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Earth and Plate Tectonics Online Workshop Booklet Dynamic Earth Science The Earth and plate tectonics Workshop prepared by: Paul Baggaley, Susan Beale, Dee Edwards, Peter Kennett, Phillip Murphy, Dave Turner, Royanne Wilding Edited by: Chris King, Susie Lydon, Cally Oldershaw, Peter Kennett and Hazel Benson © The Earth Science Education Unit Copyright is waived for original material contained in this booklet if it is required for use within the laboratory or classroom. Copyright material contained herein from other publishers rests with them. Every effort has been made to locate and contact copyright holders of materials included in this document in order to obtain their permission to publish them. Please contact us if, however, you believe your copyright is being infringed: we welcome any information that will help us to update our records. If you have any difficulty with the readability of these documents, please contact the Earth Science Education Unit for further help. The Earth Science Education Unit email: [email protected] ESEU KS4 Workshops: The Earth and Plate Tectonics Contents Workshop outcomes ....................................................................................................................... 2 The Story for Teachers: Plate Tectonics ......................................................................................... 3 The big picture and the ‘facts’ of plate tectonics .............................................................................. 4 Continental Jigsaws ........................................................................................................................ 5 Model Earth – Plasticine™ spheres .............................................................................................. 10 From Magnetic Globe to Magnetic Rock Evidence ........................................................................ 11 Geobattleships .............................................................................................................................. 14 The earthquake distribution evidence ............................................................................................ 17 Earthquakes - the slinky simulation ............................................................................................... 18 Wave Motion – student molecules ................................................................................................ 19 The seismic evidence for the structure of the Earth ....................................................................... 21 Why are the Earth’s tectonic plates called plates? ........................................................................ 23 Properties of the Mantle – potty putty™ ........................................................................................ 24 The heat flow evidence ................................................................................................................. 26 Evidence from the age of the sea floor .......................................................................................... 27 Constructive plate margins - adding new plate material ................................................................ 28 Faults in a Mars™ Bar .................................................................................................................. 29 The magnetic stripes evidence...................................................................................................... 31 Destructive plate margins - recycling material ............................................................................... 34 Partial Melting ............................................................................................................................... 35 Volcano in the Lab ........................................................................................................................ 37 Plates in Motion – cardboard replica ............................................................................................. 39 Fold Mountains in a Chocolate Box ............................................................................................... 42 Rate of Plate Movement ................................................................................................................ 43 Plate Riding – how is the plate you live on moving now? .............................................................. 44 Prediction of Earthquakes – ‘Brickquake’ ...................................................................................... 45 Tsunami – making waves .............................................................................................................. 49 How to survive an earthquake ....................................................................................................... 50 Bulging Volcanoes ........................................................................................................................ 51 How Predictable are Volcanic Eruptions? – party popper simulation ............................................. 52 Resource List ................................................................................................................................ 53 Teaching points of ESEU Workshop activities ............................................................................... 56 Risk Assessments ......................................................................................................................... 59 Summary ‘The Earth and Plate Tectonics’ workshop gets to grips with the wide-ranging evidence for the theory that underpins our detailed modern understanding of our dynamic planet – the theory of Plate Tectonics. The workshop begins with an introduction and progresses through a series of activities that are designed to help students develop their understanding. It uses several independent sources of evidence supporting the theory, including using rock and fossil evidence, seismic records, geothermal patterns, geomagnetism, and large-scale topographical features, both above and below sea-level. The workshop provides a reconstruction of plate movements over the past 450 million years which explains the record contained in the rocks of the UK - of an amazing journey across the face of our planet. It concludes by investigating some of the Earth hazards linked to plate tectonics, and how we can reduce loss of life. 1 V.Mar 12 © The Earth Science Education Unit http://www.earthscienceeducation.com KS4 Workshops The Earth and Plate Tectonics Workshop outcomes The workshop and its activities provide the following outcomes: • an introduction to plate tectonics; • distinction between the ‘facts’ of plate tectonics and the evidence used to support plate tectonic theory; • a survey of some of the evidence supporting plate tectonic theory; • an introduction to the evidence for the structure of the Earth and the links between the structure of the outer Earth and plate tectonics; • explanation of some of the hazards caused by plate tectonic processes - earthquakes and eruptions; • methods of teaching the abstract concepts of plate tectonics, using a wide range of teaching approaches, including practical and electronic simulations; • approaches to activities designed to develop the thinking and investigational skills of students; • an integrated overview of the plate tectonic concepts commonly taught to secondary pupils. 2 V.Mar12 © The Earth Science Education Unit http://www.earthscienceeducation.com KS4 Workshops The Earth and Plate Tectonics The Story for Teachers: Plate Tectonics Plate Tectonics If you could sit in space and study the Earth you Some plates carry continents and if a plate is might see some strange patterns through the subducted beneath a continent, a trench, swirls of cloud. Many of the mountains are found volcanoes and earthquakes are formed but the in long chains; many of the islands form long base of the continent is also partially melted curved chains; the coastline of South America fits producing magma very rich in silica and very the coast of Africa almost exactly. If you could viscous. This rarely reaches the surface but probe beneath the oceans, more patterns would usually forms large igneous bodies within the be revealed: there is a long ridge of mountains continent that cool slowly, baking and near the centres of most oceans and there are metamorphosing the surrounding rock. The slow- often deep sea trenches near island chains. cooling magma forms the coarse silica-rich rock called granite. If the silica-rich magma does reach These patterns and more can be explained by the surface it forms highly explosive volcanoes. plate tectonics. The evidence from earthquake The two converging plates also crumple up the waves shows that the outer part of the Earth is layered sediments and sedimentary rocks into made of a thin rigid sheet of lithosphere that is mountain chains, causing compressional faulting, broken into pieces called plates. Beneath the folding and metamorphosing. If both plates carry lithosphere is a thin layer called the continents, the collision is even more intense and asthenosphere where earthquake waves are highest mountain ranges on Earth can be slowed down by small pockets of molten rock. The produced as the continents are ‘welded’ together rock was melted by the heat produced from the by the new mountain chain rocks. decay of radioactive isotopes. The heat causes the mainly solid asthenosphere to flow plastically Earthquake waves show the structure of the in convection currents and these currents carry whole Earth. The
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