Title: Natural Hazards, 2e
1Natural Hazards, 2e
2Learning 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
3Learning 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
4Introduction
- Most volcanoes are near plate boundaries.
- Plate boundaries are where the magma is.
- Magma is molten rock.
- Lava is magma on the earths surface.
- Some active plate boundaries
- Subduction zones
- Mid-ocean ridges
- Continental rift zones
5Magma
- 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
6Tephra
- 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.
7Magma Types
- Basaltic
- Low silica content, low viscosity
- Andesitic
- Intermediate silica content, intermediate
viscosity - Rhyolitic
- High silica content, high viscosity
8Volcano Types
9Shield Volcanoes
- Largest volcanoes in the world
- Built almost entirely of lava flows
- Resemble a warriors shield
- Associated with basaltic magma
- Low viscosity, low gas content
- Gentle flowing lava with nonexplosive eruptions
- Can form lava tubes underground
10Shield Volcanoes, cont.
- Found in Hawaiian Islands, Iceland, and around
Indian Ocean
Figure 4.4
11Composite 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
12Composite Volcanoes
- Ex. Mt. St. Helens, Mt. Rainer, Mt. Fuji
Figure 4.6
13Volcanic Domes
- Made from highly viscous rhyolite magma
- Exhibit highly explosive eruptions
- Ex. Lassen Peak and Mono Craters
Figure 4.7
14Cinder 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
15Cinder Cone Volcanoes, cont.
Figure 4.8
16Volcanic 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
17Volcanic Features, cont.
- Hot springs
- Hot rocks heat groundwater discharged at surface
- Geysers
- Groundwater boils, erupting steam at surface
Figure 4.11b
18Volcanic 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
19Caldera Eruptions
Figure 4.14
Figure 4.15
20Volcanic Activity and Plate Tectonics
Figure 4.16
21Volcano 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
22Volcano 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
23Geographic Regions
- Ring of fire
- Pacific Ocean subduction zones
- Hot spots
- Hawaii and Yellowstone Park
- Mid-ocean ridges
- Iceland
- Rift valleys
- East Africa
24Figure 4.19
25Effects of Volcanoes
- 5060 volcanoes erupt each year.
- In U.S. 23 volcanoes
- 500 million people live close to volcanoes.
- Japan, Mexico, Philippines, and Indonesia
- Several U.S. cities vulnerable
26(No Transcript)
27Figure 4.20
28Lava Flows
- Rhyolitic, andesitic, and basaltic lavas
- Basaltic lavas flow most abundantly
- Pahoehoe 1 m/hr
- AA-1-3 m/day
Figure 4.21
Figure 4.22
29Pyroclastic 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.
30Ash Fall
- Vegetation destroyed
- Contaminates surface water
- Damage to buildings
- Health hazards
- Aircraft engine failure
Figure 4.24
31Pyroclastic Flow
- Responsible for more deaths than any other hazard
- Flow at 160 km/hr (100 mph)
- Temperatures gt1000C
32Poisonous 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
Figure 4.26b
33Debris 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.
34Figure 4.28
Figure 4.29
35Landslides
- Secondary effects of volcanoes
- Can cause tsunamis
36Mt. St. Helens
- Scene of volcanic explosion in recent history
- Well-studied example of Cascade volcanic eruption
Figure 4.30a
37Mt. St. Helens Before
Figure 4.30b
38Mt. St. Helens After
Figure 4.30c
39Mt. 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, 832 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)
40Bulge Avalanche
Figure 4.31a
Figure 4.31b
41Lateral Blast Vertical Eruption
Figure 4.31c
Figure 4.31d
42Mt. 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).
43Debris Avalanche and Ash Cloud
Figure 4.32a
Figure 4.32b
44Mt. St. Helens Summary
- 57 people were killed
- Flooding destroyed gt100 homes
- 800 feet of timber flattened
- Damage gt1 billion
- September 23, 2004, Mt. St. Helens reawakens
- Lava dome begins to form on crater floor
- Continues to form today
45Figure 4.34
46Links to other Hazards
- Earthquakes
- Landslides
- Fire
- Hot lava ignites plants and structures.
- Climate Change
- CO2 (and other gasses) from eruption alters
climate.
47Benefits 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.
48Benefits of Volcanoes cont.
- Recreation
- Health spas and hot springs
- Hiking, snow sports, and education
- Kilauea National Park
- Creation of New Land
- Hawaiian Islands
49Forecasting 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.
50Forecasting 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.
51Volcanic Alert or Warning
52Attempts to Control Lava Flows
- Hydraulic chilling
- Water used to chill and control the lava flow
- Iceland
- Wall construction
- Walls used to redirect lava flow
53End