1 Cosmology and the Earth
2 Journey to the Center of the Earth
3 Drifting Continents and Spreading Seas
4 The Way the Earth Works: Plate Tectonics
5 Patterns in Nature: Minerals
6 Up from the Inferno: Magma and Igneous Rocks
7 A Surface Veneer: Sediments, Soils, and Sedimentary Rocks
8 Metamorphism: A Process of Change
9 The Wrath of Vulcan: Volcanic Eruptions
10 A Violent Pulse: Earthquakes
11 Crags, Cracks, and Crumples: Crustal Deformations and Mountain Building
12 Deep Time: How Old Is Old?
13 A Biography of Earth
14 Squeezing Power from a Stone: Energy Resources
15 Riches in Rock: Mineral Resources
16 Unsafe Ground: Landslides and Other Mass Movements
17 Streams and Floods: The Geology of Running Water
18 Restless Realm: Oceans and Coasts
19 A Hidden Reserve: Groundwater
20 An Envelope of Gas: Earth’s Atmosphere and Climate
21 Dry Regions: The Geology of Deserts
22 Amazing Ice: Glaciers and Ice Ages
23 Global Change in the Earth System
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Chapter 9: The Wrath of Vulcan: Volcanic Eruptions

Animations

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Click on the links below to view animations created specifically for Earth: Portrait of a Planet. Animations require Macromedia's Flash Plug-in.

Watch Eruption of Vesuvius

What a Geologist Imagines: Eruption of Vesuvius

Pompeii, once buried by 6 m of volcanic debris from Mt. Vesuvius, was excavated by archaeologists in the late nineteenth century. Vesuvius rises in the distance. When Mt. Vesuvius erupted in 79 C.E., it was probably much larger, as depicted in this sketch. The dark pellets are hot volcanic bombs and lapilli. For more information, see page 268 and Figure 9.1 in your textbook.

Watch Growth of a Stratovolcano

Animation: Growth of a Stratovolcano

A stratovolcano such as Japan’s Mount Fuji consists of alternating layers of ash and lava. This animation examines the processes by which a stratovolcano forms. For more information, see Figures 9.11 and 9.12 on p. 277 in your textbook.

See Zoomable Art: VolcanoZoomable Art: Volcano

Volcanic eruptions are a sight to behold and, in some cases, a hazard to fear. Beneath a volcano, magma formed in the upper mantle or the lower crust rises to fill a magma chamber near the Earth’s surface. When the pressure in this magma chamber becomes great enough, magma is forced upward through a conduit, or crack, to the ground surface and erupts. For more information, see the Featured Painting on pp. 278-79 in your textbook.

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