In situ 10Be
exposure ages from Norway: age-altitude diagrams
Linge, H1, Brook, E.J.2, Dahl, S.O.1,3, Mickelson, D.M.4, Nesje, A.1,5,
Raisbeck,
G.M.5 and Yiou, F.5
1 Bjerknes Centre for Climate Research,
Allégaten 55, N-5007 Bergen, Norway.
2 Department of Geosciences, Oregon State
University, Corvallis, Oregon 97331, USA.
3 Department of Geography, University of
Bergen, Breiviksveien 40, N-5045 Bergen, Norway.
4 Department of Geology and Geophysics,
University of Wisconsin, Madison, WI 53706, USA
5 Department of Earth Sciences, University
of Bergen, Allégaten 41, N-5007 Bergen, Norway.
6 Centre de Spectrométrie Nucléaire et de
Spectrométrie de Masse, Bât 108, 91495 Orsay, France.
More than 150 10Be exposure ages have been obtained from
various sites in Norway for the purpose of reconstructing Weichselian glacier
geometry in time and space. Typically, glacially moulded surfaces below
trimlines yield ages in the range 10 to 15 ka, i.e. the time elapsed since
deglaciation, whereas exposure ages from bedrock outcrops and/or block surfaces
in blockfields are in the range 25 to >80 ka. An additional trend is seen
for mountain summits lacking evidence of glacial erosion; summit peaks highly
exposed to weathering give younger ages than surfaces that have more shielded,
near-summit elevations. However, old exposure ages are not unambiguous evidence
for the existence of nunataks, and young ages are not necessarily synonymous
with glacial erosion occurring during the Late Glacial Maximum (LGM); in both
cases burial by cold-based, low-erosive ice may be of importance. More
meaningful differences, possibly linked to thermal regimes and ice thicknesses,
can be found in the general exposure age patterns between the western, eastern
and northern regions.
Recognizing that
the Quaternary glacial history of Scandinavia is more complex than a glacial
on-off signal, we seek to explore the Weichselian glacial history further by
continued exposure dating activity. Whereas one of the overall aims is to
reconstruct ice sheet configurations in the Weichselian period, 10Be
exposure dating in addition offers information on subglacial conditions,
subaerial weathering rates for various bedrock types, and duration of
sediment/glacial burial when combined with a second cosmogenic isotope and/or
with optically stimulated luminescence (OSL) dating.
Bjerknes Centenary 2004; Climate Change in High Latitudes, p 90-91,
Bergen, Norway.

S Norway – (Gaustatoppen and Skorve) – reference no. 1

Eastern southern Norway – (Elgåhogna and Rendalssølen) – reference no. 1

W-E transect, southern Norway - reference 2 and 3

NW Norway, Romsdalsfjord – reference no. 4+5+6

W Norway, Ulvanosi –reference no. 7

N Norway, Nordland, W-E transect – reference no. 8

N Norway, Lofoten-Vesterålen – reference no. 9
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