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TitleSurficial geology, Avalikuarjuk River, Nunavut, NTS 56-P/13 and 14
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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 413, 2022, 1 sheet, https://doi.org/10.4095/315017 Open Access logo Open Access
LinksSurficial geology map collection
LinksCollection de données de géologie de surface
Image
Year2022
Alt SeriesCanada-Nunavut Geoscience Office Open File Map 2022-04
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, 1:50,000
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
ProvinceNunavut
NTS56P/13; 56P/14
AreaAvalikuarjuk River
Lat/Long WENS -90.0000 -89.0000 68.0000 67.7500
Subjectssurficial geology/geomorphology; geochronology; Nature and Environment; Science and Technology; postglacial deposits; organic deposits; alluvial fans; landslide deposits; debris flows; debris fans; marine sediments; glacial deposits; glacial landforms; glacial features; tills; moraines; eskers; meltwater channels; paleocurrents; glacial striations; ice flow; kames; kettles; silts; sands; gravels; boulders; clays; periglacial features; felsenmeer; frost heaving; solifluction; landforms; scarps; escarpments; depositional environment; sedimentary structures; glacial history; glaciation; Wisconsinian glacial stage; deglaciation; ice retreat; ice margins; shoreline changes; deformation; radiometric dating; radiocarbon dating; alluvial sediments; alluvial floodplain sediments; alluvial terraced sediments; colluvial and mass-wasting deposits; colluvial and mass-wasting veneer; colluvial and mass-wasting blanket; Avalanches; marine deltaic sediments; marine intertidal sediments; marine nearshore sediments; marine offshore sediments; marine veneer; marine blanket; glaciomarine sediments; glaciomarine deltaic sediments; glaciofluvial sediments; glaciofluvial outwash plain sediments; glaciofluvial terraced sediments; glaciofluvial hummocky sediments; glaciofluvial veneer; glaciofluvial blanket; hummocky tills; till veneer; till blanket; moraine ridges; geological contacts; landslide escarpments; terrace scarps; beach crests; ice-contact scarps; ice-flow directions; dated sample locations; station 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 3 (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 3 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.
GEOSCAN ID315017

 
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