1. Volcanoes

4. 7.1 Volcanoes and Plate Tectonics Magma – hot liquid rock Volcanism – movement of magma toward suface Lava – magma on the surface Vent – structure which magma flows to surface Volcano – material built up around the vent Fissures – cracks, Iceland Hot spots – volcanism in plate

5. http://www.nationalgeographic.com/forcesofnature/interactive/index.html?section=v

6. Where are Volcanoes? P.11 Subduction zones Mid-ocean ridges Hot spots - found within a plate not at a plate boundary

7. Magma p.12 Magma is a complex high-temperature fluid substance. Temperatures of most magmas are in the range 700°C to 1300°C May reach as hot as 1600°C. Called magma when in the earth and lava when it is on the surface of the earth.

8. Felsic Magma p.13 –SiO 2 >70% –Fe-Mg: ~ 2% –Temp: < 900°C –Viscosity: High –Eruptive behavior: explosive –Distribution: hot spots in continental crust (Yellowstone National Park), continental rifts, island arcsYellowstone National Park

9. Yellowstone The Yellowstone Caldera is the largest volcanic system in North America. It has been termed a "supervolcano" because the caldera was formed by exceptionally large explosive eruptions.Yellowstone Calderasupervolcano The amount of ash and gases released into the atmosphere probably caused significant impacts to world weather patterns and led to the extinction of many species, primarily in North America. extinction

10. Gases from Volcanoes p.14 Water vapor is typically the most abundant volcanic gas, followed by carbon dioxide and sulfur dioxide. Sulfur dioxide kills vegetation and can cause acid rain.

12. Homework After viewing the video, write a paragraph that states what fact you found the most interesting (disturbing) and why?

14. Eruptions

15. 7.2 Volcanic Eruptions A. Kinds of Eruptions B. Volcanic Rock Fragments C. Volcanic Features 1. Types of volcanoes 2. Craters and Calderas D. Predicting Volcanic Eruptions

16. Volcanic Eruptions 2 types of lava chemically, effects eruptions intensity 1. mafic lava – dark, rich in Mg and Fe From ocean crust Less explosive, quiet 2. felsic lava – lighter color, lots of silica, much less Mg and Fe Found in continental crust More explosive, contains dissolved gases Other types are in between Pahoehoe – mafic lava cooling rapidly will wrinkle Aa – when the lava breaks into chunks Pillow lava – midocean ridge cools so rapidly forms round blobs

17. Pahoehoe

18. Aa

19. A. Kinds of Eruptions If magma has a lot of gases more explosive Ocean islands usually quiet Continental volcanoes with felsic lava have cooler and thicker lava so traps gases (H2O and CO2) big explosions

21. B. Volcanic Rock Fragments Felsic lava explodes so throws materials Pyroclastic material – rock fragments (some still molten, others cooled) Volcanic ash - <2 mm Volcanic dust - <.25 mm Lapilli - <.64 mm Volcanic bombs – red-hot lava cools in the air in shape of spiral or round bomb Volcanic blocks – big solid rocks as big as a house

22. bombs

23. Volcanoes Can Cause Climate Change! Ash from a large volcano can shut out the sunlight for hundreds of miles.

24. C. Volcanic Features What it looks like 1. Types of volcanoes 2. Craters and Calderas

26. 1. Types of volcanoes 1. Shield volcanoes – cones with broad base and gentle slope, made up of lava layers Hawaii 2. Cinder cones – cone is made up of fragments ejected 3. Composite volcanoes (stratovolcanoes) Combination of layers of lava and fragments from some quiet and expolsive eruptions Ex. Mt. Fuji, Rainier, Hood, Shasta St. Helens

27. Types

28. 2. Craters and Calderas Crater – funnel-shaped on the top vent Explosion forms Caldera – depression from collapsed crater Crater Lake National Park

29. Caldera

30. Crater Lake - Oregon

31. D. Predicting Volcanic Eruptions Not where we need to be yet Saves lives Seismographs Temp Pressure Bulging surface Gases given off History/past Dormant for long periods can be active

32. 7.3 Extraterrestrial volcanism Moon Mars Lo

33. Moon Surface covered with craters – meteorites Lava flow evidence does show volcanic activity long ago Nothing active No plates for movement or convection current evidence ? Not sure how

34. Mars See pictures of None prove active They are much larger than earths because no continental drift

35. Lo Moon of Jupiter Pictures of active volcanoe Think the material is sulfur and sulfur dioxide from color Constantly erupting