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Covering all the major peaks east of the Matterhorn, the Zermatt and Saas valleys, this guide book is aimed at alpinists wishing to climb in the area.'
This comprehensive book is an excellent planning resource for those who wish to venture into the Swiss Alps. Whether you are planning a walk, scramble, climb or ski tour this larger format guide describes each mountain area throughout Switzerland - the peaks, passes, valleys and bases - to help readers identify the best destinations for their chosen mountain activity. Dozens of individual valleys are described, together with the mountains that wall them, with recommendations given for their finest walks, treks and climbs. Working eastwards across the country, this guide is divided into seven chapters: Chablais Alps, Pennine Alp, Lepontine and Adula Alps, Bernina, Bregaglia and Albula Alps, Bernese Alps, Central Swiss Alps and the Silvretta and Ratikon Alps, each devoted to a specific range or group of connecting ranges. However, this is not a route guide and detailed descriptions are not provided. The aim of the book is to inspire as well as inform; to show first-time visitors just what the Swiss Alps have to offer and provide a new perspective for those who have been before.
Geodynamics of the Alps consists of three volumes. This first volume describes the recent and present-day structure and tectonic setting of the Alpine chain, from the lithospheric mantle to brittle crust and surface topography. It also provides a historical overview of Alpine research, with two chapters covering specific Alpine regions (Corsica and the Eastern Alps) through all phases of Alpine history. The aim of this book is to create a space for experts on Alpine research to present the state of the art of specific subjects and provide their own interpretations.
The Alps, Carpathians and Dinarides form a complex, highly curved and strongly coupled orogenic system. Motions of the European and Adriatic plates gave birth to a number of 'oceans' and microplates that led to several distinct stages of collision. Although the Alps serve as a classical example of collisional orogens, it becomes clearer that substantial questions on their evolution can only be answered in the Carpathians and Dinarides. Our understanding of the geodynamic evolution of the Alpine-Dinaride-Carpathian System has substantially improved and will continue to develop; this is thanks to collaboration between eastern and western Europe, but also due to the application of new methods and the launch of research initiatives. The largely field-based contributions investigate the following subjects: pre-Alpine heritage and Alpine reactivation; Mesozoic palaeogeography and Alpine subduction and collision processes; extrusion tectonics from the Eastern Alps to the Carpathians and the Pannonian Basin; orogen-parallel and orogen-perpendicular extension; record of orogeny in foreland basins; tectonometamorphic evolution; and relations between the Alps, Apennines and Corsica.