This book provides a synthesis of the physiography and geodynamics of the entire Pyrenean orogen and its foreland basins, providing the "big picture" (structure of the orogen and chronology of its formation, overview of its post-orogenic evolution, and Quaternary and recent landscape history). One part of the book proposes a 6–7 day itinerary across the eastern and east-central Pyrenees, two areas that currently provide the richest, best-documented, and most carefully curated database on the post-orogenic evolution of the mountain belt. The book deals with three complementary topics: (i) geodynamics, i.e. the long-term post-orogenic evolution of the Pyrenees since the declining stages of tectonic collision ca. 30 million years ago, and within the wider reference frame of Iberia, the Western Mediterranean, and the Atlantic margin; (ii) geomorphological processes and landforms that have conspired to shape the eastern part of the French and Spanish Pyrenees in response to base-level and climate-related changes over than same time period; (iii) geoheritage, i.e. educational vignettes of the flagship landscape units and typical geological sections of the study area. Written as a field guide, it is designed to help readers to construct discovery-based itineraries through the region (with options and variants depending on time and physical ability), allowing them to appreciate the key landscape and geoheritage features over the course of 1 week, with potential for much more. This GeoGuide is primarily aimed at confirmed geoscientists from most disciplines in Earth science, at postgraduate students engaged in field studies, and at curiosity-driven, educated amateurs keen to enhance their understanding of spectacular or enigmatic features encountered on their travels.

Pursuing an innovative, global approach, this unique book provides an updated review of the geology of Iberia and its continental margins from a geodynamic perspective. Owing to its location close to successive plate margins, Iberia has played a pivotal role in the geodynamic evolution of the Gondwanan, Rheic, Pangea, Tethys and Eurasian plates over the last 600 Ma of Earth’s history. The geological record starts with the amalgamation of Gondwana in the Neoproterozoic, which was succeeded by the rifting and spreading of the Rheic ocean; its demise, which led to the amalgamation of Pangea in the late Paleozoic; the rifting and spreading of several arms of the Neotethys ocean in the Mesozoic Era and their ongoing closure, which was responsible for the Alpine orogeny. The significant advances in the last 20 years have increasingly attracted international interest in exploring the geology of the Iberian Peninsula. This volume focuses on the Cenozoic basins of the Iberian Geology and consequently the most recent sedimentary features in the Iberian Geology apart of the active ones. In this book, you will find a detailed explanation of the alpine foreland basins, the extension of the west Mediterranean as well as the latest magmatism in Iberia.

This book helps a novice to explore the terrain independently. Geoscience fieldwork with a focus on structural geology and tectonics has become more important in the last few years from both academic and industrial perspectives. This book also works as a resource material for batches of students or geological survey professional undergoing training as parts of their course curriculum. Industry persons, on the other hand, can get a first-hand idea about what to expect in the field, in case no academic person is available with the team. This book focused on structural geology and tectonics compiles for the very first time terrains from several regions of the globe.