001452392 000__ 03864cam\a22005297i\4500 001452392 001__ 1452392 001452392 003__ OCoLC 001452392 005__ 20230310003353.0 001452392 006__ m\\\\\o\\d\\\\\\\\ 001452392 007__ cr\cn\nnnunnun 001452392 008__ 230125s2022\\\\sz\a\\\\ob\\\\000\0\eng\d 001452392 019__ $$a1356796018$$a1356797010$$a1357017130$$a1363110024 001452392 020__ $$a9783031148958$$q(electronic bk.) 001452392 020__ $$a3031148959$$q(electronic bk.) 001452392 020__ $$z9783031148941 001452392 020__ $$z3031148940 001452392 0247_ $$a10.1007/978-3-031-14895-8$$2doi 001452392 035__ $$aSP(OCoLC)1365395464 001452392 040__ $$aGW5XE$$beng$$erda$$epn$$cGW5XE$$dYDX$$dEBLCP$$dOCLCQ$$dYDX$$dN$T$$dHTM$$dUKAHL 001452392 043__ $$ae------ 001452392 049__ $$aISEA 001452392 050_4 $$aGB648.42$$b.P47 2022 001452392 08204 $$a551.3/84094$$223/eng/20230125 001452392 24500 $$aPeriglacial landscapes of Europe /$$cMarc Oliva, Daniel Nývlt, José M. Fernández-Fernández, editors. 001452392 264_1 $$aCham, Switzerland :$$bSpringer,$$c2022. 001452392 300__ $$a1 online resource (1 volume) :$$billustrations (some colour). 001452392 336__ $$atext$$btxt$$2rdacontent 001452392 337__ $$acomputer$$bc$$2rdamedia 001452392 338__ $$aonline resource$$bcr$$2rdacarrier 001452392 504__ $$aIncludes bibliographical references (pages vi-vii). 001452392 5050_ $$aChapter 1 - Introduction -- Part 1 - Regional Setting -- Chapter 2. Quaternary climate variability and periglacial dynamics -- Chapter 3 - Periglacial Landforms Across Europe -- Part 2 - Periglacial Landforms in Southern Europe -- Chapter 4. The Iberian Peninsula -- Chapter 5. The Italian Peninsula -- Chapter 6. The Balkans (without Carpathians) -- Chapter 7. The Anatonian Peninsula -- Chapter 8. The Mediterranean islands -- Part 3 - Periglacial Landforms in Central and Eastern Europe -- Chapter 9. European Alps -- Chapter 10. The Central European Variscan ranges -- Chapter 11. The Carpathians -- Chapter 12. The North European Plain -- Part 4 - Periglacial Landforms in Northern Europe -- Chapter 13. Great Britain and Ireland -- Chapter 14. Scandinavia -- Chapter 15. Iceland -- Part 5 - Conclusions -- Chapter 16. The periglaciation of Europe. 001452392 506__ $$aAccess limited to authorized users. 001452392 520__ $$aThis book comprehensively presents the geography of landforms linked to periglacial processes across Europe. The landscape of the European cold climate regions, both at high latitudes and in mountainous environments, represent the lingering, minimal expression of the glaciers. In addition, periglacial elements can be found in temperate regions, where temperatures no longer favor periglacial processes, so landforms are therefore inherited from previous cold phases. The book is divided into five parts: an introductory section on climate variability responsible for periglacial dynamics across Europe; a second part including 3 blocks on periglacial landforms in southern, central and northern Europe; and a final chapter providing a more general perspective on the impact of periglacial processes on the landscape of Europe. The book offers a valuable reference guide for scientists from all disciplines interested in cold climate processes, as well as readers outside academia (territorial managers, environmentalists, mountaineers, politicians, engineers, etc.). . 001452392 588__ $$aDescription based on print version record. 001452392 650_0 $$aPeriglacial processes$$zEurope. 001452392 651_0 $$aCold regions. 001452392 655_0 $$aElectronic books. 001452392 7001_ $$aOliva, Marc,$$eeditor. 001452392 7001_ $$aNývlt, Daniel,$$eeditor. 001452392 7001_ $$aFernández-Fernández, José M,$$eeditor. 001452392 77608 $$iPrint version:$$tPeriglacial landscapes of Europe.$$dCham : Springer, 2022$$z9783031148941$$w(OCoLC)1346943650 001452392 852__ $$bebk 001452392 85640 $$3Springer Nature$$uhttps://univsouthin.idm.oclc.org/login?url=https://link.springer.com/10.1007/978-3-031-14895-8$$zOnline Access$$91397441.1 001452392 909CO $$ooai:library.usi.edu:1452392$$pGLOBAL_SET 001452392 980__ $$aBIB 001452392 980__ $$aEBOOK 001452392 982__ $$aEbook 001452392 983__ $$aOnline 001452392 994__ $$a92$$bISE