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TitleSurficial geology, Cape Weynton, Nunavut, NTS 56-P/9, 10
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 394, 2022, 1 sheet, Open Access logo Open Access
LinksSurficial geology map collection
LinksCollection de données de géologie de surface
Alt SeriesCanada-Nunavut Geoscience Office Open File Map 2022-02
PublisherNatural Resources Canada
PublisherCanada-Nunavut Geoscience Office
Editionsurficial data model v.2.3.14 conversion
Maps1 map
Map Info.surficial geology, sediments, landforms, features, 1:50,000
ProjectionUniversal Transverse Mercator Projection, UTM zone 16 (NAD83)
Mediadigital; on-line
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); pdf
NTS56P/09; 56P/10
AreaCape Weynton
Lat/Long WENS -89.0000 -88.0000 67.7500 67.5000
Subjectssurficial geology/geomorphology; landslide deposits; debris flow deposits; fans; marine sediments; glacial deposits; glacial landforms; glacial features; tills; till ridges; till plains; moraines; drumlinoids; crag and tail; glacial flutings; glacial striations; ice flow; eskers; kames; meltwater channels; paleocurrents; clays; silts; sands; gravels; boulders; periglacial features; frost heaving; solifluction; felsenmeer; landforms; scarps; escarpments; depositional environment; sedimentary structures; glacial history; glaciation; Wisconsinian glacial stage; deglaciation; shoreline changes; colluvial and mass-wasting deposits; colluvial and mass-wasting veneer; colluvial and mass-wasting blanket; Avalanches; alluvial floodplain sediments; alluvial terraced sediments; lacustrine sediments; lacustrine deltaic sediments; lacustrine blanket; marine beach sediments; marine deltaic sediments; marine intertidal sediments; marine nearshore sediments; marine offshore sediments; marine blanket; glaciomarine sediments; glaciomarine deltaic sediments; glaciolacustrine sediments; glaciolacustrine deltaic sediments; glaciolacustrine blanket; glaciofluvial sediments; glaciofluvial outwash plain sediments; glaciofluvial terraced sediments; glaciofluvial hummocky sediments; glaciofluvial veneer; glaciofluvial blanket; hummocky tills; till veneer; till blanket; geological contacts; terrace scarps; ice-contact scarps; beach crests; moraine ridges; ice-flow directions; dated sample locations; sample locations; Phanerozoic; Cenozoic; Quaternary
Illustrationslocation maps; index maps; tables
ProgramGEM2: Geo-mapping for Energy and Minerals Geological Map Flow
Released2022 12 13
AbstractThis new surficial geology map product represents the conversion of Open File 5016, map 1 (Little, 2006) and its legend only, 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 5016, map 1 that conformed to the SDM were maintained during the conversion process. Supplementary legacy information (descriptive notes) on the original map is not included here. Limited legacy information was added to complement the converted geoscience data. This consists of striations (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 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 aerial photograph 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.

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