The Quttinirpaaq National Park region is mountainous including the highest peak in eastern North America. Glaciers cover about half of the map area, including...
A detailed study of the surficial geology of the east coast of Vancouver Island from Deep Bay to Nanoose Harbour was undertaken as part of the Nanaimo Lowland...
The map area on the flank of North Shore Mountains is incised by three glacially-widened valleys. Glacial cycles caused sporadic erosion and deposition of...
The Mw 7.8 Haida Gwaii earthquake on October 28th, 2012 (October 27th local time) was caused by northeast thrusting of the Pacific plate beneath Haida Gwaii,...
Kwokullie Lake map area (NTS 94P/07) covers the northeast part of the Etsho Plateau whose northern boundary is defined by a large meltwater channel that is now...
The Chu Chua Creek (west half) map area is a gently rolling to rugged upland 900 to 1700 m in elevation. The topography is controlled by the underlying...
The Louis Creek (west half) is a rugged upland lying 1200 to 1800 m above sea level. The eastern half of the map area is underlain by Paleozoic volcanic,...
The Clearwater map area consists of gently rolling to rugged uplands at about 1200 m in elevation, with summits reaching over 1900 m in three separate areas....
The surficial geology of the Pesh Creek (NTS 94 P/8) map area is dominated by the effects of continental glaciation during the Late Wisconsinan (ca. 25 000-10...
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