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Transcript
Chapter 6- Volcanoes
Which statement concerning
volcanoes is accurate?
A. All volcanoes erupt explosively.
B. Lava is the most deadly thing about
volcanoes.
C. Volcanic eruptions can influence
the climate of Earth.
D. Volcanoes occur in random
locations on the surface of Earth.
Volcanoes
• expulsion of molten rock (Lava), gases and
water vapor onto the surface of the Earth.
sometimes violently, sometimes not
- 1500 active volcanoes
> Active = erupted in recorded history
- e.g. Mauna Loa and Kilauea (Hawaii)
- Mt. St. Helens (Washington)
- Mt. Pinatubo (Philippines)
- Mt. Fujiyama (Japan)
- Mont Serrat (Caribbean)
Mt. Fujiyama, Japan
Dormant vs Extinct Volcanoes
•• Dormant volcanoes
- have not erupted recently, but may do so again.
> Mt. Vesuvius (Italy)
Extinct or
volcanoes
• -Extinct
inactive
volcanoes
have not recently
erupted
nor do they give indications
of erupting in the future.
> Thousands of these
types of volcanoes exist.
Mt. Kilamanjaro (Tanzania,Africa)
Types of Volcanoes
A small shield volcano in Iceland
What materials are not
commonly associated with
volcanic eruptions?
A. Lava
B. Steam
C. Gasses
D. All of the above are associated
with volcanic eruptions
Discussion: Why do some volcanoes erupt
explosively, whereas others erupt in a more
subdued fashion that is not explosive?
Water in magma
more water = more explosive
Magma composition
high silica content = high viscosity (flow resistance)
high viscosity = more explosive
Magma Temperature
cooler = higher viscosity (see above)
Gas content
more gas = more explosive
All factors are related to tectonic location
Composite Volcanoes
• a.k.a.- stratovolcanoes
- interbedded pyroclastics and lavas.
- typically andesitic to rhyolitic lava
> intermediate to felsic magma composition
- Found on continents and island arcs
> mostly associated with convergent plate
boundaries (subductive)
>
examples of composite
Mt. St. Helens, Mt. Vesuvius, Mt. Pinatubo,
Mt. Fujiyama, Mt. Kilamanjaro., Mt. Rainier
(photo)
Stratovolcano formation
Composite or Stratovolcanoes
Mayon volcano, Philippines, is a
nearly symmetrical composite
volcano.
View of Mount St. Helens,
Washington in 1978.
Cinder Cones
Primarily cinder-sized (0.25-1.0 mm) material.
but may have other sizes too.
Cinders fall to Earth and collect around the vent.
have steep slopes up to 33 degrees
smaller than shield volcanoes, usually less than
400 m tall
Form on the flanks of larger volcanoes.
Cinders and volcanic ash
QuickTime™ and a
Cinepak decompressor
are needed to see this picture.
Lava Types
Pahoehoe lava (smooth & ropey) in
Hawaii.
Lower viscosity lava
Aa lava (rough and blocky) also
in Hawaii.
Higher viscosity lava
Pillow Lavas
These bulbous
bulbous masses
pillow
These
masses of
of pillow
lava formed
formed when
when lava
lava erupted
erupted&&
lava
cooled under
cooled
under water.
water.
1 meter
Lava Fountain
QuickTime™ and a
Cinepak decompressor
are needed to see this picture.
It is possible to drive faster
than lava flows to escape it?
A. True
B. False
It is possible to outrun a
pyroclastic flow in a car.
A. True
B. False
Pyroclastic Ash Flow
'
aka Nuee Ardentes
Pyroclastic ash- lava blown up into the air
• smaller stuff is ash, larger stuff are
called "bombs"
Pyroclastic Ash Flow
• extremely fast (100's m/sec)
QuickTime™ and a
• extremely hot
TIFF (Uncompressed) decompressor
are needed to see this picture.
- sometimes glowing redhot
• extremely lethal
- many deaths associated with volcanic
eruptions are related to these events
>
e.g., Pompeii and Herculanum
Ash plume from a stratovolcano eruption
QuickTime™ and a
TIFF (Uncompressed) decompressor
are needed to see this picture.
Pyroclastic
flow
,
Nuee Ardente
QuickTime™ and a
H.263 decompressor
are needed to see this picture.
Lahar - volcanic
mudflow
QuickTime™
and a
decompressor
are needed to see this picture.
,
Lahars & Nuee Ardentes
• Lahars are mud flows that often occur after eruptions.
• Nuée ardentes are mobile dense clouds of incandescent ash that can move downhill at
speeds up to 100
, km/hr.
Mt Pelee destroyed St. Pierre on the island of Martinique, West Indies in 1902
The effects of explosive volcanic activity
Casts of people from
Pompeii, killed by ash from
Mt. Vesuvius, Italy
Gases and Magma
• Volcanic gases
- water vapor
- nitrogen
- hydrogen sulfide
• Felsic magmas
-
- carbon dioxide
- sulfur oxides
- chlorine
highly viscous : Si-rich
inhibits the expansion of gases
pressure builds up
explosive eruptions, like Mt. St. Helens.
• Mafic magmas
QuickTime™ and a
TIFF (Uncompressed) decompressor
are needed to see this picture.
- lower viscosity
- lower gas pressure
- erupt rather quietly, like Hawaiian Volcanoes.
Lake Nyos, a volcanic lake in Cameroon, Africa
CO2 emitted from the acidic lake killed 1700 villagers
near the lake in 1986
QuickTime™ and a
TIFF (Uncompressed) decompressor
are needed to see this picture.
Mt. St. Helens- May 18, 1980
QuickTime™ and a
Cinepak decompressor
are needed to see this picture.
Yellowstone
Caldera
QuickTime™ and a
Cinepak decompressor
are needed to see this picture.
QuickTime™ and a
TIFF (Uncompressed) decompressor
are needed to see this picture.
Bathymetry map of Crater lake, Oregon
QuickTime™ and a
TIFF (Uncompressed) decompressor
are needed to see this picture.
Volcanoes are randomly distributed
around the world with no discernable
pattern?
A. True
B. False
Distribution of volcanoes is not random
• related to plate tectonics
• commonly found along plate boundaries
Effects of Volcanoes and their activity
• builds up mountains and new land or destroys old
- (geosphere)
• kills many living things
- (biosphere)
• ejects ash and gases into the air
• Changing weather and climate patterns for several
months to a year
(atmosphere)
Causes changes in drainage patterns, and pollutes
•
many water sources
(hydrosphere)
Ash blocks incoming sunlight from space
(exosphere)