Section: Plate Tectonics Unit II: Plate Boundaries (3.5 pts) Plate Boundaries We will now discuss
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 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 informationSCIENCE IN THE NEWS Plate Tectonics
SCIENCE IN THE NEWS Plate Tectonics From VOA Learning English, this is Science in the News. I m Anna Matteo. And I m Christopher Cruise. Scientists who study the Earth tell us the continents and ocean
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 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 informationUNIT 3 GEOLOGY VOCABULARY FLASHCARDS THESE KEY VOCABULARY WORDS AND PHRASES APPEAR ON THE UNIT 3 CBA
UNIT 3 GEOLOGY VOCABULARY FLASHCARDS THESE KEY VOCABULARY WORDS AND PHRASES APPEAR ON THE UNIT 3 CBA A map that shows Earth s Topographic Map surface topography, which is Earth s shape and features Contour
More informationDo Now: Vocabulary: Objectives. Vocabulary: 1/5/2016. Wegener? (Can they move?) the idea that continents have moved over time?
Do Now: 1. Who was Alfred Wegener? 2. What was Pangaea? 3. Are continents fixed? (Can they move?) 4. What evidence supports the idea that continents have moved over time? Objectives What evidence suggests
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 informationChanging Earth: Plate Tectonics
Changing Earth: Plate Tectonics Static Earth Theory People used to believe that the Earth and its continents could not change since it was created They thought that earthquakes and volcanoes were caused
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 information10/27/2014. Before We Begin, You Need to Understand These Terms: Earth s Structural Key Elements & the Hazards of Plate Movement
Earth s Structural Key Elements & the Hazards of Plate Movement Before We Begin, You Need to Understand These Terms: Density Convection Currents AICE EM: Lithosphere Key Content 1 & 2 Density: heat rises,
More informationDiscusssion / Activity 1 Suggested Answers. INSPECTION COPY for schools only
Earth Structure Discusssion / Activity 1 Suggested Answers 1. Clearly label the diagram to show the main layers of the Earth. 2. What is the lithosphere? The lithosphere is the crust, plus a thin part
More informationPlate Tectonics: A Scientific Revolution Unfolds
Chapter 2 Lecture Earth: An Introduction to Physical Geology Eleventh Edition Plate Tectonics: A Scientific Revolution Unfolds Tarbuck and Lutgens From Continental Drift to Plate Tectonics Prior to the
More informationdeep within the planet. They are also shaped by conditions on the planet s surface. In
Chapter 4 Landforms, Water, and Natural Resources Earth is home to many different types of landforms. These landforms are shaped by forces deep within the planet. They are also shaped by conditions on
More informationPlate Tectonics. Essentials of Geology, 11 th edition Chapter 15
1 Plate Tectonics Essentials of Geology, 11 th edition Chapter 15 2 3 4 5 6 7 8 9 10 11 12 13 14 15 Plate Tectonics: summary in haiku form Alfred Wegener gave us Continental Drift. Fifty years later...
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 informationCh 17 Plate Tectonics Big Idea: Most geologic activity occurs at the boundaries between plates.
Ch 17 Plate Tectonics Big Idea: Most geologic activity occurs at the boundaries between plates. 17.1 Drifting Continents 17.2 Seafloor Spreading 17.3 Plate Boundaries 17.4 Causes of Plate Motions Learning
More informationSeafloor spreading is a geologic process in which tectonic plates large slabs of Earth's lithosphere split apart from each other.
This website would like to remind you: Your browser (Apple Safari 4) is out of date. Update your browser for more security, comfort and the best experience on this site. Encyclopedic Entry seafloor spreading
More informationSlow and Steady By ReadWorks
By ReadWorks How did all the amazing things on our planet form? How did magnificent mountain ranges rise up in one place and beautiful beaches form elsewhere? Why do some places experience earthquakes
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 informationBeneath our Feet: The 4 Layers of the Earty by Kelly Hashway
Beneath our Feet: The 4 Layers of the Earty by Kelly Hashway The Earth is more than a giant ball made up of dirt, rocks, and minerals. The Earth may look like a giant ball from when looking at it from
More informationPlate Tectonics. Earth has distinctive layers - Like an onion
Plate Tectonics Earth has distinctive layers - Like an onion Earth s Interior Core: Metallic (Iron, Nickel) Inner (hot, solid, dense, Iron, Nickel) Outer (cooler, liquid, less dense) Crust (outermost layer):
More informationPlate Tectonics. Chapter 5
Plate Tectonics Chapter 5 Earth s Interior Scientists learn about the interior of Earth in 2 ways Direct Method Rock Samples Drilling Caves Earth s Interior Indirect Method Seismic Waves Speed of waves
More informationLecture Outline Friday January 12 Friday January 19, 2018
Lecture Outline Friday January 12 Friday January 19, 2018 Questions?? Key Points for today The structure of the Earth Introduction to Plate Tectonic Theory and Convection Chapter 2 Development of the Plate
More informationScience in the News - Plate Tectonics 1. Story
Science in the News - Plate Tectonics 1. Story Scientists who study the Earth tell us the continents and ocean floors are always moving. This movement sometimes can be violent, causing death and destruction.
More informationMohorovicic discontinuity separates the crust and the upper mantle.
Structure of the Earth Chapter 7 The Earth is divided into 3 Main Layers 1. Crust outermost layer 1% of the Earth s mass thickness varies: 5 100 km two types: oceanic denser continental Mohorovicic discontinuity
More informationSection 2: How Mountains Form
Section 2: How Mountains Form Preview Objectives Mountain Ranges and Systems Plate Tectonics and Mountains Types of Mountains Objectives Identify the types of plate collisions that form mountains. Identify
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 informationPlate Tectonics: The New Paradigm
Earth s major plates Plate Tectonics: The New Paradigm Associated with Earth's strong, rigid outer layer: Known as the lithosphere Consists of uppermost mantle and overlying crust Overlies a weaker region
More informationForces That Shape Earth. How do continents move? What forces can change rocks? How does plate motion affect the rock cycle?
Forces That Shape Earth How do continents move? What forces can change rocks? How does plate motion affect the rock cycle? Plate Motion Mountain ranges are produced by plate tectonics. The theory of plate
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* If occurs, fossils that formed in shallow water may be found in water. Subsidence mean the crust is.
Name Notes: Topic 5B Topic 5B: The Dynamic Crust A. What evidence exists that proves the Earth s Crust is and has moved? Earth Science 1. Tilted, folded or faulted strata Strata is a term that refers to.
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 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 information