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Volcanoes – Part 1: Introduction 1 of 35 © Boardworks Ltd 2006 Learning objectives What is a volcano? Why do volcanoes occur? What happens when a volcano erupts? 2 of 35 © Boardworks Ltd 2006 What is a volcano? A volcano is an opening or vent in the earth’s surface through which molten material erupts and solidifies as lava. Volcanic vent 3 of 35 © Boardworks Ltd 2006 Label this cross section of a volcano Volcanic bombs, ash, lava, gases Magma chamber Secondary cone Crater Main vent 4 of 35 © Boardworks Ltd 2006 Cross section of a volcano Crater Volcanic bombs, ash and gases Secondary cone Main vent Magma chamber 5 of 35 © Boardworks Ltd 2006 Cross section of a volcano 6 of 35 © Boardworks Ltd 2006 Volcanic emissions 7 of 35 © Boardworks Ltd 2006 Volcanic emissions 8 of 35 © Boardworks Ltd 2006 Do all volcanoes erupt? Active volcano – liable to erupt e.g. Mt Etna. Dormant (sleeping) volcano – a volcano which has not erupted for many years. For example, Mt Pinatubo erupted in 1991 after 500 years of dormancy. Extinct volcano – a volcano which has not erupted for many thousands or millions of years e.g. Edinburgh. However, it is often very difficult to tell whether a volcano will erupt again…El Chichon, Mexico erupted in 1982 after being dormant for approximately 1200 years! 9 of 35 © Boardworks Ltd 2006 Learning objectives What is a volcano? Why do volcanoes occur? What happens when a volcano erupts? 10 of 35 © Boardworks Ltd 2006 Why do they happen? A destructive plate boundary is found where a continental plate meets an oceanic plate. The oceanic plate descends under the continental plate because it is denser. As the plate descends it starts to melt due to the friction caused by the movement between the plates. This melted plate is now hot, liquid rock (magma). The magma rises through the gaps in the continental plate. If it reaches the surface, the liquid rock forms a volcano. 11 of 35 © Boardworks Ltd 2006 Destructive plate boundary 12 of 35 © Boardworks Ltd 2006 Destructive plate boundary 13 of 35 © Boardworks Ltd 2006 Destructive plate boundary 14 of 35 © Boardworks Ltd 2006 Why do they happen? At a constructive plate boundary, two plates move apart. As the two plates move apart, magma rises up to fill the gap. This causes volcanoes. However, since the magma can escape easily at the surface, the volcano does not erupt with much force. 15 of 35 © Boardworks Ltd 2006 Constructive plate boundary 16 of 35 © Boardworks Ltd 2006 Constructive plate boundary 17 of 35 © Boardworks Ltd 2006 Constructive plate boundary 18 of 35 © Boardworks Ltd 2006 Types of Volcanoes Volcanoes are divided into three main types depending upon the material thrown out in an eruption 1. Composite Cone Volcano (ex. Mount St. Helens, Mount Etna) 2. Acid Lava Volcano (ex. Mount Pelee) 3. Shield Volcano (ex. Mauna Loa) 19 of 35 © Boardworks Ltd 2006 Volcano shapes Why do volcanoes have different shapes? 20 of 35 © Boardworks Ltd 2006 Volcano shapes 21 of 35 © Boardworks Ltd 2006 Volcano shapes 22 of 35 © Boardworks Ltd 2006 Volcanic activity at plate margins 23 of 35 © Boardworks Ltd 2006 Volcanic activity at plate margins 24 of 35 © Boardworks Ltd 2006 Learning objectives What is a volcano? Why do volcanoes occur? What happens when a volcano erupts? 25 of 35 © Boardworks Ltd 2006 Task 1 • Read Interactions pgs. 34-35 (see next slide). • Do “Activities” nos. 2, 3 and 4 in your exercise book. 26 of 35 © Boardworks Ltd 2006 27 of 35 © Boardworks Ltd 2006 Task 2 • Download and print out a copy of the following worksheet “Cross section of a volcano outline.doc” • Using Interactions pgs. 32-33 (see next slide)copy and complete the following worksheet the same way as Diagram A on pg. 32. 28 of 35 © Boardworks Ltd 2006 29 of 35 © Boardworks Ltd 2006