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Volcanoes

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Volcanoes Convergent Volcanism Most volcanoes on land occur because oceanic plates subduct under continental plates. As the oceanic plate descends, magma forms. – PowerPoint PPT presentation

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Title: Volcanoes


1
Volcanoes
2
Learning Targets
  • Describe how plate tectonics influences the
    formation of volcanoes
  • Locate major zones of volcanism
  • Identify the parts of a volcano
  • Differentiate between volcanic landforms

3
Volcanism
  • All the processes associated with the discharge
    of magma, hot fluids, and gases.
  • In any given year, 60 volcanic eruptions will
    occur.

4
Volcanism
  • The majority of volcanoes are found at plate
    boundaries.
  • Most are found at convergent boundaries or
    divergent boundaries.

5
Convergent Volcanism
  • Most volcanoes on land occur because oceanic
    plates subduct under continental plates.
  • As the oceanic plate descends, magma forms.
  • Eventually the magma moves up because it is less
    dense.
  • These volcanoes have explosive eruptions.

6
Convergent Volcanism
  • Most convergent volcanoes are found in two major
    geographic belts
  • Pacific Ring of Fire (Circum-Pacific)
  • Mediterranean Belt

7
Pacific Ring of Fire
8
Mediterranean Volcanic Belt
9
Divergent Volcanism
  • At divergent boundaries in the ocean, new ocean
    floor is produced as magma fills up the new gaps.
  • These volcanoes are rarely explosive.

10
Hot Spots
  • Some volcanoes form far away from plate
    boundaries.
  • These are called hot spot volcanoes.
  • It is theorized that hot spots form in unusually
    hot regions of Earths mantle
  • Most are formed under the ocean and form islands
    (Hawaii).

11
Learning Target
  • Describe how plate tectonics influences the
    formation of volcanoes.
  • Where are the major zones of volcanism? What is
    significant about their locations?

12
Anatomy Of A Volcano
13
Anatomy of a Volcano
  • Conduit tube structure through which lava
    travels to reach the surface
  • Vent an opening in the conduit to allow lava to
    leave the conduit
  • Crater a bowl shaped depression formed around
    the vent
  • Caldera a larger depression that can form later

14
Types of Volcanoes
  • Shield Volcano
  • Mountain with broad sloping sides and circular
    base
  • Largest volcano
  • Usually not very explosive

15
Types of Volcano
  • Cinder Cones
  • Steep sides generally small
  • Form when small pieces of magma pile up around
    the vent
  • Often form around larger volcanoes

16
Types of Volcanoes
  • Composite Volcanoes
  • Formed from hardened chunks of lava from very
    violent eruptions
  • Cone shaped but are larger than cinder cones
  • Very explosive generally

17
Learning Targets
  • List the parts of a volcano and then define each.
  • Differentiate between volcanic landforms.

18
Magma Formation
  • Magma can be formed by
  • Melting the crust
  • Melting in the mantle
  • Four main factors are involved
  • Temperature
  • Pressure
  • Water Content
  • Mineral content of crust

19
Magma Formation
  • Temperature increases with depth in Earths crust
  • Pressure also increases with depth due to weight
    of overlying rocks
  • Water content rocks often have water in them
    which changes melting point of rocks as water
    content increases, melting point decreases

20
Magma Formation
  • Mineral Content
  • Different minerals have different melting points
  • Basalt has a high melting point
  • Granite is lower
  • Generally rocks with high iron and magnesium melt
    at higher temperatures

21
Magma Formation
  • Viscosity
  • The physical property that describes a materials
    resistance to flow
  • Cooler magma has a higher viscosity (its
    thicker) it resists flowing

22
Formation of Magma
23
Types of Magma
  • Balsaltic magma
  • Forms when rocks in upper mantle melt
  • Less than 50 silica
  • Low viscosity
  • Found in quiet eruptions
  • Kilauea in Hawaii

24
Types of Magma
  • Andesitic magma
  • 50-60 silica
  • Found along oceanic-continental subduction zones
  • Intermediate viscosity
  • Intermediate explosivity

25
Types of Magma
  • Rhyolitic magma
  • More than 60 silica
  • High viscosity
  • Very explosive

26
Explosive Eruptions
  • When lava is too viscous to flow freely, pressure
    builds up until the volcano explodes. This throws
    lava and rock into the air.
  • Tephra is the pieces of lava or pieces of crust
    thrown into the air

27
Explosive Eruptions
  • Pyroclastic flows
  • Tephra that is rapidly moving mixed with hot
    (over 700oC) suffocating gases
  • Mt. Pelee in the Carbbean Sea killed 29,000.
  • Death caused by suffocation or burned to death

28
Learning Targets
  • Explain how magma type influences volcanic
    activity.
  • Discuss the role of temperature, pressure and
    dissolved gases in eruptions.
  • Recognize classifications of material ejected by
    eruptions.

29
Mount Rainer, Washington 4392 m.
  • Mount Rainer is potentially the most dangerous
    volcano in the Cascades because it is very steep,
    covered in large amounts of ice and snow, and
    near a large population that lives downhill.

30
Mount Erebus, Antarctica 3794 m
  • -Southernmost historically active glacier
  • -Capped by an elliptical 500 x 600 m. wide. 110
    m. deep summit crater with an active lava lake
    continuous activity since 1972
  • -Occasional strombolian eruptions eject lava
    bombs onto crater rim

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Devils Tower, Wyoming
http//volcano.und.nodak.edu/vwdocs/kids/legends.h
tml
33
Caldera
  • A large depression created by the collapse of a
    volcano
  • Magma chamber drains
  • Loss of structural support
  • Collapse of overlying material

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Volcanoes are good!
  • Produced our atmosphere
  • Volcanic soil very fertile
  • Beautiful scenery
  • Mineral resources
  • -Diamonds, copper, gold, lead, zinc, etc.
  • -Pumice, BBQ rocks, Aquarium stones
  • Geothermal heat
  • Geologic time markers
  • Eruptions make for a good story line!

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