Antarctica is commonly perceived as a vast expanse of glacial ice. The typical image is that of a researcher enduring severe winds and challenging conditions. However, few consider that this immense frozen continent contains active volcanic systems, rock strata emitting considerable geothermal heat beneath the glaciers, or subterranean chambers of molten magma influencing its geological uplift. The impact of geological forces on virtually every facet of the Antarctic continent is often significantly underestimated. For instance, Mount Erebus, as referenced above, stands at 12,441 feet on Antarctica's western edge. It has remained active since 1972 and has experienced multiple significant eruptions over the past 70 years. This book aims to demonstrate that geological activity is a principal factor influencing numerous dynamics within Antarctica, particularly in relation to glacier melting.