Natural Resources CanadaGovernment of Canada
 
 Français ÿ  Contact us ÿ  Help ÿ  Search ÿ  Canada site
 ESS Home ÿ  Priorities ÿ  Products &
 services
ÿ  About the
 Sector
ÿ  Site map
Satellite image of Canada
Natural Resources Canada
Geoscape Canada
.Home
Northern Saskatchewan
.Home
.If rocks could talk...
.Athabasca sedimentary basin
.The ice age
.Meteorite impact
.Jobs in mining
.Hidden treasures
.How we use our land
.Waterways of the canadian shield
.How long is time?
.Want to know more?
.Credits & citation
.How to obtain the poster
Related links
.Geoscape Southern Saskatchewan


Proactive disclosure


Print version Print versionÿ
ÿGeoscape Canada
Natural Resources Canada > Earth Sciences Sector > Priorities > Geoscape Canada > Northern Saskatchewan
Geoscape Northern Saskatchewan
Geoscience for our Canadian Shield Community
Athabasca sedimentary basin: source of clean electric power for the world
Previous (If rocks could talk...)Index (Geoscape Northern SaskatchewanGeoscience for our Canadian Shield Community)Next (The ice age: shaping our landscape)

Further on in the Precambrian shield story...
Further on in the Precambrian shield story...
larger image
[JPEG, 337.4 kb, 1000 X 579, notice]

Thin layers in rocks, formed in sand carried by rivers, slope downstream (to left), and indicate the direction in which ancient rivers flowed. (Courtesy of  Saskatchewan Industry and Resources)
Thin layers in rocks, formed in sand carried by rivers, slope downstream (to left), and indicate the direction in which ancient rivers flowed.
(Courtesy of Saskatchewan Industry and Resources)

larger image
[JPEG, 232.4 kb, 879 X 840, notice]

Quartz, from which these white pebbles are formed, is the most abundant mineral in the sedimentary rocks of Athabasca Basin. (Courtesy of  Saskatchewan Industry and Resources)
Quartz, from which these white pebbles are formed, is the most abundant mineral in the sedimentary rocks of Athabasca Basin.
(Courtesy of Saskatchewan Industry and Resources)

larger image
[JPEG, 287.2 kb, 1026 X 691, notice]


Life existed in these ancient shallow lakes in the form of cabbage-shaped, banded structures called stromatolites produced by photosynthetic bacteria. (Courtesy of Saskatchewan Industry and Resources)
Life existed in these ancient shallow lakes in the form of cabbage-shaped, banded structures called stromatolites produced by photosynthetic bacteria.
(Courtesy of Saskatchewan Industry and Resources)

larger image
[JPEG, 145.0 kb, 839 X 597, notice]

Poor hunting: Frequently burned, pine- and spruce-dominated forests on the dry sandy soils of the Athabasca Plain eco-region support smaller, less diverse wildlife populations than farther east and south.
Poor hunting: Frequently burned, pine- and spruce-dominated forests on the dry sandy soils of the Athabasca Plain eco-region support smaller, less diverse wildlife populations than farther east and south.
larger image
[JPEG, 288.8 kb, 908 X 681, notice]


Mudcracks preserved in rock show that the ancient rivers periodically dried up. (Courtesy of Saskatchewan Industry and Resources)
Mudcracks preserved in rock show that the ancient rivers periodically dried up.
(Courtesy of Saskatchewan Industry and Resources)

larger image
[JPEG, 61.0 kb, 413 X 671, notice]

Unconformity - Athabasca Group sandstone 1700 million years old. Conglomerate 1820 million years old. Unconformities (erosional surfaces), such as the one shown here on the north shore of Lake Athabasca, indicate major time breaks in the geological record. This unconformity marks the erosion of the great mountain belt formed 1800 million years ago. Most of the uranium deposits in Athabasca Basin are associated with fault zones (breaks in the crust with movement) that cut this unconformity. These deposits are the richest known in the world. Ones near the surface are mined from open pits, but deeper ones are mined underground. (Courtesy of Saskatchewan Industry and Resources)
Unconformity - Athabasca Group sandstone 1700 million years old. Conglomerate 1820 million years old. Unconformities (erosional surfaces), such as the one shown here on the north shore of Lake Athabasca, indicate major time breaks in the geological record. This unconformity marks the erosion of the great mountain belt formed 1800 million years ago. Most of the uranium deposits in Athabasca Basin are associated with fault zones (breaks in the crust with movement) that cut this unconformity. These deposits are the richest known in the world. Ones near the surface are mined from open pits, but deeper ones are mined underground.
(Courtesy of Saskatchewan Industry and Resources)

larger image
[JPEG, 225.2 kb, 991 X 622, notice]


Open pit uranium mine. (Courtesy of Cameco Corporation)
Open pit uranium mine.
(Courtesy of Cameco Corporation)

larger image
[JPEG, 116.8 kb, 1035 X 434, notice]

Underground uranium mine. Clean energy: nuclear reactors produce no greenhouse gases, although depleted uranium fuel cells need to be stored safely. (Courtesy of Cameco Corporation)
Underground uranium mine. Clean energy: nuclear reactors produce no greenhouse gases, although depleted uranium fuel cells need to be stored safely.
(Courtesy of Cameco Corporation)

larger image
[JPEG, 123.2 kb, 799 X 599, notice]



Did You Know ?
  • stromatolites are the oldest fossils in Saskatchewan.

  • 14% of Canada's (and 18% of the world's) electricity comes from nuclear power plants.

Previous (If rocks could talk...)Index (Geoscape Northern SaskatchewanGeoscience for our Canadian Shield Community)Next (The ice age: shaping our landscape)


2006-05-05Important notices