An interpretation of bedrock geology, topography and other sources of information that shows the potential for karst formations. This is a reconnaissance level map for all of British Columbia

A polygon coverage showing the location of coalfields with coalbed methane (cbm) potential in BC

This layer contains polygon features that represent geological units in New Brunswick. The associated Bedrock Geology Relate Table contains details about each map unit, including: a brief legend description, Group name, Formation name, and rock age. This layer is the result of nearly 50 years of bedrock mapping and it continues to change as new interpretations are made and more data is collected through field work and analysis.

This layer contains polygon features that represent geological units in New Brunswick. The associated Bedrock Geology Relate Table contains details about each map unit, including: a brief legend description, Group name, Formation name, and rock age. This layer is the result of nearly 50 years of bedrock mapping and it continues to change as new interpretations are made and more data is collected through field work and analysis.

This layer contains polygon features that represent the generalized surficial geology of New Brunswick. Unconsolidated materials occurring over bedrock, are classified according to physical attributes and genesis, and categorized into map units. This layer is intended to be used at small scales (e.g., provincial scale). It is an update of the 2002 Generalized Surficial Geology Map of New Brunswick, the updates reflect re-interpretation of the geology based on additional field investigations.

This layer contains polygon features that represent the generalized surficial geology of New Brunswick. Unconsolidated materials occurring over bedrock, are classified according to physical attributes and genesis, and categorized into map units. This layer is intended to be used at small scales (e.g., provincial scale). It is an update of the 2002 Generalized Surficial Geology Map of New Brunswick, the updates reflect re-interpretation of the geology based on additional field investigations.

This map service provides access to the Chronology dataset shown on the GeoAtlas application. **Please Note – All published Saskatchewan Geological Survey datasets, including those available through the Saskatchewan Mining and Petroleum GeoAtlas, are sourced from the Enterprise GIS Data Warehouse. They are therefore identical and share the same refresh schedule. This dataset represents the chronology for the Province of Saskatchewan at 1:1 million scale. It is a regional distribution of bedrock categorized by age into Archean, Archean or Proterozoic, Proterozoic, Helikian, Ordovician, Silurian, Devonian, Cretaceous, and Tertiary for the province of Saskatchewan, Canada. Mapping in support of this dataset was over many years of compiling bedrock data and integrating into this product. The data was created as a file geodatabase feature class and output for public distribution.

Grouping can include up to a maximum of 750 placer claims. All placer claims must be contiguous, i.e. they must be adjoining. Any solitary placer claims that do not share at least one boundary with the placer claims to be grouped cannot be included in the grouping. 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)

Yukon Territory has been glaciated by Cordilleran and montane glaciers at various times throughout the Pleistocene, as well as by continental ice, the Laurentine Ice Sheet in the Late Pleistocene. Throughout the Late Cenozoic, each successive glaciation appears to have been less extensive than the previous one. In west-central Yukon the earliest glaciation occurred between 2.6 and 2.9 Ma. ago (Duk-Rodkin and Barendregt, 1997). This glaciation was the most extensive and formed a continuous carapace of ice covering all the mountain ranges, except for a small area of Dawson Range and a more extensive area in northern Yukon. The Mid Pleistocene Cordilleran glaciation was less extensive than older glaciations but it formed an extensive ice sheet covering most of the northern Cordillera. The Late Pleistocene glaciation was the most restrictive and formed a continuous carapace of ice from the continental divide to the Saint Elias Mountains, but only restricted ice caps formed on the Ogilvie Mountains. During the last glaciation, the Laurentide Ice Sheet, flowing from the east, reached the northeast part of the Yukon Territory ca. 30 ka ago. 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)

This data set represents the digital information on all known mineral occurrences in the Province of Saskatchewan. This data shows information on all known mineral occurrences in Saskatchewan. Additional occurrences are added as new public domain geoscience information is analyzed. The data was created as a file geodatabase feature class and output for public distribution. Current definitions for the mineral deposit categories used in the Saskatchewan Mineral Deposit Index can be found by searching “Mineral Deposit Category Definition Tables” on the Publications Saskatchewan website. To view or download more datasets from the Saskatchewan Geological Survey, please visit our GeoHub page (https://er-saskatchewan.hub.arcgis.com/pages/saskatchewan-geological-survey) or our Saskatchewan Mining and Petroleum GeoAtlas (https://gisappl.saskatchewan.ca/geoatlas). **Please Note – All published Saskatchewan Geological Survey datasets, including those available through the Saskatchewan Mining and Petroleum GeoAtlas, are sourced from the Enterprise GIS Data Warehouse.  They are therefore identical and share the same refresh schedule.