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Iberia, Land of Glaciers - How The Mountains Were Shaped By Glaciers (Paperback): Marc Oliva, David Palacios, Jose M.... Iberia, Land of Glaciers - How The Mountains Were Shaped By Glaciers (Paperback)
Marc Oliva, David Palacios, Jose M. Fernandez-Fernandez
R3,342 Discovery Miles 33 420 Ships in 10 - 15 working days

Iberia, Land of Glaciers: How The Mountains Were Shaped By Glaciers discusses the impact of past glaciers in the current landscape of Iberia. Currently, there are only small glaciers in the highest peaks of the Pyrenees that are the legacy of the last cold period that ended at the end of the 19th century: The Little Ice Age. However, an accurate observation of the landscape of the highest peaks and adjacent valleys of the Iberian Peninsula reveals a past shaped by the successive passage of glaciers with hundreds of meters of ice, similar to what happens today in the Alps or Patagonia. Iberian glaciation has resulted in ice expansion through valleys that are now used by the road network and where important populations settle; in addition, large accumulations of sediments deposited by those glaciers are still unstable today and can trigger risks for mountain populations. Iberia, Land of Glaciers presents the impact of the glaciers in the landscape of mountains following a more educational perspective with examples of 21 Iberian massifs written by specialists from each of the areas.

Periglacial Landscapes of Europe (Hardcover, 1st ed. 2022): Marc Oliva, Daniel Nyvlt, Jose M. Fernandez-Fernandez Periglacial Landscapes of Europe (Hardcover, 1st ed. 2022)
Marc Oliva, Daniel Nyvlt, Jose M. Fernandez-Fernandez
R2,069 Discovery Miles 20 690 Ships in 10 - 15 working days

This book comprehensively presents the geography of landforms linked to periglacial processes across Europe. The landscape of the European cold climate regions, both at high latitudes and in mountainous environments, represent the lingering, minimal expression of the glaciers. In addition, periglacial elements can be found in temperate regions, where temperatures no longer favor periglacial processes, so landforms are therefore inherited from previous cold phases. The book is divided into five parts: an introductory section on climate variability responsible for periglacial dynamics across Europe; a second part including 3 blocks on periglacial landforms in southern, central and northern Europe; and a final chapter providing a more general perspective on the impact of periglacial processes on the landscape of Europe. The book offers a valuable reference guide for scientists from all disciplines interested in cold climate processes, as well as readers outside academia (territorial managers, environmentalists, mountaineers, politicians, engineers, etc.).

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