In November 2005, participants at the Workshop on Geological Storage of CO2 at Princeton University agreed on the need for a common test problem to assess various models to simulate the fate of CO2 injected into the subsurface. Alberta Geological Survey offered to make available the data for the Wabamun Lake area in Alberta, Canada, which were assembled to develop a comprehensive model for studying CO2 geological storage. The Wabamun Lake area, southwest of Edmonton in central Alberta, was selected as the test area because a variety of favourable conditions identified it as a potential site for future, large-scale CO2 injection. Several large, industrial CO2 point sources are in the area, resulting in short transportation distances of the captured gas. Various deep saline formations with sufficient capacity to accept and store large volumes of CO2 in supercritical phase exist at the appropriate depth and are overlain by thick confining shale units. Most importantly, a wealth of data exist (i.e., stratigraphy, rock properties, mineralogy, fluid composition, formation pressure, information about well completions, etc.), collected by the petroleum industry and submitted to the Alberta Energy and Utilities Board. For these reasons, the Wabamun Lake area is an ideal location to characterize a CO2 storage site and analyze the potential risks.

In November 2005, participants at the Workshop on Geological Storage of CO2 at Princeton University agreed on the need for a common test problem to assess various models to simulate the fate of CO2 injected into the subsurface. Alberta Geological Survey offered to make available the data for the Wabamun Lake area in Alberta, Canada, which were assembled to develop a comprehensive model for studying CO2 geological storage. The Wabamun Lake area, southwest of Edmonton in central Alberta, was selected as the test area because a variety of favourable conditions identified it as a potential site for future, large-scale CO2 injection. Several large, industrial CO2 point sources are in the area, resulting in short transportation distances of the captured gas. Various deep saline formations with sufficient capacity to accept and store large volumes of CO2 in supercritical phase exist at the appropriate depth and are overlain by thick confining shale units. Most importantly, a wealth of data exist (i.e., stratigraphy, rock properties, mineralogy, fluid composition, formation pressure, information about well completions, etc.), collected by the petroleum industry and submitted to the Alberta Energy and Utilities Board. For these reasons, the Wabamun Lake area is an ideal location to characterize a CO2 storage site and analyze the potential risks.

In November 2005, participants at the Workshop on Geological Storage of CO2 at Princeton University agreed on the need for a common test problem to assess various models to simulate the fate of CO2 injected into the subsurface. Alberta Geological Survey offered to make available the data for the Wabamun Lake area in Alberta, Canada, which were assembled to develop a comprehensive model for studying CO2 geological storage. The Wabamun Lake area, southwest of Edmonton in central Alberta, was selected as the test area because a variety of favourable conditions identified it as a potential site for future, large-scale CO2 injection. Several large, industrial CO2 point sources are in the area, resulting in short transportation distances of the captured gas. Various deep saline formations with sufficient capacity to accept and store large volumes of CO2 in supercritical phase exist at the appropriate depth and are overlain by thick confining shale units. Most importantly, a wealth of data exist (i.e., stratigraphy, rock properties, mineralogy, fluid composition, formation pressure, information about well completions, etc.), collected by the petroleum industry and submitted to the Alberta Energy and Utilities Board. For these reasons, the Wabamun Lake area is an ideal location to characterize a CO2 storage site and analyze the potential risks.

In November 2005, participants at the Workshop on Geological Storage of CO2 at Princeton University agreed on the need for a common test problem to assess various models to simulate the fate of CO2 injected into the subsurface. Alberta Geological Survey offered to make available the data for the Wabamun Lake area in Alberta, Canada, which were assembled to develop a comprehensive model for studying CO2 geological storage. The Wabamun Lake area, southwest of Edmonton in central Alberta, was selected as the test area because a variety of favourable conditions identified it as a potential site for future, large-scale CO2 injection. Several large, industrial CO2 point sources are in the area, resulting in short transportation distances of the captured gas. Various deep saline formations with sufficient capacity to accept and store large volumes of CO2 in supercritical phase exist at the appropriate depth and are overlain by thick confining shale units. Most importantly, a wealth of data exist (i.e., stratigraphy, rock properties, mineralogy, fluid composition, formation pressure, information about well completions, etc.), collected by the petroleum industry and submitted to the Alberta Energy and Utilities Board. For these reasons, the Wabamun Lake area is an ideal location to characterize a CO2 storage site and analyze the potential risks.

In November 2005, participants at the Workshop on Geological Storage of CO2 at Princeton University agreed on the need for a common test problem to assess various models to simulate the fate of CO2 injected into the subsurface. Alberta Geological Survey offered to make available the data for the Wabamun Lake area in Alberta, Canada, which were assembled to develop a comprehensive model for studying CO2 geological storage. The Wabamun Lake area, southwest of Edmonton in central Alberta, was selected as the test area because a variety of favourable conditions identified it as a potential site for future, large-scale CO2 injection. Several large, industrial CO2 point sources are in the area, resulting in short transportation distances of the captured gas. Various deep saline formations with sufficient capacity to accept and store large volumes of CO2 in supercritical phase exist at the appropriate depth and are overlain by thick confining shale units. Most importantly, a wealth of data exist (i.e., stratigraphy, rock properties, mineralogy, fluid composition, formation pressure, information about well completions, etc.), collected by the petroleum industry and submitted to the Alberta Energy and Utilities Board. For these reasons, the Wabamun Lake area is an ideal location to characterize a CO2 storage site and analyze the potential risks.

This GIS dataset depicts the structural bedrock top surface in the Edmonton-Calgary Corridor based on water-well litholog data, including bedrock outcrop locations. We sourced the well data from an internal Edmonton-Calgary Corridor geological mapping database. This surface provides a geological model for the region. These data comprise the raster surface of Alberta Geological Survey Map 549, Bedrock Topography of the Edmonton-Calgary Corridor, Alberta.

This GIS dataset depicts the result of a geostatistical model of the bedrock topography in Alberta. This model is based on water-well litholog data, stratigraphic picks made on oil and gas petrophysical logs, data derived from digitized contour interpretations on bedrock topography maps, including bedrock outcrop locations and the 60 m grid-spaced Shuttle Rader Topography Mission digital elevation model. These data comprise the raster surface of Alberta Geological Survey Map 550, Bedrock Topography of Alberta, Canada.

The bedrock topography of Alberta is the surface of the top of Upper Cretaceous and Paleogene bedrock, and reveals geomorphic features created by Paleogene to Recent river systems and Quaternary glaciation. This grid is a computer-generated geostatistical model of the bedrock topography of Alberta using previously published information from Alberta Geological Survey (AGS) maps and reports, as well as new data. The quality of this data has been assessed and then a quality-weighting approach was applied to the dataset prior to interpolation. The surface was modelled using a 500m x 500m grid cell spacing, and as such should not be used for local scale studies. This grid represents the surface portrayed in AGS Map 602, Bedrock Topography of Alberta, and this grid will continue to be updated as part of the Alberta Geological Framework project. Explanatory notes, references, and data sources appear on a supplementary page to accompany Map 602. These notes describe the distribution of physiographic terrain elements of the bedrock surface across Alberta, and the data sources and geostatistical methods used to interpolate this surface.

The bedrock topography of Alberta is the surface of the top of Upper Cretaceous and Paleogene bedrock, and reveals geomorphic features created by Paleogene to Recent river systems and Quaternary glaciation. This dataset consists of previously published information from Alberta Geological Survey (AGS) maps and reports, as well as new data for which the quality has been assessed in order to apply a quality-weighting approach prior to modelling the bedrock topography surface. It is the data used to produce AGS Map 602, Bedrock Topography of Alberta. Explanatory notes, references, and data sources appear on a supplementary page to accompany Map 602. These notes describe the distribution of physiographic terrain elements of the bedrock surface across Alberta, and the sources and quality of the data that were used to interpolate this surface.