Canadas Managed Forests 2020 Vector Tile Layer

Population density in Canada based on the 2006 and 2011 census data at three levels of geography: census division (CD) (1:5,000,001 and over), census sub-division (CSD) (1:5,000,000 to 1:288,897) and dissemination areas (DA) (1:288,897 and under). Population density is the number of people per square kilometer. Population density change measures the rate of change calculated by the difference in total population density values for each area between 2006 and 2011, divided by the total population density of 2006. The CD and CSD boundaries are based on 2011 data. The 2006 population figures have been adjusted accordingly. The DA boundaries are based on 2006 data. All areas with no data are indicated with a value of -999.

Polygon feature layer of Manitoba's economic regions This feature layer depicts the boundaries of economic regions in Manitoba. There are eight regions in Manitoba, defined by Statistics Canada. Fields included [Alias (Field Name): Field description] Economic Region (Economic_Region): The name of the economic region For more information, see Regional Economic Profiles on the Manitoba  government  website.FF

Bird Studies Canada WMS/WFS Server for bird distribution and abundance data, and related information. Bird Studies Canada gratefully acknowledges the support of Environment Canada - Canadian Information System for the Environment in developing this service.

The Canadian Aquatic Biomonitoring Network (CABIN) is an integrated national network for the collection, management, assessment, and distribution of bioassessment data. CABIN aims to provide long-term monitoring and assessment of aquatic ecosystem health by utilizing the Reference Condition Approach (RCA) applied to benthic macro-invertebrates. The CABIN web portal provides access to sampling protocols, on-line data entry and management, and on-line analytical, reporting and visualization tools. Participation in CABIN is encouraged at all levels of expertise; groups interested in becoming involved can contact the program coordinator through the web page (cabin.cciw.ca).

The Canadian Aquatic Biomonitoring Network (CABIN) is an integrated national network for the collection, management, assessment, and distribution of bioassessment data. CABIN aims to provide long-term monitoring and assessment of aquatic ecosystem health by utilizing the Reference Condition Approach (RCA) applied to benthic macro-invertebrates. The CABIN web portal provides access to sampling protocols, on-line data entry and management, and on-line analytical, reporting and visualization tools. Participation in CABIN is encouraged at all levels of expertise; groups interested in becoming involved can contact the program coordinator through the web page (cabin.cciw.ca).

The BORHOLES layer represents the compilation of available data from various boreholes throughout the Yukon and near the Yukon border. This data set includes oil and gas exploration wells, mineral exploration boreholes, water supply wells and environmental monitoring well. The data points include information on the borehole location, purpose, status, depth, temperature data, water flow and chemistry data where available along with references where further detailed information may be available.

This layer is part of the Geological Survey of Canada's earthquake monitoring network. There are some blank fields toward the beginning of the listing, from the time the network was being installed and hence parameters were often unknown. Also, all depths in the table are "fixed" to a depth which is an integer multiple of 5km, according to lowest obtainable residuals and known crustal structure. The number and magnitude of located events are also dependent on the time recorded, as the magnitude threshold lowered as more stations were installed. The larger, potentially damaging earthquakes, however, were likely recorded from the inception of the network as these events produce waves which reach the entire western network. Distributed from [GeoYukon](https://yukon.ca/geoyukon) by the [Government of Yukon](https://yukon.ca/maps) . Discover more digital map data and interactive maps from Yukon's digital map data collection. For more information: [geomatics.help@yukon.ca](mailto:geomatics.help@yukon.ca)

Background: More than 80% of the heat produced in the Earth's crust comes from granitoid rocks. When granitoid rocks form they naturally concentrate radioactive elements such as U, Th, and K, and the radiogenic decay of these elements is an exothermic reaction. The radioactive decay of these elements within a granitoid body may generate local heat anomalies and elevated geothermal gradient at relatively shallow crustal levels. In combination with other local rock properties (e.g, porosity, permeability, thermal conductivity), radiogenic heat has the potential to generate a geothermal resource. The decay of radioactive elements converts mass into radiation energy, which in turn gets converted to heat. While all naturally radioactive isotopes generate some heat, significant heat generation only occurs from the decay of 238 U ,235 U ,232 Th and 40 K. Therefore, potential heat production is governed by the concentrations of U ,Th and K in the rock. In igneous rocks, radiogenic heat production is dependent on the bulk chemistry of the rock and decreases from acidic (e.g. granite) through basic to ultra basic rock types. Therefore, granites with anomalously high concentrations of U ,Th and K are targets for calculating potential radiogenic heat production. Potential radiogenic heat production (A)from plutonic rocks can be calculated using this equation: A (\\u03BCW/m 3 )=10 -5 \\u1D29 (9.52c u +2.56c K +3.48c Th ) where "c" is the concentration of radioactive elements "U" and "Th" in ppm, and "K" in %; and "\\u1D29" is the rock density. Heat production constants of the natural radio-elements U, Th, K are 9.525x10 -5 , 2.561x10 -5 and 3.477x10 -9 W/kg, respectively. Data and Methods: Geochemical data from \~1760 samples of plutonic rocks from Yukon are used to calculate potential heat production. The calculated values for radiogenic heat production (A) are plotted over the mapped distribution of Paleozoic and younger plutonic rocks and major crustal faults are also shown for reference.