volcanoes
Download
Skip this Video
Download Presentation
Volcanoes

Loading in 2 Seconds...

play fullscreen
1 / 12

Volcanoes - PowerPoint PPT Presentation


  • 262 Views
  • Uploaded on

Volcanoes. Chapter 7. Volcano – weak spot in the crust where a mountain forms when layers of lava and volcanic ash erupt and build up and push through

loader
I am the owner, or an agent authorized to act on behalf of the owner, of the copyrighted work described.
capcha
Download Presentation

PowerPoint Slideshow about 'Volcanoes' - Roberta


An Image/Link below is provided (as is) to download presentation

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.


- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -
Presentation Transcript
volcanoes

Volcanoes

Chapter 7

volcanoes and plate tectonics
Volcano – weak spot in the crust where a mountain forms when layers of lava and volcanic ash erupt and build up and push through

Magma - less dense than the rock around it so it is very slowly forced upward toward Earth’s surface made up of gases, water molten rock forming stuff

Lava – magma that reaches the earths surface

Volcanoes and Plate Tectonics
where volcanoes occur
Where Volcanoes Occur?
  • Volcanic Belts form along boundaries of Earth’s crust, one major is the Pacific Ring of Fire
  • 1. Divergent Boundary – plates moving apart – seafloor spreading
    • Example: N. Atlantic Ocean. The North American plate is moving away from Eurasia and African plates.
    • Iceland formed by the separation of these plates at the rift
  • 2. Convergent Boundary – 2 plates collide, rumple up and cause mountains instead of volcano
    • Juan de Fuca Plate is converging with the N. American plate
slide5
Convergent Plates (cont)
    • Magma that is forced upward forms volcanoes of the Cascade Mountains
    • Pacific Ring of Fire – area around the Pacific Plate where there are earthquakes and volcano’s
  • Hot Spots – middle of a plate, area’s in Earth’s mantle that are hotter than neighboring areas
  • Magma forms and rises towards the crust
  • Example: Hawaiian islands, plates move and form islands when it gets over the hot spot
types of eruptions depend on the pressure build up and material
Types of Eruptions – depend on the pressure build up and material
  • 2 factors:
  • 1. Water Vapor and other gases trapped within the magma,
    • if they escape easily – quiet eruptions
    • Gas trapped under high pressure eventually escapes – explosive eruptions
  • 2. Magma is either basaltic or granitic
    • Basaltic magma – contains less silica, is very fluid and produces quiet, non-explosive eruptions magma runs down the side like in Hawaii
slide7
Granitic magma – thick and contains lots of silica and has a high water content, it gets trapped in vents, causing pressure to build up so when it erupts the gases expand rapidly carrying pieces of lava
3 forms of volcanoes
3 Forms of Volcanoes
  • 1. Shield Volcano – Quiet eruptions that spread out basaltic lava in broad, flat layers Hawaiian Islands (pg 399)
  • 2. Cinder Cone Volcano – Explosive eruptions that throw lava into the air forms steep sided consolidated volcano ( pg 400) Paricutin
    • Tephra – various sizes of this lava after it has cooled
      • Ash – fine
      • Bombs – large heavy rocks
slide9
3. Composite Volcano – formed at convergent plate boundaries above subduction zone, this type of volcano alternates between quiet and explosive tephra layer alternating with a lava layer Mt. St. Helens (pg 400)
  • Subduction Zone – area where an ocean plate descends into the upper mantle
volcano features
Volcano Features
  • Magma that cools underground forms igneus rock (most magma does not reach the surface)
  • Balholith – largest igneous rock bodies, hundreds of km wide and thick Yosemete has exposed one
  • Dike – magma squeezed into a vertical crack and hardened
  • Sill – magma squeezed into a horizontal crack
  • Laccolith – dome of rock
  • Volcanic Neck – cone of the volcano erodes and leaves the igneous rock Ship Rock New Mexico
  • Caldera – formed after eruption when the top collapses down into magma chamber Crater Lake
slide11
Vent – opening in the surface which magma reaches the earths surface through (1000 yrs)

Crater – opening at the top of a volcano’s vent

geothermal energy from volcanoes
Geothermal Energy from Volcanoes
  • Geothermal energy – utilizing the heat from magma and converting it to electricity by heating water which produces steam that turns the turbines that run the generators to make electricity (fig 15-5)
  • Geothermal energy used in 20 countries and US
  • Hawaii wants to heat by geothermal energy of Kilauea
  • Many people are against this because some of the rain forest must be cleared for roads, drilling etc, they say it will cut down cultural trees
ad