when quantitative estimates of bedrock erosion and weathering rates are made (eg, Larsen and Mangerud, 1981; Hallet et al., 1996). One can easily imagine situations where sediment recycling has been underestimated or not recognized, with the result that bedrock erosion has been overestimated. Progla...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1029.3303 2023-05-15T16:21:59+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1029.3303 http://hol.sagepub.com/content/19/3/415.full.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1029.3303 http://hol.sagepub.com/content/19/3/415.full.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://hol.sagepub.com/content/19/3/415.full.pdf text ftciteseerx 2016-10-30T00:07:58Z when quantitative estimates of bedrock erosion and weathering rates are made (eg, Larsen and Mangerud, 1981; Hallet et al., 1996). One can easily imagine situations where sediment recycling has been underestimated or not recognized, with the result that bedrock erosion has been overestimated. Proglacial areas of the Jostedalsbreen ice field in western Norway were affected by numerous Holocene glacial advances (Figure 1; eg, Matthews, 1991; Nesje and Kvamme, 1991; Nesje et al., 2001). One striking observation on the glacier foreland is that the size of the glacial, depositional landforms is seemingly at odds with the present-day sediment-poor outlet glaciers of the Jostedalsbreen ice field (Matthews et al., 1979; Lien and Rye, 1988; Winkler and Nesje, 1999; Burki et al., 2009). In addition, large proportions of rounded boulders have been observed in the valleys inside the ‘Little Ice Age ’ (LIA) maximum moraine. This last observation is the focus of this paper in which we aim to explain the atypically, apparently high content of rounded boul-ders in lateral moraines. These lateral moraines were formed dur-ing the advance to the LIA maximum and during the subsequent Text glacier Unknown Norway Hallet ENVELOPE(6.662,6.662,63.003,63.003) Nesje ENVELOPE(13.767,13.767,68.300,68.300) |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
when quantitative estimates of bedrock erosion and weathering rates are made (eg, Larsen and Mangerud, 1981; Hallet et al., 1996). One can easily imagine situations where sediment recycling has been underestimated or not recognized, with the result that bedrock erosion has been overestimated. Proglacial areas of the Jostedalsbreen ice field in western Norway were affected by numerous Holocene glacial advances (Figure 1; eg, Matthews, 1991; Nesje and Kvamme, 1991; Nesje et al., 2001). One striking observation on the glacier foreland is that the size of the glacial, depositional landforms is seemingly at odds with the present-day sediment-poor outlet glaciers of the Jostedalsbreen ice field (Matthews et al., 1979; Lien and Rye, 1988; Winkler and Nesje, 1999; Burki et al., 2009). In addition, large proportions of rounded boulders have been observed in the valleys inside the ‘Little Ice Age ’ (LIA) maximum moraine. This last observation is the focus of this paper in which we aim to explain the atypically, apparently high content of rounded boul-ders in lateral moraines. These lateral moraines were formed dur-ing the advance to the LIA maximum and during the subsequent |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1029.3303 http://hol.sagepub.com/content/19/3/415.full.pdf |
long_lat |
ENVELOPE(6.662,6.662,63.003,63.003) ENVELOPE(13.767,13.767,68.300,68.300) |
geographic |
Norway Hallet Nesje |
geographic_facet |
Norway Hallet Nesje |
genre |
glacier |
genre_facet |
glacier |
op_source |
http://hol.sagepub.com/content/19/3/415.full.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1029.3303 http://hol.sagepub.com/content/19/3/415.full.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766009960038137856 |