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SPE 010

Quaternary Stratigraphy and Surficial Geology Peace River, Final Report

Deglaciation is marked in the uplands by deposition from stagnant ice and erosion by meltwater channels flowing predominantly down slope; and by the formation of glacial lakes within the plateaus surrounding the towns of Manning and Peace ... Show Abstract

Leslie, L.E.  Fenton, M.M.  2001-01-01

OFR 1994-20

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

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. Indicator minerals were picked from thick ... Show Abstract

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