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Volcanoes

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Volcanoes Let s Talk Magma Felsic Magma High silica content Thick Light colored Slow moving Mafic Magma Low silica content Thinner Dark colored Easy flow Magma ... – PowerPoint PPT presentation

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Title: Volcanoes


1
Volcanoes
2
Lets Talk Magma
  • Felsic Magma
  • High silica content
  • Thick
  • Light colored
  • Slow moving
  • Mafic Magma
  • Low silica content
  • Thinner
  • Dark colored
  • Easy flow

3
Magmas Journey
  • Magma rises from the asthenosphere to cracks in
    the lithosphere
  • On its way to the surface, decreasing pressure
    lets dissolved gases expand
  • Once on the surface, magma becomes LAVA (because
    previously dissolved gases have escaped to the
    atmosphere and new materials have been added, the
    chemical composition has changed)

4
Lava Fragments
  • Tephra solid fragments of lava
  • Ash smallest pieces of tephra
  • Blocks large pieces of tephra erupted as solids
  • Bombs large pieces of tephra erupted as liquid
    (they harden as they fall)
  • Tephra Gases Superheated cloud

5
Types of Volcanoes
  • Cinder Cones
  • Shield Volcanoes
  • Composite Volcanoes
  • Volcanic Domes

6
Shield Volcanoes
  • The common product of hotspots, but they can also
    be found along subduction-related volcanic arcs
    or all by themselves
  • Almost exclusively BASALT (which is very fluid
    when erupted)
  • Slow, steady, non-explosive flow gives it a
    shield-like shape
  • Magma mixes with only oceanic crust on the way to
    the surface
  • Lava has a LOW silica content (50), so it has a
    LOW viscosity (resistance to flow)

7
Composite Volcanoes
  • Occur from the build-up of multiple eruptions
    that can be hundreds of years apart
  • Almost exclusively ANDESITE
  • Volcanologists call these "strato-" volcanoes
    because they consist of layers of solid lava
    flows mixed with layers of sand- or gravel-like
    volcanic rock called cinders or volcanic ash.
  • Magma mixes with oceanic (basalt) and continental
    (rhyolite) crust on the way to the surface
  • Lava has an intermediate silica content (60),
    soit moves at a medium pace

8
Volcanic Domes
  • Highly explosive!
  • Mainly RHYOLITE
  • Magma is typically too viscous to move far from
    the vent before cooling and crystallizing.
    Sothey are very steep sided
  • Magma mixes only with continental crust on way to
    surface
  • Lava has a high silica content (70) and moves
    slowly!
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