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The Nature of Volcanic Eruptions

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Title: The Nature of Volcanic Eruptions


1
The Nature of Volcanic Eruptions
  • Chapter 10, Section 1

2
Factors Affecting Eruptions
  • The primary factors that determine whether a
    volcano erupts violently or quietly include magma
    composition, magma temperature, and the amount of
    dissolved gases in the magma
  • Viscosity a substances resistance to flow
  • Something that is more viscous flows more slowly
    as a lava flow cools, it becomes more viscous as
    the lava slows down
  • The more silica there is in a lava, the more
    viscous that lava is
  • During explosive eruptions, the gases trapped in
    magma provide the force to eject molten rock from
    the vent, an opening to the surface

3
Factors Affecting Eruptions
4
Volcanic Material
  • The less silica content there is in a basaltic
    lava, the faster it will flow, lava flows are
    common in Hawaii
  • Magma contains varied amounts of dissolved gases
    held in the molten rock by confining pressure, it
    only is about 1 to 6 percent of the total weight
    of the magma
  • It is important to study the composition of
    volcanic gases, because they are the gases that
    formed the atmosphere in the past
  • Pyroclastic material name given to particles
    produced in volcanic eruptions
  • The fragments ejected during eruptions range in
    size from very fine dust and volcanic ash (less
    than 2 millimeters) to pieces that weigh several
    tons (blocks and lava bombs)

5
Volcanic Material
6
Concept Check
  • What is a volcanic bomb?
  • A large streamlined chunk of pyroclastic material
    that is larger than 64 mm in diameter.

7
Anatomy of a Volcano
  • The three main volcanic types are shield
    volcanoes, cinder cones, and composite cones
  • Volcanic activity often starts with a fissure, or
    crack, develops and magma is forced through it
  • Volcano a mountain built by repeated eruptions
    of lava or pyroclastic material often separated
    by long inactive periods
  • Crater steep-walled depression located at the
    top of many volcanoes
  • The form of the volcano is largely determined by
    the composition of the magma

8
Anatomy of a Volcano
9
Shield Volcanoes
  • Shield Volcano produced by the accumulation of
    fluid basaltic lavas
  • Shape broad, slightly domed structure that
    resembles a warriors shield
  • Most have grown from the ocean-floor to form
    islands (Hawaii and Iceland)

10
Shield Volcanoes
11
Cinder Cones
  • Cinder Cone built by ejected lava fragments the
    size of cinders, which harden in the air
  • Product of relatively gas-rich basaltic magma
  • Shape determined by the steep-sided slope that
    loose pyroclastic material maintains as it comes
    to rest
  • Usually the product of a single eruption that
    lasts only a few weeks, rarely a few years
  • The magma in the pipe solidifies after the
    eruption, and the volcano doesnt erupt again
  • Cinder cones are small, 30-300 meters and less
    than 700 meters in height
  • There are thousands of cinder cones around the
    world

12
Cinder Cones
13
Composite Cones
  • Composite Cone (Stratovolcano) large, nearly
    symmetrical structure composed of layers of both
    lava and pyroclastic deposits
  • The silica-rich magmas typical of composite cones
    generate viscous lavas that can only travel short
    distances
  • May generate the most explosive eruptions that
    eject huge quantities of pyroclastic materials
  • About 50 of these have erupted in the U.S. in the
    last 200 years
  • The most dangerous results of one of these
    eruptions is a pyroclastic flow (hot gases and
    rock fragments), coming at a speed of 200 km/hr
  • Lahars destructive mudflow created when
    volcanic debris becomes saturated with water and
    rapidly moves down the volcano, often following
    stream valleys

14
Composite Cones
15
Concept Check
  • What is a lahar?
  • A mudflow down the slope of a volcano.

16
Profiles of Volcanic Landforms
17
Other Volcanic Landforms
  • Caldera a large depression in a volcano
  • Forms by (1) collapse of the top of a composite
    volcano after an explosive eruption, or (2)
    collapse of the top of a shield volcano after the
    magma chamber is drained
  • Most volcanoes are fed magma through conduits,
    called pipes, connecting a magma chamber to the
    surface
  • When the volcano has been eroded, especially
    cinder cones, the harder solidified magma will
    remain and become a volcanic neck
  • Lava Plateau the greatest volume of volcanic
    material doesnt build volcanoes, but is extruded
    through fissures and flows over a large area

18
Formation of Crater Lake, Oregon
19
Volcanic Areas in the Northwestern United States
20
Assignment
  • Read Chapter 10, Section 1 (pg. 280-288)
  • Do Section 10.1 Assessment 1-7 (pg. 288)
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