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Drainage of these lakes occurred by both marginal and subglacial routes; in the latter case, the sudden outburst may be responsible for anomalously coarse flood deposits found downstream. It is argued that glacial lakes were a much more common feature of the deglacial landscape than recent reviews have suggested and their presence at the ice margin may have glaciological implications, as inferred by the often distinctive landform-sediment assemblages involved.<\/jats:p>","DOI":"10.1144\/sjg30020147","type":"journal-article","created":{"date-parts":[[2010,1,15]],"date-time":"2010-01-15T00:30:59Z","timestamp":1263515459000},"page":"147-158","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":4,"title":["Former glacial lakes in the Dee valley: origin, drainage and significance"],"prefix":"10.1144","volume":"30","author":[{"given":"Iain M.","family":"Brown","sequence":"first","affiliation":[{"name":"Department of Geography, University of Aberdeen, Elphinstone Road, Aberdeen AB9 2UF"}]}],"member":"1881","published-online":{"date-parts":[[2022,6,7]]},"reference":[{"key":"e_1_2_1_2_1","unstructured":"AITKEN J. F. 1991. 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