Proactive disclosure Print version ![Print version Print version](/web/20061103013058im_/http://geoscape.nrcan.gc.ca/esst_images/_printversion2.gif) ![ÿ](/web/20061103013058im_/http://geoscape.nrcan.gc.ca/esst_images/_spacer.gif) | ![ÿ](/web/20061103013058im_/http://geoscape.nrcan.gc.ca/esst_images/_spacer.gif) | ![Geoscape Canada Geoscape Canada](/web/20061103013058im_/http://geoscape.nrcan.gc.ca/esst_images/geoscape_e.jpeg) Natural Resources Canada > Earth Sciences Sector > Priorities > Geoscape Canada > Fort Fraser
Geoscape Fort Fraser Physiography
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![Figure 20. Physiography is the surface form of the Earth. Fort Fraser map area includes flat and rolling lowlands, rolling uplands, and low-lying mountains. The mountains increase elevation to the north. Uplands of glacial till and glacial river sediment flank the mountains. Lowlands are areas of glacial lake sediment cut by modern rivers and creeks. Figure 20. Physiography is the surface form of the Earth. Fort Fraser map area includes flat and rolling lowlands, rolling uplands, and low-lying mountains. The mountains increase elevation to the north. Uplands of glacial till and glacial river sediment flank the mountains. Lowlands are areas of glacial lake sediment cut by modern rivers and creeks.](/web/20061103013058im_/http://geoscape.nrcan.gc.ca/fortfraser/images/physio_e_.jpg) Figure 20. Physiography is the surface form of the Earth. Fort Fraser map area includes flat and rolling lowlands, rolling uplands, and low-lying mountains. The mountains increase elevation to the north. Uplands of glacial till and glacial river sediment flank the mountains. Lowlands are areas of glacial lake sediment cut by modern rivers and creeks.
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