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ویرایش: 1 نویسندگان: David Palacios (editor), Philip D. Hughes (editor), Jose M. Garcia-Ruiz (editor), Nuria de Andrés (editor) سری: ISBN (شابک) : 0128234989, 9780128234983 ناشر: Elsevier سال نشر: 2021 تعداد صفحات: 503 زبان: English فرمت فایل : PDF (درصورت درخواست کاربر به PDF، EPUB یا AZW3 تبدیل می شود) حجم فایل: 125 مگابایت
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در صورت تبدیل فایل کتاب European Glacial Landscapes: Maximum Extent of Glaciations به فرمت های PDF، EPUB، AZW3، MOBI و یا DJVU می توانید به پشتیبان اطلاع دهید تا فایل مورد نظر را تبدیل نمایند.
توجه داشته باشید کتاب مناظر یخبندان اروپا: حداکثر گستره یخبندان نسخه زبان اصلی می باشد و کتاب ترجمه شده به فارسی نمی باشد. وبسایت اینترنشنال لایبرری ارائه دهنده کتاب های زبان اصلی می باشد و هیچ گونه کتاب ترجمه شده یا نوشته شده به فارسی را ارائه نمی دهد.
مناظر یخبندان اروپا: حداکثر گستره یخبندان کارشناسان مربوطه را در مورد تاریخ یخچالها و تأثیر آنها بر چشم انداز مناطق اصلی اروپا گرد هم می آورد. در برخی مناطق، بزرگترین یخبندان های ثبت شده قبل از آخرین چرخه یخبندان، در یکی از چرخه های یخبندان اصلی پلیستوسن میانی رخ داده است. با این حال، بهترین شواهد حفظ شده از یخبندان در مناظر مربوط به آخرین چرخه یخبندان (پلیستوسن پسین) است. این کتاب همچنین به تجزیه و تحلیل این لندفرم های یخچالی قدیمی می پردازد که گاهی اوقات هنوز در چشم انداز امروزی دیده می شوند. این تحلیل درک بهتری از توالی یخبندان های پلیستوسن و دوره های بین یخبندان میانی ارائه می دهد و همزمانی احتمالی قاره ای یا ناهمزمانی رفتار یخچال های گذشته را بررسی می کند. نتیجه این تجزیه و تحلیل، بینشها و اطلاعات مهم جدیدی را در مورد منشاء و اثرات تغییرات آب و هوایی و ژئومورفولوژیکی در سراسر اروپا به دست میدهد.
مناظر یخچالی اروپا: حداکثر گستره یخبندان مناظر تولید شده را بررسی میکند. توسط یخچالهای طبیعی در سراسر اروپا، اثرات ژئومورفولوژیکی یخبندانها، و همچنین گاهشماری و تکامل یخچالهای طبیعی گذشته، با هدف درک رابطه متقابل بین گسترش یخبندان و تغییرات آب و هوایی در این قاره. این کتاب ابزار ارزشمندی برای جغرافیدانان، زمین شناسان، دانشمندان محیط زیست، محققان فیزیک و علوم زمین است.
European Glacial Landscapes: Maximum Extent of Glaciations brings together relevant experts on the history of glaciers and their impact on the landscape of the main regions of Europe. In some regions the largest recorded glaciations occurred before the Last Glacial Cycle, in one of the major glacial cycles of the Middle Pleistocene. However, the best-preserved evidence of glaciation in the landscape is from the Last Glacial Cycle (Late Pleistocene). The book also analyses these older glacial landforms that can sometimes still be seen in the landscape today. This analysis provides a better understanding of the succession of Pleistocene glaciations and the intervening interglacial periods, examining their possible continental synchrony or asynchrony of past glacier behaviour. The result of this analysis gives important new insights and information on the origin and effects of climatic and geomorphological variability across Europe.
European Glacial Landscapes: Maximum Extent of Glaciations examines the landscapes produced by glaciers throughout Europe, the geomorphological effects of glaciations, as well as the chronology and evolution of the past glaciers, with the aim of understanding the interrelationship between glacial expansion and climate changes on this continent. This book is a valuable tool for geographers, geologist, environmental scientists, researchers in physics and earth sciences.
Cover European Glacial Landscapes Copyright Contents List of contributors About the editors Part 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 PART II The distribution of glacial landscapes in Europe Section 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 Section 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 PART III Climate changes during the Last Glacial Cycle in the eastern North Atlantic region SECTION 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 Part 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 Section 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 Chapter-30---Northern-Central-Europe--glacial-landform_2022_European-Glacial 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 Section 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 Section 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 Part V The European glacial landforms from the Last Glacial Maximum (2919 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 Section 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 47.3 Cold-based ice landscapes of the LGM EISC 47.4 Outlook References 48 Fennoscandia: glacial landforms from the Last Glacial Maximum 48.1 Introduction 48.2 Denmark and Skåne 48.3 Fennoscandian Shield 48.4 Ice sheet thickness: the Baltic Sea and the Scandinavian Mountains References 49 Northern Central Europe: glacial landforms from the Last Glacial Maximum References 50 European Russia: glacial landforms from the Last Glacial Maximum References 51 The Eurasian Arctic: glacial landforms from the Last Glacial Maximum 51.1 Introduction 51.2 Barents Sea 51.3 High Arctic islands and archipelagos 51.4 Kara Sea and Arctic Russia References 52 The North Sea and Mid-Norwegian continental margin: glacial landforms from the Last Glacial Maximum References 53 Britain and Ireland: glacial landforms from the Last Glacial Maximum 53.1 The evolving limits of the Last Glacial Maximum in Britain and Ireland 53.2 Lateral limits 53.3 Vertical limits 53.4 Timing of advance and maximum extension of the BIIS in the Late Devensian (MIS 2) and the geomorphological legacy References Section 2 European regions that were not covered by the EISC 54 The Ural Mountains: glacial landforms from the Last Glacial Maximum 54.1 Introduction and background 54.2 LGM moraines in the forefield of the Chernov Glacier 54.3 Moraines in forefield of Moscow University Glacier 54.4 Moraine ridge in the Hynotayakha Valley SW of Bol. Shchuchye 54.5 Lake sediments in Bol. Shchuchye 54.6 Enigmatic moraine ridge on the northern tip of the Polar Urals 54.7 The emergence of mountain glaciers and their size and distribution during the LGM 54.8 Summary References 55 Iceland: glacial landforms from the Last Glacial Maximum 55.1 Introduction 55.2 Last Glacial Maximum limits on the southern Iceland shelf 55.3 Last Glacial Maximum limits around the West Fjords Peninsula 55.4 Geomorphological signatures of Last Glacial Maximum ice flow 55.5 Modelling perspectives of the Iceland Ice Sheet during Last Glacial Maximum 55.6 Problems and potentials of the Iceland Ice Sheet during Last Glacial Maximum References 56 The Tatra Mountains: glacial landforms from the Last Glacial Maximum References 57 The Romanian Carpathians: glacial landforms from the Last Glacial Maximum (29–19ka) 57.1 Introduction 57.2 Eastern Carpathians 57.3 Southern Carpathians 57.4 Apuseni Mountains References 58 The Alps: glacial landforms from the Last Glacial Maximum References 59 The Pyrenees: glacial landforms from the Last Glacial Maximum 59.1 Introduction 59.2 Precise constraints on LGM glacier positions in the eastern half of the range 59.3 Imprecise constraints on LGM glacier positions in the western half of the range 59.4 A precipitation gradient between the Atlantic and Mediterranean during the LGM? References 60 The Iberian Mountains: glacial landforms from the Last Glacial Maximum 60.1 Introduction 60.2 Cantabrian Mountains 60.3 NW ranges 60.4 Iberian Range 60.5 Central Range 60.6 Betic Range References 61 The Italian mountains: glacial landforms from the Last Glacial Maximum 61.1 Introduction 61.2 Northern Apennines 61.3 Central Apennines 61.4 Southern Apennines 61.5 Sicily Acknowledgments References 62 The Balkans: glacial landforms from the Last Glacial Maximum 62.1 Introduction 62.2 Greece 62.3 Bulgaria 62.4 North Macedonia/Kosovo 62.5 Montenegro 62.6 Bosnia and Herzegovina 62.7 Croatia 62.8 Slovenia 62.9 Conclusion References 63 The Anatolian Mountains: glacial landforms from the Last Glacial Maximum 63.1 Introduction 63.2 Eastern Black Sea Mountains 63.3 Western Taurus Mountains 63.4 Central Taurus Mountains 63.5 Northwestern Anatolia 63.6 Central Anatolia 63.7 Anatolian LGM glaciations: a synthesis References Section 3 Synthesis of Part IV 64 The European glacial landscapes from the Last Glacial Maximum - synthesis 64.1 Glacial landforms of the European Ice Sheet Complex from the Last Glacial Maximum 64.2 Glacial landforms beyond the EISC: Iceland, the Urals, and the mountains of Central and Southern Europe 64.3 Major similarities/differences between regions and their causes 64.4 The European landscapes in a global context 64.5 Pending research References Part VI Synthesis of the European Landscapes from maximum glacial extension 65 The importance of European glacial landscapes in a context of great climatic variability 65.1 Maximum glaciations—final summary 65.2 The importance of European glacial landscapes in the context of global climate change 65.3 The importance of European glacial landscapes as geoheritage 65.4 Deglaciation—the end of widespread glaciation in Europe References Index Index_2022_European-Glacial-Landscapes Backcover