Cooperative geological mapping strategies across Canada |
Projects by Provinces/Territories |
Proactive disclosure Print version ![Print version Print version](/web/20061103034604im_/http://www.gsc.nrcan.gc.ca/esst_images/_printversion2.gif) ![ÿ](/web/20061103034604im_/http://www.gsc.nrcan.gc.ca/esst_images/_spacer.gif) | ![ÿ](/web/20061103034604im_/http://www.gsc.nrcan.gc.ca/esst_images/_spacer.gif) | ![Consolidating Canada's geoscience knowledge Consolidating Canada's geoscience knowledge](/web/20061103034604im_/http://www.gsc.nrcan.gc.ca/esst_images/2002ccgk_e.jpeg) Natural Resources Canada > Earth Sciences Sector > Priorities > Sustainable development of natural resources > Consolidating Canada's geoscience knowledge > COGMAPS
Co-operative Geological Mapping Strategies Across Canada : COGMAPS Projects in the Province of British Columbia
Choose a project of interest from the following map of British Columbia
![This view, looking to the northwest, shows the town of Atlin nestled on the banks of Atlin Lake. The low elevations around the town are underlain by ultramafic rocks. The two white patches east of the town are hydro-magnesite swamps formed from the naturally-occurring alteration of these rocks. The peneplained peaks of granitic and metamorphic rocks in the Coast Mountains form a picturesque backdrop. Glacially fed creeks give the lake its deep colour. Courtesy of Wayne Towriss. This view, looking to the northwest, shows the town of Atlin nestled on the banks of Atlin Lake. The low elevations around the town are underlain by ultramafic rocks. The two white patches east of the town are hydro-magnesite swamps formed from the naturally-occurring alteration of these rocks. The peneplained peaks of granitic and metamorphic rocks in the Coast Mountains form a picturesque backdrop. Glacially fed creeks give the lake its deep colour. Courtesy of Wayne Towriss.](/web/20061103034604im_/http://www.gsc.nrcan.gc.ca/cogmaps/prov/images/bc_photo.jpg) This view, looking to the northwest, shows the town of Atlin nestled on the banks of Atlin Lake. The low elevations around the town are underlain by ultramafic rocks. The two white patches east of the town are hydro-magnesite swamps formed from the naturally-occurring alteration of these rocks. The peneplained peaks of granitic and metamorphic rocks in the Coast Mountains form a picturesque backdrop. Glacially fed creeks give the lake its deep colour. Courtesy of Wayne Towriss. |
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