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Fenwick Creek (105D/3) and Alligator Lake (105D/6) map areas, located southwest of Whitehorse, Yukon, were mapped at 1:50 000 scale during the 1987 field season. The map areas are within the Teslin Plateau and the Boundary Ranges physiographic regions. Cretaceous Coast Plutonic Complex and Upper Triassic volcanic and sedimentary rocks of the Whitehorse Trough are separated by the 40 km long 140 degree trending "Tally-Ho Shear Zone." East of the shear zone, limestone containing late Upper Trassic conodonts is interbedded with volcanics previously mapped as Mesozoic volcanics, and now considered part of the Lewes River Group.

Over the past five decades, many lakes, ponds, and wetlands (generically termed basins) of the Peace Sector of the Peace-Athabasca Delta (PAD), a significant component of the Wood Buffalo National Park (WBNP), have experienced drying trends in-between infrequent flooding generated by major spring ice jams that form in the lower Peace River. As a result of the 2017 UNESCO Monitoring Mission report, numerous remedial recommendations were made in the Wood Buffalo National Park (WBNP) Action Plan that has been prepared by Parks Canada in conjunction with various stakeholders, e.g. first nations, industry, provincial and territorial governments, federal departments. One of these recommendations is to develop a protocol for spring flow releases from the Peace Canyon Dam (or Site-C Dam in the future), which can enhance anticipated ice-jam flooding of the PAD.

Percentage of enterprises for which specific long-term strategies were the most important, by North American Industry Classification System (NAICS) code and enterprise size, over the next five years. The most important long-term strategies include main focus on good or service positioning, main focus on low-price and cost leadership, and good or service positioning and low-price and cost leadership are equally important.

This data provides the integrated cadastral framework for the specified Canada Land. The cadastral framework consists of active and superseded cadastral parcel, roads, easements, administrative areas, active lines, points and annotations. The cadastral lines form the boundaries of the parcels. COGO attributes are associated to the lines and depict the adjusted framework of the cadastral fabric.

This data provides the integrated cadastral framework for the specified Canada Land. The cadastral framework consists of active and superseded cadastral parcel, roads, easements, administrative areas, active lines, points and annotations. The cadastral lines form the boundaries of the parcels. COGO attributes are associated to the lines and depict the adjusted framework of the cadastral fabric.

Data on place of work status by industry sectors (2-digit code) from the North American Industry Classification System (NAICS) 2017, work activity during the reference year, age and gender for Canada, provinces and territories, census divisions and census subdivisions.

Monthly operating and financial statistics (number of thousands of: passengers, passenger-kilometres, available seat-kilometres, load factor, hours flown, turbo fuel consumed in litres, and total operating revenues) for major Canadian airlines.

Map of harbours critical to fishing and aquaculture industries managed by harbour authorities (Core fishing harbours), harbours that support fishing and aquaculture industries that aren’t managed by harbour authorities (Non-core fishing harbours), and harbours that support the recreational community (Recreational harbours).

Borehole geophysical log number QC-SE-MS-12006. Located in Selbaie, QC.

The Geological Survey of Canada owns and operates slim hole geophysical sondes and recording equipment for use in PVC cased boreholes in unconsolidated overburden. Such holes are commonly drilled and cased for overburden stratigraphic or geotechnical studies related to on-going GSC projects. These boreholes have been located in various parts of Canada and in a variety of differing material types, including glacial, fluvial and lacustrine deposits. Most (but not all) sediments are of Quaternary age.