Title | Reconnaissance surficial geology, Hardisty Lake, Northwest Territories, NTS 86-C |
Download | Downloads |
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Licence | Please note the adoption of the Open Government Licence - Canada
supersedes any previous licences. |
Author | Kerr, D E; O'Neill, H B |
Source | Geological Survey of Canada, Canadian Geoscience Map 337, 2018, 1 sheet, https://doi.org/10.4095/306290 Open Access |
Links | Surficial geology map collection
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Links | Collection de données de géologie de surface
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Image |  |
Year | 2018 |
Publisher | Natural Resources Canada |
Edition | prelim. |
Document | serial |
Lang. | English |
Maps | 1 map |
Map Info. | surficial geology, sediments, landforms, features, 1:125,000 |
Projection | Universal Transverse Mercator Projection, UTM zone 11 (NAD83) |
Media | on-line; digital |
Related | NRCan photo(s) in this
publication |
File format | readme
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File format | pdf (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) |
Province | Northwest Territories |
NTS | 86C |
Area | Hardisty Lake; Rae Lake; Faber Lake; Ingray Lake |
Lat/Long WENS | -118.0000 -116.0000 65.0000 64.0000 |
Subjects | surficial geology/geomorphology; postglacial deposits; organic deposits; peat; bogs; eolian deposits; dunes; dunes, parabolic; colluvial deposits; talus slopes; alluvial deposits; flood plains;
terraces; lacustrine deposits; deltaic sediments; glacial deposits; glacial landforms; glacial features; glaciolacustrine deposits; glacial lakes; beach deposits; glaciofluvial deposits; outwash plains; outwash fans; ice contact deposits; kettles;
eskers; hummocks; tills; moraines; moraine, end; till ridges; crag and tail; drumlinoids; glacial scours; till plains; glacial flutings; glacial striations; ice flow; ice movement directions; meltwater channels; flow trajectories; kames; roches
moutonnees; raised beaches; isostatic rebound; shoreline changes; submergence; emergence; scarps; escarpments; sands; gravels; silts; boulders; clays; glacial history; glaciation; Wisconsinian glacial stage; deglaciation; erosion; permafrost;
periglacial features; thermokarst; frost heaving; ice wedges; patterned ground; ground ice; depositional environment; sedimentary structures; bedrock geology; lithology; Glacial Lake McConnell; Late Wisconsin Maximum; Rebesca Moraine; Laurentide Ice
Sheet; icings; snowpacks; Phanerozoic; Cenozoic; Quaternary |
Illustrations | location maps; index maps; photographs |
Program | GEM2: Geo-mapping for Energy and Minerals Mackenzie Corridor, North Bear Surficial Mapping |
Released | 2018 01 11 |
Abstract | The glaciated landscape of the Hardisty Lake region of the Northwest Territories exhibits striations and large ice-flow features such as drumlinoids, crag-and-tail features, and fluted bedrock that
record westward to southwestward ice flow during the last glaciation. Glacially scoured bedrock, with till-veneer patches in depressions, dominates much of the map area, but extensive till deposits occur in the more elevated regions of the southwest.
Glaciofluvial landforms, including eskers, kames, and outwash plains, are part of poorly defined meltwater corridors, and generally trend southwestward. During deglaciation of the map-sheet area, which began about 10.5 ka BP, a discontinuous line of
recessional moraines was created east of Rebesca Lake. Glaciolacustrine sediments, associated with glacial Lake McConnell, were deposited in the central and western regions. Associated glaciolacustrine deltas and beaches occur between 210 m and 310 m
elevation, but washing limits are found as high as 340 m locally on the eastern flanks of the till highlands. |
Summary | (Plain Language Summary, not published) The Hardisty Lake map (NTS 86-C) identifies surficial materials and associated landforms left by the retreat of the last glaciers. The surficial geology
is based on aerial photograph interpretation, with striations from previous publications. This work provides new geological knowledge and improves our understanding of the distribution and nature of the surficial geology cover, and the glacial
history of this region. It contributes to resource assessments and effective land use management. |
GEOSCAN ID | 306290 |
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