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Proactive disclosure Print version ![Print version Print version](/web/20061103022955im_/http://ess.nrcan.gc.ca/esst_images/_printversion2.gif) ![ÿ](/web/20061103022955im_/http://ess.nrcan.gc.ca/esst_images/_spacer.gif) | ![ÿ](/web/20061103022955im_/http://ess.nrcan.gc.ca/esst_images/_spacer.gif) | ![Earth Sciences Information Centre Earth Sciences Information Centre](/web/20061103022955im_/http://ess.nrcan.gc.ca/esst_images/esic_e.jpeg) Natural Resources Canada > Earth Sciences Sector > Priorities > Earth Sciences Information Centre
Photo Gallery Our Dynamic Earth
Courtesy of the Geological Survey of Canada
[Click on an image thumbnail to view a larger image, notice] ![No. kgs-2262Mount Logan, 5951 m., Yukon Territory. No. kgs-2262Mount Logan, 5951 m., Yukon Territory.](/web/20061103022955im_/http://ess.nrcan.gc.ca/esic/gallery/images/kgs-2262_.jpg)
| No. kgs-2262 Mount Logan, 5951 m., Yukon Territory.Photo by C.J. Yorath
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![No. 180345Steeply dipping axial plane cleavage. These folded sedimentary layers exposed near Sullivan River in southeastern British Columbia dramatically illustrate the awesome forces constantly at work reshaping the features of the earth. One of the Geological Survey of Canada's tasks is to examine, study, and report on the effects and the causes of such forces. No. 180345Steeply dipping axial plane cleavage. These folded sedimentary layers exposed near Sullivan River in southeastern British Columbia dramatically illustrate the awesome forces constantly at work reshaping the features of the earth. One of the Geological Survey of Canada's tasks is to examine, study, and report on the effects and the causes of such forces.](/web/20061103022955im_/http://ess.nrcan.gc.ca/esic/gallery/images/180345_.jpg)
| No. 180345 Steeply dipping axial plane cleavage. These folded sedimentary layers exposed near Sullivan River in southeastern British Columbia dramatically illustrate the awesome forces constantly at work reshaping the features of the earth. One of the Geological Survey of Canada's tasks is to examine, study, and report on the effects and the causes of such forces.Photo taken by R.A. Price
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![No. 46600Badlands topography carved from flat-lying Upper Cretaceous strata; west of Little Sandhills Creek, Alberta. No. 46600Badlands topography carved from flat-lying Upper Cretaceous strata; west of Little Sandhills Creek, Alberta.](/web/20061103022955im_/http://ess.nrcan.gc.ca/esic/gallery/images/46600_.jpg)
| No. 46600 Badlands topography carved from flat-lying Upper Cretaceous strata; west of Little Sandhills Creek, Alberta.Photo taken by C.M. Sternberg
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![No.1994-731 PDeep sea vents: pipe organ vent, Juan de Fuca Ridge, black smoker. No.1994-731 PDeep sea vents: pipe organ vent, Juan de Fuca Ridge, black smoker.](/web/20061103022955im_/http://ess.nrcan.gc.ca/esic/gallery/images/1994-731.p_.jpg)
| No.1994-731 P Deep sea vents: pipe organ vent, Juan de Fuca Ridge, black smoker.Photo taken by I.R. Jonasson, 1992
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![No.120457Folded strata of the Humber Arm Group, Western Newfoundland. These Lower Ordovician rocks are exposed at Black Point, East Bay, 3.5 miles northeast of Port au Port. They are part of an extensive area of klippe ocks. No.120457Folded strata of the Humber Arm Group, Western Newfoundland. These Lower Ordovician rocks are exposed at Black Point, East Bay, 3.5 miles northeast of Port au Port. They are part of an extensive area of klippe ocks.](/web/20061103022955im_/http://ess.nrcan.gc.ca/esic/gallery/images/120457_.jpg)
| No.120457 Folded strata of the Humber Arm Group, Western Newfoundland. These Lower Ordovician rocks are exposed at Black Point, East Bay, 3.5 miles northeast of Port au Port. They are part of an extensive area of klippe ocks.Photo taken by L.M. Cumming, 1964
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![No. 1994-536 BFractures, quartz-filled. No. 1994-536 BFractures, quartz-filled.](/web/20061103022955im_/http://ess.nrcan.gc.ca/esic/gallery/images/1994-536.b_.jpg)
| No. 1994-536 B Fractures, quartz-filled.Photo taken by I. Ermanovics
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![No. 1996-081 AA beaver lodge style uranium mineralization. Kazan Falls, Northwest Territories. No. 1996-081 AA beaver lodge style uranium mineralization. Kazan Falls, Northwest Territories.](/web/20061103022955im_/http://ess.nrcan.gc.ca/esic/gallery/images/1996-081.a_.jpg)
| No. 1996-081 A A beaver lodge style uranium mineralization. Kazan Falls, Northwest Territories.Photo taken by A. Miller
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![No. 1995-360Oblique aerial photograph of folded siliciclastic units in the hinge zone of the northwest-plunging Lake Harbour Group synclinorium, southern Baffin Island, Northwest Territories. View is towards southwest. Width of the middle field of view is 2 km. No. 1995-360Oblique aerial photograph of folded siliciclastic units in the hinge zone of the northwest-plunging Lake Harbour Group synclinorium, southern Baffin Island, Northwest Territories. View is towards southwest. Width of the middle field of view is 2 km.](/web/20061103022955im_/http://ess.nrcan.gc.ca/esic/gallery/images/1995-360_.jpg)
| No. 1995-360 Oblique aerial photograph of folded siliciclastic units in the hinge zone of the northwest-plunging Lake Harbour Group synclinorium, southern Baffin Island, Northwest Territories. View is towards southwest. Width of the middle field of view is 2 km. Photo taken by Marc St.-Onge
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