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Volcanoes Plate Tectonics Icons key: For more detailed instructions, see the Getting Started presentation. Flash activity. These activities are not editable. Accompanying worksheet. 1 of 38 Printable activity. Teacher’s notes included in the Notes Page. Useful web links. © Boardworks Ltd 2008 What is a volcano? Why do volcanoes occur? Where are volcanoes found? Contents A case study: Mount St Helens Can eruptions be predicted? Why do people live in volcanic areas? Summary activities The key concepts covered are: Place, Space and Physical and human processes. 2 of 38 © Boardworks Ltd 2008 Whatisisaa volcano? volcano? What By the end of this section, you will: Know what a volcano is and what happens beneath the surface of a volcano. Understand about the different types of volcano that exist. 3 of 38 © Boardworks Ltd 2008 What is a volcano? A volcano is an opening, or vent, in the earth’s surface. Volcanic vent This opening allows molten lava to erupt through it and solidify as igneous rock. Other materials are also ejected. What happens beneath the surface to cause an eruption? 4 of 38 © Boardworks Ltd 2008 Inside a volcano 5 of 38 © Boardworks Ltd 2008 Cross section of a volcano 6 of 38 © Boardworks Ltd 2008 Cross section of a volcano 7 of 38 © Boardworks Ltd 2008 Volcanic production 8 of 38 © Boardworks Ltd 2008 Volcanic emissions 9 of 38 © Boardworks Ltd 2008 Volcanic emissions 10 of 38 © Boardworks Ltd 2008 Volcano types There are three different types of volcano. Geographers call the categories active, dormant or extinct. An active volcano is liable to erupt at any time, e.g. Mt Etna. A dormant volcano has not erupted for years. Mt Pinatubo erupted in 1991 after 500 years of dormancy. An extinct volcano has not erupted for a very long time and is unlikely to erupt again, e.g. Edinburgh. Categorizing volcanoes can be tough. Chaitén in Chile erupted in 2008 for the first time since 7400BC! 11 of 38 © Boardworks Ltd 2008 What type? 12 of 38 © Boardworks Ltd 2008 Why do volcanoes Why do volcanoes occur? occur? By the end of this section, you will: Know more about how plate tectonics cause the formation of volcanoes. Understand the role destructive and constructive boundaries play in the formation of volcanoes. 13 of 38 © Boardworks Ltd 2008 Plate movements The surface of the Earth is covered in plates that are in constant motion. The motion of the plates can cause problems to the surface of the Earth. Most of these problems occur at plate boundaries. A plate boundary is where the edges of two plates meet. The vast majority of the Earth’s volcanoes can be found on a plate boundary. 14 of 38 © Boardworks Ltd 2008 Important boundaries 15 of 38 © Boardworks Ltd 2008 Destructive plate boundary 16 of 38 © Boardworks Ltd 2008 Constructive plate boundary 17 of 38 © Boardworks Ltd 2008 Volcanic activity at plate margins 18 of 38 © Boardworks Ltd 2008 Where volcanoes found? Where areare volcanoes found? By the end of this section, you will: Be able to recognize the areas of the Earth where volcanoes are usually found. Know what is meant by the term ‘Ring of Fire’. Know what is meant by a hot spot volcano. 19 of 38 © Boardworks Ltd 2008 Where are volcanoes found? Volcanoes are usually found at plate boundaries. One area of the world is well-known for the number of volcanoes around it. This area is known as the ‘Ring of Fire’. The Ring of Fire is located around the Pacific rim. Can you think of any volcanoes that are located on the Ring of Fire? 20 of 38 © Boardworks Ltd 2008 The Ring of Fire 21 of 38 © Boardworks Ltd 2008 Hawaii The Hawaiian islands are a chain of volcanic islands that are situated in the Pacific Ocean. Why is this an unusual place for them to be located? Most volcanoes are located on plate boundaries. Hawaii is nowhere near a plate boundary. Why are the Hawaiian islands volcanic? 22 of 38 © Boardworks Ltd 2008 Hot spot volcanoes 23 of 38 © Boardworks Ltd 2008 A casestudy: study – Mount Mount StSt Helens A case Helens By the end of this section, you will: Have a better understanding of what happened in the Mount St Helens eruption. Understand what some of the consequences of the eruption were. Realize what damage the eruption caused. 24 of 38 © Boardworks Ltd 2008 Mt St Helens – the eruption 25 of 38 © Boardworks Ltd 2008 Mt St Helens – consequences of the eruption The effects of the Mount St Helens eruption were enormous. The pyroclastic surge spread 27km from the volcano and flattened acres of woodland. Ash clouds stretched 26km above sea level. However, there were some positives. Some plants and animals were resilient enough to survive. The lack of human interference encouraged nature to spring forth again. 26 of 38 © Boardworks Ltd 2008 How great was the damage? 27 of 38 © Boardworks Ltd 2008 Back to the future What does the future hold for Mount St Helens? Since 1980, there has been more activity on Mount St Helens. Between 1980 and 1986 a new lava dome was formed. Magma reached the surface of the mountain in October 2004. In 2005, a 36,000 foot plume of steam was emitted. There was also a small earthquake. It seems likely that Mount St Helens will erupt again in the future. Will we be able to tell when? 28 of 38 © Boardworks Ltd 2008 Can eruptions be predicted? Can eruptions be predicted? By the end of this section, you will: Know what a volcanologist does. Understand some of the difficulties that are associated with predicting volcanic eruptions. 29 of 38 © Boardworks Ltd 2008 The problem of prediction Volcanologists – people who study volcanoes – are skilled at predicting the likelihood of an eruption. However, it is difficult to pinpoint when an eruption will happen. The movement of magma may be detected, but often no eruption occurs. Instead it cools below the surface. Monitoring potential eruptions is expensive. With many volcanoes erupting only every few hundred years, it's not possible to monitor every site. 30 of 38 © Boardworks Ltd 2008 Predicting eruptions 31 of 38 © Boardworks Ltd 2008 Why do people live in volcanic Why do people live in areas? volcanic areas? By the end of this section, you will: Know why people are attracted to live near volcanic areas. Realize some of the pros and cons of living alongside a volcano. 32 of 38 © Boardworks Ltd 2008 Why do people live in volcanic areas? Although volcanic areas are exceptionally dangerous, there are still a lot of people who live in zones that are affected by volcanic eruptions. Why? Tourists are attracted to areas of volcanic activity. This provides money for the local economy. The lava produced by the volcano is weathered (broken down) to form a fertile soil. This is perfect for growing crops. Geothermal energy can be produced in many volcanic areas. Can you think of any other reasons? 33 of 38 © Boardworks Ltd 2008 Pros and cons 34 of 38 © Boardworks Ltd 2008 Summary activities Summary activities By the end of this section, you will: Know the key points of volcanoes and volcanic eruptions. Understand important words and phrases relating to volcanoes. 35 of 38 © Boardworks Ltd 2008 Summary quiz 36 of 38 © Boardworks Ltd 2008 Glossary 37 of 38 © Boardworks Ltd 2008 Anagrams 38 of 38 © Boardworks Ltd 2008