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

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

Chapter 4 - Section 4.8 - Intrusive Igneous Activity - Concept Checks - Page 134: 3

Answer

Batholiths, stocks, and laccoliths are all types of intrusive igneous bodies, but they differ in terms of their size and shape. Here's a distinction between them: Batholiths: - Batholiths are the largest and most extensive intrusive igneous bodies. - They cover an area of more than 100 square kilometers. - Batholiths are characterized by their great depth and considerable thickness, often extending several kilometers into the Earth's crust. - They have a roughly circular or elongated shape and can be hundreds of kilometers in length. - Batholiths are composed of a variety of igneous rocks, typically granitic or granodioritic in composition. - They are formed through the solidification of large volumes of magma over a long period of time deep within the Earth's crust. Stocks: - Stocks are smaller in size compared to batholiths. - They have a surface exposure of less than 100 square kilometers. - Stocks are relatively shallow and have a smaller vertical extent compared to batholiths, usually a few hundred meters to a few kilometers in depth. - They have a more irregular or circular shape, often forming small hills or domes on the Earth's surface. - Stocks are composed of various types of igneous rocks, including granitic, dioritic, or even volcanic rocks. - They are formed through the solidification of smaller volumes of magma that are emplaced within the Earth's crust. Laccoliths: - Laccoliths are intermediate in size between stocks and batholiths. - They have a surface exposure of typically less than 100 square kilometers. - Laccoliths are characterized by their lens-shaped or mushroom-shaped geometry. - They are formed when magma is injected between the layers of sedimentary or volcanic rocks, causing the overlying rocks to uplift and form a dome-shaped structure. - Laccoliths are composed of various igneous rocks, commonly granitic or dioritic in composition. - They are formed through the emplacement of magma at shallow to intermediate depths within the Earth's crust. In summary, batholiths are large, deep, and extensive intrusive bodies, stocks are smaller and shallower intrusive bodies, and laccoliths are intermediate-sized lens-shaped intrusions. Batholiths cover vast areas, stocks have a smaller surface exposure, and laccoliths form distinctive dome-shaped structures.

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