Structurally-controlled fluvioglacial erosion features near Schefferville, Québec

Bibliographic Data

ID3825327
AuthorsWerner Barr (0000-0003-0064-0211, corresponding author), William Barr (0000-0001-7711-7758)
Year2005
Volume13
Issue30
Pages295-320
Publication date2005-04-12
Open AccessNo
TypeARTICLE
VenueCahiers de géographie du Québec (JOURNAL)
Journal identifiersISSN: 0007-9766 • E-ISSN: 1708-8968
PublisherConsortium Erudit (PUBLISHER • CA)
DOI10.7202/020880ar
OpenAlexW2118108550
LanguageEN
References cited6

The coincidence as to location of a late-Wisconsin ice disintegration centre, with an earlier ice dispersal centre, some 30 miles north-west of Schefferville, Québec, resulted in large scale englacial meltwater flow from north-north-west to south-south-east across the Schefferville area. The direction of flow was controlled by the englacial hydraulic gradient, controlled in turn by the ice surface gradient. The Schefferville area is underlain by Proterozoic metasediments, exhibiting a series of parallel folds and thrust-faults aligned NW-SE ; this structure is reflected in the marked parallelism of the ridges and valleys. When the englacial meltwater streams were let down on to this substrate, structurally controlled alignment of the meltwater channels resulted. Generally, this has resulted in remarkably straight channels aligned along the strike or along faults. In the Houston Mountain area, however, steeply pitching anticlinos in slates oroduced a striking series of subglacial arcuate channels. At several points in the Schefferville area, subglacial meltwater flow down a hillside at right angles to the strike, and in the opposite direction to the dip, in zones of steeply dipping, well-bedded sediments, has produced the features referred to in literature as vallons, and earlier explained as being largely periglacial in origin. These are a special type of structurally controlled subglacial chute, in which there has been only slight periglacial modification of the original fluvioglacial form

Erosion · Geochemistry · Geomorphology · Glacial period · Meltwater · SLATES · Cryospheric studies and observations · Geology · Geology and Paleoclimatology Research · Landslides and related hazards · Paleontology

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