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TitleReconnaissance surficial geology, Deep Rose Lake, Nunavut, NTS 66-G north
LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorSt-Onge, D A; Kerr, D E
SourceGeological Survey of Canada, Canadian Geoscience Map 208, 2015, 1 sheet, Open Access logo Open Access
LinksSurficial geology map collection
LinksCollection de données de géologie de surface
PublisherNatural Resources Canada
Maps1 map
Map Info.surficial geology, glacial deposits and landforms, 1:125,000
ProjectionUniversal Transverse Mercator Projection, UTM zone 14 (NAD83)
Mediaon-line; digital
RelatedThis publication is superceded by Reconnaissance surficial geology, Deep Rose Lake, Nunavut, NTS 66-G north
RelatedThis publication is related to Surficial geology, Amer Lake, Nunavut, NTS 66-H
File formatreadme
File formatpdf; rtf; shp; xml; xls; jpg
NTS66G/09; 66G/10; 66G/11; 66G/12; 66G/13; 66G/14; 66G/15; 66G/16
AreaDeep Rose Lake; Back River; Lower Garry Lake
Lat/Long WENS-100.0000 -98.0000 66.0000 65.5000
Subjectssurficial geology/geomorphology; Nature and Environment; glacial features; glacial deposits; glacial landforms; tills; sands; gravels; glaciolacustrine deposits; glaciofluvial deposits; glaciomarine deposits; organic deposits; alluvial deposits; colluvial deposits; eolian deposits; lacustrine deposits; moraines; Cenozoic; Quaternary
ProgramClimate Change Geoscience Land-based Infrastructure
Released2015 07 21
AbstractPreliminary surficial geology studies, based on air photo interpretation and limited legacy and recent field data, were undertaken in the north half of the Deep Rose Lake map area to provide an understanding of the distribution and nature of surficial materials, and regional glacial history.
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 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.

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