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Overdeepening is a characteristic of basins and valleys eroded by glaciers. An overdeepened valley profile is often eroded to depths which are hundreds of metres below the lowest continuous surface line (the thalweg) along a valley or watercourse. This phenomenon is observed under modern-day glaciers, in saltwater fjords and freshwater lakes remaining…
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ice water glacier valleys glacial erosion bedrock subglacial sediment overdeepened lakes fjords fjord tunnel sea valley flow glaciers level filled
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Overdeepening | is a | characteristic of basins and valleys eroded by glaciers | 0.90 | text |
| northwest of the valley | instance of | Similarly tunnel channels in the Flathead Valley beneath Flathead Lake were formed by subglacial drainage from multiple sources | 0.80 | text |
| that now covering Antarctica | instance of | U-shaped valley originally cut under the glacial ice near the margin of continental ice sheets | 0.80 | text |
| formerly covering portions of all continents during past glacial ages | instance of | U-shaped valley originally cut under the glacial ice near the margin of continental ice sheets | 0.80 | text |
| those produced by strong diurnal melt cycles result in temporary water pressure excursions | instance of | Episodic increases in water input | 0.80 | text |
| mountain passes produced enhanced erosion beneath thicker | instance of | rain and surface lake drainage events will cause movement.Analytic glacial erosion models suggest that ice flows passing through constrained spaces | 0.80 | text |
| faster ice flows | instance of | rain and surface lake drainage events will cause movement.Analytic glacial erosion models suggest that ice flows passing through constrained spaces | 0.80 | text |
| which deepens the channel below areas both upstream | instance of | rain and surface lake drainage events will cause movement.Analytic glacial erosion models suggest that ice flows passing through constrained spaces | 0.80 | text |
| downstream | instance of | rain and surface lake drainage events will cause movement.Analytic glacial erosion models suggest that ice flows passing through constrained spaces | 0.80 | text |
| Overdeepening | related to Adverse slope zone | As | 0.60 | section |
| Overdeepening | related to Adverse slope zone | The | 0.60 | section |
| Overdeepening | related to Adverse slope zone | At | 0.60 | section |
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