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OFR 2013-01

LiDAR-Based Landslide Classification and Inventory, Peace River, Alberta (NTS 84C)

The report also introduces preliminary work investigating the relationship between surface roughness derived from bare-earth light detection and ranging (LiDAR) and landslide activity. Field-based mapping and remote-sensing data sources, such as ... Show Abstract

Morgan, A.J.  Chao, D.K.  Froese, C.R.  2013-01-31

OFR 2012-18

Grosmont Formation Outcrops (T108-R6W5) at Vermilion Chutes, Peace River, North-Central Alberta (NTS 84J/07)

The outcrop at the Mikkwa Formation exposed at the lower Vermilion Chutes is considered equivalent to the Grosmont Formation based on the- similar lithology and paleontology to the Grosmont Formation in the subsurface, - lack of a mappable Mikkwa ... Show Abstract

Schneider, C.L.  Fenton, M.M.  Weiss, J.A.  2013-04-10

OFR 2010-11

Surficial Geology and Quaternary History of the Cleardale Area, Northwestern Alberta (NTS 84D/SW)

Due to the down-drainage retreat of the Laurentide Ice Sheet, subaerial and glacial meltwater discharge that converged toward the ice margin infilled this basin, forming the western part of a regional proglacial lake termed Glacial Lake ... Show Abstract

Atkinson, N.  Paulen, R.C.  2010-09-30

OFR 2012-04

Geological Setting for Large Landslides at the Town of Peace River, Alberta (NTS 84C)

The Peace River lowlands of Alberta and British Columbia are one of the most historically active mass-movement areas of Western Canada. The Alberta Geological Survey (AGS), with the support of various stakeholders, initiated a multidisciplinary ... Show Abstract

Morgan, A.J.  Paulen, R.C.  Slattery, S.R.  Froese, C.R.  2013-03-07

OFR 2009-18

Results of Sediment Coring at the Town of Peace River, Northwestern Alberta (NTS 84C)

The Peace River Lowlands of Alberta and British Columbia is one of the most historically active mass-movement areas in western Canada. Alberta Geological Survey (AGS), in collaboration with other stakeholders, has initiated a multiyear study, ... Show Abstract

Morgan, A.J.  Slattery, S.R.  Froese, C.R.  2009-10-20

OFR 2009-08

Implementation of a Web-GIS Application with ArcGIS Server 9.2 for the Peace River Landslide Project, Alberta

Implementation of a Web-GIS Application with ArcGIS Server 9.2 for the Peace River Landslide Project, Alberta Alberta Geological Survey created a Web-GIS application for the Peace River Landslide Project to provide access to significant geological, ... Show Abstract

Chao, D.K.  Chowdhury, S.   Lan, H.  Morgan, A.J.  Froese, C.R.  2009-06-09

OFR 1998-08

Frac Sand Evaluation Peace River Silica Sand Deposit - Final Report

Frac Sand Evaluation Peace River Silica Sand Deposit - Final Report The Peace River sand deposit has been known and recognized for many years as a potential source of high-grade silica sand. Considerable exploration drilling and investigation of ... Show Abstract

Alberta Geological Survey  1989-07-01

OFR 1991-21

Sand and Gravel Resources of the Peace River Area

Sand and Gravel Resources of the Peace River Area A portion of Peace River (84C) map sheet was studied in 1988 to determine the distribution and characteristics of the sand and gravel resource. The study area, approximately 3250 km2 in size, is ... Show Abstract

Scafe, D.W.  Edwards, W.A.D.  Boisvert, D.R.  1989-01-01

OFR 1973-34

Peace River Iron Deposits

The Peace River iron deposits are in the Clear Hills district of northern Alberta, about 300 miles northwest of Edmonton. Sedimentary (oolitic) iron deposits of Late Cretaceous underlie the Clear Hills district in the Peace River area of ... Show Abstract

Bertram, E.F.  Mellon, G.B.  1973-01-01

OFR 1972-01

Geology of the Peace-Athabasca River Delta Region, Alberta

The Delta receives sediment only during high flood stage of the Peace River so that area extension from sediment deposition is small. The Peace Delta is now effectively inactive and will remain so with the upstream regulation of water levels.A ... Show Abstract

Bayrock, L.A.  Root, J.D.  1972-05-01