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- W2022630096 abstract "The central Glomdal caves, Storbekkgrotta and Kalkrastgrotta, are found within a 30 m (approximately) thick band of white marble. The karst system is allogenic and the cave morphology and surface topography provide evidence of several phases of development: 1. Phreatic conduit development. 2. Drainage and vadose incision. 3. Partial or complete infill with clastic (glaciogenic) sediments. 4. Glacial truncation of the conduits. 5. Reversed, phreatic flow in the up-hill direction, producing paragenetic halftubes and rock pendants. 6. Partial outwash of the previous infilling sediment. 7. Holocene vadose invasion. Since the paragenetic features are superimposed onto vadose features, the reversed flow must have occurred after base-level (i.e. bedrock) lowering. Together with the topographical situation of the karst, phase 5 (paragenesis under reversed flow) may be explained by subglacial water flow. This implies a temperate glacier sole at a time when the icefield could over-ride the local valley topography and provide an up-hill directed englacial hydraulic gradient. The results suggest that sub-glacial water flow may utilize pre-existing karst conduits (which are extremely stable Nye-channels in the glaciohydrologic context) and enlarge them somewhat. It is still not proven that entire cave passages with radii of 1 to 2 m may form under such sub-glacial conditions, as suggested by Horn in 1947. The chemistry and conduit hydrology of deep sub-glacial waters are crucial parameters in this regard." @default.
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- W2022630096 date "1984-01-01" @default.
- W2022630096 modified "2023-10-03" @default.
- W2022630096 title "Evidence of subglacial karstification in Glomdal, Svartisen, Norway" @default.
- W2022630096 doi "https://doi.org/10.1080/00291958408552122" @default.
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