Class Announcements Term Break extra credit option due by end of period today. Sign up to attend a...

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Class Announcements Class Announcements Term Break extra credit option due by end of period today. Sign up to attend a Papago Park extra credit field trip (worth 20 points). Options: Wed., April 16: 10-11AM or 4-5 PM
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Page 1: Class Announcements Term Break extra credit option due by end of period today. Sign up to attend a Papago Park extra credit field trip (worth 20 points).

Class AnnouncementsClass AnnouncementsTerm Break extra credit option due by end of period today.

Sign up to attend a Papago Park extra credit field trip (worth 20 points).

Options:

Wed., April 16: 10-11AM or 4-5 PM

Thurs., April 17: 10-11AM or 2-3 PM

Page 2: Class Announcements Term Break extra credit option due by end of period today. Sign up to attend a Papago Park extra credit field trip (worth 20 points).

Today’s Lecture:Today’s Lecture: Chap. 9 Chap. 9 VolcanoesVolcanoes

Class presentations:

Cancer-causing gas in Beverly Hills CA - Michael Zara

Mt. Rainier - Nathan Policar

Intermediate volcanoes (cont.)

Calderas

Volcanic hazards

Case Study: Mt. Saint Helens

Economic aspects:

Hydrothermal activity

Mineral deposits

Volcanic Activity on Other Planets

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a.a. Calderas Calderas

b.b. Lava domes Lava domes

summit crater greater than 1 km wide from collapse of summit

viscous felsic magma usually form after explosive eruption of gas-rich magma

Some Other Important Volcanic Features

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Fig. 09.11ab

W. W. Norton

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Volcano startsto erupt.

Full magmachamber

Main explosiveeruption

Magma chamberempties.

Newly formedcaldera

Collapsed blocks

Empty magmachamber

New volcaniccone grows.

Lake fillscaldera.

Ash and debris

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Fig. 09.29b

© 1997 Birke Schreiber

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Mount St. Helen’s

Lava dome

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Case study: Mt. St. Helens

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Case study:Mt. St. Helens

•Located in the Cascade volcanic range, NW US.

•Result of past/present subduction of oceanic crust in the Cascadia Trench

•Many volcanoes there are still active

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9500’

8150’(1350’ shorter!)

Case study:Mt. St. Helens

Ejected nearly a cubic kilometer of ash & rock debris

59 deaths

Ash blown over 11 miles high!

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Fig. 09.15

W. W. Norton

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Fig. 09.16abc

W. W. Norton

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Fig. 09.22e

Photo by J. Marso, U.S. Geological Survey

Volcanic mudflows

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Mount Saint Helens

A lava dome

formed

in crater

after major

eruption.

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Hydrothermal Systems:

Develop anywhere that fluids coexist with a heat source.

Typical heat source a magma intrusion.

Effects: Alteration of adjacent rocks and deposition of mineral deposits, often of economic importance.

Also a source of geothermal energy.

GENERAL FEATURES OF HYDROTHERMAL

SYSTEMS

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Hydrothermal Springs: Natural Laboratories for studying microbial fossilization.

Grand Prismatic Spring

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1: Lava flows

2: Ash falls

3: Ash flows

4: Mud flows

Videos: Types of Volcanic Eruptions

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VENUS

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Volcanoes Elsewhere in Solar System

MARS

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Fig. 09.30a

JPL / NASA

Olympus Mons: Largest Volcano in the Solar System

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Olympus Mons, Mars

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Jupiter’s moon “Io”

From Scientific American, Feb 2000

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Jupiter’s moon “Io”

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Fig. 09.30b

JPL / NASA

Volcanic Eruptions in Progress on Io