Lateglacial and early Holocene palaeoclimatic reconstruction based on glacier fluctuations and equilibrium-line altitudes at northern Folgefonna, Hardanger, western Norway

2005 ◽  
Vol 20 (2) ◽  
pp. 179-198 ◽  
Author(s):  
Jostein Bakke ◽  
Svein Olaf Dahl ◽  
Atle Nesje
Keyword(s):  
Early Holocene ◽  
Equilibrium Line ◽  
Glacier Fluctuations ◽  
Western Norway ◽  
Palaeoclimatic Reconstruction

Timing, equilibrium-line altitudes and climatic implications of two early-Holocene glacier readvances during the Erdalen Event at Jostedalsbreen, western Norway

The Holocene ◽  
2002 ◽  
Vol 12 (1) ◽  
pp. 17-25 ◽  
Author(s):  
Svein Olaf Dahl ◽  
Atle Nesje ◽  
Øyvind Lie ◽  
Kristine Fjordheim ◽  
John A. Matthews
Keyword(s):  
Early Holocene ◽  
Equilibrium Line ◽  
Western Norway

scholarly journals Glacier fluctuations, equilibrium-line altitudes and palaeoclimate in Lyngen, northern Norway, during the Lateglacial and Holocene

The Holocene ◽  
2005 ◽  
Vol 15 (4) ◽  
pp. 518-540 ◽  
Author(s):  
Jostein Bakke ◽  
Svein Olaf Dahl ◽  
Øyvind Paasche ◽  
Reidar Løvlie ◽  
Atle Nesje
Keyword(s):  
Equilibrium Line ◽  
Northern Norway ◽  
Glacier Fluctuations

Neoglaciation in the southern Coast Mountains of British Columbia: chronology prior to the late Neoglacial maximum

1986 ◽  
Vol 23 (3) ◽  
pp. 273-287 ◽  
Author(s):  
J. M. Ryder ◽  
B. Thomson
Keyword(s):  
British Columbia ◽  
Early Holocene ◽  
Southern Coast ◽  
Radiocarbon Dates ◽  
Coast Mountains ◽  
Glacier Fluctuations ◽  
Related Information ◽  
Eighteenth And Nineteenth Centuries

Moraine stratigraphy and morphology, radiocarbon dates from Klinaklini, Franklin, Tiedemann, Gilbert, and Bridge glaciers, and related information from elsewhere in the Coast Mountains are used to construct a chronology for glacier fluctuations. The Garibaldi phase of glacier expansion, 6000–5000 14C years BP, at the end of the early Holocene xerothermic interval, is indicated by overridden tree stumps. The mid-Neoglacial Tiedemann advance, 3300–1900 14C years BP, is represented by moraines, till, and meltwater sediments at three glaciers, but only Tiedemann Glacier attained its greatest Holocene extent at this time. Late Neoglacial expansion commenced before 900 14C years BP and continued without notable interruption until glaciers achieved their maximum post-Pleistocene expansion during the eighteenth and nineteenth centuries. Evidence for the Garibaldi and Tiedemann events is scarce within the Coast Mountains because of the more extensive late Neoglacial advance. However, correlative advances have been recognized in adjacent mountains within British Columbia, Washington, and Alaska.

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