Drift Thickness of Pelican River Area, Alberta (NTS 83P) (GIS data, line features)

Drift Thickness of Pelican River Area, Alberta (NTS 83P) (GIS data, line features) The drift thickness map of the Pelican River area (NTS 83P) shows the variation in thickness of unconsolidated sediment lying between the bedrock surface and the present-day land surface, and complements the regional drift thickness map of Alberta (Pawlowicz and Fenton, 1995). The thickness of the drift varies from less than 20 metres in uplands, such as the Pelican Mountains, to a little over 260 metres in the Wiau Valley in the northeast part of the map area. The thickest drift fills the paleovalleys containing the major valleys: the Wiau Valley and the Leismer Valley in the northeast, and the north-trending Amesbury Valley in the central portion of the area. 2022-04-13 Government of Alberta AGS-Info@aer.ca Form DescriptorsNature and EnvironmentScience and Technology83palbertabedrock topographyburied valleyscanadadrift thicknessgeoscientificinformationgis datapelican riverthalwegsGovernment information Drift Thickness of Pelican River Area, Alberta (NTS 83P) (GIS data, line features) - (HTML)HTML https://geodiscover.alberta.ca/geoportal/rest/metadata/item/2b0e9bbfdf7f4776b826f9677dfd623b/html Drift Thickness of Pelican River Area, Alberta (NTS 83P) (GIS data, line features) - (SHP)SHP https://static.ags.aer.ca/files/document/DIG/DIG_2004_0049.zip Drift Thickness of Pelican River Area, Alberta (NTS 83P) (GIS data, line features) - (XML)XML https://geodiscover.alberta.ca/geoportal/rest/metadata/item/2b0e9bbfdf7f4776b826f9677dfd623b/xml Alberta GeoportalHTML https://open.alberta.ca/opendata/2fd3f5ec-65de-4cd5-bcf1-21e59ef4033b

The drift thickness map of the Pelican River area (NTS 83P) shows the variation in thickness of unconsolidated sediment lying between the bedrock surface and the present-day land surface, and complements the regional drift thickness map of Alberta (Pawlowicz and Fenton, 1995). The thickness of the drift varies from less than 20 metres in uplands, such as the Pelican Mountains, to a little over 260 metres in the Wiau Valley in the northeast part of the map area. The thickest drift fills the paleovalleys containing the major valleys: the Wiau Valley and the Leismer Valley in the northeast, and the north-trending Amesbury Valley in the central portion of the area.

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