Submarine Mass Movements and Their Consequences

<p>1  Submarine Mass Movements and Their Consequences</p><p>Part I Physical Properties of Sediments and Slope Stability Assessment</p><p>2  Risk Assessment for Earthquake-Induced Submarine Slides </p><p>3  Shallow Landslides and Their Dynamics in Coastal and Deepwater Environments, Norway</p><p>4  Physical Properties and Age of Continental Slope Sediments Dredged from the Eastern Australian Continental Margin – Implications for Timing of Slope Failure</p><p>5  Submarine Landslides on the Upper Southeast Australian Passive Continental Margin – Preliminary Findings</p><p>6  Development and Potential Triggering Mechanisms for a Large Holocene Landslide in the Lower</p><p>St. Lawrence Estuary</p><p>7  Spatially Fixed Initial Break Point and Fault-Rock Development in a Landslide Area</p><p>8  Pore Water Geochemistry as a Tool for Identifying and Dating Recent Mass-Transport Deposits</p><p>9  An In-Situ Free-Fall Piezocone Penetrometer for Characterizing Soft and Sensitive Clays at Finneidfjord (Northern Norway)</p><p>10  Static and Cyclic Shear Strength of Cohesive and Non-cohesive Sediments</p><p>11  Upstream Migration of Knickpoints: Geotechnical Considerations<br><br>Part II Seafloor Geomorphology for Trigger Mechanisms and Landslide Dynamics<br><br>12  A Reevaluation of the Munson-Nygren-Retriever Submarine Landslide Complex, Georges Bank Lower Slope, Western North Atlantic</p><p>13  Submarine Landslides in Arctic Sedimentation: Canada Basin</p><p>14  Extensive Erosion of the Deep Seafloor – Implications for the Behavior of Flows Resulting from Continental Slope Instability</p><p>15  Investigations of Slides at the Upper Continental Slope Off Vesterålen, North Norway</p><p>16  Dakar Slide Offshore Senegal, NW-Africa: Interaction of Stacked Giant Mass Wasting Events and Canyon Evolution</p><p>17  Large-Scale Mass Wasting on the Northwest African Continental Margin: Some General Implications for Mass Wasting on Passive Continental Margins</p><p>18  Deep-Seated Bedrock Landslides and Submarine Canyon Evolution in an Active Tectonic Margin: Cook Strait, New Zealand</p><p>19  Polyphase Emplacement of a 30 km3 Blocky Debris Avalanche and Its Role in Slope-Gully Development</p><p>20  Slope Failure and Canyon Development Along the Northern South China Sea Margin</p><p>21  Distinguishing Sediment Bedforms from Sediment Deformation in Prodeltas of the Mediterranean Sea</p><p>22  Hydroacoustic Analysis of Mass Wasting Deposits in Lake Ohrid (FYR Macedonia/Albania)</p><p>23  New Evidence of Holocene Mass Wasting Events in Recent Volcanic Lakes from the French Massif Central (Lakes Pavin, Montcineyre and Chauvet) and Implications for Natural Hazards<br><br>Part III Role of Fluid Flow in Slope Instability<br><br>24  A Review of Overpressure, Flow Focusing, and Slope Failure</p><p>25  How Do ~2° Slopes Fail in Areas of Slow Sedimentation? A Sensitivity Study on the Influence of Accumulation Rate and Permeability on Submarine Slope Stability</p><p>26  The BGR Slide Off Costa Rica: Preconditioning Factors, Trigger, and Slide Dynamics </p><p>27  Detailed Observation of Topography and Geologic Architecture of a Submarine Landslide Scar in a Toe of an Accretionary Prism</p><p>28  Possible Ground Instability Factor Implied by Slumping and Dewatering Structures in High-Methane-Flux Continental Slope</p><p>29  Identification of Weak Layers and Their Role for the Stability of Slopes at Finneidfjord, Northern Norway</p><p>30 Mass Movements in a Transform Margin Setting: The Example of the Eastern Demerara Rise<br><br></p><p>Part IV Mechanics of Mass-Wasting in Subduction Margins<br><br></p><p>31  Slope Failures in Analogue Models of Accretionary Wedges</p><p>32  Systematic Development of Submarine Slope Failures at Subduction Margins: Fossil Record of Accretion-Related Slope Failure in the Miocene Hota Accretionary Complex, Central Japan</p><p>33  Morphologic Expression of Accretionary Processes and Recent Submarine Landslides Along the Southwestern Pacific Margin of Colombia</p><p>34  Submarine Mass Wasting Off Southern Central Chile: Distribution and Possible Mechanisms of Slope Failure at an Active Continental Margin</p><p>35  An Overview of the Role of Long-Term Tectonics and Incoming Plate Structure on Segmentation of Submarine Mass Wasting Phenomena Along the Middle America Trench</p><p>Part V Post-Failure Dynamics<br><br>36  Dynamics of Submarine Liquefied Sediment Flows: Theory, Experiments and Analysis of Field Behavior</p><p>37  Undrained Sediment Loading Key to Long-Runout Submarine Mass Movements: Evidence from the Caribbean Volcanic Arc</p><p>38  Impact Drag Forces on Pipelines Caused by Submarine Glide Blocks or Out-Runner Blocks</p><p>39  A Surging Behaviour of Glacigenic Debris Flows</p><p>40  Failure Processes and Gravity-Flow Transformation Revealed by High-Resolution AUV Swath Bathymetry on the Nice Continental Slope (Ligurian Sea)</p><p>41  Submarine Landslides, Gulf of Mexico Continental Slope: Insights into Transport Processes from Fabrics and Geotechnical Data <br><br></p><p>Part VI Landslide Generated Tsunamis<br><br></p><p>42  Tsunamis Generated by Submarine Landslides</p><p>43  Micro-bathymetric Evidence for the Effect of Submarine Mass Movement on Tsunami Generation During the 2009 Suruga Bay Earthquake, Japan</p><p>44  Re-evaluation of the 1771 Meiwa Tsunami Source Model, Southern Ryukyu Islands, Japan</p><p>45  The 1978 Quick Clay Landslide at Rissa, Mid Norway: Subaqueous Morphology and Tsunami Simulations</p><p>46  Geowave Validation with Case Studies: Accurate Geology Reproduces Observations</p><p>47  Tsunami Hazards for Nuclear Power Plants: Mass Failures, Uncertainty, and Warning<br><br></p><p>Part VII Witnessing and Quasi-Witnessing of Slope Failures</p><p>48  Submarine Slope Response to Earthquake Shaking Within Western Sagami Bay, Central Japan</p><p>49  Discovery of Submarine Landslide Evidence Due to the 2009 Suruga Bay Earthquake</p><p>50  Settling of Earthquake-Induced Turbidity on the Accretionary Prism Slope of the Central Nankai Subduction Zone</p><p>51  Study of Recent Small-Scale Landslides in Geologically Active Marine Areas Through Repeated Multibeam Surveys: Examples from the Southern Italy </p><p>Part VIII Architecture of Mass Transport Deposits/Complexes</p><p>52  Sedimentary Mélanges and Fossil Mass-Transport Complexes: A Key for Better Understanding Submarine Mass Movements?</p><p>53  The Specchio Unit (Northern Apennines, Italy): An Ancient Mass Transport Complex Originated from Near-Coastal Areas in an Intra-Slope Setting</p><p>54  Internal Stress Fields of a Large-Scale Submarine Debris Flow</p><p>55  Distribution of Submarine Mass Movement Deposits: An Exhumed Basin Perspective</p><p>56  Seismic-Scale Rafted and Remnant Blocks over Salt Ridges in the Espírito Santo Basin, Brazil</p><p>57  Permian and Triassic Submarine Landslide Deposits in a Jurassic Accretionary Complex in Central Japan</p><p>58  Systematic Spatial Variations in the Fabric and Physical Properties of Mass-Transport Deposits in the Ursa Region, Northern Gulf of Mexico</p><p>59  Records of Submarine Landslides in Subduction Input Recovered by IODP Expedition 322, Nankai Trough, Japan</p><p>60  Scientific Drilling of Mass-Transport Deposits in the Nankai Accretionary Wedge: First Results from IODP Expedition 333</p><p>61  Rock-Magnetostratigraphy of Hawaiian Archipelagic Sediments: Timing of Giant Submarine Landslides of the Hawaiian Ridge</p><p>62  Gravity Flow Deposits in the Deep Rockall Trough, Northeast Atlantic</p><p>Part IX Relevance of Natural Climate Change in Triggering Slope Failures</p><p><br>63  Submarine Mass Wasting in Isfjorden, Spitsbergen</p><p>64  Comparison of Quaternary Glaciogenic Debris Flows with Blocky Mass-Transport Deposits in Orphan Basin, Offshore Eastern Canada</p><p>65  Recent Submarine Landslides on the Continental Slope of Storfjorden and Kveithola Trough-Mouth Fans (North West Barents Sea)</p><p>66  One Million Years of Climatic Generated Landslide Events on the Northwestern Barents Sea Continental Margin</p><p>Author Index</p><p>Subject Index</p>