Now showing items 1-7 of 7
Evaluation of Modern Sedimentation Processes in a Proglacial Lake: Linnévatnet, Spitzbergen, Svalbard
Patty studied the texture and lamination stratigraphy preserved in the sediment traps recovered from Lake Linne'. These traps were deployed from summer 2006 to summer 2007 and a few large diameter traps deployed from April ...
Fjord Sedimentation Associated with a Submarine jet and Plume Discharging into Kongsfjorden, Svalbard, Norway
Luke, studied the modern processes associated with meltwater discharge along the front of a calving tidewater glacier (Kongsbreen) near NyAlesund, Svalbard, Norway
Ice-marginal Delta Formation and Sedimentaty Processes of Kongsvegen Glacier in Kongsfjorden, Svalbard, Norway.
Ryan's research focussed on formation and deposition of a submarine meltwater delta in the proglacial fjord environment of Kongfjorden
Sedimentation in High-Arctic Lake, Linnévatnet, Svalbard: A Modern Process Study Using Sediment Traps
Megan studied the sediment trap records from Lake Linne' that were deployed during the 07/08 sedimentation year. She related textural changes in the various sediment traps to one another and to measured weather parameters, ...
Comparison of lamination stratigraphies of cores recovered from the proximal basin of Lake Linne, Svalbard, Norway
Bennett's research was directed at correlating the lamination stratigraphy of adjacent cores recovered from a proximal basin in Lake Linne'. His work showed that small changes in position and bathymetry can cause changes ...
Mechanisms and Processes of Suspended Sediment Transport and Deposition in High Arctic Proglacial Lake Linne'vatnet, Spitsbergen, Svalbard
Ben's research was directed at better understanding how and under what conditions sediment was distributed and deposited in Lake Linne' during the 2005/2006 sedimentation year.
Characterization of Climatic Influences on Modern Sedimentation in an Arctic Lake, Svalbard, Norway
Nick, was the first student to study the sediment traps recovered from Lake Linne' and to relate the measured textural changes from trap to trap and to measured weather parameters in the valley