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Volcanic Hazards p. 138-140, web reading • Volcano Facts • Volcano Hazards • Fall processes • Flow processes • Other types • Predicting Volcanic Eruptions

Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

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Page 1: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Volcanic Hazardsp. 138-140, web reading

• Volcano Facts• Volcano Hazards

• Fall processes• Flow processes• Other types

• Predicting Volcanic Eruptions

Page 2: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

YellowstoneOld Faithful

Giant Caldera Volcano: Yellowstone

Ground collapse ~ Area of NYCMaterial ejected ~1000 km3

Ash Fall

Page 3: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Toba, IndonesiaThe Biggest Eruption?

• 75,000 years ago

Page 4: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Toba, IndonesiaThe Biggest Eruption?

• Caldera diameter 100x35 km• Volume erupted 2,800 km3

– 10 cm of ash fell in India, 3000 km away

• Volcanic winter for a decade– With global cooling 3-5°C

• Might have affected human evolution

Page 5: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Volcanic Eruptions over the last 10,000 years

• 1300 active volcanoes• 550 eruptions (< 2000 yrs)• <10% potentially destructive volcanoes

have been studied in detail

~800 million people worldwide @ risk>50% of world’s volcanoes in nations with per capita GDP <20% US

Page 6: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Volcanic Hazards

Fall ProcessesFlow Processes

Web reading

Page 7: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Lava FlowsBasaltic lava (low viscosity)Usually slow moving (<10 mph)Rarely life threatening

Page 8: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Nyiragongo volcano, CongoGoma, Jan. 19, 2002

Page 9: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Nyiragongo volcano, CongoGoma, Jan. 19, 2002

Page 10: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Pyroclastic Flows

High density mixture of hot ash, rock, and hot gases Temp. >500CVelocity > 80-100 mph

Page 11: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Pyroclastic Flows

Page 12: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Mt Unzen, Japan• Pyroclastic flows• Eruption in June,

1991, killed 40 journalists and 3 experienced volcanologists

Page 13: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Ash Falls (Tephra Falls)

Mount Pinatubo, Philippines June 1991

•can cover large areas for days to weeks•ash will last on the ground for months to years•making land and water unusable•provide material for future hazards (lahars)

Page 14: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Ash fall in Rabaul, Papua New Guinea, 1994

Page 15: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Volcanic Ash–Danger to Aircraft

Volcanic ash can be a serious hazard to aviation even thousands of miles from an eruption. Airborne ash can diminish visibility, damage flight control systems, and cause jet engines to fail.

USGS

Part of a 747 engine

Page 16: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Poisonous Gas Emissions

Lake Nyos, Cameroon

CO2, SO2, HCl, HFH2S

Volcanic Smog-Vog

Page 17: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

CO2 gas from Magma

Bottom of lakeSaturated in CO2

Lake Nyos

Poisonous Gas EmissionsLake Nyos, Cameroon (1986)

“River” of CO2

50 m thick layer

Controlled degassing, 1995

Page 18: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Volcanic LandslidesMt. St. HelensMay 18, 1980Debris Flow2.3 km3 of material

Largest debris landslide in recorded history

Page 19: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

The avalanche traveled approximately 15 miles downstream at a velocity exceeding 150 mph. It left behind a hummocky deposit with an average thickness of 150 feet and a maximum thickness of 600 feet.

Page 20: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Figure 5.10

Mt. St. Helens May 18, 1980

Page 21: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Mt. St. Helens

Page 22: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Lahars (Mudflows)

• A mixture of volcanic fragments and water

• Mudflows are channeled along valleys on the flanks of volcanoes.

• Mudflows have the consistency of wet concrete and move at high speeds (up to 20-60 mph).

Pinatubo

Page 23: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Nevado del RuizNov. 13, 1985Canyon that

channeled the lahar that destroyed Armero and killed 23,000 people

Page 24: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

The November 13, 1985 lahar from Nevado del Ruiz

Town of Armero

Page 25: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions
Page 26: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Volcano Monitoring and Prediction

Goal: Prevent a Volcanic Crisis from turning into a Volcanic Disaster

Page 27: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Volcanoes of the “Lower

48”

Page 28: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Volcano Monitoring and Prediction

Long-Term based on Historical Records and Geologic History

Age-dating ofvolcanic deposits Eruption Frequency

Types and amounts oferuption products Size of Eruption

Page 29: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Volcano Monitoring and PredictionShort Term: systematic observations of volcano’s visible and subsurface activity

SeismicityGround tiltGas emissions

Page 30: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Rising MagmaGround DeformationRising magma and increasing pressure exerted by

gases often cause volcanoes to deform, or swell, before an eruption

Page 31: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Rising Magma

Magma rises into reservoir beneath volcano

Rising magma and volcanic gases exert pressure

Moving Magma and Volcanic Fluids Trigger Earthquakes

High pressure causes rocks to break, triggering earthquakes

Page 32: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Forecasting Volcanic Activity• Ideal Forecast includes

– Location– Timing– Character of eruption and

magnitude

Page 33: Volcanic Hazards p. 138-140, web reading Volcano Facts Volcano Hazards Fall processes Flow processes Other types Predicting Volcanic Eruptions

Forecasting Volcanic Activity• Ideal Forecast includes

– Location– Timing– Character of eruption and

magnitude

•Effective Forecasting involves•Scientists•Public officials•News media•Informed Public

Friday VideoPath of a Killer VolcanoMt. Pinatubo eruption of 1991