15 Pleistocene to Modern Landforms and Change: Using Field and High-resolution Topographic Data to Unravel Landscape History and Quantify Change

Sunday, 20 March 2022
1:30 PM - 5:30 PM
Commonwealth Salon 2


POST-GLACIAL SEDIMENT DELIVERY CONTINUUM TO AN IMPOUNDED VALLEY REACH IN CENTRAL MAINE: A MULTI-DISCIPLINARY APPROACH

Paper number: 15-5
Program: Theme Sessions
Time: 2:40 PM – 3:00 PM


Authors


Abstract

Freshwater lakes in the northern United States and Canada archive stratigraphy that can provide records of sediment supply since deglaciation. The records are unique due to the presence of glacial sediments, glacially-carved pools in the longitudinal profiles of stream and river valleys, and the influence of dams and human activities on surface water hydraulic conditions. We use ground-penetrating radar (GPR), sedimentary core analysis, acoustic bottom mapping, existing high-resolution topography, and empirical modeling to investigate dynamics from para- and post-glacial periods through the present. We map sediment sources and the stratigraphy and volume of deposits associated with a 175 ha freshwater lake system with a 33.1 km2 watershed on the Kennebec-Penobscot watershed divide (Kingsbury Pond, central Maine, USA). A combination of core data and GPR analysis indicate that high inorganic sediment delivery (1,417–1,913 Mg yr-1) dominated Kingsbury’s sedimentary environment until 8,550–8,410 cal yr BP—implying longer paraglacial conditions than assumed—after which sediment load decreased by more than an order of magnitude (to just 65–87 Mg yr-1). We compare these calculations to empirical estimates of water erosion for the watershed and discuss the implications and limitations of such comparisons. We also examine topographic evidence that suggests that much of the inorganic sediment may have been excavated from large outwash channels during deglaciation, and potentially that an extended paraglacial watershed configuration delayed the transition from inorganic to organic-dominant sediment.

Geological Society of America Abstracts with Programs. Vol. 54, No. 3

doi: 10.1130/abs/2022NE-374798

© Copyright 2022 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.