10.1 The nature of volcanic eruptions
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Transcript 10.1 The nature of volcanic eruptions
What causes a Volcano?
Volcanic activity often starts when a
crack develops in the crust. Magma is
then forced toward the surface.
Repeated eruptions of lava or
pyroclastic materials eventually build a
mountain which is called a volcano
Factors Affecting Eruptions
The primary factors that determine
whether a volcano erupts violently or not
include:
Magma Composition
Magma Temperature
Amount of dissolved gasses in the magma
Viscosity – is a substance’s resistance to flow
Ex- Syrup is thicker than water
Magma from a more explosive volcano can be 1000x
more viscous than that of a “quieter” volcano
Higher Temperature = less viscous
Lower Temperature = more viscous (hardens) =
mobility decreases
More Silica in magma = higher viscosity
Dissolved Gases
Gases are mostly water vapor and CO2
As magma gets closer to the surface,
the pressure of the magma is reduced,
which allows for the dissolved gases to
be released
Volcanic Material
Lava Flows
Depends on silica content
○ High silica = harder to flow
○ Low silica = more fluid like
Gases
Pyroclastic Materials
Particles that are produced in a volcanic
eruption
Fragments ejected during an eruption range in
size from extremely fine dust & ash to pieces
that weigh several tons
Types of Volcanoes
Shield Volcanoes
Cinder Cones
Composite Cones
Shield Volcanoes
Produced by the build up of fluid basaltic
lava
Shape = broad & slightly domed
Have “grown up” and from the sea floor
and have formed islands
Examples: Hawaiian Islands & Iceland
Cinder Cones
Cinder cones are built from ejected lava
fragments which harden in the air
Fragments range in size
Typically a result of gas rich basaltic
magma
Composed mostly of Pyroclastic
material
Occasionally releases lava
Shape: simple & smaller; determined by
the steep sided slopes
Usually the result of a single eruption
that lasts only a few weeks and very
rarely more than a few years
The eruption only occurs once due to
the fact that the pipe connecting the vent
to the magma chamber hardens
Composite Cones
Large & symmetrical
Composed of layers of lava &
pyroclastic material
Viscous lava (travel short distances)
Beautiful & possibly the most dangerous
Located in a narrow zone along the
Pacific Ocean “Ring of Fire”
Other Volcanic Landforms
Calderas – a large depression in a
volcano
Form in 1 of 2 ways: collapse of the top of a
shield volcano OR collapse of the top of a
composite volcano
Necks & Pipes
In most volcanoes, magma travels through
pipes that connect the magma chamber to
the surface
Lava Plateaus
The greatest volume of material comes from
fissures
Basaltic lava flows from the fissures (which
covers a large area)
Resources
http://video.nationalgeographic.com/vide
o/101-videos/volcanoes-101
http://discoverykids.com/games/volcanoexplorer/
Sources
Google
Prentice Hall Earth Science Book
National Geographic
Discovery