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Welcome to Science 10/25

Learn about different types of volcanoes and how they erupt. Explore quiet and explosive eruptions, magma composition, and stages of volcanic activity.

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Welcome to Science 10/25

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  1. Welcome to Science 10/25 • Get out your lab sheet. You have 3 minutes to create the type of volcano listed on your card. Have your group help you if needed. • Today’s Schedule • 1. Finish/Review Volcano Types Lab • 2. Outline/Notes Volcanic Eruptions • 3. Yokum Construction Co. will be open for business to sell building materials.

  2. Volcano Types • Shield, Cinder-Cone, and Composite. • What causes these different types of volcanoes to form? • The different ways in which they erupt and the different materials that are erupted.

  3. Volcanic Eruptions Section. 3

  4. Pele

  5. I. Kinds of Volcanic Eruptions • Eruptions are classified as either quiet or explosive. • How a volcano erupts depends on the gasses, silica, and viscosity of the magma. • Silica-similar to sand, one of the key components of magma • Viscosity- the resistance of a liquid to flow

  6. II. How the Eruption Works • A volcanic eruption is similar to an exploding pop can. • Gasses inside the volcano build up. As gas builds up, so does the pressure. When the pressure is too great, the volcano erupts. BBC NEWS | Science/Nature | Animated guide: Volcanoes • OUR RESTLESS PLANET

  7. III. Quiet Eruptions • Magma has low silica, low viscosity, and low gasses so it flows easily. • Hawaiian Islands were made this way. • OUR RESTLESS PLANET • What type of volcano is formed by quiet eruptions? • Shield

  8. IV. Explosive Eruptions • Magma has high-silica and high viscosity, making it thick and sticky. High Gas. • Magma does not flow. • Builds up in the pipe like a cork in a bottle . • Pressure builds up until the volcano explodes. • :: Make a Volcano

  9. Mount St. Helens mt. st. helens - Google Videos# During Eruption

  10. Mount St. Helens Before Eruption After Eruption "Mt. Saint Helens' Powerful Erruption"

  11. Mt. St. Helens 2003 Mt. St. Helens 1984

  12. V. Explosive Eruptions • Explosive eruptions break lava into fragments that quickly cool into pieces of different sizes. • Large pieces = bombs • Small pieces = cinders • Pyroclastic flow- mixture of hot gas, ash, cinders, and bombs • -pyroclastic-flow-video.htm

  13. VI. Stages of Volcanic Activity • Active, dormant, or extinct? • Active- erupting or shows signs of erupting. • Dormant- may awaken in the future. • Extinct- unlikely to erupt again • Is a volcano ever really extinct? • No, at anytime a volcano thought to be extinct could reawaken.

  14. How It All Starts • Magma from the mantle rises up through the crust because it is less dense. • Magma becomes trapped beneath layers of rock. • Weak spots in the crust allow trapped magma to reach the surface, forming a volcano.

  15. At the Surface Pipe, Vent, Magma Chamber, Crater, Lava Flow • Magma Chamber- pocket of magma beneath a volcano • Pipe- long tube that connects the magma chamber to the surface • Vent- opening where molten rock and gas leave the volcano

  16. At the Surface • Lava flow- area covered by lava as it pours out of a vent. • Crater- bowl shaped area that may form at the top of a volcano.

  17. Correctly the match the stages of volcanoes with the definitions. A. A volcano that is unlikely to erupt again. B. A volcano that is erupting or shows signs of erupting. C. A volcano that may awaken in the future Active Dormant Extinct Question of the Day

  18. Today’s Objectives • 1. Question of the Day • 2. Open book quiz • 3. Continue research on volcanoes

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