Sinking Slabs and Convection Connections

Slides:



Advertisements
Similar presentations
Warm Up 11/26 The Hawaiian Islands were formed when the Pacific Plate moved over ____. a. a hot spot c. the Aleutian Plate b. a subduction zone d.
Advertisements

Unit 1 Physical Geography: The Restless Earth Unit Lessons Why is the earth’s crust so unstable? What happens at plate margins? How are our highest and.
Section 17.4 Causes of plate motion
EQ: What is the theory of plate tectonics?
Structure of the Earth Crust = solid outermost layer Mantle = middle layer Core = inner layer outer core = liquid inner core = solid.
Earth’s Geology – 3 primary layers Core, Mantle, and Crust Inner core is solid metal (iron and nickle) Outer Core is molten metal Rocky mantle (solid.
Volcanoes and Plate Tectonics
 Composition: Silicon, Oxygen, and Aluminum  Types: › Continental Crust: solid & rocky outer layer › Oceanic Crust: thin & dense material.
Plate tectonics volcanoes EEn Explain how plate tectonics, and volcanoes impact the lithosphere. I. Plate Tectonics Chapter 9, Section 2 A. Actions.
Plate Tectonics Earth’s Interior Convection and the Mantle Drifting Continents Sea-Floor Spreading The Theory of Plate Tectonics Table of Contents.
Chapter 8 Volcanoes Section 1, Why Volcanoes Form
Section 1: Volcanoes and Plate Tectonics
Meteor Crater, Arizona 1.2 kilometers (0.7 miles) 40,000 years old.
EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens 
The Theory of Plate Tectonics Earth’s crust is made of many ________ These plates move as a result of ______________ in the mantle Earth’s surface is.
LESSON Essential Questions 7.3 The Theory of Plate Tectonics What is the theory of plate tectonics? What are the three types of plate boundaries? What.
Warm Up 11/5 Why are subduction zones not commonly found at convergent continental-continental boundaries? a. Oceanic lithosphere is too buoyant to be.
Essential Question: How does the constant movement of lithospheric plates cause major geological events on the earth’s surface? Standard: S6E5e. Recognize.
9.3 Theory of Plate Tectonics. I. Earth’s Moving Plates A.Earth’s crust is broken into LARGE pieces called “plates” 1.Plates contain continents and oceans.
12.2 Features of Plate Tectonics. OVERVIEW There is lots of evidence that the Earth’s interior is NOT simply a solid ball of rock:  Earthquakes  Volcanoes.
Theory of Plate Tectonics Chapter 10.3 pg SPI
Intro Objective 10/15/12 Describe the three forces thought to move tectonic plates. Pick up worksheet from front table. Weekly Worksheet #8: What do you.
Plate Tectonics EARTH STRUCTURE & HEAT LAYERS OF THE EARTH CRUST MANTLE OUTER CORE INNER CORE.
EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens 
Shaping the Face of Earth – The Lithosphere We are going to focus on the Lithosphere Lithosphere: the layer of earth that contains the earth's crust, Tectonic.
Plate Tectonics Earth Science Chapter 9. Continental Drift  scientific theory proposing the slow, steady movement of Earth’s continents  Alfred Wegener:
THE MECHANISMS OF PLATE MOTION
The Theory of Plate Tectonics Chapter 14 Lesson 3 p
Plate Tectonics Chapter 17.  All of the phenomena that we will discuss in the upcoming weeks are all a result of plate tectonics.  Plate Tectonics is.
BC Science Connections 8
Plate Tectonics Earth Science.
Handout 1 Standard 2, Objective 3
Cause, Effect and Evidence
Convection currents in the mantle result in the movement of lithospheric plates. The motion and interactions of the plates can create patterns in the.
Plate Tectonics.
Plate Tectonics.
8.E.5B.1 Analyze and interpret data to describe patterns in the location of volcanoes and earthquakes related to tectonic plate boundaries, interactions,
Plate Tectonics.
A new theory that combined continental drift and seafloor spreading was developed known as the theory of Plate Tectonics.
Chapter 8 Volcanoes Section 1, Why Volcanoes Form
Handout 3 Standard 2-2 Plate Tectonics.
Mid Ocean Ridge.
Continental Drift to Plate Tectonics: From hypothesis to theory
What is the evidence for Plate Tectonics?
The Theory of Plate Tectonics
Theory of Plate Tectonics
PLATES AND TECTONIC MOVEMENT
9-3 Theory of Plate Tectonics
TRANSFORM BOUNDARIES Transform
The Big Crack Up!.
OBJECTIVE: Explain the theory of Plate Tectonics.
9-4 Mechanisms of Plate Motion
Continental Drift.
Volcanoes and Plate Tectonics
9.5 – Mechanisms of Plate Motion
Plate Tectonics The theory that the Earth’s outermost layer is fragmented into a dozen or more large and small plates that move relative to one another.
Chapter 9 Plate Tectonics.
Mechanisms of Plate Motion
Plate Tectonics How do the plates move?.
TESTING PLATE TECTONICS
Theory of Plate Tectonics
In this presentation you will:
2. Evidence of Plate Tectonics
Theory of Plate Tectonics (Part 1)
Theory of Plate Tectonics (Part 1)
Other Notes on Earth’s Changing Surface
5% of all known volcanoes in the world are not located close to a plate margin. These are known as intraplate volcanoes and occur as a result of mantle.
The Unifying Theory of Earth Science
The Theory of Plate Tectonics
Ch – 15 Plate Tectonics II.
Presentation transcript:

Sinking Slabs and Convection Connections Explore: p. 672 - 678

I can use simple models to simulate the forces acting on tectonic plates. I can compare directions of plate motions with locations of hot spots, spreading ridges, and trenches I can determine the velocity of the North American Plate relative to the Yellowstone hot spot I can examine the depth-distance relationship for earthquakes in a subduction zone. Learning Targets

What do you remember about the relationship between density and temperature from IS1? What happens to the density of a substance as it is heated? What happens to the density of a substance as it cools? How do differences in density cause substances to rise or fall? Entry Task

Process & Procedure p. 672 Read Introduction on pg. 672 #1. Video Demo #1a. – d. Answer in your science notebook. Process & Procedure p. 672

2. Read the paragraph. Take notes on anything that is new to you – especially vocabulary: mantle, plume, upwelling, hot spots, mantle convection. 3. Which part of your sketch represents upwelling? Downwelling?. Process & Procedure p. 672

Mantle – the layer of Earth that lies beneath Earth’s crust. Plume – a rising column of heat. Plumes occur in the mantle where hot material moves upward from the lower mantle, in some cases, to erupt at Earth’s surface. Upwelling – refers to the upward motion of material in plumes through the mantle. Process & Procedure p. 672

hot spots – outpouring of molten rock (lava) at volcanoes caused by plumes of heat rising from Earth’s core through the mantle. Mantle convection – the slow movement of the mantle due to upwelling and sinking. The circular motion of the mantle as it transports hot material and heat upward, and then transports cooled material downward. The hot material is lower in density, so it rises. The colder material is higher in density and sinks. Process & Procedure p. 672

Process & Procedure p. 672 Video Convection & Plate Tectonics Video Hotspots Animation Slab Pull Process & Procedure p. 672

If plate motion is driven by mantle convection and upwelling, then plates should be moving __________ from hot spots. B. If plate motions is only driven by plates being pulled, then plates should be moving ________ subduction zones. Process & Procedure #6

Complete P&P #7 a-e with your partner Complete P&P #7 a-e with your partner. Use specific examples in your explanations! Process & Procedure #7

P&P #7 7b. About 53 hotspots are shown. 7c. In general, plates pass over hot spots. There is little, if any, correlation between hot spots and plate direction. For a relatively small number of hot spots on spreading ridges, the plate moves away from the hot spots (e.g., Iceland, Galapagos, or Afar at the base of the Red Sea). Many more are distributed beneath oceanic plates or continents. Geologic evidence indicates that those hot spots are generally relatively stationary for tens of millions of years (although detailed recent work shows that they can at times drift or migrate through the mantle). P&P #7

7d. Plates move towards subduction zones 7d. Plates move towards subduction zones. For example, the Pacific Plate has a rapid velocity to the northwest toward the Japan and Aleutian trenches. Also, the Australian-Indian Plate is being subducted at the Java Trench, which led to the Andaman-Sumatra earthquake and tsunami in December 2004. Closer to home, the Juan de Fuca Plate is being subducted beneath the Cascadian volcanic arc. P&P #7

7e. From a strict correlation point of view, plate motions do not correlate well with the location of hot spots. Hot spots indicate upwelling and convection in the mantle. This suggests that convection by itself is not a sufficient explanation for plate tectonic motions. Thus, the “pull” of oceanic crust entering subduction zones correlates much better with the direction of plate motions, and the tectonic patterns and landforms on Earth’s surface. P&P #7

R&C #1 p. 676 1a. What part of the world is shown? 1b. What tectonic plates are included in the figure? 1c. What is the relationship between earthquakes and depth? 1d. What kind of tectonic setting is shown by the pattern of earthquakes? R&C #1 p. 676

1e. Sketch in your science notebook where earthquakes occur along this line. What does the depth of the earthquakes indicate? R&C #1 p. 676

R&C #2-3 p. 676 Complete R&C #2 and 3. Remember to use graph paper for your graph! Read “Shakin’ Like Jell-O” Earthquake proof building R&C #2-3 p. 676