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Primary terms
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upper Quaternary (1)
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Tertiary
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Asmari Formation (1)
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Columbia River Basalt Group (1)
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upper Miocene
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Pliocene (5)
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upper Neogene (1)
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Paleogene
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Chordata
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Indian Ocean
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Integrated Ocean Drilling Program
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Expedition 323
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intrusions (6)
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Invertebrata
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soils
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soils
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Bristol Glacier
The location of Bristol Glacier, SW Greenland (modified from Statham et a...
Mark Skidmore sampling early season runoff in front of Bristol Glacier, Gre...
Mark Skidmore sampling runoff, some distance from the front of Bristol Glac...
Variations in air temperature, discharge and conductivity from Bristol Glac...
Concentrations of truly dissolved (<30 nM) amd colloidal (20-400 nM) Fe ...
Piper plots of Subglacial Lake Whillans (West Antarctica) lake-water and po...
8. Moving to the Greenland and Antarctic Ice Sheets (MT)
Glacier-influenced sedimentation on high-latitude continental margins: introduction and overview
Abstract The papers in this volume are the outcome of a Geological Society (London) meeting concerning glacier-influenced sedimentation on high-latitude continental margins, held at the University of Bristol, UK, in 2001. Since the publication of the Geological Society Special Publication Glacimarine Environments: Processes and Sediments (Dowdeswell & Scourse 1990), the intervening 11 years have seen a significant increase in research into the processes and patterns of glacimarine sedimentation, and the relationship between ice dynamics and the sediments and landforms preserved in the glacimarine environment. In this introduction, we outline the papers that make up the volume and we highlight the main findings and significance of each. First, however, we highlight three areas relating to sedimentation in glacimarine environments where we believe significant progress has been made in the last 11 years. These are: (1) glacially-influenced continental slope sedimentation; (2) iceberg-rafting processes and events; and (3) reconstructing the dynamics of former marineterminating ice sheets from glacial geomorphological evidence on continental shelves. Each of these areas is represented by papers in this volume.