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TitleSurficial geology, Broughton Island-Padloping Island, Baffin Island, Nunavut, NTS 16-M, NTS 16-N, and parts of NTS 26-P
AuthorDyke, A S
SourceGeological Survey of Canada, Canadian Geoscience Map 23, 2013, 1 sheet, (Open Access)
PublisherNatural Resources Canada
Maps1 map
Map Info.surficial geology, glacial deposits and landforms, 1:100,000
ProjectionUniversal Transverse Mercator Projection, UTM zone 20 (NAD83)
Mediapaper; on-line; digital
File formatreadme
File formatpdf; rtf; xml; shp; JPEG2000; xls
NTS16M/01; 16M/02; 16M/03; 16M/04; 16M/05; 16M/06; 16M/12; 16N/04; 26P/01; 26P/08; 26P/09
AreaBroughton Island; Padloping Island; Baffin Island
Lat/Long WENS-64.0833 -61.9167 67.6667 67.0000
Subjectssurficial geology/geomorphology; glacial features; glacial deposits; glacial landforms; glaciofluvial deposits; glaciolacustrine deposits; fluvial deposits; marine deposits; tills; moraines; Cenozoic; Quaternary
ProgramMultiple Metals - Cumberland Peninsula (Baffin Island, Nunavut), GEM: Geo-mapping for Energy and Minerals
Released2013 11 08
AbstractIn 2009, as part of the GEM program of the Geological Survey of Canada, Cumberland Peninsula east and southeast of the National Park was mapped. Mapping included several aspects of the regional Precambrian geology, as well as the Quaternary geology. Regional till was sampled for sedimentological and geochemical purposes, and moraines and other deposits were sampled for cosmogenic exposure dating. The eastern part of the peninsula is today an area of intensive alpine glaciation and evidently has experienced this style of glaciation throughout the Quaternary. During the last glacial maximum (28-12ka), alpine glaciers thickened to form regional ice divides over the mountains. Ice flow from these divides covered most, possibly all, of the region and supplied ice streams along several fiords. This local ice coalesced with the Laurentide Ice Sheet in Cumberland Sound. Despite possibly repeated glaciation, substantial areas show little or no sign of glacial erosion and retain Tertiary surfaces mantled with block fields and tors.
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 fieldwork. This work provides new geological knowledge and improves our understanding of the distribution, nature and glacial history of surficial materials.