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- W1982183907 abstract ". Geomorphological and sedimentological evidence of former glaciation in the Bizzle valley in the Cheviot Hills of northern England and southern Scotland was used to reconstruct the dimensions of a small topographically constrained glacier with an equilibrium line altitude (ELA) of 535 m. This was interpreted as having formed during Younger Dryas cooling; this is the only glacier to have been described from the area and is the most easterly site of Younger Dryas glaciation in the British Isles. Whilst glaciation at this time was extensive in the Lake District to the southwest, the restricted nature of Cheviot ice cover suggests that a steep west–east precipitation gradient existed in this region during the Younger Dryas." @default.
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- W1982183907 date "2006-10-01" @default.
- W1982183907 modified "2023-09-24" @default.
- W1982183907 title "The eastern margin of glaciation in the british isles during the younger dryas: the bizzle cirque, southern scotland" @default.
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- W1982183907 doi "https://doi.org/10.1111/j.1468-0459.2006.00295.x" @default.
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