17 Lake Research and Monitoring Networks in the Northeast

Sunday, 18 March 2018
1:30 PM - 5:30 PM
Emerald Ballroom I

SEISMIC TRIGGER LACUSTRINE LANDSLIDES IN LAKE CHAMPLAIN

Paper number: 17-1
Program: Theme Sessions
Time: 1:30 PM – 1:50 PM

Authors

Abstract

Lacustrine slumps and debris flows (landslides) have been identified in Lake Champlain via Multibeam and CHIRP (compressed high intensity radar pulse) seismic profile imager. Numerous large landslides studied by Ghosh (2012), Rosales-Underbrink (2015), and Silverhart (2016) have shown that many of these landslides are coeval. All landslides failed on a specific interface between marine Champlain Sea and modern lacustrine Lake Champlain sediments. Utilizing radionuclide dating on sediment from the unfailed slopes or undisturbed sediment above failed deposits, sedimentation rates were determined and used to calculate the approximate failure ages for each of the landslides studied. The northernmost failure, south of the Bouquet River, occurred about 950-1200 cal yr BP and is the first mass wasting event of this age to be recorded on Lake Champlain. The remaining landslides failed about 4500-5200 cal yr BP and agree with nearby Western Quebec Seismic Zone (WQSZ) where clusters of terrestrial landslides occurring at 1000 and 5000 cal yr BP, and are triggered by large earthquakes (Brooks, 2015) along the same interface. The 5000 cal yr BP event has been attributed to a M 6.4 or greater earthquake within the WQSZ. The landslides observed in Lake Champlain are likely triggered by this same earthquake. Additionally, lake tsunami models show that these simultaneous landslide failures can generate a surface water wave of 30 feet that can impact the Lake Champlain shoreline within 3-10 minutes after the earthquake.

Geological Society of America Abstracts with Programs. Vol. 50, No. 2

doi: 10.1130/abs/2018NE-310497

© Copyright 2018 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.