Late quaternary geology and geomorphology in the Lake Maskinongé area, Québec by Denis, Robert Phd.

Cover of: Late quaternary geology and geomorphology in the Lake Maskinongé area, Québec | Denis, Robert Phd.

Published by Uppsala universitet, Naturgeografiska institutionen in Uppsala .

Written in English

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  • Geomorphology -- Québec (Province) -- Lake Maskinongé region.,
  • Geology -- Québec (Province) -- Lake Maskinongé region.,
  • Glacial epoch -- Québec (Province) -- Lake Maskinongé region.,
  • Geology, Stratigraphic -- Quaternary.

Edition Notes

Book details

StatementRobert Denis.
SeriesUNGI rapport -- 28
LC ClassificationsGB5 .U66 no.28, GB428.5C3 D4
The Physical Object
Pagination125 p. :
Number of Pages125
ID Numbers
Open LibraryOL19785084M

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Late Quaternary geology and geomorphology in the Lake Maskinongé area, Québec. [Robert Denis] Book: All Authors / Contributors: Robert Denis. Find more information about: OCLC Number: Notes: Originally presented as the author's thesis, Uppsala, Quaternary Geology and Geomorphology (《第四纪地质学与地貌学》)is a teaching and researching textbook for higher teaching institutions in China.

It was first published by Geology Press in AugustQuébec book the chief editors of the book are TianMingZhong, ChengJie, and so : teaching textbook. "Late Quaternary Geology and Geomorphology in the Lake Maskinonge Area, Quebec." Univ.

Uppsala Dept. Physical Geography, UNGI Rept. Denis, R., and Prichonnet, G. Aspects EMPLACEMENT OF THE ST. NARCISSE MORAINE du Quaternaire dans la region au nord de Joliette.

In "Le Quaternaire du Quebec, 2nd Symposium, OctoberField Cited by: The Quaternary is the youngest geological period, beginning Ma ago and including the present day; it is therefore the only geological period that is continuously growing.

During the first epoch of the Quaternary, the Pleistocene, extremely cold and warm conditions alternated, frequently over. The late Quaternary geology of the Chalk River region, Ontario and Quebec N. Catto; deposited till on the marine sediments.

Following the final retreat of the ice from the area, lacustrine and aeolian deposition occurred locally for a short 10 years ago, the North Bay drainage route opened, greatly increasing the discharge Cited by: Pleistocene geology and geomorphology of the Riding Mountain and Duck Mountain areas, Manitoba-Saskatchewan.

Geological Survey of Canada, Memoirp. Klassen, R.W. Quaternary geology of the southern Canadian Interior Plains. In: Chapter 2 of Quaternary Geology of Canada and Greenland, R.J.

Fulton (ed.). Serge Occhietti, É. Govare, in Developments in Quaternary Sciences, The Major Northward Appalachian Ice-Flow Reversal. A Late-glacial reversal in ice flow is well documented by striations and rat-tails in the eastern part of the southern Appalachians of Québec (Lamarche,; Lortie and Martineau, ; Rappol, ).This reversal was a powerful event as it caused a.

Alexis Nutz, Jean‐François Ghienne, Mathieu Schuster, Pierre Dietrich, Claude Roquin, Murray B. Hay, Frédéric Bouchette and Pierre A. Cousineau, Forced regressive deposits of a deglaciation sequence: Example from the Late Quaternary succession in the Lake Saint‐Jean basin (Québec, Canada), Sedimentology, 62, 6, (), ().

Synopsis. Saltmarshes and mangroves are wetlands formed in the intertidal zone of sheltered coasts, notably in bays, lagoons and estuaries. The vegetation of the two environments is quite different: mangroves are composed of a number of tree species, while saltmarshes are. The Lake Saint-Jean lowland is a particular area in eastern Canada as it constitutes an important Late Quaternary depocenter compared with other surrounding onshore regions.

Far North Geomapping Initiative: Quaternary geology of the Great Island - Kellas Lake area, northern Manitoba (parts of NTS 54L, M, 64I, P) Technical Report Jan Late-quaternary morpho-sedimentology and submarine mass movements of the Betsiamites area, Lower St.

Lawrence Estuary, Quebec, Canada. Marine Geology Crossref, Google Scholar. Chapron E, Van Rensbergen P, Beck C, De Batist M, Paillet A. The South Saskatchewan River has a long term average discharge of m 3 /sec, with flood peaks in the range of to m 3 /sec. South of Saskatoon, the four major types of geomorphological elements recognised are channels, slipface‐bounded bars, sand flats and vegetated islands and floodplains.

Major channels are 3‐5 m deep, up to m wide, and flow around sand flats which are. Quaternary geology of northern New Jersey and the Trenton area.

Subitzky, S. Geology of Selected Areas in New Jersey and Eastern Pennsylvania and Guidebook of Excursions Rutgers University Press New Brunswick, N.J – Quaternary Science Reviews, 20(), Elverhøi, A.

(ed.), Glacial and Oceanic History of the Polar North Atlantic Margins, Quaternary Science Reviews, 17(), Forman, S.L. et al. A review of postglacial emergence on Svalbard, Franz Josef Land and Novaya Zemlya, northern Eurasia.

Quaternary Science Revi – Abstracts Abstract Abstract. The deglacial marine-limit surface is a virtual topography that shows the increase of elevation since deglaciation. The currently available set of marine-limit elevations (n = ), about three times the number available in the most recent synthesis, allows a fairly detailed rendering of the surface across most of glaciated North America and Greenland.

Vol. T, Quaternary Geology of the Great Basin: Inglewood, California to Salt Lake City, Utah June 27–July 8, Vol. T/, Overflight of the Tectonic Boundary Between the Colorado Plateau and the Basin Range Provinces: Northwest Arizona July 6–7, July 20–21, After I mapped the geomorphology, stratigraphy, and pedology of Clinton Co., Ohio, Doc G (who was the director of the Byrd Polar Institute at OSU) gave me the opportunity to go to Antarctica as a member of a team of 6 to study the late Paleozoic clastic sequence, which included the Gondwana tillites, and Cenozoic glacial sediments.

Teller, J. T., Lake Agassiz and its contribution to flow through the Ottawa – St. Lawrence system. In Gadd, N. (ed.), The Late Quaternary Development of the Champlain Sea Basin.

Geological Association of Canada. Special Pa pp. – Google Scholar. Quaternary Glaciations - Extent and Chronology: A closer look (Developments in Quaternary Science 15) J. Ehlers, P.L. Gibbard, P.D.

Hughes The book presents an up-to-date, detailed overview of the Quaternary glaciations all over the world, not only with regard to stratigraphy but also with regard to major glacial landforms and the extent of. Quaternary geology and ice flow history in the northwest part of the McLeod Lake map area (NTS J), central British Columbia: Implications for mineral exploration.

Joint Annual Meeting of Geological Association of Canada, the Mineralogical Association of Canada, the Society of Economic Geologists and the Society for Geology Applied to Mineral. Takuvik was created by University Laval (UL - Canada) and the Centre National de la Recherche Scientifique (CRNS - France) as a joint laboratory studying the Arctic ecosystems.

It was launched on January 1, Takuvik is located at UL, in Québec city, Canada where the CNRS employees are also located on a full-time basis. The Takuvik program is designed to study both ocean, under the. Quaternary and Late-Pleistocene Periglacial Environments PART IV Applied Periglacial Geomorphology Preface to First Edition.

This book is intended for use by second- and third-year level geography students in universities or colleges of higher education in the United Kingdom.

Start studying Ch 4 - Geomorphology/Surficial Processes/Quaternary Geology. Learn vocabulary, terms, and more with flashcards, games, and other study tools. Arbogast, A.F. Late-Quaternary Paleoenvironments and Landscape Evolution on the Great Bend Sand Prairie.

Kansas Geological Survey Bulletin #, 74 pp. Arbogast, A.F., and W.C. Johnson. Late-Quaternary Landscape Response to Environmental Change in South-Central Kansas.

Annals of the Association of American Geographers Caron, O., M. Lamothe, and W.W. Shilts,Glacial Lake Gayhurst: Contribution into the Midwisconsinan history of the southeastern sector of the Laurentide Ice Sheet and the late Quaternary stratigraphic record of southeastern Quebec; paperGeological Society of America, Northeastern Section Annual Meeting.

Geological Society of. Quaternary (/ k w ə ˈ t ɜːr n ə r i, ˈ k w ɒ t. ər ˌ n ɛr. i / kwə-TUR-nə-ree, KWOT-ər-nerr-ee) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS).

It follows the Neogene Period and spans from ± million years ago to the present. The Quaternary Period is divided into. Simulations () were undertaken to evaluate the impact of typical Lake Agassiz outbursts on the upper Great Lakes under plausible variations in lake surface areas and sill widths.

Flows over sills out of lakes are modelled using the equation for a broad-crested weir, with the model time increment set to one day.

The model was evaluated for Lake Agassiz outlet sill widths of 1, 4, and 10 km. The wooded mountainside’s mark the height of the ice in the valley during the Late Wisconsinian glaciation, about m elevation, or m thick in this valley (Gadd ).

near Banff, on a day trip to see local rocks in the area. The lake was still covered by a thick layer of softening ice when suddenly a strong wind blew up the valley. Historian and Board Member for Quaternary Geology and Geomorphology Division, Geological Society of America, Public Service Board Member for Pemigewasset Valley Search and Rescue Team (PVSART), - Present Member for Bristol Lodge Soup Kitchen, - Present Member for Dartmouth Outing Club Trails Program, - Present.

Attig, J.W., and Batten, W.G.,Quaternary geology of the Peshtigo River State Forest area: Wisconsin Geological and Natural History Survey Open-File. Late Quaternary zonation of vegetation in the eastern Grand Canyon.

Science Cole, K.L. and L. Mayer. Use of packrat middens to determine rates of cliff retreat in the eastern Grand Canyon, Arizona.

Geology – Late Cenozoic stratigraphy and structure of the west margin of the central San Joaquin Valley, California. – Correlation and age of Quaternary alluvial-fan sequences, Basin and Range province, southwestern United States. – Pliocene / Quaternary geology, geomorphology, and tectonics of.

Fairchild, H. / PROCEEDINGS OF THE 11th ANNUAL MEETING HELD AT NEW YORK CITY, Decemberextracted from the GSA Bulletin, Vol pages -6 plates,afb, - 5 - $ 90 [Includes the MEMOIR AND BIBLIOGRAPHY OF JAMES HALL; Ordovician faunas of Lake Champlain area; Landslip in Porneuf County, Quebec; Thames River Terraces.

Purchase Quaternary Glaciations - Extent and Chronology, Volume 15 - 1st Edition. Print Book & E-Book. ISBN- quaternary geomorphology of the uk, inheritance is in 3 phases: glacial, periglacial, fluvial. Marine oxygen isotope record: the terrestrial record of the pleistocene ages is incomplete - the marine record is much better - deep ocean sediments have a record of sea volume changes.

Elected Panel Member, GSA Quaternary Geology and Geomorphology Division. Editorial Board Member of the journal Quaternary International. Elected Secretary, American Quaternary Association. National Science Foundation, Division of Polar Programs, Earth Sciences Proposal Review Panel Member.

Geomorphology, stability and mobility of the Currituck slide,Marine Geology () - Late Quaternary evolution of channel and lobe complexes of Monterey Fan,Marine Geology () - Seafloor geology of the Monterey Bay area continental shelf,Marine Geology () - Quaternary Geology and Geomorphology Division Distinguished Career Award Lecture: Mickelson, D.M.,Changes in glacial landforms and subglacial conditions in the ice-marginal zone of the Laurentide Ice Sheet from southern Wisconsin to Minnesota: Geological Society.

The Quaternary Geologic Map of the Lake Superior 4° x 6° Quadrangle was mapped as part of the Quaternary Geologic Atlas of the United States. The atlas was begun as an effort to depict the areal distribution of surficial geologic deposits and other materials that accumulated or formed during the past 2+ million years, the period that includes all activities of the human species.

Elected Panel Member, GSA Quaternary Geology and Geomorphology. Division. Editorial Board Member of the journal Quaternary International. Elected Secretary, American Quaternary Association.

National Science Foundation, Division of Polar Programs, Earth Sciences. Proposal Review Panel Member.Geology of the Wunnummin Lake area. Ontario De­ Quaternary geology, geomorphology and hydrology of the Atlantic Provinces.

Guidebook for field trips A and C 61, 24th International Geological Congress, Montréal. S., Late Quaternary history of Magdalen Island, Quebec. Maritime Sediments, Geology geomorphology, hydrogeology (wetlands, streams, soils, landscape formation, Quaternary climate change, environmental geology) Research Interests Landscape development during the Cenozoic - Central Appalachians and Mid Atlantic Coastal PlainHydrologic and geomorphic changes during Quaternary climate change eventsWetland hydrology and.

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