European Margin Sediment Dynamics

"European Margin Sediment Dynamics" by Jürgen Mienert, Phillip Weaver is a physics book focused on Astronomical Data. Best for students, educators, and scientifically curious readers.

Topic: Astronomical Data

Author: Jürgen Mienert, Phillip Weaver

Who this is for:

• Physics students
• Science-minded readers
• Readers building technical understanding

Why this book matters: It provides structured coverage of physics concepts in a way that supports deeper understanding and continued study.

Of Geophysical Techniques -- The Norwegian Margin -- GLORIA Lang-Range Sidescan Sonar Mosaic of the North Norwegian Margin (67-75°N) -- Large-Scale Slides on the North Norwegian Margin Imaged by GLORIA -- The Northern Storegga Slide Escarpment -- Morphology and Features -- A Weak Layer Feature on the Northern Storegga Slide Escarpment -- Morphology of a Non-glacigenic Debris Flow Lobe in the Helland Hansen Area Investigated with 3D Seismic Data -- The Trænadjupet Slide: Sediment Disintegration and Flow -- Morphology and Acoustic Character of the Middle and Lower North Sea Fan -- Debris Flow Activity on the Bear Island and Trough Mouth Fan from GLORIA and 3.5 kHz Records. -- Submarine Glacigenic Debris Flows on the Bear Island Trough Mouth Fan, Western Barents Sea: Aspects of Flow Behaviour -- Morphology of Glacigenic Debris Flows on the Upper North Sea Fan -- Canyon and Channel Systems in the Lofoten Basin, Norwegian Margin -- Morphology of the Lofoten Basin Channel -- The Lofoten Contourite Drift: High-Resolution Seismic Stratigraphy -- Gas Hydrates at Storegga Slide. -- Seabed and Subsurface Features on the Southern Vøring Plateau and Northern Storegga Slide Escarpment -- The Håkon Mosby Mud Volcano -- The Faeroe-Shetland Margin -- Leng-Range Side-Scan Sonar Imagery of the North Faeroes Margin -- A Major Channel System on the North Faeroes Margin from Side-Scan Sonar Records -- A Record of Mid-Cenozoic Strong Deep-Water Erosion on the Faeroe-Shetland Channel -- Morphology of an Ice-Sheet Limit and Constructional Glacially-Fed Slope Front, Faeroe-Shetland Channel -- Sandy Contourites and Pathways of the Norwegian Sea Overflow Water, West of the Faeroe Bank Channel -- The Rockall-Porcupine Margin -- Images of Sliding and Slumping Along the Porcupine and SW Rockall Trough Margins -- Holocene Shelf-Margin Submarine Landslides, Donegal Fan, Eastern Rockall Trough -- Canyon Heads and Channel Architecture of the Gollum Channel, Porcupine Seabight -- The Continental Rise West of Porcupine Seabight, Northeast Atlantic -- Growth and Partial Destruction of a Neogene Sediment Drift, Western Rockall Trough -- Development of a Sediment Drift: Feni Drift, NE Atlantic Margin -- Giant Carbonate Mounds and Current-Swept Seafloors on the Slopes of the Southern Rockall Trough -- Giant Carbonate Mounds Along the Porcupine and SW Rockall Trough Margins -- Mounds and Sediment Drift in the Porcupine Basin, West of Ireland -- The Celtic and Armorican Margins -- a New View -- Morphology and Seismic Stratigraphy of the Manche Paleoriver System, Western Approaches -- The Celtic Deep-Sea Fan: Seismic Facies, Architecture and Stratigraphy -- Morphology and Depositional Processes of the Celtic Fan, Bay of Biscay -- Physiography of the Armorican Turbidite System (Bay of Biscay) -- The Iberian and Canaries Margin including NW Africa -- Sediment Dynamic Features on the Eastern Gulf of Cadiz (SW Spain) -- Reassessment of Sedimentary Evidence for Deep Contour Currents West of Iberia -- Debris Avalanche Deposits on the Flanks of the Canary Islands: Contrasts Between El Hierro and Tenerife -- Flow Processes in the Saharan Debris Plow -- Turbidity Current Processes and Deposits in the Moroccan Turbidite System -- Oligocene to Recent Processes on the Agadir Continental Margin and Basin (Central Eastern Atlantic) -- Canyon Switching in the Moroccan Turbidite System, Northwest African Margin -- Large-Scale Slides on the Flanks of the Canary Islands -- Giant Landslides off the Islands of La Palma -- El Hierro: Shaping of an Oceanic Island by Mass Wasting.