Age determination and grwoth rates of stalagmites and stalactites from the Okshola cave, Fauske, northern Norway

The sensitivity of terrestrial environments to past changes in heat transport is expected to be manifested in Holocene climate proxy records on millennial to seasonal timescales. Stalagmite formation in the Okshola cave near Fauske (northern Norway) began at about 10.4 ka, soon after the valley was...

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Bibliographic Details
Main Authors: Linge, Henriette, Lauritzen, Stein-Erik, Andersson, Carin, Hansen, J K, Skoglund, Rannveig O, Sundqvist, H S
Format: Dataset
Language:English
Published: PANGAEA 2009
Subjects:
FM3
SPS
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.728964
https://doi.org/10.1594/PANGAEA.728964