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  • 1
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Sedimentation and deposition. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (315 pages)
    Edition: 1st ed.
    ISBN: 9780080932194
    DDC: 551.43
    Language: English
    Note: Front Cover -- Mid-Latitude Slope Deposits (Cover Beds) -- Copyright -- Contents -- Contributors -- Preface -- Chapter 1: Introduction -- 1.1. Scope of the Book -- 1.2. Structure of the Book -- 1.3. Terminology -- 1.4. History of Ideas -- 1.5. Cover Beds in the Context of the ``Earth's Critical-Zone´´ Concept -- Chapter 2: Subdued Mountains of Central Europe -- 2.1. Introduction -- 2.2. Sedimentary Properties of Layers -- 2.2.1. The Basal Layer -- 2.2.2. The Intermediate Layer -- 2.2.3. The Upper Layer -- 2.3. Distribution and Thickness of Layers -- 2.3.1. The Basal Layer -- 2.3.2. The Intermediate Layer -- 2.3.3. The Upper Layer -- 2.3.4. Overview of the Distribution of Periglacial Cover Beds -- 2.4. Classification Issues -- 2.4.1. Discrimination Among Pleistocene Cover Beds -- 2.4.2. Anthropogenic Layers -- 2.4.2.1. Genesis and Classification of Anthropogenic Layers -- 2.4.2.2. Properties of Anthropogenic Layers -- 2.4.2.3. Discrimination of Anthropogenic Layers from Periglacial Cover Beds -- 2.5. Statistical Approach to Layer Properties and Distribution -- 2.5.1. Approach -- 2.5.2. Basal-Layer Properties -- 2.5.3. Intermediate-Layer Properties -- 2.5.4. Upper-Layer Properties -- 2.5.5. Overall View on Statistical Results -- 2.6. Genesis of Cover Beds -- 2.6.1. The Basal Layer -- 2.6.2. The Intermediate Layer -- 2.6.3. The Upper Layer -- 2.6.4. Incorporation of Substrates -- 2.6.4.1. Incorporation Processes -- 2.6.4.2. Case Study I: Sandreuth, Northeastern Bavaria -- 2.6.4.3. Case Study II: Spessart Mountains, Southeastern Hesse -- 2.7. Chronology of Periglacial Cover Beds -- 2.7.1. Relative-Age Criteria -- 2.7.1.1. Introduction -- 2.7.1.2. Age of the Basal Layer -- 2.7.1.3. Age of the Intermediate Layer -- 2.7.1.4. Age of the Upper Layer -- 2.7.2. Numerical Dating of Periglacial Cover Beds -- 2.7.2.1. Introduction. , 2.7.2.2. Methodical Difficulties in Dating Cover Beds -- 2.7.2.3. Luminescence-Dating Results from Basal Layers -- 2.7.2.4. Luminescence-Dating Results from Intermediate Layers -- 2.7.2.5. Luminescence-Dating Results from Upper Layers -- 2.7.2.6. Conclusions -- 2.8. Regional Differences in Cover-Bed Properties and Distribution -- 2.8.1. Highest Altitudes of Subdued Mountains -- 2.8.2. Rhenish Massif -- 2.8.3. Carbonate Rocks of the Eastern Thuringian Basin -- 2.8.3.1. Introduction -- 2.8.3.2. Properties and Distribution of Cover Beds -- 2.8.3.3. Conclusions -- Chapter 3: Influence of Cover Beds on Soils -- 3.1. Introduction -- 3.2. An Integrated Soil-Evolution Model for Lithologically Discontinuous Soil -- 3.3. Pedogenesis in Cover Beds -- 3.4. Consequences for Soil Properties -- 3.4.1. Theory of Soil Properties in Lithologically Discontinuous Soil -- 3.4.2. Physical Soil Properties -- 3.4.2.1. Texture in Lithologically Discontinuous Soil -- 3.4.2.2. Soil Water in Lithologically Discontinuous Soil -- 3.4.3. Chemical Soil Properties -- 3.4.3.1. Geochemical Composition of Cover Beds -- 3.4.3.2. Heavy Metals -- 3.4.3.3. Oxalate- and Dithionite-Extractable Iron -- 3.4.3.4. pH Value and Acidification -- 3.4.3.5. Stratigraphic Approach to Alteration in Soils from Cover Beds -- 3.5. Conclusions -- Chapter 4: Influence of Cover Beds on Slope Hydrology -- 4.1. Introduction -- 4.2. Basic Hypotheses -- 4.3. Case Studies -- 4.3.1. Overview -- 4.3.2. Frankenwald Mountains -- 4.3.2.1. Introduction -- 4.3.2.2. Results -- 4.3.2.3. Conclusions -- 4.3.3. Sauerland -- 4.3.4. Erzgebirge -- 4.4. Conclusions -- Chapter 5: Geotechnical Properties of Cover Beds -- 5.1. Introduction -- 5.2. Internal Stability of Cover Beds Derived from the ``Infinite Mechanical Slope Model´´ -- 5.3. Case Studies. , 5.3.1. Stability of Cover Beds in the Flysch Zone of the Vienna Forest (Austria) -- 5.3.1.1. Study Area -- 5.3.1.2. Distribution and Composition of Slope Deposits in the Hagenbach Valley -- 5.3.1.3. Soil-Mechanical Stability of Cover Beds and Bedrock -- 5.3.2. Stability of Cover Beds on Early Triassic Sandstones of Southern Lower Saxony (Germany) -- 5.3.2.1. Study Area -- 5.3.2.2. Distribution and Composition of Slope Deposits -- 5.3.2.3. Soil Mechanic Characteristics and Stability of Slope Deposits -- 5.3.2.4. Calculation of Soil Mechanic Stability of Slope Deposits -- 5.4. Perspectives -- Chapter 6: Transferring the Concept of Cover Beds -- 6.1. Introduction -- 6.2. Basins and Lowlands of the Mid-Latitudes -- 6.2.1. Northern Russian Plain -- 6.2.1.1. Successions of Cover Beds -- 6.2.1.2. Sequence-Stratigraphic Approach -- 6.2.1.3. Comparison to Central European Successions -- 6.2.2. Northern Great Basin, USA -- 6.2.2.1. Buried Cover Beds -- 6.2.2.2. Surficial Cover Beds -- 6.2.2.3. Genesis and Paleoenvironmental Implications of Great Basin Cover Beds -- 6.2.2.3.1. Late Wisconsinan Paleoenvironments -- 6.2.2.3.2. Late Illinoian to Mid-Wisconsinan -- 6.2.3. Konya Basin of South-Central Turkey -- 6.3. High Mountains of the Mid-Latitudes -- 6.3.1. European Alps -- 6.3.1.1. Cover Beds Below Modern Timberline -- 6.3.1.2. Cover Beds Above Timberline -- 6.3.2. Mountains of the Western USA -- 6.3.2.1. Cover Beds Below Timberline -- 6.3.2.2. Cover Beds in the Colorado Front Range Above Timberline -- 6.4. Conclusions -- 6.4.1. Significance of Cover Beds -- 6.4.2. Cover Beds in Humid Areas -- 6.4.3. Cover Beds in Semi-arid Areas -- 6.4.4. Cover Beds and Elevation -- Chapter 7: Relative Dating with Cover Beds -- 7.1. Introduction -- 7.2. Case Study at the Swabian Jurassic Escarpment -- 7.2.1. Study Area -- 7.2.2. Geomorphological Setting in Landslide Areas. , 7.2.3. Pedological and Sedimentological Setting in Landslide Areas -- 7.2.3.1. Unstable, Active Slope Areas of the Swabian Alb -- 7.2.3.2. Stable Slope Areas of the Swabian Alb -- 7.2.4. Model of the Distribution of Periglacial Layers and Soils in Landslide Areas -- 7.3. Case Studies in the Western USA -- 7.3.1. Introduction -- 7.3.2. River Terraces of Castle Valley, Southeast Utah -- 7.3.3. A Case of Misleading Tephrochronology? -- 7.3.4. Ice-Wedge Casts in South-Central Wyoming -- 7.3.5. Moraines in the Ruby Mountains, Northeast Nevada -- 7.4. Conclusions -- Chapter 8: Conclusions -- 8.1. Takeouts of this Book -- 8.2. Future Research Demands on Cover Beds -- References -- Index.
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  • 2
    Publication Date: 2021-03-29
    Description: The route of the field trip described in this excursion guide follows a section through Germany from North to South, from the area of the Northern glaciation, to the Alpine glacial advances. It includes several places of historical importance, where milestones in Quaternary research have been achieved in the past, as well as new interesting sites where results of recent research is presented.
    Description: excursionguide
    Keywords: 551 ; V 000 ; VCA 520 ; Geologische Wissenschaften ; Quartärgeologie ; coastal evolution; Rügen ; Geopark Mecklenburg Ice Age Landscape ; tourism ; quaternary ; Halle ; Main ; sedimentology ; landslide ; natural hazards ; danube ; rhine ; pleistocene ; holocene ; geology
    Language: English
    Type: anthology , publishedVersion
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Soil Science Society of America journal 62 (1998), S. 1647-1650 
    ISSN: 1435-0661
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Quantifying post-depositional alteration of mineral soil material is complicated by the fact that many soils consist of layered parent materials with varying indigenous composition. Part of our study site in the Steigerwald Mountains of northern Bavaria was cultivated during the Middle Ages and later reforested. Soil erosion removed the upper materials, exposing a deposit to contamination from the surface, whereas nearby, the deposit remained protected by overlying layers. We compared heavy metal concentrations within that deposit across this boundary of varying protection. No significant results were obtained for Cd; however, the concentrations of Pb and Cu increase by about 100% or more where the protecting cover thins. The Pb and Cu values provide a measure of the gross post-depositional alteration of that deposit. We expect this procedure can help quantify various pedogenic alterations by comparison with essentially the same, unaltered parent material.
    Type of Medium: Electronic Resource
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