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TitleSurficial geology, Arrowsmith River south, Nunavut, NTS 56-O south
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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 397, 2023, 1 sheet, https://doi.org/10.4095/314543 Open Access logo Open Access
LinksSurficial geology map collection
LinksCollection de données de géologie de surface
Image
Year2023
Alt SeriesCanada-Nunavut Geoscience Office Open File Map 2023-01
PublisherNatural Resources Canada
PublisherCanada-Nunavut Geoscience Office
Editionsurficial data model v.2.3.14 conversion
Documentserial
Lang.English
Maps1 map
Map Info.surficial geology, sediments, landforms, features, 1:100,000
ProjectionUniversal Transverse Mercator Projection, UTM zone 15 (NAD83)
Mediaon-line; digital
RelatedThis publication is related to the following publications
File formatreadme
File formatpdf (Adobe® Reader®); rtf; gdb (ESRI® ArcGIS(TM) v.10.x); shp (ESRI® ArcGIS(TM) v.10.x); xml (ESRI® ArcGIS(TM) v.10.x); mxd (ESRI® ArcGIS(TM) v.10.x); tiff; pdf
ProvinceNunavut
NTS56O/01; 56O/02; 56O/03; 56O/04; 56O/05; 56O/06; 56O/07; 56O/08
AreaArrowsmith River
Lat/Long WENS -92.0000 -90.0000 67.5000 67.0000
Subjectssurficial geology/geomorphology; postglacial deposits; colluvial deposits; landslide deposits; debris flow deposits; glacial deposits; glacial features; glacial landforms; tills; till plains; glacial erosion; meltwater channels; paleocurrents; moraines; eskers; drumlinoids; glacial flutings; crag and tail; kames; glacial striations; ice flow; glacial grooves; drumlins; roches moutonnees; glacial lakes; sands; silts; gravels; clays; boulders; felsenmeer; permafrost; ground ice; periglacial features; frost action; frost heaving; solifluction; glacial history; glaciation; Wisconsinian glacial stage; deglaciation; shoreline changes; depositional environment; sedimentary structures; Laurentide Till; colluvial and mass-wasting veneer; colluvial and mass-wasting blanket; alluvial sediments; alluvial floodplain sediments; alluvial terraced sediments; glaciolacustrine sediments; glaciolacustrine deltaic sediments; glaciolacustrine blanket; glaciofluvial sediments; glaciofluvial outwash plain sediments; glaciofluvial terraced sediments; glaciofluvial hummocky sediments; glaciofluvial veneer; hummocky tills; till veneer; till blanket; moraine ridges; ice-flow directions; geological contacts; beach crests; drumlinoid ridges; Avalanches; Phanerozoic; Cenozoic; Quaternary
Illustrationslocation maps; index maps
ProgramGEM2: Geo-mapping for Energy and Minerals Geological Map Flow
Released2023 01 18
AbstractThis new surficial geology map product represents the conversion of Open File 4281 (Ozyer, 2004) 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 Open File 4281 that conformed to the SDM were maintained during the conversion process. Additional material such as marginal notes which may exist on the original map, are not included here. Supplementary, limited legacy information was added to complement the converted geoscience data. This consists of glacial striations and roches moutonnées from McMartin et al. (2003). It is identified in the accompanying geodatabase. 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 which 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 aerial photograph interpretation, fieldwork and limited legacy 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 ID314543

 
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