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TitleSurficial geology, Conn Lake (southwest), Baffin Island, Nunavut
DownloadDownloads
AuthorUtting, D J; Little, E C; Kerr, D E
SourceGeological Survey of Canada, Canadian Geoscience Map 36, 2013, 1 sheet, https://doi.org/10.4095/292365
Year2013
PublisherNatural Resources Canada
Editionprelim.
Documentserial
Lang.English
Maps1 map
Map Info.surficial geology, glacial deposits and landforms, 1:100,000
ProjectionUniversal Transverse Mercator Projection, zone 18 (NAD83)
Mediaon-line; digital
RelatedThis publication is superceded by Utting, D J; Little, E C; Kerr, D E; (2015). Surficial geology, Conn Lake (southwest), Baffin Island, Nunavut, NTS 37-E/3, NTS 37-E/4, NTS 37-E/5, and NTS 37-E/6, Geological Survey of Canada, Canadian Geoscience Map no. 36, ed. 2, Prelim.
File formatreadme
File formatpdf; rtf; shp; xml; xls; jpg; JPEG2000
ProvinceNunavut
NTS67E/03; 67E/04; 67E/05; 67E/06
AreaConn Lake
Lat/Long WENS-76.0000 -74.0000 70.5000 70.0000
Subjectssurficial geology/geomorphology; glacial features; glacial deposits; glacial landforms; tills; sands; gravels; colluvial deposits; alluvial deposits; lacustrine deposits; glaciolacustrine deposits; glaciofluvial deposits; Cenozoic; Quaternary
ProgramGEM Tri-Territorial Information management & databases (Tri-Territorial Surficial Framework), GEM: Geo-mapping for Energy and Minerals
Image
Released2013 03 26
AbstractThe southwest part of the Conn Lake map sheet lies within the Baffin Uplands Physiographic Region, where bedrock is extensively covered by thick glacial deposits. Some areas exhibiting scour were eroded by active, warm-based ice for longer periods of time than regions of cold-based ice. A northeastward early Holocene flow is associated with ice in Foxe Basin to the northeast. Four phases of ice flow were recognized. The Last Glacial maximum relates to phase 1, northeastward, when the region was covered by actively eroding warm-based ice. The second is a north-northeastward flow during the early stages of the Barnes Ice Cap. The next two phases (a later readvance, phase 3, and continued deglaciation, phase 4) are thought to relate to the proto-Barnes Ice Cap.
GEOSCAN ID292365