Earth: An Introduction to Physical Geology (12th Edition)

Published by Pearson
ISBN 10: 0134074254
ISBN 13: 978-0-13407-425-2

Chapter 5 - Section 5.2 - Materials Extruded During an Eruption - Concept Checks - Page 150: 4

Answer

Volcanic bombs and blocks are both types of pyroclastic debris ejected during volcanic eruptions, but they differ in their formation and characteristics. Volcanic Bombs: - Volcanic bombs are large, rounded or elongated fragments of molten or semi-molten lava that are ejected during explosive eruptions. - They are usually formed when the magma is thrown into the air and undergoes aerodynamic shaping while still in a plastic or fluid state. - Due to their molten or partially molten nature, volcanic bombs often have a smooth or spiny surface texture. - Their size can range from a few centimeters to several meters in diameter, and they can travel significant distances from the volcano before landing. - The shape of volcanic bombs is typically streamlined or aerodynamically shaped, resembling a teardrop or spindle. Blocks: - Blocks, on the other hand, are solid fragments of pre-existing rock that are torn from the volcano during explosive eruptions. - They are derived from the volcano's conduit walls or from previously erupted volcanic material. - Blocks are usually composed of the same rock type as the volcano itself, such as basalt, andesite, or rhyolite. - Unlike volcanic bombs, blocks are not molten or semi-molten but are solid and retain their original rock texture. - Blocks can vary in size from small pieces to massive chunks weighing several tons. - They typically have angular or irregular shapes, reflecting their fragmented nature. In summary, volcanic bombs are formed from ejected molten or semi-molten lava, have a rounded or elongated shape, and exhibit a surface texture related to their plastic state. Blocks, on the other hand, are solid fragments of pre-existing rock torn from the volcano, retain their original texture, and have an angular or irregular shape.

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