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This table provides the current expenditure forecast for each statutory authority within a department or agency, for which a financial requirement has been identified.
The Riparian Area Assessment of the North Saskatchewan and Battle River Watersheds project focused on assessing riparian habitat along lake, creek, stream and river shorelines. The majority of the shorelines of interest were located within the NSR or Battle River watersheds. however, an additional shoreline was also assessed within municipalities that partially intersect, but are not completely contained within, either the NSR or Battle River watersheds. In addition to assessing new shorelines, an important component of this project was compiling data for shorelines that had been previously assessed in central Alberta using the same assessment methodology.
This downloadable data product includes the federal boundary files from previous census years. Data included are the historical boundary files of the year indicated and should not be considered the most recent official boundaries. Layers in each geodatabase include Economic Regions, Census Divisions, Census Subdivisions, Census Metropolitan Areas and Census Agglomerations, Census Tracts, and Disseminations. Current years for the historical dataset include 1996, 2001, 2006, 2011, and 2016.
This downloadable data product includes the federal boundary files from the most recent census year. The official boundaries are updated every 5 years with the census and should be considered the most recent official boundaries. Layers in each geodatabase include Economic Regions, Census Divisions, Census Subdivisions, Census Metropolitan Areas and Census Agglomerations, Census Tracts, and Dissemination Areas. The current boundaries are from the 2021 Census of population.
The mineral potential of the Northern Kluane Wildlife Sanctuary (KWS) is rated as HIGH. Within the KWS, rocks of the Wrangellia Terrane rate the highest as they include two mineral deposits with proven reserves, one past producer, favorable stratigraphy for a variety of mineral deposits with production history and proven reserves elsewhere in the Cordillera as well as over 45 mineral occurrences within the boundaries of the KWS. Ultramafic hosted Ni-Cu-PGE; Fe, Cu, Au skarn, replacement or basaltic copper, VMS and polymetallic vein deposits are hosted in this belt of extremely high mineral potential. Pennsylvanian and post-accretionnary Cretaceous and Tertiary plutons are also of high potential for a variety of mineral deposit types including porphyry copper, epithermal gold and silver, skarns and polymetallic veins.