By Jamie Woodward
This quantity explores the climates, landscapes, ecosystems and dangers that include the Mediterranean global. It strains the advance of the Mediterranean panorama over very lengthy timescales and examines glossy tactics and key environmental concerns in a variety of settings. The Mediterranean is the one sector on the earth the place 3 continents meet and this interplay has produced a truly particular actual Geography. This booklet examines the landscapes and procedures on the margins of those continents and the distinct marine setting among them. Catastrophic earthquakes, explosive volcanic eruptions and devastating storms and floods are in detail certain up in the heritage and mythology of the Mediterranean global. this can be a key zone for the learn of ordinary dangers since it deals unrivalled entry to lengthy files of threat prevalence and impression via documentary, archaeological and geological files. The Mediterranean is additionally a biodiversity hotspot; it's been a gathering position for vegetation, animals and people from 3 continents all through a lot of its heritage. The Quaternary files of those interactions are extra various and higher preserved than in the other a part of the realm. those documents have supplied vital new insights into the pace of weather, panorama and environment switch within the Mediterranean area and past. The area is exclusive as a result of the very early and frequent effect of people in panorama and atmosphere switch - and the richness of the archaeological and geological information that chronicle this impression. This ebook examines this historical past and those interactions and areas present environmental matters in long-term context.
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Additional info for The Physical Geography of the Mediterranean (Oxford Regional Environments)
Geodynamics of the Mediterranean The active nature of the tectonics in the Mediterranean is revealed by the combination of raised (and drowned) shorelines (Chapter 13). For example, when sea levels Impact on landforms Quaternary volcanic and seismic activity is focused around the migrating arcs. Steep basin and range relief formed by the migrating arcs is associated with the development of a range of landform features. g. by tectonically driven river incision/delta deposition) and seismic activity.
In 2001 with Eelco Rohling in Southampton. He is a specialist in benthic foraminifera and the application of their abundance variations and stable isotope ratios in palaeoenvironmental research, with emphasis on the eastern Mediterranean. Harriet Allen is a lecturer and researcher in the Department of Geography, University of Cambridge. Her research interests focus on the response of ecosystems to environmental change. This includes the integration of high resolution remote sensing data with ecological surveys to assess contemporary ecosystem changes, and pollen and sedimentological research to reconstruct longer-term ecosystem changes.
With regard to a glacio-eustatic fall, the proposed 60 m drop in sea level in the Messinian is insufficient to have closed all the marine gateways. 02 Ma Tectonic Setting and Landscape Development does not correspond with the benthic glacio-eustatic ‰18 O signature, suggesting that the Messinian Salinity Crisis is unlikely to be related to glacio-eustasy (Krijgsman et al. 1999b; Hodell et al. 2001). Palynological work in the Rifian corridor of northern Morocco (Warny et al. 2003) suggests that the regional climate was stable before, during, and after the Messinian Salinity Crisis.
The Physical Geography of the Mediterranean (Oxford Regional Environments) by Jamie Woodward