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Stratigraphic architecture and infill history of a deglaciated bedrock valley based on georadar, seismic profiling and drilling
Author(s) -
HANSEN LOUISE,
BEYLICH ACHIM,
BURKI VALENTIN,
EILERTSEN RAYMOND S.,
FREDIN OLA,
LARSEN EILIV,
LYSÅ ASTRID,
NESJE ATLE,
STALSBERG KNUT,
TØNNESEN JAN F.
Publication year - 2009
Publication title -
sedimentology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.494
H-Index - 108
eISSN - 1365-3091
pISSN - 0037-0746
DOI - 10.1111/j.1365-3091.2009.01056.x
Subject(s) - geology , bedrock , deglaciation , geomorphology , fluvial , alluvial fan , structural basin , moraine , outwash plain , glacier , paleontology , glacial period
The sediment fill of a silled bedrock valley in Western Norway has been investigated with respect to stratigraphy and infill history using a combination of mapping, georadar, seismic profiling and drilling. A small outlet glacier occupies the head of the valley that displays a stepwise down‐valley profile and terminates in a lake at 29 m above sea‐level. The valley is surrounded by high, steep bedrock slopes and is characterized by a series of filled basins each limited by sills of bedrock or moraine accumulations. Till, glacial outwash and/or rockslide deposits fill in the lower half of the two larger basins. (Fan) delta deposits fringed by the deposits of alluvial fans and colluvial cones dominate the upper fill of most basins. (Fan) delta deposits interfinger downstream with lake sediments in the larger basins and fluvial deposits comprise the top fill. The overall infill pattern was controlled by deglaciation as well as basin size and shape. An overall decreasing sediment supply following deglaciation is shown in the fill of a larger basin down‐valley, whereas a recently increasing sediment supply during glacier growth is reflected primarily in an upstream basin. Only the lowermost basin was exposed to a sea‐level drop from 75 m above sea‐level to the present lake level associated with incision and river migration. This observation is in contrast to the basins above marine influence where incision has been limited due to fixed downstream sills resulting in insignificant erosion except for some fan‐head entrenchment. It follows that the fills of these small valley basins display progradational and aggradational trends of deposition and paraglacial reworking has been limited. Additionally, the study demonstrates that georadar profiling, combined with other methods, is very useful for comprehensive investigation of valley basins.