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- W2000413215 abstract "It is suggested that a kamiform gravel-moraine can be traced along the Eddleston and Meldon valleys to continue up the Stobo reach of the Tweed valley. The supplying glacier was fed from the west. The main Eddleston kame is now extensively opened, and its material dips steeply, transversely, to the east. The lower Eddleston valley seems to have been sheltered during the kame episode by the Meldon valley to the west. In all three valleys it looks as if the glacier tended to be limited by valley-bottom marginal torrents." @default.
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- W2000413215 date "1956-01-01" @default.
- W2000413215 modified "2023-09-26" @default.
- W2000413215 title "Eddleston Gravel moraine" @default.
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- W2000413215 doi "https://doi.org/10.1144/transed.16.3.254" @default.
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