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1 The Earth in Context
2 The Way the Earth Works: Plate Tectonics
3 Patterns in Nature: Minerals
4 Up From the Inferno: Magma and Igneous Rocks
5 A Surface Veneer: Sediments and Sedimentary Rocks
6 Change in the Solid State: Metamorphic Rocks
7 The Wrath of Vulcan: Volcanic Eruptions
8 A Violent Pulse: Earthquakes
9 Crags, Cracks, and Crumples: Crustal Deformation and Mountain Building
10 Deep Time: How Old is Old?
11 A Biography of Earth
12 Riches in Rock: Energy and Mineral Resources
13 Unsafe Ground: Landslides and Other Mass Movements
14 Streams and Floods: The Geology of Running Water
15 Restless Realm: Oceans and Coasts
16 A Hidden Reserve: Groundwater
17 Dry Regions: The Geology of Deserts
18 Amazing Ice: Glaciers and Ice Ages
19 Global Change in the Earth System


The Amazing Amethyst of the Paraná Basalt Province

by Stephen Marshak
Overview Image

Amazing Amethyst

Credit: 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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