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Seismology and Volcanology Seismology Seismology • Seismology is the study of earthquakes and their effects. • When there is an earthquake a great deal of energy is released. • This energy travels in the form of waves. Seismology • There are two kinds of seismic waves 1. Body waves 2. Surface waves Body waves Body waves • Body waves travel through the ground and move very quickly. • There are two kinds of body waves. Body waves • Body waves travel through the ground and move very quickly. • There are two kinds of body waves. 1. Primary waves 2. Secondary waves Body waves • Primary waves - also called “P waves” • Travel at about 6 km/s (they are the fastest seismic waves) • Can move through both solids and liquids • The ground compresses and stretches in the direction they travel. Body waves • Secondary waves - also called “S waves” • They travel at about 3.5 km/s (They are the second fastest seismic waves) • Can move through solids but not liquids • They cause the ground to squeeze and stretch at right angles to the wave direction. Surface waves Surface waves • Love waves – also called “L waves” • They travel more slowly than body waves but because they travel along the surface of the Earth they cause more damage than body waves. So? What good is it knowing all that stuff about seismic waves? Seismology Seismology • By analyzing seismic waves geologists can figure out a lot about the conditions below the surface of the Earth including the thickness and composition of each layer. Volcanology Volcanology • There are three types of volcanoes Volcanology 1. Composite Volcanoes Volcanology 1. Composite Volcanoes • • • Large cone-shaped volcanoes. The “classic” volcano image. The cone shape results from recurring eruptions of ash and lava which builds up layers over time. Volcanology 1. Composite Volcanoes • • • The magma for these volcanoes is very thick These volcanoes can have very explosive eruptions. Mt. Fuji, Mt St. Helens, and Mt. Vesuvius are composite volcanoes Composite Volcanoes Composite Volcanoes Composite Volcanoes Volcanology 2. Shield Volcanoes Volcanology 2. Shield Volcanoes • These volcanoes form at weak parts of the Earth’s crust called “Hot Spots” where lava/magma can burst through. Volcanology 2. Shield Volcanoes • These volcanoes form at weak parts of the Earth’s crust called “Hot Spots” where lava/magma can burst through. • The lava forming these volcanoes is much more fluid than the kind at composite volcanoes. Volcanology 2. Shield Volcanoes • The result is non-explosive eruptions and not very steep slopes. But these are the largest volcanoes in the world. • The Hawaiian Islands, Iceland, and the Galapagos Islands are examples of Shield Volcanoes. Volcanology 2. Shield Volcanoes • The result is non-explosive eruptions and not very steep slopes. But these are the largest volcanoes in the world. • The Hawaiian Islands, Iceland, and the Galapagos Islands are examples of Shield Volcanoes. • Video Shield Volcanoes Shield Volcanoes Shield Volcanoes Volcanology 3. Rift Eruptions Volcanology 3. Rift Eruptions • These occur where ridges are spreading • Lava comes up through the long cracks • These are not violent eruptions but they can release a lot of lava • The Columbia River Plateau is a 30 m.y. old rift eruption where the lava is about 3 km thick. Rift Eruptions Video Interlude • Video Volcanology Q: What comes out of a volcano? Volcanology Q: What comes out of a volcano? Volcanology Q: What comes out of a volcano? • Gases - water vapour, CO2, sulfur. • Tephra - solid fragments like ash, lapilli, blocks and bombs. • Lava – it used to be magma, now it’s lava. Volcanology Q: What comes out of a volcano that will most likely kill you? Volcanology Q: What comes out of a volcano that will most likely kill you? A: The Pyroclastic Flow – a mixture of gas, steam and ash, superheated to over 1000⁰C, and capable of travelling at over 300 km/h. Volcanology Q: What comes out of a volcano that will most likely kill you? A: A Lahar occurs when the volcano is covered in snow or ice. The mud, water, ash and debris can cover large distances very quickly. Volcanology The End