GEOSCAN Search Results: Fastlink

GEOSCAN Menu


TitlePreliminary modelling of ground ice abundance in the Slave Geological Province, Northwest Territories and Nunavut
DownloadDownloads
 
LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorO'Neill, H BORCID logo; Wolfe, S AORCID logo; Duchesne, CORCID logo
SourceGeological Survey of Canada, Scientific Presentation 135, 2022, 1 sheet, https://doi.org/10.4095/329815 Open Access logo Open Access
Image
Year2022
PublisherNatural Resources Canada
MeetingArcticNet Annual Scientific Meeting 2021; December 6-10, 2021
Documentserial
Lang.English
Mediadigital; on-line
RelatedThis publication is related to the following publications
File formatpdf
ProvinceNorthwest Territories; Nunavut
NTS75L; 75M; 76D; 76E; 76L; 76M; 85I; 85J; 85O; 85P; 86A; 86B; 86G; 86H; 86I; 86J; 86O; 86P
AreaYellowknife; Grays Bay
Lat/Long WENS-116.0000 -110.0000 68.0000 62.0000
Subjectssurficial geology/geomorphology; environmental geology; Science and Technology; Nature and Environment; modelling; permafrost; ground ice; periglacial features; sediments; marine sediments; glacial deposits; tills; bedrock geology; Slave Province; Methodology; Infrastructures; Planning; Management; alluvial sediments; glaciofluvial sediments; glaciolacustrine sediments; lacustrine sediments
Illustrationsgeoscientific sketch maps; bar graphs
ProgramGEM-GeoNorth: Geo-mapping for Energy and Minerals GEM Program Coordination
Released2022 03 23
AbstractNew infrastructure corridors within the Slave Geological Province could provide transportation, electric, and communications links to mineral-rich areas of northern Canada, and connect southern highway systems and Arctic shipping routes. Relatively little information on permafrost and ground ice is available compared to other regions, particularly in the north of the corridor. Improved knowledge of permafrost and ground ice conditions is required to inform planning and management of infrastructure. Work within the Geological Survey of Canada's (GSC) GEM-GeoNorth program includes mapping periglacial terrain features, synthesizing existing permafrost and surficial data, and modelling ground ice conditions along the Yellowknife-Grays Bay corridor. Here we present initial modelling of ground ice abundance in the region using a methodology developed for the national scale Ground ice map of Canada (GIMC), and higher resolution surficial geology mapping. The results highlight the increased estimated abundance of potentially ice-rich deposits compared to the GIMC when using more detailed surficial geology as model inputs.
Summary(Plain Language Summary, not published)
New infrastructure corridors within the Slave Geological Province could provide transportation, electric, and communications links to mineral-rich areas of northern Canada, and connect southern highway systems and Arctic shipping routes. Relatively little information on permafrost and ground ice is available compared to other regions, particularly in the north of the corridor. Here we present initial modelling of ground ice abundance in the region using a methodology developed for the national scale Ground ice map of Canada (GIMC), and higher resolution surficial geology mapping. The results highlight the increased estimated abundance of potentially ice-rich deposits compared to the GIMC when using more detailed surficial geology as model inputs.
GEOSCAN ID329815

 
Date modified: