Open AccessGlacial advance, occupation and retreat sediments associated with multi‐stage ice‐dammed lakes: north‐central Alberta, Canada
Author(s) -
Slomka Jessica M.,
Utting Daniel J.
Publication year - 2018
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/bor.12257
Subject(s) - geology , glacial period , sedimentary depositional environment , ice sheet , glacial lake , shelf ice , stage (stratigraphy) , geomorphology , moraine , facies , ice stream , physical geography , paleontology , structural basin , oceanography , cryosphere , sea ice , geography
Ice sheets that advance upvalley, against the regional gradient, commonly block drainage and result in ice‐dammed proglacial lakes along their margins during advance and retreat phases. Ice‐dammed glacial lakes described in regional depositional models, in which ice blocks a major lake outlet, are often confined to basins in which the glacial lake palaeogeographical position generally remains semi‐stable (e.g. Great Lakes basins). However, in places where ice retreats downvalley, blocking regional drainage, the palaeogeographical position and lake level of glacial lakes evolve temporally in response to the position of the ice margin (referred to here as ‘multi‐stage’ lakes). In order to understand the sedimentary record of multi‐stage lakes, sediments were examined in 14 cored boreholes in the Peace and Wabasca valleys in north‐central Alberta, Canada. Three facies associations ( FAI – III ) were identified from core, and record Middle Wisconsinan ice‐distal to ice‐proximal glaciolacustrine ( FAI ) sediments deposited during ice advance, Late Wisconsinan subglacial and ice‐marginal sediments ( FAII ) deposited during ice‐occupation, and glaciolacustrine sediments ( FAIII ) that record ice retreat from the study area. Modelling of the lateral extent of FA s using water wells and gamma‐ray logs, combined with interpreted outlets and mapped moraines based on Li DAR imagery, facilitated palaeogeographical reconstruction of lakes and the identification of four major retreat‐phase lake stages. These lake reconstructions, together with the vertical succession of FA s, are used to develop a depositional model for ice‐dammed lakes during a cycle of glacial advance and retreat. This depositional model may be applied in other areas where meltwater was impounded by glacial ice advancing up the regional gradient, in order to understand the complex interaction between depositional processes, ice‐marginal position, and supply of meltwater and sediment in the lake basin. In particular, this model could be applied to decipher the genetic origin of diamicts previously interpreted to record strictly subglacial deposition or multiple re‐advances.