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Volcanoes

  Mr. Silva
Vocabulary
Vocabulary
ā€¢ Volcano-
Vocabulary
ā€¢ Volcano-
  ā€“ Lava and pyroclastoc material built up on the
    earthā€™s surface around a vent.
Vocabulary
ā€¢ Volcano-
  ā€“ Lava and pyroclastoc material built up on the
    earthā€™s surface around a vent.
ā€¢ Volcanism-
Vocabulary
ā€¢ Volcano-
  ā€“ Lava and pyroclastoc material built up on the
    earthā€™s surface around a vent.
ā€¢ Volcanism-
  ā€“ Any activity that includes the movement of
    magma toward or onto the earthā€™s surface.
Vocabulary
ā€¢ Volcano-
  ā€“ Lava and pyroclastoc material built up on the
    earthā€™s surface around a vent.
ā€¢ Volcanism-
  ā€“ Any activity that includes the movement of
    magma toward or onto the earthā€™s surface.
ā€¢ Vent-
Vocabulary
ā€¢ Volcano-
  ā€“ Lava and pyroclastoc material built up on the
    earthā€™s surface around a vent.
ā€¢ Volcanism-
  ā€“ Any activity that includes the movement of
    magma toward or onto the earthā€™s surface.
ā€¢ Vent-
  ā€“ Opening through which molten rock ļ¬‚ows onto
    the earthā€™s surface.
Vocabulary
ā€¢ Magma-
  ā€“ Liquid rock produced deep inside the earth
ā€¢ Lava-
  ā€“ Magma that reaches the earthā€™s surface
ā€¢ Fissures-
  ā€“ Cracks through which lava ļ¬‚ows
ā€¢ Hot Spots-
  ā€“ Areas of volcanism within plates
Notes
Notes
1. Most of the asthenosphere remains solid,
   because of the great pressure of the
   surrounding rock
Notes
1. Most of the asthenosphere remains solid,
   because of the great pressure of the
   surrounding rock
Notes
1. Most of the asthenosphere remains solid,
   because of the great pressure of the
   surrounding rock

  i.   Magma forms when mantle material flows to
       areas of lower pressure, or when fluids such as
       water are added
Notes
Notes
2. Volcanism involves any activity that includes
   the movement of magma toward or onto the
   Earthā€™s surface
Notes
2. Volcanism involves any activity that includes
   the movement of magma toward or onto the
   Earthā€™s surface
Notes
2. Volcanism involves any activity that includes
   the movement of magma toward or onto the
   Earthā€™s surface

  a. Lava is magma that erupts onto the Earthā€™s surface
Notes
2. Volcanism involves any activity that includes
   the movement of magma toward or onto the
   Earthā€™s surface

  a. Lava is magma that erupts onto the Earthā€™s surface
     i. Vent- the opening that molten rock flows
        through to reach the surface
Notes
2. Volcanism involves any activity that includes
   the movement of magma toward or onto the
   Earthā€™s surface

  a. Lava is magma that erupts onto the Earthā€™s surface
     i. Vent- the opening that molten rock flows
         through to reach the surface
     ii. Volcano- the structure formed by the vent and
         volcanic material that builds up around the vent
Notes Conā€™t
Notes Conā€™t
3.   Major Volcanic Zones
Notes Conā€™t
3.          Major Volcanic Zones
     a. Subduction Zones
Notes Conā€™t
3.           Major Volcanic Zones
     a. Subduction Zones
       i. When an oceanic and a continental plate meet,
          the oceanic plate, the oceanic plate subducts,
          because it is more dense
Notes Conā€™t
3.           Major Volcanic Zones
     a. Subduction Zones
       i. When an oceanic and a continental plate meet,
           the oceanic plate, the oceanic plate subducts,
           because it is more dense
       ii. The subducted plate dives deep into the
           asthenosphere, causing water to combine with
           nearby mantle material
Notes Conā€™t
3.           Major Volcanic Zones
     a. Subduction Zones
       i. When an oceanic and a continental plate meet,
            the oceanic plate, the oceanic plate subducts,
            because it is more dense
       ii. The subducted plate dives deep into the
            asthenosphere, causing water to combine with
            nearby mantle material
       iii. This forms magma
Notes Conā€™t
3.           Major Volcanic Zones
     a. Subduction Zones
       i. When an oceanic and a continental plate meet,
            the oceanic plate, the oceanic plate subducts,
            because it is more dense
       ii. The subducted plate dives deep into the
            asthenosphere, causing water to combine with
            nearby mantle material
       iii. This forms magma
       iv. Some magma erupts through the Earthā€™s surface
            forming:
Notes Conā€™t
3.           Major Volcanic Zones
     a. Subduction Zones
       i. When an oceanic and a continental plate meet,
            the oceanic plate, the oceanic plate subducts,
            because it is more dense
       ii. The subducted plate dives deep into the
            asthenosphere, causing water to combine with
            nearby mantle material
       iii. This forms magma
       iv. Some magma erupts through the Earthā€™s surface
            forming:
       1. Volcanic mountains- where a continental plate
            collides with an oceanic plate
Notes Conā€™t
3.           Major Volcanic Zones
     a. Subduction Zones
       i. When an oceanic and a continental plate meet,
            the oceanic plate, the oceanic plate subducts,
            because it is more dense
       ii. The subducted plate dives deep into the
            asthenosphere, causing water to combine with
            nearby mantle material
       iii. This forms magma
       iv. Some magma erupts through the Earthā€™s surface
            forming:
       1. Volcanic mountains- where a continental plate
            collides with an oceanic plate
       2. Island arcs- where two oceanic plates collide
Notes
Notes
b. Mid-Ocean Ridges
Notes
b. Mid-Ocean Ridges
  i.   As the plates pull apart, magma wells up
       along the rift zone
       1. The magma adds new lithosphere to the ridge
Notes
b. Mid-Ocean Ridges
  i.   As the plates pull apart, magma wells up
       along the rift zone
       1. The magma adds new lithosphere to the ridge
Notes
b. Mid-Ocean Ridges
  i.   As the plates pull apart, magma wells up
       along the rift zone
       1. The magma adds new lithosphere to the ridge


c. Hot Spots
Notes
b. Mid-Ocean Ridges
  i.   As the plates pull apart, magma wells up
       along the rift zone
       1. The magma adds new lithosphere to the ridge


c. Hot Spots
  i.   Volcanoes that do not form at plate
       boundaries
Notes
b. Mid-Ocean Ridges
  i.   As the plates pull apart, magma wells up
       along the rift zone
       1. The magma adds new lithosphere to the ridge


c. Hot Spots
  i.  Volcanoes that do not form at plate
      boundaries
  ii. Hot spot is beneath the lithospheric plate,
      and the plate moves over it
4.3 volcanoes

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4.3 volcanoes

  • 4. Vocabulary ā€¢ Volcano- ā€“ Lava and pyroclastoc material built up on the earthā€™s surface around a vent.
  • 5. Vocabulary ā€¢ Volcano- ā€“ Lava and pyroclastoc material built up on the earthā€™s surface around a vent. ā€¢ Volcanism-
  • 6. Vocabulary ā€¢ Volcano- ā€“ Lava and pyroclastoc material built up on the earthā€™s surface around a vent. ā€¢ Volcanism- ā€“ Any activity that includes the movement of magma toward or onto the earthā€™s surface.
  • 7. Vocabulary ā€¢ Volcano- ā€“ Lava and pyroclastoc material built up on the earthā€™s surface around a vent. ā€¢ Volcanism- ā€“ Any activity that includes the movement of magma toward or onto the earthā€™s surface. ā€¢ Vent-
  • 8. Vocabulary ā€¢ Volcano- ā€“ Lava and pyroclastoc material built up on the earthā€™s surface around a vent. ā€¢ Volcanism- ā€“ Any activity that includes the movement of magma toward or onto the earthā€™s surface. ā€¢ Vent- ā€“ Opening through which molten rock ļ¬‚ows onto the earthā€™s surface.
  • 9. Vocabulary ā€¢ Magma- ā€“ Liquid rock produced deep inside the earth ā€¢ Lava- ā€“ Magma that reaches the earthā€™s surface ā€¢ Fissures- ā€“ Cracks through which lava ļ¬‚ows ā€¢ Hot Spots- ā€“ Areas of volcanism within plates
  • 10. Notes
  • 11. Notes 1. Most of the asthenosphere remains solid, because of the great pressure of the surrounding rock
  • 12. Notes 1. Most of the asthenosphere remains solid, because of the great pressure of the surrounding rock
  • 13. Notes 1. Most of the asthenosphere remains solid, because of the great pressure of the surrounding rock i. Magma forms when mantle material flows to areas of lower pressure, or when fluids such as water are added
  • 14. Notes
  • 15. Notes 2. Volcanism involves any activity that includes the movement of magma toward or onto the Earthā€™s surface
  • 16. Notes 2. Volcanism involves any activity that includes the movement of magma toward or onto the Earthā€™s surface
  • 17. Notes 2. Volcanism involves any activity that includes the movement of magma toward or onto the Earthā€™s surface a. Lava is magma that erupts onto the Earthā€™s surface
  • 18. Notes 2. Volcanism involves any activity that includes the movement of magma toward or onto the Earthā€™s surface a. Lava is magma that erupts onto the Earthā€™s surface i. Vent- the opening that molten rock flows through to reach the surface
  • 19. Notes 2. Volcanism involves any activity that includes the movement of magma toward or onto the Earthā€™s surface a. Lava is magma that erupts onto the Earthā€™s surface i. Vent- the opening that molten rock flows through to reach the surface ii. Volcano- the structure formed by the vent and volcanic material that builds up around the vent
  • 21. Notes Conā€™t 3. Major Volcanic Zones
  • 22. Notes Conā€™t 3. Major Volcanic Zones a. Subduction Zones
  • 23. Notes Conā€™t 3. Major Volcanic Zones a. Subduction Zones i. When an oceanic and a continental plate meet, the oceanic plate, the oceanic plate subducts, because it is more dense
  • 24. Notes Conā€™t 3. Major Volcanic Zones a. Subduction Zones i. When an oceanic and a continental plate meet, the oceanic plate, the oceanic plate subducts, because it is more dense ii. The subducted plate dives deep into the asthenosphere, causing water to combine with nearby mantle material
  • 25. Notes Conā€™t 3. Major Volcanic Zones a. Subduction Zones i. When an oceanic and a continental plate meet, the oceanic plate, the oceanic plate subducts, because it is more dense ii. The subducted plate dives deep into the asthenosphere, causing water to combine with nearby mantle material iii. This forms magma
  • 26. Notes Conā€™t 3. Major Volcanic Zones a. Subduction Zones i. When an oceanic and a continental plate meet, the oceanic plate, the oceanic plate subducts, because it is more dense ii. The subducted plate dives deep into the asthenosphere, causing water to combine with nearby mantle material iii. This forms magma iv. Some magma erupts through the Earthā€™s surface forming:
  • 27. Notes Conā€™t 3. Major Volcanic Zones a. Subduction Zones i. When an oceanic and a continental plate meet, the oceanic plate, the oceanic plate subducts, because it is more dense ii. The subducted plate dives deep into the asthenosphere, causing water to combine with nearby mantle material iii. This forms magma iv. Some magma erupts through the Earthā€™s surface forming: 1. Volcanic mountains- where a continental plate collides with an oceanic plate
  • 28. Notes Conā€™t 3. Major Volcanic Zones a. Subduction Zones i. When an oceanic and a continental plate meet, the oceanic plate, the oceanic plate subducts, because it is more dense ii. The subducted plate dives deep into the asthenosphere, causing water to combine with nearby mantle material iii. This forms magma iv. Some magma erupts through the Earthā€™s surface forming: 1. Volcanic mountains- where a continental plate collides with an oceanic plate 2. Island arcs- where two oceanic plates collide
  • 29. Notes
  • 31. Notes b. Mid-Ocean Ridges i. As the plates pull apart, magma wells up along the rift zone 1. The magma adds new lithosphere to the ridge
  • 32. Notes b. Mid-Ocean Ridges i. As the plates pull apart, magma wells up along the rift zone 1. The magma adds new lithosphere to the ridge
  • 33. Notes b. Mid-Ocean Ridges i. As the plates pull apart, magma wells up along the rift zone 1. The magma adds new lithosphere to the ridge c. Hot Spots
  • 34. Notes b. Mid-Ocean Ridges i. As the plates pull apart, magma wells up along the rift zone 1. The magma adds new lithosphere to the ridge c. Hot Spots i. Volcanoes that do not form at plate boundaries
  • 35. Notes b. Mid-Ocean Ridges i. As the plates pull apart, magma wells up along the rift zone 1. The magma adds new lithosphere to the ridge c. Hot Spots i. Volcanoes that do not form at plate boundaries ii. Hot spot is beneath the lithospheric plate, and the plate moves over it

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