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- W2132486572 abstract "AbstractObservations are presented of a newly deposited snow-push ridge superimposed on a Holocene moraine in Coire an Lochain in the Cairngorm Mountains. The ridge formed when a sliding snow slab was thrust up the proximal slope of the moraine, entraining till gravel and redepositing it on the moraine crest. The process was a late-stage event during the complex wastage of a large snowfield resting on a rock slab, involving basal sliding, avalanching and melting. Snow-push landforms appear to be rare in Scotland. Nevertheless, these observations suggest that fresh material may be added to relict moraine crests in the present-day climate, with implications for exposure-age dating of moraines. However, in this case the addition of debris by snow push to a late Holocene moraine crest does not affect the interpretation of moraine age." @default.
- W2132486572 created "2016-06-24" @default.
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- W2132486572 date "2015-08-18" @default.
- W2132486572 modified "2023-09-26" @default.
- W2132486572 title "A Snow-Push Mechanism for Ridge Formation in the Cairngorm Mountains, Scotland" @default.
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- W2132486572 doi "https://doi.org/10.1080/14702541.2015.1068948" @default.
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