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VOLCANOES!.

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Presentation on theme: "VOLCANOES!."— Presentation transcript:

1 VOLCANOES!

2 Factors Affecting Eruptions
Magma temperature Hotter flows easier… Magma viscosity – determined by temp and composition. High silica = high viscosity (thickness) High viscosity = violent eruptions… Dissolved gases More gasses means more violent eruptions…

3 Volcanic Materials- Lava
3 TYPES OF LAVA FLOWS Aa- rough and jagged 2) Pahoehoe - wrinkly and ropey texture 3) Pillow - forms underwater at boundaries

4 Aa Pahoehoe Pillow

5 Volcanic Materials- Gases
Water Vapor, Carbon Dioxide, Nitrogen, Sulfur Dioxide, and Chlorine Kilauea Volcano, Hawai`i From emitted 1,000-2,000 metric tons of SO2 every day!

6 Volcanic Materials Pyroclastic Materials = Ejected fragments
Ash – fine material Cinders and lapilli = medium/pebble sized Bombs and blocks (big stuff) block = hard, bombs = lava

7 Ash Bombs & Blocks Cinders

8 Volcanic Terms Crater – steep walled depression at top
Caldera – large depression in a volcano due to collapse of volcano

9 Volcanic Terms Conduit – pipe connecting magma chamber to the surface Vent – top of the conduit

10 Volcanic Terms Lava plateau – raised flat area of lava
Volcanic neck – remnant of eroded volcano

11 Columbia Lava Plateau- covers parts of Washington, Oregon, and Idaho

12 Composite Cinder Cone Shield
Types of Volcanoes Composite Cinder Cone Shield

13 Shield Volcanoes broad base with gently sloping sides
Huge in size, mild eruptions, mostly flows, ex: Hawaii Mauna Kea, Hawaii

14 Cinder Cone Narrow base and steep sides
-Small, violent for size, pyroclastic eruptions, ex: Mt. Paricutin, Sunset crater in AZ

15 Composite Cone Medium base and moderately sloped size (volcano looking) Medium size, violent eruptions, andesitic lava, combination of flows and pyroclastic eruptions, ex: Mt. St. Helens

16 Mt. St. Helens Before & After

17 Igneous Activity Plutons (intrusive igneous bodies)
Classified by shape, size, and relationship to surrounding rock layers Sill – horizontal and between rock layers Dike – vertical and cut across rock layers Laccolith – dome/mushroom shaped plutons Batholith – more than 100 km2 of exposed rock Stock – less than 100 km2 of exposed rock

18 Volcano Dangers Pyroclastic flows – hot gases, glowing ash, and larger rock fragments Very hot (like cook your butt hot) Can attain 200 km/hr Lahars – mudflow formed from volcanic ash and water (melted snow or rain) Eruptions – you’re there one minute and gone the next…can you say vaporized

19 Origin of Magma Read pages 291 – 292 The role of heat
The role of pressure The role of water

20 Volcano Locations Convergent plates Divergent plates
Subducting plate melts and magma rises Japan and Mt St Helens Divergent plates Plate diverge and magma rises through the rift Mid-ocean ridge Iceland East African Rift Intraplate (hot spots) Mantle plume rises towards the surface Hawaii and Yellowstone


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