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

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The Rest of the Story: The Amazing Amethyst of the Paraná Basalt Province

by Stephen Marshak

The Paraná Basin, in southern Brazil, contains about 1.2 million square km of flood basalt, one of the largest flood-basalt provinces in the world. The basin also has two other distinctions. First, it is host to the largest waterfall in the world, the Iguaçu Falls, where immense volumes of water spill over a cliff in the basalt sheets. Second, its basalts contain some of the world's largest known vesicles (preserved gas bubbles). These bubbles appear when magma rises and undergoes decompression; they're like the bubbles you see in a carbonated drink when you open it. In most basalts, vesicles range in diameter from millimeters to a few centimeters, but the Paraná's reached a meter in length. Through time, water percolating through the basalt precipitated spectacular crystals of amethyst (purple quartz) along the surface of these vesicles. After millions of years, in some places tropical chemical weathering transformed the basalt into weak, clay-rich soil. This weathering, however, does not affect the amethyst-lined vesicles because amethyst (quartz) is very resistant to weathering. Thus, the vesicles, well known to gem collectors worldwide, remain as intact spherical-to-ellipsoidal geodes. Miners quarry these geodes out of the weak matrix. When cracked open, they look like giant eggs lined with gems.

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