chapter 5 volcanoes and volcanism. introduction about 550 volcanoes have been active in historical...
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Chapter 5
Volcanoes and Volcanism
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Introduction
About 550 volcanoes have been active in historical times.
About 12 or so erupt each year; most eruptions are small and go unnoticed
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Introduction
Volcanism is the eruption of magma and associated gases at the surface.
Some magma erupts explosively as pyroclastic ("fire-broken") rock and others erupt as lava flows.
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Introduction
How can volcanism be both constructive and destructive? Volcanism may cause
injuries and fatalities, and destroy property.
Volcanism is also responsible for the origin of many oceanic islands, fertile farmland, and critical atmospheric gases.
Fig. 5.1, p. 111Pompeii and Mount Vesuvius
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Volcanoes and Volcanism
Types of Volcanoes Not all volcanoes erupt from giant cones, some erupt
from fissures (fractures) in the Earth's crust.
Volcanoes were once active on all the inner planets of our Solar System and our Moon. Today, volcanoes are still active on Earth and possibly on Venus.
Jupiter's moon, Io, has active sulfur volcanoes.
Triton, a moon of Neptune, probably has volcanoes that erupt liquid methane (natural gas or CH4).
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Volcanoes and Volcanism
Volcanic Gases
Gases, primarily water vapor, constitute only a small portion of magmas
Lesser amounts of carbon dioxide, nitrogen, sulfur dioxide, and hydrogen sulfide
Very small amounts of carbon monoxide, hydrogen, and chlorine
Fig. 5.2, p. 112
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Volcanoes and Volcanism
Volcanic Gases Most volcanic gases dissipate
without harm to humans
Chlorine gas may contribute to the deterioration of the ozone layer, which protects organisms from ultraviolet radiation (Geo-Focus, pp. 122-123)
Sulfur gases from large eruptions may cool global climates for 1-2 years
Fig. 5.2, p. 112
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Volcanoes and Volcanism
Low Viscosity Mafic Lava Flows
Mafic lavas may flow through near surface lava tubes
Mafic lava flows may reach speeds of 50 km/hr
Fig. 5.4, p. 113
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Volcanoes and Volcanism
Mafic Lava Flows on Land Aa lava flows consist of angular blocks and
fragments. Pahoehoe lava flows have a smooth
surface, much like taffy.
Fig. 5.5, p. 114
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Volcanoes and Volcanism
Underwater Mafic Lava Flows
Pillow lavas are bulbous, interconnecting masses that result from underwater eruption of basaltic lavas.
Fig. 5.6a, p. 114
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Volcanoes and Volcanism
Lava Flows
Columnar Joints Columnar joints form in response to the cooling
and contraction of lava. They most commonly occur in basalt and andesite lava flows.
Fig. 5.7, p. 115
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Fig. 5-7, p. 115
Stepped Art
As lava cools and contracts, three-pronged cracks form that grow and intersect to form four- to seven-sided columns, most of which are six-sided.
Surface view of the columns from (b). The straight lines and polish resultedfrom abrasion by a glacier that moved over this surface.
Columnar joints in a basalt lava flow at Devil’s Postpile NationalMonument in California. The rubble in the foreground is collapsed columns.
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Pyroclastic Materials
Volcanoes and Volcanism
Pyroclastic materials are magma fragments that are explosively ejected by volcanoes, most are solid
Ash < 2mm in diameter (smaller than sand grains)
Lapilli, 2-64 mm Bombs, partially molten, >64 mm Blocks, solid, >64 mm
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Volcanoes and Volcanism
Pyroclastic Materials Volcanic ash, unlike larger pyroclastic materials, may be
transported by winds over long distances.
Ash is unhealthy for lungs and dangerous to aircraft because it fouls jet engines.
Ash falls settle out of the atmosphere.
Ash flows are turbulent clouds of ash and gas that travel close to the surface during pyroclastic eruptions.
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Types of Volcanoes
A volcano is a hill or mountain that forms around a vent, where lava, pyroclastic materials and gases erupt.
Fig. 5.12c, p. 119
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Types of Volcanoes
Calderas
A caldera is a large oval to circular volcanic depression that forms when the summit of a volcano collapses into its magma chamber following voluminous eruptions.
Fig. 5.8, p. 116
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Types of Volcanoes
Shield Volcanoes
Shield volcanoes have gentle slopes and are largely composed of basalt with possibly some mafic pyroclasts. The Hawaiian volcanoes are shield volcanoes.
They are usually non-explosive and pose little danger to humans.
Fig. 5.9, p. 117
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Types of Volcanoes
Shield Volcanoes
The largest volcano in the Solar System, Olympus Mons on Mars, is a shield volcano.
Fig. 5.10b, p. 117
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Types of Volcanoes
Cinder Cones
Cinder cones consist of cinders and other pyroclastic materials. They accumulate as steep-sloped cones that rarely exceed 400 meters high.
Fig. 5.11, p. 118
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Types of Volcanoes
Composite Volcanoes (Stratovolcanoes)
Composed of layers of lava flows, pyroclastic debris and volcanic mud flows (lahars). They are explosive and are the most dangerous to humans. The volcanoes rimming the Pacific ocean are mostly composite volcanoes. Most composite volcanoes have intermediate compositions.
Fig. 5.12a,b, p. 119
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Types of Volcanoes
Some Notable Volcanic Eruptions, Many Involving Deadly Composite Volcanoes
Table 5.1, p. 120
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Table 5.1, p. 120
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Types of Volcanoes
Composite Volcanoes (Stratovolcanoes)
Lahars are mudflows consisting of mixtures of liquid water and pyroclastic materials. They may be hot or cold, and often form from rain during eruptions.
Fig. 5.13, p. 119
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Types of Volcanoes
Composite Volcanoes (Stratovolcanoes)
Lahars may also form without an eruption if a submit of a volcano heats up, catastrophically melts snow and ice, and the resulting water mixes with pyroclastic materials from previous eruptions.
Fig. 5.13, p. 119
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Types of Volcanoes
Lava Domes
Bulbous lava domes form when viscous, usually felsic or intermediate, lavas are forced up through the conduits of some volcanoes. These volcanoes can erupt explosively and commonly eject nuée ardentes (hot clouds of pyroclastic materials and gas).
Fig. 5.14, p. 120
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Types of Volcanoes
Lava Domes
Nuée ardentes are hot clouds of pyroclastic materials and gas that are released by explosive eruptions.
In 1902, a nuée ardente engulfed the city of St. Pierre on Martinique in the Caribbean. 28,000 people were killed.
Fig. 5.15, p. 121
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Types of Volcanoes
Supervolcano Eruptions
No supervolcano eruptions have occurred within recorded history
Erupt hundreds of square kilometers of material and produce huge calderas
Three supervolcano eruptions have occurred in Yellowstone within the past 2 million years
Figure 5.16, p. 124
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Other Volcanic Landforms
Fissure Eruptions and Basalt Plateaus Basalt plateaus form when fluid mafic lava erupts
from long fissures (not vents), known as a fissure eruption. Basalt plateaus are made up of numerous overlapping basalt lava flows.
Fig. 5.17a,b, p. 124
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Other Volcanic Landforms
Pyroclastic Sheet Deposits Huge sheet-like eruptions of pyroclastic
materials, especially ash, can cover large areas when erupted from fissures during caldera formation.
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Volcano Belts
Volcanoes are usually not randomly distributed, but occur in well-
defined zones or belts along plate boundaries.
Fig. 5.18, p. 125
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Volcano Belts
About 60% circum-Pacific belt, 20% Mediterranean, belt, 20% are at or near mid-oceanic ridges
Fig. 5.18, p. 125
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North America’s Active Volcanoes
Alaska’s Volcanoes Alaska’s volcanoes stretch from the mainland of
Alaska through the Aleutian Islands.
Fig. 5.18, p. 125
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North America’s Active Volcanoes
Alaska’s Volcanoes Most are composite volcanoes, some with huge calderas. This
volcanic arc is extremely active with many explosive eruptions.
Fig. 5.18, p. 125
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North America’s Active Volcanoes
The Cascade Range: Lassen Peak in California to British Columbia, Canada
Mostly composite volcanoes, but there are also two huge shield volcanoes and numerous cinder cones
Fig. 5.19 a-c, p. 127
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North America’s Active Volcanoes
The Cascade Range: Lassen Peak in California to British Columbia, Canada
Results from the subduction of the oceanic Juan de Fuca Plate underneath the continental North American Plate
Fig. 5.19 a-c, p. 127
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Plate Tectonics, Volcanoes, and Plutons
Igneous Activity at Divergent Plate Boundaries
Volcanic activity at or near mid-oceanic ridges is mainly submarine, but in a few places such as Iceland, it occurs above sea level. The volcanoes that form are mostly mafic shield volcanoes.
Fig. 5.6a, p. 114
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Plate Tectonics, Volcanoes, and Plutons
Igneous Activity at Convergent Plate Boundaries
The volcanism in the circum-Pacific and Mediterranean belts results from subduction.
Most of the magmas are produced by the partial melting of the subducted plates.
Fig. 5.18, p. 125
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Plate Tectonics, Volcanoes, and Plutons
Intraplate Volcanism
Mafic hotspot volcanism
The Hawaiian Islands formed as a series of volcanoes originating from a stationary mantle plume as the Pacific Plate moved over it.
Fig. 5.4, p. 113
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Volcanic Hazards, Volcano Monitoring, and Forecasting Eruptions
Lava dome eruptions with huge amounts of pyroclastic materials and gases are the most dangerous volcanic eruptions.
Lahars are also dangerous and they may occur without an eruption.
Fig. 5.20, p. 129
What are the most dangerous manifestations of volcanoes?
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Volcanic Hazards, Volcano Monitoring, and Forecasting Eruptions
How Large Is an Eruption and How Long Do Eruptions Last?
VEI - the most widely used indication of the size of a volcanic eruption is the volcanic explosivity index
The VEI measures the explosive intensity of an eruption using: volume of material erupted eruption cloud height
Fig. 5.21, p. 130
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Fig. 5.21, p. 130
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Plinian
VEI 4-7
CATACLYSMIC
Fig. 5-21, p. 130
Stepped Art
EXPLOSIVE
Strombolian
VEI 1-3Vulcanian
VEI 3-5
GENTLE
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Volcanic Hazards, Volcano Monitoring, and Forecasting Eruptions
Is It Possible to Forecast Eruptions?
Monitoring volcanoes helps geologists to forecast imminent eruptions
Fig. 5.22, p. 130
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Fig. 5.22, p. 130
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Volcanic Hazards, Volcano Monitoring, and Forecasting Eruptions
Is It Possible to Forecast Eruptions?
Monitoring involves recording and analyzing both physical and chemical changes at volcanoes
Tiltmeters and geodimeters to detect changes in slope, elevation, and shape of the volcano
Fig. 5.22, p. 130
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Volcanic Hazards, Volcano Monitoring, and Forecasting Eruptions
Is It Possible to Forecast Eruptions?
Monitoring involves recording and analyzing both physical and chemical changes at volcanoes
Seismometers to detect harmonic tremors
Gas emissions are also measured
Fig. 5.22, p. 130
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Volcanic Activity and Extinction