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TitleSurficial geology, Grinnell Peninsula, Devon Island, Nunavut, NTS 59-B, parts of 59-C, 58-G, 69-A, and 69-D
DownloadDownloads
 
LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorGeological Survey of Canada
SourceGeological Survey of Canada, Canadian Geoscience Map 426, 2023, 1 sheet, https://doi.org/10.4095/322192 Open Access logo Open Access
LinksSurficial geology map collection
LinksCollection de données de géologie de surface
Image
Year2023
PublisherNatural Resources Canada
EditionSurficial Data Model v.2.3.14 conversion
Documentserial
Lang.English
Maps1 map
Map Info.surficial geology, sediments, landforms, features, 1:250,000
ProjectionUniversal Transverse Mercator Projection, UTM zone 15 (NAD83); Universal Transverse Mercator Projection, UTM zone 15 (NAD83)
Mediaon-line; digital
RelatedThis publication is related to the following publications
File formatreadme
File formatpdf; rtf; gdb (ESRI® ArcGIS(TM) 10.x); shp (ESRI® ArcGIS(TM) 10.x); xml (ESRI® ArcGIS(TM) 10.x); mxd (ESRI® ArcGIS(TM) 10.x)
ProvinceNunavut
NTS58G/14; 58G/16; 59B; 59C/03; 59C/04; 69A/08; 69A/09; 69A/10; 69A/15; 69A/16; 69D/01
AreaDevon Island; Grinnell Peninsula
Lat/Long WENS -98.0000 -92.0000 77.3333 75.6667
Subjectssurficial geology/geomorphology; geochronology; Nature and Environment; Science and Technology; glaciers; ice; icefields; permafrost; ground ice; periglacial features; ice-wedge polygons; frost action; felsenmeer; postglacial deposits; talus; rock glaciers; landslides; debris flows; landslide deposits; alluvial fans; marine sediments; glacial deposits; glacial landforms; glacial features; glacial lakes; tills; moraines; moraine, end; moraine, lateral; meltwater channels; paleocurrents; drumlinoids; glacial flutings; sediment dispersal; glacial striations; glacial erosion; glacial scours; gravels; sands; silts; clays; muds; escarpments; glacial history; glaciation; Wisconsinian glacial stage; ice flow; ice movement directions; deglaciation; sea level changes; shoreline changes; submergence; emergence; depositional environment; radiometric dates; radiocarbon dates; Little Ice Age; colluvial and mass-wasting deposits; alluvial sediments; alluvial floodplain sediments; alluvial terraced sediments; marine beach sediments; marine deltaic sediments; glaciomarine sediments; glaciomarine offshore sediments; glaciomarine veneer; glaciolacustrine sediments; glaciolacustrine deltaic sediments; glaciolacustrine veneer; glaciofluvial sediments; glaciofluvial outwash plain sediments; glaciofluvial terraced sediments; glaciofluvial outwash fan sediments; till veneer; till blanket; geological contacts; limit of submergence, marine; limit of submergence, glaciolacustrine; spillways; dispersal trains; dispersal train margins; ice divides; bedrock scarps; station locations, ground observation; dated sample locations; Phanerozoic; Cenozoic; Quaternary
Illustrationslocation maps; index maps; tables
ProgramGEM2: Geo-mapping for Energy and Minerals Information Management
Released2023 03 03
AbstractThis new surficial geology map product represents the conversion of Map 1973A (Dyke, 2001) and its legend, using the Geological Survey of Canada's Surficial Data Model (SDM version 2.3.14, Deblonde et al., 2018). All geoscience knowledge and information from Map 1973A that conformed to the SDM were maintained during the conversion process. The purpose of converting legacy map data to a common science language and common legend is to enable and facilitate the efficient digital compilation, interpretation, management, and dissemination of geological map information in a structured and consistent manner. This provides an effective knowledge-management tool designed around a geodatabase that can expand, following the type of information to appear on new surficial geology maps.
Summary(Plain Language Summary, not published)
The map identifies surficial materials and associated landforms left by the retreat of the last glaciers. The surficial geology is based on air photo interpretation and fieldwork. This work provides new geological knowledge and improves our understanding of the distribution, nature and glacial history of surficial materials. It contributes to resource assessments and effective land use management.
GEOSCAN ID322192

 
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