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  • 1
    Keywords: Katla (Iceland). ; Electronic books.
    Description / Table of Contents: Lowland glaciers are usually considered the best analogs for formerly glaciated areas and as such, many Icelandic glaciers have been intensively investigated with regard to process-orientated sediment-landform interrelationships. The Mýrdalsjökull ice cap has, thus, served as an excellent "ice-age laboratory." Furthermore, a substantial effort has been directed toward understanding the interaction between volcanic activity and glacier response, such as meltwater outbursts (jökulhlaups) and sudden events of rapidly flowing glacier ice. The book reviews the following themes related to Mýrdalsjökull: glaciology, glacial and quaternary geology, sedimentology, tephrochronology and eruption history of Katla, and crustal movements. All authors are involved in research about the subglacial Katla volcano and Mýrdalsjökull. Book covers all aspects of the ice cap and volcano dynamics Comprehensive reviews with updated results Editors and authors are well established scientists with research experience from Myrdalsjokull Standard reference work for Myrdalsjokull.
    Type of Medium: Online Resource
    Pages: 1 online resource (219 pages)
    Edition: 1st ed.
    ISBN: 9780080932002
    Series Statement: Issn Series ; v.Volume 13
    DDC: 551.31094912
    Language: English
    Note: Front cover -- The Mýrdalsjökull Ice Cap, Iceland. Glacial Processes, Sediments and Landforms on an Active Volcano -- Copyright page -- Contents -- List of Contributors -- Preface -- Chapter 1. The Mýrdalsjökull Ice Cap, Iceland: Glacial Processes, Sediments and Landforms on an Active Volcano: An Introduction -- 1.1. The Unique Geological Qualities of the Mýrdalsjökull Area -- 1.2. General Geology and Topography -- 1.3. Aim of This Book -- Chapter 2. Katla and Eyjafjallajökull Volcanoes -- 2.1. Introduction -- 2.2. Tectonic Setting -- 2.3. Structure and Eruptive Products of the Volcanoes -- 2.4. Recent Unrest in Katla -- 2.5. Recent Unrest in Eyjafjallajökull -- 2.6. Earthquakes -- 2.7. Crustal Deformation -- 2.8. Discussion -- Acknowledgements -- References -- Chapter 3. Katla: Tephrochronology and Eruption History -- 3.1. Introduction -- 3.2. Geological Setting -- 3.3. Holocene Eruptions in the Katla Volcanic System -- 3.4. Jökulhlaups Associated with Eruptions in the KVS -- 3.5. Environmental Changes -- 3.6. Summary -- Acknowledgement -- References -- Chapter 4. Deglaciation and Holocene Glacial History of Iceland -- 4.1. Introduction and Terminology -- 4.2. The Icelandic Ice Sheet at LGM (gt25.0cal. kyr BP) -- 4.3. Bølling (15.4-13.9cal. kyr BP) Deglaciation and Relative Sea Level -- 4.4. Allerød (13.6-13.0cal. kyr BP) Environmental Developments -- 4.5. The Younger Dryas (13.0-11.5cal. kyr BP) Glacial and Climatic Event -- 4.6. Early Preboreal (11.5-10.1cal. kyr BP) Glaciation -- 4.7. Deglaciation of Central South Iceland -- 4.8. Relative Sea Level Changes -- 4.9. Holocene Glacier History -- 4.10. Pre-LIA Glacial History of the My´rdalsjökull Area -- 4.11. Little Ice Age Glacial History of the My´rdalsjökull Area -- 4.12. Summary and Conclusions -- References -- Chapter 5. Variations of Mýrdalsjökull during Postglacial and Historical Times. , 5.1. Introduction -- 5.2. Glacier Place Names -- 5.3. Causes of Changes in Glacier Mass -- 5.4. Postglacial Oscillations of Mýrdalsjökull -- 5.5. Debris Known as 'Jökull' -- 5.6. Tephra Horizons and Turnover Time of Ice Mass -- 5.7. Conclusions -- References -- Chapter 6. Ice-Marginal Environments: Geomorphic and Structural Genesis of Marginal Moraines at Mýrdalsjökull -- 6.1. Introduction -- 6.2. Ice-marginal moraine formation at Kötlujökull -- 6.3. Ice-marginal moraine formation at Sléttjökull -- 6.4. Neoglacial ice-marginal moraine ridges -- 6.5. Conclusions -- Acknowledgements -- References -- Chapter 7. Dead-Ice Environments: A Landsystems Model for a Debris-Charged, Stagnant Lowland Glacier Margin, Kötlujökull -- 7.1. Introduction -- 7.2. Glacier Dynamics and Sources of Supraglacial Sediments -- 7.3. Stages of Dead-Ice Moraine Development -- 7.4. A Landsystems Model -- 7.5. Melting Rates Under Other Climate Conditions -- 7.6. Conclusions -- References -- Chapter 8. Subglacial Environments, Sediments and Landforms at the Margins of Mýrdalsjökull -- 8.1. Introduction -- 8.2. Study Areas -- 8.3. The Subglacial Environment -- 8.4. Subglacial Sediments and Landforms -- 8.5. A Marginal-Subglacial-Proglacial landsystem in front of Sléttjökull -- 8.6. Conclusions -- Acknowledgements -- References -- Chapter 9. Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland - A Case Study -- 9.1. Introduction -- 9.2. Setting -- 9.3. Methodology -- 9.4. The Geological Section -- 9.5. Description and Interpretation of the Facies Associations -- 9.6. Discussion -- 9.7. Event Stratigraphy -- 9.8. Conclusions -- References -- Chapter 10. Mýrdalsjökull's Forefields Under the Microscope. The Micromorphology of Meltout and Subglacial Tills -- 10.1. Introduction -- 10.2. Micromorphology -- 10.3. Sample Sites. , 10.4. Samples -- 10.5. Description -- 10.6. Discussion -- 10.7. Conclusion -- Acknowledgements -- References -- Chapter 11. Volcanogenic Jökulhlaups (Glacier Outburst Floods) from Mýrdalsjökull: Impacts on Proglacial Environments -- 11.1. Introduction -- 11.2. Volcanic and Jökulhlaup History -- 11.3. Jökulhlaups from Kötlujökull Draining across Mýrdalssandur -- 11.4. Sólheimasandur and Skógasandur -- 11.5. Jökulhlaups from the Northwestern Sector of Mýrdalsjökull Draining into the Markarfljót -- 11.6. Conclusions -- Acknowledgements -- References -- Subject Index.
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  • 2
    Publication Date: 2022-04-12
    Description: The deglaciation history and Holocene environmental evolution of northern Wijdefjorden, Svalbard, are reconstructed using sediment cores and acoustic data (multibeam swath bathymetry and sub-bottom profiler data). Results reveal that the fjord mouth was deglaciated prior to 14.5±0.3 cal. ka BP and deglaciation occurred stepwise. Biomarker analyses show rapid variations in water temperature and sea ice cover during the deglaciation, and cold conditions during the Younger Dryas, followed by minimum sea ice cover throughout the Early Holocene, until c. 7 cal. ka BP. Most of the glaciers in Wijdefjorden had retreated onto land by c. 7.6±0.2 cal. ka BP. Subsequently, the sea-ice extent increased and remained high throughout the last part of the Holocene. We interpret a high Late Holocene sediment accumulation rate in the northernmost core to reflect increased sediment flux to the site from the outlet of the adjacent lake Femmilsjøen, related to glacier growth in the Femmilsjøen catchment area. Furthermore, increased sea ice cover, lower water temperatures and the re-occurrence of ice-rafted debris indicate increased local glacier activity and overall cooler conditions in Wijdefjorden after c. 0.5 cal. ka BP. We summarize our findings in a conceptual model for the depositional environment in northern Wijdefjorden from the Late Weichselian until present.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 3
    Publication Date: 2023-06-27
    Description: TOC, IP25, HBI Z-triene (HBI-III), C46-GDGT data and median ages from a marine sediment core, northern Wijdefjorden, Svalbard. The dataset spans from the last deglaciation until present. It has been used to reconstruct the sea-ice history and sea water temperature variations.
    Keywords: 2,6,10,14-Tetramethyl-7-(3-methylpent-4-enyl)pentadecane, per unit mass total organic carbon; 2,6,10,14-Tetramethyl-7-(3-methylpent-4-enyl)pentadecane per unit sediment mass; AGE; Branched and isoprenoid tetraether index; Carbon, organic, total; Core; CORE; DEPTH, sediment/rock; HH17‐1079‐GC‐MF; Highly branched isoprenoids (Z), triunsatured, per unit mass total organic carbon; Holocene glacial history; Hydroxylated acyclic glycerol dialkyl glycerol tetraether; Hydroxylated dicyclic glycerol dialkyl glycerol tetraether; Hydroxylated monocyclic glycerol dialkyl glycerol tetraether; Ring index of hydroxylated glycerol dialkyl glycerol tetraethers; sea-ice; Sea surface temperature; sea water temperatures; SST, from Ri OH-GDGTs, Lü et al. (2015); Svalbard
    Type: Dataset
    Format: text/tab-separated-values, 548 data points
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  • 4
    Publication Date: 2024-04-20
    Description: The Svalhola database: standardized and re-calibrated Holocene radiocarbon, luminescence and cosmogenic exposure ages from Svalbard. In total 1837 individual ages from 722 discrete locations. The data are organised in three individual (excel) tables: S1 contains all Holocene C14-ages and tephra layers identified in Svalbard, S2 contains all Holocene luminescence ages from Svalbard and S3 contains all Holocene cosmogenic exposure ages from Svalbard. There is a corresponding .shp file created for each one of the tables.
    Keywords: Binary Object; Binary Object (File Size); Binary Object (Media Type); C-14; chronologies; Holocene; MULT; Multiple investigations; OSL; PDI-24556; Svalbard; Svalhola; TCN
    Type: Dataset
    Format: text/tab-separated-values, 7 data points
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