Processes and 2, 3 and 4 mark questions

Slides:



Advertisements
Similar presentations
The main physical features of the Earth. 1 Atlantic Ocean Indian Ocean Pacific Ocean Southern Ocean North America South America Africa Europe Asia Oceania.
Advertisements

Chapter 7 Plate Tectonics
Chapter 7: Plate Tectonics
PLATE TECTONICS Chapter 7 – Inside the Restless Earth
Plate boundaries LO: to be able to explain what happens when plates meet.
Plate boundaries LO: to be able to explain what happens when plates meet.
Why does Earth have mountains?
Have a seat with your lab group and get out your papers that you completed in class yesterday. Today’s Schedule 1. Review Yesterday’s Assignment 2. Review.
Tectonic Activity Plates. –Tectonic Plates –Convection Currents –Destructive Plate Boundaries –Constructive Plate Boundaries –Conservative Plate Boundaries.
Journey to the Center of Earth
Plate Tectonics. Objectives Describe and draw the internal workings of the earth Describe and draw the internal workings of the earth Explain the structure.
Earth Materials – Geology Plate tectonics Why have all the mountains not worn away by now? 100’s of free ppt’s from library
Warm-Up Find the mistakes!
The Structure of the Earth and Plate Tectonics. Structure of the Earth The Earth is made up of 3 main layers: –Core –Mantle –Crust Inner core Outer core.
Plate Tectonics. The Structure of the Earth A thin crust km thick A mantle – has the properties of a solid but it can also flow A core – made.
Theory of Plate Tectonics Plate Tectonics Plate Boundaries Causes of Plate Tectonics.
Plate Boundary Volcanism Reference: Tarbuck and Lutgens Pages Volcanoes are associated with two of the three types of plate boundaries, these.
Theory of Plate Tectonics
1 Plate Tectonics 5 November 2015 Chapter 17 Great Idea: The entire Earth is still changing, due to the slow convection of soft, hot rocks deep within.
Convection Current in the Mantle SAYRO PAW. The Four Layers of Earth Inner Core Outer Core Mantle Crust The inner core is the hottest layer in the Earth.
Theory of Plate Tectonics Chapter 10.3 pg SPI
1 The Theory of Plate Tectonics Earth’s Interior and Surface Plate Movements n Chapter 13 – n Time for Change The guy who started it all: Alfred Lothar.
 In 1912, German scientist Alfred Wegener proposed the idea of continental drift.  Based on evidence he saw, he believed that the continents must have.
Features of Plate Boundaries
Plate Tectonics the movement of Earth.
Plate Tectonics Ocean Floor Earth Layers Potpourri
Chapter 8 Earth Systems and Resources.  Core - the innermost zone of the planet made of nickel and iron.  Mantle - above the core containing magma 
Plate Movement Chapter 17 Section 3. Plate Tectonics Theory that describes how tectonic plates move and shape Earth’s surface –They move in different.
The Theory of Plate Tectonics Chapter 14 Lesson 3 p
Section 1: Earth’s Interior and Plate Tectonics
Journey to the Center of Earth
Section 2: The Theory of Plate Tectonics
LAYERS OF THE EARTH PLATE BOUNDARIES PLATE TECTONICS CONTINENTAL DRIFT
Section 11-3 What is the theory of plate tectonics?
Continental Drift Theory
Plate Tectonics - Part A - Theory of Plate Tectonics
Plate Tectonics The crust in motion.
Earth Materials – Geology Plate tectonics
Handout 3 Standard 2-2 Plate Tectonics.
Geology Notes Part 6.
Oreo plate tectonics.
Continental Drift Theory
2 Plate Tectonics.
Boundaries, Stresses, and Faults OH MY!
Earth’s Layers Three main layers Crust, Mantle, and Core
TODAY: Fill in the blanks-Plate Tectonics Worksheet
Layers of the Earth & Plate Boundaries
On a separate sheet of paper:
The Tectonic Plates L.O – To be able to name the different types of plate boundaries and explain how they shape the Earth’s surface.
Science Starter: THUR WEEK 5
Continental Drift to Plate Tectonics: From Hypothesis to Theory
Go through and highlight important information.
The Earth’s Fractured Surface
Year 3 Revision for test on tectonics
Oreo plate tectonics.
Plate Tectonics L.O: To know about different plate margins and what happens when they push together or move apart.
To understand why the earth’s structure is always changing
Revision Year 3 Test 2 Semester A
Boundaries, Stresses, and Faults OH MY!
Chapter 7 Plate Tectonics
Theory of Plate Tectonics (Part 1)
I-4 & I-5 Flashcards.
Theory of Plate Tectonics (Part 1)
Jeopardy Phillips Prep.
Types of plate margin There are 2 types of crust:
Boundaries, Stresses, and Faults OH MY!
Welcome to (insert name) class.
Earth Science Plate Tectonics Chapter 12.
Volcanoes – see separate sheet for more information
Presentation transcript:

Processes and 2, 3 and 4 mark questions Restless Earth Processes and 2, 3 and 4 mark questions We will be turning our books into revision guides. Glue in contents sheet showing which topics and case studies we will be doing. Glue onto the front of your book. For now just do the Restless Earth Section. We will call this Chapter 1!

Processes Do you know your layers? Play until 2.38. Then it moves on to convection currents and plate movement.

Convection currents Draw a diagram to show how they work. Convection currents in the magma drive plate tectonics. Heat generated from the radioactive decay of elements deep in the interior of the Earth creates magma (molten rock) in the asthenosphere. The asthenosphere (70 ~ 250 km) is part of the mantle, the middle sphere of the Earth that extends to 2900 km. Convection currents Draw a diagram to show how they work. Can you explain? Large convection currents in the asthenosphere transfer heat to the surface, where plumes of less dense magma break apart the plates at the spreading centers, creating divergent plate boundaries. As the plates move away from the spreading centers, they cool, and the higher density basalt rocks that make up ocean crust get consumed at the ocean trenches/subduction zones. The crust is recycled back into the asthenosphere.

Plate Boundaries It all starts with Alfred Wegener’s theory of continental drift. Plates move! Can you name some plates? Play from 2.50 Can you describe what happens? The most important is to be able to explain why volcanoes and earthquakes happen at each boundary. Could you give an example of each?

Explain why volcanoes occur at CONSTRUCTIVE or DESTRUCTIVE plate margins. Usually a 4 or 6 mark question. Possibly with a diagram. Oceanic crust Continental crust Key words to use would be CONVECTION CURRENTS SUBDUCT and sequence your answer! Firstly….and then….

You may also be asked why earthquakes happen at specific plate margins. Key word CONVECTION CURRENTS, FRICTION and PRESSURE released. Sequencing and explain. Use the train… FIRSTLY,.....secondly, and then….

With the aid of a diagram explain the formation of... What about a composite cone? http://study.com/academy/lesson/what-is-a-shield-volcano-definition-facts-examples.html

Explain how young fold mountains are formed. The formation of fold mountains Where an area of sea separates two plates, sediments settle on the sea floor in depressions called geosynclines. These sediments gradually become compressed into sedimentary rock. When the two plates move towards each other again, the layers of sedimentary rock on the sea floor become crumpled and folded. Eventually the sedimentary rock appears above sea level as a range of fold mountains. Again don’t forget to use sequencing! Firstly.. Where the rocks are folded upwards, they are called anticlines. Where the rocks are folded downwards, they are called synclines. Severely folded and faulted rocks are called nappes.

Lets have a go at some questions. Complete the paragraph below to explain why earthquakes happen at conservative plate margins (4 marks) At conservative plate boundaries, plates move .................................. each other. They .................................. each other. The plates often stick and .................................. builds up. The sudden release of the plates causes a .................................. movement and an earthquake occurs. Draw a labelled diagram to explain why earthquakes occur at conservative plate margins. (6 marks)

Are the following statements about continental crust and oceanic crust true or false? (3 marks) Oceanic crust can be destroyed T or F Oceanic crust is generally lighter than continental crust T or F Continental crust is generally older than oceanic crust T or F Give 2 differences between continental and oceanic crust. (2 marks)

3) Explain how volcanoes form at constructive plate margins. (4 marks) 4) Outline how the Richter scale is used to measure earthquakes. (3 marks) 5) What is the difference between the focus and epicentre of an earthquake? (2 marks) 6) Outline the characteristics of a shield volcano (3 marks) 7) Explain the formation of a composite volcano (4 marks)