Open AccessA Younger Dryas (Loch Lomond Stadial) jökulhlaup deposit, Fort Augustus, Scotland
Author(s) -
RUSSELL ANDREW J.,
MARREN PHILIP M.
Publication year - 1998
Publication title -
boreas
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.95
H-Index - 74
eISSN - 1502-3885
pISSN - 0300-9483
DOI - 10.1111/j.1502-3885.1998.tb01418.x
Subject(s) - geology , sedimentology , stadial , sedimentary rock , younger dryas , pleistocene , pebble , meltwater , sediment , sedimentary structures , terrace (agriculture) , geomorphology , deposition (geology) , glacial period , sedimentary depositional environment , geochemistry , paleontology , archaeology , structural basin , history
This study provides an insight into the impact of probably the largest flood ever to have been identified in mainland Britain by examining new sedimentary evidence from the Auchteraw terrace, Fort Augustus, Scotland. Study of three sections reveals a succession consisting of: (1) sheet gravels; (2) large trough‐shaped depressions infilled with cross‐stratified sands and gravels; (3) smaller‐scale, finer‐grained cross‐strata; and (4) sheet‐like, occasionally channelized, bimodal sand and gravel beds. This study shows that both the sedimentology and morphology of the Auchteraw terrace are consistent with jökulhlaup deposition and reveal a greater variety of lithofacies types than identified in previous studies of jökulhlaups from ice‐dammed lakes. The fine‐grained nature of the sediment discussed in this study emphasizes the importance of sediment supply for the formation of distinctive jökulhlaup successions. The sedimentary evidence recorded here provides a valuable tool for the interpretation of the magnitude and frequency of proglacial meltwater flows associated with Pleistocene ice sheets worldwide.