Useful Websites http://primaryhomeworkhelp.co.uk/mountains/volcanoes.htm Child-friendly description of volcanoes http://www.weatherwizkids.com/weather-volcano.htm Some helpful animations http://www.kids-fun-science.com/ring-of-fire-volcanoes.html Ring of fire volcanoes http://www.volcanolive.com/index.html News, photographs and webcams http://www.geography4kids.com/files/earth_volcano.html Description of different types of volcanoes & lava http://www.kidscosmos.org/mars/kids/kids_volcanoes_types.php Types of volcanoes http://science-at-home.org/more-about-volcanoes/ Interesting facts http://library.thinkquest.org/17457/volcanoes/erupt.php Volcanic eruptions http://news.bbc.co.uk/cbbcnews/hi/find_out/guides/tech/volcanoes/ne wsid_1768000/1768595.stm Newsround information © Original resource copyright Hamilton Trust, who give permission for it to be adapted as wished by individual users. We refer you to our warning, at the top of the You Will Need document, about links to other websites Y3 Sc Rocks Session C Volcano Facts Volcanoes are geological landforms (usually mountains) where gas and molten rock (magma) from the interior of the Earth erupts through the surface of the planet. Essentially, volcanoes are like giant natural safety valves, which release the pressure that builds up inside the Earth. The Earth’s crust is made up of huge slabs called tectonic plates, which fit together a bit like a jigsaw. These pieces move, sliding into each other or apart, and the friction caused by their movement produces earthquakes and volcanoes. Inside the Earth there is a load of boiling hot, molten minerals. The pressure from this boiling mass of minerals builds up, and it sometimes needs to release itself. The pressure forces up hot gas and molten rock through cracks or ‘fissures’ in the Earth’s crust until it erupts through the surface. The points where these eruptions occur are known as volcanoes. There are different kinds and shapes of volcano. The archetypal image is of a cone mountain with the top chopped off and lava spewing forth from the crater. However, there are many other types and shapes of volcano, which all differ in the amount, the regularity, and the type of eruption they produce. These include shield, cinder cone & composite volcanoes and lava domes. Volcanoes can occur on land or underwater. There are currently about 1500 known active volcanoes on Earth, and about 80 or more which are under the sea. In fact, about 75% of all annual magma output occurs via underwater volcanoes. Volcanoes also occur on other planets! Mars, Venus, and even the Moon all demonstrate or have demonstrated the existence of volcanic activity. An active volcano is one that erupts regularly. A dormant volcano is one in which there is still some activity deep inside, but which hasn’t erupted in many years. © Original resource copyright Hamilton Trust, who give permission for it to be adapted as wished by individual users. We refer you to our warning, at the top of the You Will Need document, about links to other websites Y3 Sc Rocks Session C An extinct volcano is one that has not erupted for a very long time and is no longer active. Magma is the liquid rock inside the volcano. Lava is the liquid rock once it has broken the surface and is flowing out of a volcano. Geysers are springs that fountain boiling hot water high into the air. This water has been heated underground by volcanic activity until it has become so hot that the pressure sends it gushing upwards out of the earth. The word ‘volcano’ comes from ‘Vulcan’, the god of fire in Roman mythology. The study of volcanoes is known as volcanology (sometimes spelled vulcanology). Volcano eruptions are very dangerous and destructive, more dangerous the bigger the volcano is. However, because lava deposits are rich in minerals, the soil surrounding volcanoes is usually very fertile. This is why so many people live close to active volcanoes despite the danger (about 1 in 10 people live near a dangerous volcano). Eruptions can destroy property, bury houses and people in lava or ash, release poisonous gasses that kill animals, plants and people, cover everything in dust that causes illnesses like pneumonia in survivors, and darken skies to such an extent that severe winds and heavy rains may follow the eruption for months afterwards. The biggest volcano on Earth is Mauna Loa in Hawaii. From the sea floor it is about six miles high (that’s larger than Mount Everest!). It is a ‘shield’ volcano. © Original resource copyright Hamilton Trust, who give permission for it to be adapted as wished by individual users. We refer you to our warning, at the top of the You Will Need document, about links to other websites Y3 Sc Rocks Session C Volcanic Eruptions It is so hot deep within the Earth that the rocks slowly melt and become a thick flowing substance called magma. Because magma is lighter than the solid rock around it (gases), it rises and collects in magma chambers and the pressure builds up. Eventually some of the magma pushes through vents and fissures in the Earth's surface. These may be present from earlier eruptions or are caused by movements of the plates in the Earth’s crust. Magma that has erupted is called lava. Some volcanic eruptions are explosive and others are not. How explosive an eruption is depends on how runny or sticky the magma is. If magma is thin and runny, gases can escape easily from it. When this type of magma erupts, it flows out of the volcano. Lava flows rarely kill people because they move slowly enough for people to get out of their way. Lava flows, however, can cause considerable destruction to buildings in their path. If magma is thick and sticky, gases cannot escape easily. Pressure builds up until the gases escape violently and explode. In this type of eruption, the magma blasts into the air and breaks apart into pieces ranging in size from tiny particles of ash to house-size boulders. Ash erupted into the sky falls back to Earth like powdery snow. If thick enough, blankets of ash can suffocate plants, animals, and humans. When hot volcanic materials mix with water from streams or melted snow and ice, mudflows form. © Original resource copyright Hamilton Trust, who give permission for it to be adapted as wished by individual users. We refer you to our warning, at the top of the You Will Need document, about links to other websites Y3 Sc Rocks Session C Model Volcano You will need: Baking soda (tablespoon) Soap powder/flakes (tablespoon) Water (180ml approx.) Food colouring – few drops of red or orange (optional) Vinegar (45ml approx.) Empty plastic drinks bottle or glass jar/beaker (magma chamber) Glass stirring rod or long-handled spoon (ensure it fits through the neck of the bottle – if necessary cut off the neck) Waterproof tray or drawer Playdough OR Newspaper, diluted PVA glue, paints & brushes Method: Build a volcano from playdough or papier mâché around the plastic drinks bottle or glass jar/beaker (Crumple newspaper into balls to create most of the ‘volcano’ and then cover with strips of newspaper dipped in diluted PVA glue) ensuring the ‘vent’ is left clear (*this could be prepared beforehand) When the papier mâché is dry, paint it to represent a mountain/volcano (if appropriate) Place on the waterproof tray Add the baking soda, soap powder, water & food colouring to the drinks bottle and stir well Quickly add the vinegar and stand back! Watch the volcano ‘erupt’! © Original resource copyright Hamilton Trust, who give permission for it to be adapted as wished by individual users. We refer you to our warning, at the top of the You Will Need document, about links to other websites Y3 Sc Rocks Session C Volcanoes for Research Eyjafjallajökull Vesuvius Popocatépetl Tongariro Krakatau Mount Pinatubo Mount St Helens Mauna Loa Mount Etna Nevado del Ruiz Stromboli Thera 1 Crater Lake Lassen Peak Mount Fuji © Original resource copyright Hamilton Trust, who give permission for it to be adapted as wished by individual users. We refer you to our warning, at the top of the You Will Need document, about links to other websites Y3 Sc Rocks Session C