| Title | Surficial geology, Conn Lake (southwest), Baffin Island, Nunavut |
| Download | Downloads |
| Author | Utting, D J; Little, E C; Kerr, D E |
| Source | Geological Survey of Canada, Canadian Geoscience Map 36, 2013, 1 sheet, https://doi.org/10.4095/292365 (Open Access) |
| Image |  |
| Year | 2013 |
| Publisher | Natural Resources Canada |
| Edition | prelim. |
| Document | serial |
| Lang. | English |
| Maps | 1 map |
| Map Info. | surficial geology, glacial deposits and landforms, 1:100,000 |
| Projection | Universal Transverse Mercator Projection, UTM zone 18 (NAD83) |
| Media | on-line; digital |
| Related | This publication is superceded by Utting, D J; Little, E C;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 format | readme
|
| File format | pdf; rtf; shp; xml; xls; jpg; JPEG2000 |
| Province | Nunavut |
| NTS | 67E/03; 67E/04; 67E/05; 67E/06 |
| Area | Conn Lake |
| Lat/Long WENS | -76.0000 -74.0000 70.5000 70.0000 |
| Subjects | surficial geology/geomorphology; glacial features; glacial deposits; glacial landforms; tills; sands; gravels; colluvial deposits; alluvial deposits; lacustrine deposits; glaciolacustrine deposits;
glaciofluvial deposits; Cenozoic; Quaternary |
| Program | GEM Tri-Territorial Information management & databases (Tri-Territorial Surficial Framework), GEM: Geo-mapping for Energy and Minerals |
| Released | 2013 03 26 |
| Abstract | The 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 ID | 292365 |
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