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BUL 057

Quaternary Stratigraphy and Surficial Geology of the Sand River Area (NTS 73L)

Quaternary Stratigraphy and Surficial Geology of the Sand River Area (NTS 73L) Eight glacial and nonglacial formations were defined for the Quaternary sequence in the Sand River area. The thick drift cover, combined with a paucity of exposures, ... Show Abstract

Andriashek, L.D.  Fenton, M.M.  1989-01-01

MAP 290

Surficial Geology of the Cadotte Lake Area (NTS 84C/SE)

Surficial Geology of the Cadotte Lake Area (NTS 84C/SE) Place Keywords 84c alberta cadotte lake canada harmon valley heart river Theme Keywords geology glacial lake peace glacial sedimentology quaternary stagnant ice moraine surficial geology ... Show Abstract

Paulen, R.C.  Pawlowicz, J.G.  Fenton, M.M.  2012-11-23

MAP 240

Surficial Geology of the Calling Lake Area, Alberta (NTS 83P/SW)

Surficial Geology of the Calling Lake Area, Alberta (NTS 83P/SW) Place Keywords 83p alberta canada pelican Theme Keywords geology quaternary surficial geology Place Keywords 83p alberta canada pelican Theme Keywords geology quaternary surficial ... Show Abstract

Campbell, J.E.  Fenton, M.M.  Pawlowicz, J.G.  2011-08-30

MAP 269

Surficial Geology of the Peerless Lake Area (NTS 84B)

Surficial Geology of the Peerless Lake Area (NTS 84B) Alberta Geological Survey maps 265, 266, 267 and 268. Place Keywords 84b alberta buffalo head hills canada lubicon lake peerless highlands peerless lake trout river Theme Keywords bedrock bogs ... Show Abstract

Paulen, R.C.  Fenton, M.M.  Pawlowicz, J.G.  Smith, I.R.  Plouffe, A.  2012-11-23

MAP 315

Surficial Geology of the Little Hay River Area (NTS 84L/NW)

Surficial Geology of the Little Hay River Area (NTS 84L/NW) [...]it contains basemap data. Place Keywords 84l alberta canada little hay river zama lake Theme Keywords geology glacial sedimentology outcrop quaternary stagnant ice moraine surficial ... Show Abstract

Paulen, R.C.  Fenton, M.M.  Pawlowicz, J.G.  Smith, I.R.  Plouffe, A.  2005-10-17

MAP 316

Surficial Geology of the Hay Lake Area (NTS 84L/NE)

Surficial Geology of the Hay Lake Area (NTS 84L/NE) [...]it contains basemap data. Place Keywords 84l alberta canada hay lake Theme Keywords geology glacial sedimentology outcrop quaternary stagnant ice moraine surficial geology surficial mapping ... Show Abstract

Paulen, R.C.  Fenton, M.M.  Plouffe, A.  Smith, I.R.  Weiss, J.A.  2005-10-17

MAP 541

Surficial Geology of the Whitesand River Area, Alberta (NTS 84O)

Surficial Geology of the Whitesand River Area, Alberta (NTS 84O) The map was prepared by airphoto interpretation together with limited ground-truthing. The airphotos within Wood Buffalo National Park were flown in 1975 (scale 1:54,000). The ... Show Abstract

Mougeot, C.  Fenton, M.M.  2010-04-01

MAP 540

Surficial Geology of the Dizzy Creek Area (NTS 84N/SE)

Surficial Geology of the Dizzy Creek Area (NTS 84N/SE) Place Keywords 84n alberta canada caribou lake caribou mountains dizzy creek james creek little rapids creek yates river Theme Keywords geological maps geology glacial deposits glacial lake hay ... Show Abstract

Pawley, S.M.  Mougeot, C.  Fenton, M.M.  2012-01-11

OFR 1994-20

Quaternary Stratigraphy and Surficial Geology Peace River-Winagami Region Year One Report For The End Fiscal Year 1993-94

Abstract: A reconnaissance survey of the southern half of the Peace River map area (84C/w 1/2) revealed the presence of predominantly two types of surficial glacial deposit they are: morainal and glaciolacustrine. Surficial moraine deposits that are thicker than 4 m are present in generally low lying areas and some are believed to overly deeply buried preglacial valleys. Indicator minerals were picked from thick (>10 m) till units intersected in two separate drill holes (BH-01 and -04). Surficial glaciolacustrine deposits, generally confined to the area south and east of the Peace River, range from 4 to 10 m thick and can be as much as 30 m thick locally. Synthesis of the Quaternary stratigraphy and glacial history is ongoing. Stratigraphic and geomorphic evidence collected to date, suggests that a single glacial advance has affected the area. A second field season in 1994 is planned.The Quaternary geology and stratigraphy of the Winagami region (NTS 83N/w1/2) is consistent with at least one major ice advance. Distribution of the surface units and ice directional land forms indicate a strong southwest ice movement direction. Most of the surficial deposits are associated with ice stagnation and deglaciation. Ice-contact stagnation, glaciolacustrine and aeolian deposits are really extensive and can exceed 20 m in thickness. Stratigraphic correlation of the upper Quaternary units between boreholes and large sections increases in complexity towards the north of the map area. The lowermost glacial unit in all cores is a dark grey massive till. Preliminary lithologic identification of the clasts in the till indicate a Canadian Shield origin. The thickness of Quaternary deposits varies, ranging from a few metres near Reno to well over 30 m in the southeast of the map area. Bedrock topography is irregular due to the presence of several large paleochannels. Place Keywords 83k 83n alberta canada Theme Keywords quaternary stratigraphy surficial

Balzer, S.A.  Leslie, L.E.  Fenton, M.M.  1994-10-01

OFR 1995-09

Quaternary Stratigraphy and Surficial Geology Peace River-Winagami Region, Alberta; Year Two Report For The End Fiscal Year 1994-95

The surficial morainal deposits, flutes, and morainal ridges which are generally situated in the uplands of the Clear and Whitemud Hills, are evidence of an unobstructed southerly flowing Laurentide Ice Sheet. Deglaciation is marked in the uplands ... Show Abstract

Balzer, S.A.  Leslie, L.E.  Fenton, M.M.  1995-04-01