A thoroughly revised and extended second edition of an important work for earth scientists. This updated version features yet more illustrations and maps as well as almost 100 corrections of scientific problems.

This book is an introductory text for all earth scientists interested in learning about the quantitative description of geological problems. In its style, the book is aimed at the field oriented geologist that wants to begin with learning about the quantitative description of problems. The new edition, revised and extended, features even more illustrations and maps, about 100 corrections of scientific problems, improvement of geomorphology section and shortening of several sections which obviously are too complicated. Graduate students and scientists will find the book a good starting point for a quantitative treatment of their data.

Plate Tectonics.- Energetics: Heat and Temperature.- Kinematics: Morphology and Deformation.- Mechanics: Force and Rheology.- Dynamic Processes.- Metamorphic Processes.

The large scale structure of the earth is caused by geodynamic processes which are explained using energetic, kinematic and dynamic descriptions. While "geodynamic processes" are understood to include a large variety of processes and the term is used quite loosely, the methods of their description involve well defined fields. Energetic descriptions are involved with distribu tion of energy in our planet, typically expressed in terms of heat and tempera ture. Kinematic descriptions describe movements using velocities, strains and strain rates. Dynamic descriptions indicate how stresses and forces behave. In the field, we document only the consequences of geological processes. The underlying causes are much harder to constrain directly. Nevertheless, if we want to explain the tectonic evolution of our planet, we need to interpret these causes or: "driving forces" . For this, we need to find a dynamic description of geological processes that is consistent with our observations. Our descriptions relate causes and consequences - tectonic processes with field observations. In many cases, we will use equations as a concise form to describe processes and observations in nature. As we will be dealing mostly with large scale tectonic questions, the observations that we shall use are also on a large scale. For example, we shall use observations on the elevation (Fig. 1. 1) and heat flow of mountain ranges, the thickness of continents and the water depth of the oceans.