dc.contributor.author | Moe, Dagfinn | |
dc.contributor.author | Salvesen, Per Harald | |
dc.date.accessioned | 2022-01-10T08:09:17Z | |
dc.date.available | 2022-01-10T08:09:17Z | |
dc.date.issued | 2022 | |
dc.identifier.uri | https://hdl.handle.net/11250/2836627 | |
dc.description.abstract | Marine mollusk activity initiate erosion cavities in marble and dolomite in the Saltsraumen littoral zone. Such cavities are gradually exposed above sea water by the still on-going eustatic rebound since the last Ice age. The diameter of cavities observed above the high tide zone plotted against altitude show a steady increase in size over time due to weathering processes. Weathering rates as a function of land rise are calculated and discussed. The observed growth rates are correlated with chronology of sea level changes in the same period based on alternative data. | en_US |
dc.language.iso | eng | en_US |
dc.title | Marine bio-erosion cavities in metamorphic limestone, weathering rates, and the post glacial land rise in Salten, North Norway. | en_US |
dc.type | Journal article | en_US |
dc.description.version | draft | en_US |
dc.rights.holder | Copyright the authors. All rights reserved | en_US |