The inner core consists mostly of iron and its temperature is about 5000 kelvin, whereas the liquid outer core is turbulent, rotates faster than the mantle, consists primarily of iron, and is the source of the Earth's magnetic field.
List of Figures. List of Tables. Preface. Acknowledgments. 1. Overview of Volcanic Processes. 2. Foundations of Transport Theory. 3. Properties of Igneous Materials. 4. Mantle Convection and Melt Segregation. 5. Magma Chambers. 6. Magma Ascent in Conduits. 7. Pyroclastic Dispersions. References. Index.
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