Introducing Metamorphism

Metamorphic rocks are one of the three main types of rocks. Originally formed from igneous or sedimentary rocks, metamorphic rocks are the result of changes due to heat and pressure, often at great depths within the Earth's crust, transforming into a completely new form. A classic example of the result of a metamorphic process is the transformation of sedimentary shale into schist.

"Introduction to Metamorphism" provides a concise introduction to metamorphism. Ian Sanders explains how and why rocks change during metamorphic processes. He discusses the role of water in metamorphism and describes the various types of metamorphic processes, including contact, shock, and high-pressure metamorphism, as well as metamorphism in an orogenic belt.

Richly illustrated and written for those who wish to gain a clear understanding of metamorphic processes, "Introduction to Metamorphism" is designed to make the processes that lead to the formation of these rocks comprehensible to readers. Technical terms are kept to a minimum and explained in a glossary.