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  • 1
    Online Resource
    Online Resource
    San Diego :Elsevier,
    Keywords: Glaciers. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (645 pages)
    Edition: 1st ed.
    ISBN: 9780323985116
    DDC: 551.312
    Language: English
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  • 2
    Online Resource
    Online Resource
    San Diego :Elsevier,
    Keywords: Glaciers. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (548 pages)
    Edition: 1st ed.
    ISBN: 9780128236079
    Language: English
    Note: Front Cover -- European Glacial Landscapes -- Copyright Page -- Contents -- List of contributors -- About the editors -- I. Introduction -- 1 Introduction -- 1.1 The advance in knowledge of the glacial landscapes -- 1.2 Objectives of the book -- 1.3 The glaciated European regions -- 1.4 The climatic context during the sculpting of the European glacial landscapes -- 1.5 The age and characteristics of European glacial landscapes -- 1.6 Standardised ages and maps used in the book -- References -- 2 The Quaternary ice ages -- 2.1 The discovery of the Quaternary ice ages -- 2.2 The antecedents of the Quaternary ice ages -- 2.3 Causes and characteristics of the Quaternary ice ages -- References -- 3 Previous synthesis of European Glacial Landscapes -- References -- II. The distribution of glacial landscapes in Europe -- 1 European regions that were covered by the European Ice Sheet Complex (EISC) -- 4 The European Ice Sheet Complex -- References -- 5 Glacial landscapes of Fennoscandia -- 5.1 Introduction -- 5.2 Scandinavian Mountains -- 5.3 Fennoscandian Shield -- 5.4 Baltic Sea -- 5.5 Denmark and Skåne -- 5.6 Glacial research in Fennoscandia -- References -- 6 Glacial landscapes of Northern Central Europe -- References -- 7 Glacial landscapes of European Russia -- References -- 8 The Eurasian Arctic -- 8.1 Introduction -- 8.2 Barents Sea -- 8.3 High Arctic islands and archipelagos -- 8.4 Kara Sea and Arctic Russia -- 8.5 Glacial knowledge of the Eurasian Arctic -- References -- 9 The North Sea and Mid-Norwegian continental margin -- 9.1 The North Sea -- 9.2 The Mid-Norwegian continental margin -- References -- 10 Glacial landscapes of Britain and Ireland -- 10.1 Introduction -- 10.2 Ireland -- 10.3 Wales -- 10.4 England -- 10.5 Scotland -- References -- 2 European regions that not were covered by the EISC -- 11 Glacial landscapes of the Ural Mountains. , 11.1 Brief description of the mountain range's geology and geomorphology -- 11.2 Climate -- 11.3 Today's glaciers -- 11.4 Ice Age glaciations -- 11.5 Summary -- References -- 12 Glacial landscapes of Iceland -- References -- 13 Glacial landscapes of the Tatra Mountains -- References -- 14 Glacial landscapes of the Romanian Carpathians -- 14.1 Introduction -- 14.2 The Eastern Carpathians -- 14.3 The Southern Carpathians -- 14.4 The Apuseni Mountains -- 14.5 Progress in the knowledge of the glacial landscapes -- References -- 15 Glacial landscapes of the Alps -- References -- 16 Glacial landscape of the Pyrenees -- References -- 17 The Iberian Peninsula (except for the Pyrenees) -- 17.1 Introduction -- 17.2 The Cantabrian Mountains -- 17.3 The NW ranges -- 17.4 Central Range -- 17.5 Iberian Range -- 17.6 Sierra Nevada -- 17.7 Progress in the knowledge of the glacial landscapes -- References -- 18 The Italian Peninsula -- 18.1 Introduction -- 18.2 The Northern Apennines -- 18.3 Central Apennines -- 18.4 Southern Apennines -- 18.5 Progress in the knowledge of the glacial landscapes -- References -- 19 Glacial landscapes of the Balkans -- 19.1 Introduction -- 19.2 Greece -- 19.3 Albania, North Macedonia, Kosovo -- 19.4 Dinaric Alps, Montenegro, Bosnia, Croatia, Slovenia -- 19.5 Bulgaria -- References -- 20 The Anatolian Peninsula -- References -- Further reading -- III. Climate changes during the Last Glacial Cycle in the eastern North Atlantic region -- 1 The Last Glacial Cycle -- 21 An overview of the Last Glacial Cycle -- References -- 22 Ice volume and sea-level changes during Last Glacial Cycle: evidence from marine records -- References -- 23 Definition of the Last Glacial Cycle marine stages and chronology -- References -- 24 Abrupt climatic variability: Dansgaard-Oeschger events -- References. , 25 Abrupt (or millennial or suborbital) climatic variability: Heinrich events/stadials -- References -- 26 The Global Last Glacial Maximum: the Eastern North Atlantic (marine sediments) and the Greenland Ice Sheet climatic signal -- References -- IV. European glacial landforms prior to the Last Glacial Maximum (Before 29 ka) -- 27 Concept and global context of the glacial landforms prior to the Last Glacial Maximum -- 27.1 Pleistocene glacial cycles -- 27.2 Pre-LGM glaciations in Europe -- 27.3 The importance of the pre-LGM glaciations on the landscapes of Europe -- References -- 1 European regions that were covered by the European Ice Sheet Complex (EISC) -- 28 The EISC evolution prior to the Last Glacial Maximum -- 28.1 Overview of EISC evolution -- 28.2 Implications for ice sheet-climate system interactions -- 28.3 Landscapes of the EISC prior to the LGM -- 28.4 Outlook -- References -- 29 Fennoscandia: glacial landforms prior to the Last Glacial Maximum -- 29.1 Introduction -- 29.2 Denmark and Skåne -- 29.3 Fennoscandian Shield -- 29.4 Scandinavian Mountain range -- References -- 30 Northern Central Europe: glacial landforms prior to the Last Glacial Maximum -- References -- 31 European Russia: glacial landforms prior to the Last Glacial Maximum -- 31.1 European Russia glacial landforms from MIS 16 -- 31.2 European Russia glacial landforms from Penultimate Glacial Cycle (Saalian, MIS 8-6) -- 31.3 European Russia glacial landforms from MIS 5, 4, and 3 -- References -- 32 The Eurasian Arctic: glacial landforms prior to the Last Glacial Maximum (before 29ka) -- 32.1 Introduction -- 32.2 Barents Sea -- 32.3 High Arctic islands and archipelagos -- 32.4 Kara Sea and Arctic Russia -- References -- 33 The North Sea and Mid-Norwegian Continental Margin: glacial landforms prior to the Last Glacial Maximum -- References. , 34 Britain and Ireland: glacial landforms prior to the Last Glacial Maximum -- 34.1 Middle Pleistocene glaciations -- 34.1.1 Pre-Anglian Stage glaciation -- 34.1.2 Anglian Stage glaciation -- 34.1.3 Wolstonian Stage glaciation -- 34.2 Late Pleistocene pre-Last Glacial Maximum glaciations -- 34.3 Summary -- References -- 2 European regions that not were covered by the EISC -- 35 The Ural Mountains: glacial landforms prior to the Last Glacial Maximum -- 35.1 Introduction -- 35.2 Style of glaciation -- 35.3 Middle Pleistocene glaciations -- 35.4 Pre-LGM glacial advances during the Last Glacial Cycle -- 35.4.1 Ice-sheet advances -- 35.4.2 Mountain glaciers -- 35.5 MIS 4 was a cold period with a major drop in the glacier equilibrium line altitudes -- 35.6 Ice-free interval during MIS 3 -- 35.7 Possible regrowth of glaciers during a late stage of MIS 3 -- 35.8 Summary -- References -- 36 Iceland: glacial landforms prior to the Last Glacial Maximum -- References -- 37 The Tatra Mountains: glacial landforms prior to the Last Glacial Maximum -- References -- 38 The Romanian Carpathians: glacial landforms prior to the Last Glacial Maximum -- 38.1 Introduction -- 38.2 Eastern Carpathians -- 38.3 Southern Carpathians -- References -- 39 The Alps: glacial landforms prior to the Last Glacial Maximum -- 39.1 Introduction -- 39.2 Early and Middle Pleistocene glaciations -- 39.3 Late Pleistocene (Last Glacial Cycle) glaciations -- References -- 40 The Pyrenees: glacial landforms prior to the Last Glacial Maximum -- 40.1 The most extensive glaciation of the Late Pleistocene occurred before the LGM -- 40.1.1 Evidence from northern massifs -- 40.1.2 Evidence from southern massifs -- 40.2 Preliminary indications of major glacier fluctuations during MIS 3 -- 40.3 Middle Pleistocene glaciation: still poorly documented -- References. , 41 The Iberian Mountains: glacial landforms prior to the Last Glacial Maximum -- 41.1 Introduction -- 41.2 Cantabrian Mountains -- 41.3 NW ranges -- 41.4 Central Range -- 41.5 Iberian Range -- 41.6 Betic Range -- References -- 42 The Italian mountains: glacial landforms prior to the Last Glacial Maximum -- 42.1 Introduction -- 42.2 Northern Apennines -- 42.3 Central Apennines -- Acknowledgments -- References -- 43 The Balkans: glacial landforms prior to the Last Glacial Maximum -- 43.1 Middle Pleistocene glaciations -- 43.1.1 Skamnellian Stage glaciation -- 43.1.2 Vlasian Stage glaciation -- 43.2 Late Pleistocene, pre-LGM glaciation -- References -- 44 The Anatolian mountains: glacial landforms prior to the Last Glacial Maximum -- 44.1 Introduction -- 44.2 Eastern Black Sea Mountains -- 44.3 Western Taurus Mountains -- 44.4 Northwestern Anatolia -- References -- 3 Synthesis of Part III -- 45 The European glacial landscapes prior to the Last Glacial Maximum - synthesis -- 45.1 Glacial landforms of the European Ice Sheet Complex prior to the Last Glacial Maximum -- 45.2 Glacial landforms beyond the EISC: on Iceland and in the mountains of Central and Southern Europe -- 45.3 Major similarities/differences between regions and their causes -- 45.4 The pre-LGC European landscapes in a global context -- 45.5 Pending research -- References -- V. The European glacial landforms from the Last Glacial Maximum (29-19 ka) -- 46 Concept and global context of the glacial landforms from the Last Glacial Maximum -- 46.1 The Last Glacial Maximum -- 46.2 Defining the LGM -- 46.3 The geomorphological legacy of the LGM -- References -- 1 European regions that were covered by the European Ice Sheet Complex (EISC) -- 47 European Ice Sheet Complex evolution during the Last Glacial Maximum (29-19ka) -- 47.1 EISC evolution during the Last Glacial Maximum (29-19ka). , 47.2 LGM landscapes and landforms of the EISC.
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  • 3
    Online Resource
    Online Resource
    Cham : Springer Nature Switzerland | Cham : Imprint: Springer
    Keywords: Geomorphology. ; Environmental geography. ; Geology.
    Description / Table of Contents: Introduction -- How are mountains defined and why are they so important? -- The changing world of mountains in the long term -- The discovery of mountains: from enigma to exploitation -- The climate of the mountains, originality and spatial variability -- Snow in the mountains -- Ice and glaciers in the mountains -- The main features of mountain vegetation and its altitudinal organization. The timberline -- Hydrology and fluvial morphology in mountains: those special rivers -- Landforms and geomorphological processes: from summits to valley bottoms -- Creation and organization of mountain landscapes by human societies -- Living in the mountains: The wide variety of land uses and their geo-ecological consequences -- Global change in mountains and its consequences at different scales -- Mountains: As difficult to exploit as they are to conserve. An integrative look at mountain landscapes and societies.
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(XXIII, 462 p. 191 illus., 185 illus. in color.)
    Edition: 1st ed. 2024.
    ISBN: 9783031519550
    Series Statement: Earth and Environmental Sciences Library
    Language: English
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  • 4
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    Madrid : Periodicals Archive Online (PAO)
    Estudios geográficos. 39:153 (1978:nov.) 539 
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  • 5
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  • 6
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    Madrid : Periodicals Archive Online (PAO)
    Estudios geográficos. 48:189 (1987:oct./dic.) 553 
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  • 7
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    Unknown
    Madrid : Periodicals Archive Online (PAO)
    Estudios geográficos. 39:153 (1978:nov.) 519 
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  • 8
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    Madrid : Periodicals Archive Online (PAO)
    Estudios geográficos. 39:153 (1978:nov.) 561 
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  • 9
    ISSN: 1572-9761
    Keywords: land-use change ; sustainability ; farmland abandonment ; reforestation ; soil erosion ; runoff ; mountain areas
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Land-use changes affecting Mediterranean mountains represent the intensification of use in valley bottoms, accompanied by land-use conflicts, and a generalized abandonment of the hillslopes, which in the past were perfectly integrated in the system of land management. Farmland abandonment, reforestation, diminution of the livestock pressure and substitution of cereal crops by meadows are the most outstanding features of the recent land-use changes. The question is whether the new spatial organisation is in accordance with a longterm policy of sustainable development in mountain areas. The results obtained confirm that farmland abandonment on steep slopes — and the resulting colonization of old fields by a dense shrub cover — and afforestation contribute to control both soil erosion and surface runoff. As a result some of the most important rivers and alluvial fans have recently stabilized their sedimentary structures.
    Type of Medium: Electronic Resource
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