|Title||Distribution and lithostratigraphic controls of massive ice in Northwest Territories and northern Yukon: new insights from seismic shothole drillers' logs|
|Author||Smith, I R|
|Source||CANQUA, Canadian Quaternary Association annual meeting, abstracts; 2013 p. 1|
|Alt Series||Earth Sciences Sector, Contribution Series 20130002|
|Publisher||Canadian Quaternary Association|
|Meeting||CANQUA; Edmonton; CA; August 18-21, 2013|
|Province||Northwest Territories; Yukon|
|NTS||106I; 106J; 106K; 106L; 106M; 106N; 106O; 106P; 107A; 107B; 107C/01; 107C/02; 107C/03; 107C/04; 107C/05; 107C/06; 107C/07; 107C/08; 107D; 107E/01; 107E/02; 107E/03; 107E/08|
|Area||Tuktoyaktuk Peninsula; Richards Island; Richardson Mountains; Mackenzie River|
|Lat/Long WENS||-136.0000 -128.0000 70.5000 66.0000|
|Subjects||surficial geology/geomorphology; stratigraphy; ice; ice morphology; massive ice; lithostratigraphy; Cenozoic; Quaternary|
|Program||Land-based Infrastructure, Climate Change Geoscience|
|Abstract||Massive ice and other ice-rich sediments (ground ice) are considered to be widespread in areas of northwestern mainland Canada. These conditions constitute significant existing and climate
change-amplified hazard potential related to rapid coastal erosion and thermokarst in areas of potential infrastructure development. While many massive ice occurrences have been the subject of direct and detailed field investigation, including
monitoring, the ability to detect, quantify, and predict the occurrence of such deposits over large spatial areas is often limited to outcrops and those cases where surface geomorphology (heaving or thermokarst) can be discerned, yet even here,
thickness and lateral extents remain largely unknown.|
Amongst the earliest (1970s) regional assessments of massive ice in the Tuktoyaktuk Peninsula and Richards Island area stemmed from analysis of ~15k seismic shothole drillers' log records by
Mackay, Rampton and others. Recent research by Smith (2011) who recovered all available shothole drillers' log records from Industry archives within continental NWT and Yukon has expanded this knowledge base by orders of magnitude (344k records),
from which new inferences about massive ice's thickness, depth, spatial extent, and over and under-lying lithostratigraphy can be drawn.
Massive ice is recorded in 2354 shothole drillers' logs, and ranges in thickness from an assigned 1.0 m
minimum, up to 61 m, averaging 8.8 m (an additional 13 753 shothole drillers' logs reported ground ice, many of which likely represent massive ice, or what others have classified as 'icy sediments'). The upper limit of approximately 23% of all
shothole massive ice records occur at surface (base of active layer), while ~56% initiate within the uppermost 5 m; less than 10% of massive ice bodies extend below 30 m depth. The highest concentrations of massive ice (46-51%) occur between 4 and 14
m depth. Significant variations are seen in the distribution of massive ice deposits, with highest occurrences in the Tuktoyaktuk Peninsula (51% of all massive ice records), Richards Island, Arctic Coastal Plain and northern Richardson mountains.
Lesser concentrations are found in Eagle Plain, central Richardson Mountains, lower Mackenzie River, and Colville Hills; south of these regions, massive ice deposits are rare to absent. Associations between massive ice and shothole-derived surficial
geology reinforce previous assertions that such deposits are most commonly found in areas of till cover, and that most massive ice bodies occur at the lithostratigraphic boundary between different materials (73% of the 1883 records which fully
penetrate a massive ice body). Shothole-derived lithostratigraphy confirms overall trends in overlying and underlying materials, but suggests that the overlying till/underlying sand and gravel relationship has been overestimated, and that there is
considerably greater variability in both the types of materials, and lithostratigraphic controls in different physiographic regions than has previously been identified.
Where sufficient data coverage warrants, the seismic shothole drillers'
log-derived data provides a means for better regional characterization that can become integrated into environmental assessments and infrastructure engineering design and construction particularly in consideration of susceptibility to potential
|Summary||(Plain Language Summary, not published)|
Subsurface massive ice deposits are a significant hazard in northern Canada for all infrastructures (e.g., roads, pipelines), coastal erosion, and are of
key concern to environmental assessments and engineering design. A new, vast source of geoscience information (seismic shothole drillers' logs) collected from Industry archives provides orders of magnitude more information on the location, thickness
and controls of massive ice formation. This new data has already been integrated into the design and regulatory approval of the Inuvik to Tuktoyaktuk highway, and provides significant opportunities for predicting where massive ice deposits may occur.
It can also be used to assess relative sensitivity and hazard potential of different areas to proposed climatic change. The research presented highlights major discoveries and offers insights for identifying areas where detailed field-based research
could be focussed, and where new data contradicts or supports previous reconstructions.