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

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

Chapter 4 - Give It Some Thought - Page 138: 7

Answer

The common misconception that Earth's upper mantle is a thick shell of molten rock stems from a misunderstanding of the physical properties and behavior of the mantle. In reality, the mantle is mostly solid under normal conditions. Here's an explanation of why: 1. Temperature and pressure: The upper mantle is subjected to high temperatures and pressures, but these conditions are not sufficient to melt the rock. The melting point of most mantle minerals, such as peridotite, is much higher than the temperatures found in the upper mantle. Therefore, even though the mantle is hot, the rocks remain solid. 2. Solid-state deformation: The upper mantle undergoes a process known as solid-state deformation. This means that the rocks can slowly flow and deform without undergoing melting. Under high pressures and temperatures, the minerals in the mantle can exhibit plastic behavior, allowing for the slow movement of solid rock over long geological timescales. 3. Rheology of the mantle: The mantle is composed of silicate minerals that have a crystalline structure. These minerals exhibit a property known as a high viscosity, which means they resist flow and deformation. This high viscosity prevents the mantle from behaving like a liquid and maintains its solid state even under the intense pressure and temperature conditions. 4. Partial melting zones: While the majority of the mantle is solid, there are localized regions where partial melting can occur, leading to the formation of magma. These zones are typically found in the uppermost part of the mantle near tectonic plate boundaries, such as mid-ocean ridges or subduction zones. However, these zones of partial melting represent a small fraction of the mantle volume. In summary, Earth's upper mantle is primarily solid due to the high temperatures and pressures, the solid-state deformation process, the high viscosity of mantle minerals, and the localized nature of melting zones. While the mantle does contain regions of partial melting, the misconception that it is a thick shell of molten rock is incorrect.

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