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100			_aAa, Asbjørn Rune _951447
245			_aEarly-Holocene glacier fluctuations of northern Grovabreen, western Norway/
260			_bsage _c2019
300			_aVol 29, Issue 2, 2019 : (187-196 p.).
520			_aMarginal moraines on the northern side of Grovabreen, a plateau glacier in inner Sunnfjord, Western Norway, have been mapped and morphostratigraphically correlated with the Erdalen Event and possibly the Finse Event and the ‘Little Ice Age’. Schmidt-hammer exposure-age dating was used to evaluate the age of the most distinct marginal moraines by measuring the degree of surface weathering on boulders. The lithostratigraphy of lake sediments was analysed in a core from Dalevatnet in order to correlate this stratigraphy with the marginal moraines in the catchment area of the lake and reconstruct the early-Holocene history of Grovabreen. The lake catchment was deglaciated at 10,750 cal. yr BP. Two readvances of an outlet glacier in Fagredalen were dated to between 10,340 and 9960 cal. yr BP, correlated with the two-peaked Erdalen Event. A readvance shortly after 8450 cal. yr BP can most probably be correlated with the 8200 cal. yr BP Finse Event.
650			_adistal glacier-fed lake, _951448
650			_aearly Holocene, _951415
650			_aErdalen Event, _951449
650			_a Finse Event, _951450
650			_aglacier fluctuations, _951451
650			_aGrovabreen, _951452
650			_a Holocene, _950806
650			_alake sediments, _951453
650			_aSchmidt hammer, _951454
650			_a Western Norway _951455
700			_aSønstegaard, Eivind _951456
773	0		_012756 _916504 _dLondon: Sage Publication Ltd, 2019. _tHolocene/ _x09596836
856			_uhttps://doi.org/10.1177/0959683618810392
942			_2ddc _cART
999			_c12771 _d12771