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VOLCANOES
Chapter 13 Part 2
IV. Types of Volcanoes
e.g. Hawaiian Islands are examples of Shield Volcanoes
A. Shield Volcanoes1. Eruption: Non-explosive2. Formation: repeated lava
flows wide and short
IV. Types of Volcanoes
B. Cinder Cone Volcanoes1. Eruption: Explosive2. Formation: pyroclastic materials not
cemented together angle (∠) of repose = 30-40° ∠ that
is the steepest ejecta can pile up w/out sliding downhill narrow but tall
IV. Types of Volcanoes
C. Composite Volcanoes (Stratovolcano)
1. Eruption: Alternating Explosive w/ Non-Explosive
2. Formation: alternating lava flows w/pyroclastic materials
IV. Types of Volcanoes
C. Composite Volcanoes (Stratovolcano)
3. Dangers: a) Nuee ardente (aka glowing avalanche)
= ash + steam flow @ 125 mph downhill
b) Lahars = volcanic debri + water flow (due to melting snow or rainfall) mix flow downhill @ tremendous speed
IV. Types of Volcanoes
D. CalderasA. Magma chamber empties overlying
rock loses support collapses looks like a bowl sitting on earth
B. Often fills with H2O e.g. Crater Lake, OR
C. Can repeat process e.g. Crater Lake now has a
small composite volcano in its center
V. Effects of Volcanoes on Earth Destruction of property Alteration of climate, even in remote
areas Coats leaves of plants Clogs waterways Buries vegetation Lahars Great extinction of life due to cooler
climate
VI. Predicting Volcanic Eruptions
Geothermal image of lava flows at Kilauea Volcano, Hawaii
A. Earthquake activitya) Seismographs detect shifting of
magma
B. Temperature Changesa) Geothermal imaging of
satellites detect magma rising to surface
VI. Predicting Volcanic Eruptions
C. Surface Bulgesa) Tilt meters detect pressure increases
caused by magma rising to surface
D. Measuring output of volcanic gases