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Natural Hazards, 2e. Volcanoes Chapter 4. Learning Objectives. Know the different types of volcanoes and their associated features Understand the relationship of volcanoes to plate tectonics Know what geographic regions are at risk from volcanoes

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natural hazards 2e

Natural Hazards, 2e

Volcanoes

Chapter 4

learning objectives
Learning Objectives
  • Know the different types of volcanoes and their associated features
  • Understand the relationship of volcanoes to plate tectonics
  • Know what geographic regions are at risk from volcanoes
  • Know the effects of volcanoes and how they are linked to other natural disasters
learning objectives cont
Learning Objectives, cont.
  • Recognize the potential benefits of volcanic eruptions
  • Understand how we can minimize the volcanic hazard
  • Know what adjustments we can make to avoid death and damage from volcanoes
introduction
Introduction
  • Most volcanoes are near plate boundaries.
  • Plate boundaries are where the magma is.
    • Magma is molten rock.
    • Lava is magma on the earth’s surface.
  • Some active plate boundaries:
    • Subduction zones
    • Mid-ocean ridges
    • Continental rift zones
magma
Magma
  • Described by silica content and amount of dissolved gasses.
  • Silica content affects viscosity.
    • Energy needed to make a liquid flow
    • High silica content, high viscosity
  • Gas content determines how explosive the eruption will be.
    • High gas content, greater the explosion
tephra
Tephra
  • Gasses will cause lava and other debris to be expelled from the volcano.
  • Also called pyroclastic materials.
  • Range in size from dust-sized materials, gravel-sized lapilli, to large block-sized bombs.
magma types
Magma Types
  • Basaltic
    • Low silica content, low viscosity
  • Andesitic
    • Intermediate silica content, intermediate viscosity
  • Rhyolitic
    • High silica content, high viscosity
shield volcanoes
Shield Volcanoes
  • Largest volcanoes in the world
  • Built almost entirely of lava flows
    • Resemble a warrior’s shield
  • Associated with basaltic magma
    • Low viscosity, low gas content
  • Gentle flowing lava with nonexplosive eruptions
  • Can form lava tubes underground
shield volcanoes cont
Shield Volcanoes, cont.
  • Found in Hawaiian Islands, Iceland, and around Indian Ocean

Figure 4.4

composite volcanoes
Composite Volcanoes
  • Associated with variety of magmas, basaltic to lavas between andesitic and rhyolitic
    • Higher viscosity and gas content
  • Built from a combination of lava flows and pyroclastic deposits
    • Have a cone shape, also called stratovolcanoes
  • Explosions more violent and dangerous
composite volcanoes12
Composite Volcanoes
  • Ex.: Mt. St. Helens, Mt. Rainer, Mt. Fuji

Figure 4.6

volcanic domes
Volcanic Domes
  • Made from highly viscous rhyolite magma
  • Exhibit highly explosive eruptions
  • Ex.: Lassen Peak and Mono Craters

Figure 4.7

cinder cone volcanoes
Cinder Cone Volcanoes
  • Small volcanoes
  • Built entirely from tephra
    • Small pieces of black or red lava
  • Common on larger volcanoes, normal faults, or along cracks and fissures
  • Ex.: Paricutin, Mexico
volcanic features
Volcanic Features
  • Craters
    • Depressions formed by explosion or collapse of volcano top
  • Calderas
    • Very large craters formed from violent explosions
  • Vents
    • Any opening for lava and debris
    • Can produce flood basalts
volcanic features cont
Volcanic Features, cont.
  • Hot springs
    • Hot rocks heat groundwater discharged at surface
  • Geysers
    • Groundwater boils, erupting steam at surface

Figure 4.11b

volcanic features cont18
Volcanic Features, cont.
  • Caldera eruptions
    • Very large, very violent eruptions
    • Produce calderas
    • Very rare
    • Most recent North American caldera eruptions 640 mya at Yellowstone National Park and 700 mya at Long Valley, California
caldera eruptions
Caldera Eruptions

Figure 4.14

Figure 4.15

volcano origins
Volcano Origins
  • Mid-ocean ridges
    • Basaltic magma from asthenosphere
    • Shield volcanoes
    • Ex.: Iceland at Mid-Atlantic Ridge
  • Subduction zones
    • Andesitic magma from melting tectonic plate
    • Composite volcanoes
    • Ex.: Cascade Mountains
volcano origins22
Volcano Origins
  • Hot spots beneath oceans
    • Basaltic magma
    • Shield volcanoes
    • Ex.: Big Island of Hawaii
  • Hot spots beneath continents
    • Rhyolitic magma from mixes of rising magma and continental crust
    • Caldera eruptions
    • Ex.: Yellowstone National Park
geographic regions
Geographic Regions
  • Ring of fire
    • Pacific Ocean subduction zones
  • Hot spots
    • Hawaii and Yellowstone Park
  • Mid-ocean ridges
    • Iceland
  • Rift valleys
    • East Africa
effects of volcanoes
Effects of Volcanoes
  • 50–60 volcanoes erupt each year.
    • In U.S. 2–3 volcanoes
  • 500 million people live close to volcanoes.
    • Japan, Mexico, Philippines, and Indonesia
    • Several U.S. cities vulnerable
lava flows
Rhyolitic, andesitic, and basaltic lavas

Basaltic lavas flow most abundantly:

Pahoehoe – 1 m/hr

A’A’-1-3 m/day

Lava Flows

Figure 4.21

Figure 4.22

pyroclastic activity
Pyroclastic Activity
  • Tephra is blown into atmosphere.
  • Ash fall
    • Ash is blown high into air and falls onto areas.
  • Lateral blast
    • Rock fragments are blown horizontally from volcano.
  • Pyroclastic flow
    • Avalanches of hot rock, ash, glass fragments.
ash fall
Ash Fall
  • Vegetation destroyed
  • Contaminates surface water
  • Damage to buildings
  • Health hazards
  • Aircraft engine failure

Figure 4.24

pyroclastic flow
Pyroclastic Flow
  • Responsible for more deaths than any other hazard
  • Flow at 160 km/hr (100 mph)
  • Temperatures >1000C
poisonous gases
Carbon dioxide (CO2)

Odorless, heavy gas that can displace breathable air

Sulfur dioxide

Odorous gas that causes acid rain and can contaminate rock and soil

Poisonous Gases

Figure 4.26b

debris mud flows
Debris & Mud Flows
  • Also known as lahars
  • Volcanic activity melts ice, snow, or glaciers on a volcano.
    • Water mixes with ash, other tephra
    • Mixture becomes unstable and flows down volcano
  • Populous areas of Pacific Northwest are built on old mudflows.
  • Not unlikely for new flows to occur.
slide34

Figure 4.28

Figure 4.29

landslides
Landslides
  • Secondary effects of volcanoes
  • Can cause tsunamis
mt st helens
Scene of volcanic explosion in recent history

Well-studied example of Cascade volcanic eruption

Mt. St. Helens

Figure 4.30a

mt st helens timeline
Mt. St. Helens – Timeline
  • 120 years of dormancy
  • March 1980 – seismic activity & small explosions
  • May 1 – bulge begins to grow on northern flank at rate of 1.5m (5 ft) per day
  • May 18, 8:32 am – M 5.1 earthquake triggers landslide/debris avalanche of the bulge area
  • Seconds later, lateral blast from bulge area at rate of 480 km/hr (300 mph)
bulge avalanche
Bulge & Avalanche

Figure 4.31a

Figure 4.31b

lateral blast vertical eruption
Lateral Blast & Vertical Eruption

Figure 4.31c

Figure 4.31d

mt st helens timeline cont
Mt. St. Helens – Timeline, cont.
  • One hour after blast: vertical cloud of ash extends to stratosphere.
  • 9 hours of ash falls to cover areas of Washington, northern Idaho, western and center Montana.
    • Pyroclastic flows begin at this time down the northern slope.
  • Mudflows begin at speeds of 29-55 km/hr (18-34 mph).
debris avalanche and ash cloud
Debris Avalanche and Ash Cloud

Figure 4.32a

Figure 4.32b

mt st helens summary
Mt. St. Helens – Summary
  • 57 people were killed
  • Flooding destroyed >100 homes
  • 800 feet of timber flattened
  • Damage >$1 billion
  • September 23, 2004, Mt. St. Helens reawakens
    • Lava dome begins to form on crater floor
    • Continues to form today
links to other hazards
Links to other Hazards
  • Earthquakes
  • Landslides
  • Fire
    • Hot lava ignites plants and structures.
  • Climate Change
    • CO2 (and other gasses) from eruption alters climate.
benefits of volcanoes
Benefits of Volcanoes
  • Volcanic Soils
    • Good for coffee, maize, pineapples, sugar cane, and grapes
  • Geothermal power
    • Can create energy for nearby urban areas
  • Mineral Resources
    • Gold, silver, etc. and nonmetallic rocks
    • Used for soap, building stone, aggregate for roads, railroads, etc.
benefits of volcanoes cont
Benefits of Volcanoes cont.
  • Recreation
    • Health spas and hot springs
    • Hiking, snow sports, and education
    • Kilauea National Park
  • Creation of New Land
    • Hawaiian Islands
forecasting a volcanic eruption
Forecasting a Volcanic Eruption
  • Seismic activity
    • Shallow earthquakes and swarms can precede eruption.
    • May not provide enough time for evacuation.
  • Thermal, magnetic, and hydrologic monitoring
    • Accumulation of hot magma changes temperatures, magnetic properties, and temperature position of groundwater.
forecasting a volcanic eruption50
Forecasting a Volcanic Eruption
  • Land surface monitoring
    • Monitoring growth of bulges or domes.
    • Kilauea tilts and swells.
  • Monitoring volcanic gas emissions
    • Changes in CO2 amounts correlate with volcanic processes.
  • Geologic history
    • Mapping of volcanic rocks and deposits give idea of types of effects to be expected.
attempts to control lava flows
Attempts to Control Lava Flows
  • Hydraulic chilling
    • Water used to chill and control the lava flow
    • Iceland
  • Wall construction
    • Walls used to redirect lava flow
slide53

End

Volcanoes

Chapter 4

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