3 edition of Quaternary geology of Cumberland Peninsula, Baffin Island, District of Franklin found in the catalog.
Quaternary geology of Cumberland Peninsula, Baffin Island, District of Franklin
Arthur S. Dyke
|Statement||Arthur S. Dyke, John T. Andrews, Gifford H. Miller.|
|Series||Memoir / Geological Survey of Canada ;, 403, Memoir (Geological Survey of Canada) ;, 403.|
|Contributions||Andrews, John T., Miller, Gifford H.|
|LC Classifications||QE185 .A2 no. 403, QE696 .A2 no. 403|
|The Physical Object|
|Pagination||32 p. :|
|Number of Pages||32|
|LC Control Number||82202682|
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Get this from a library. Quaternary geology of Cumberland Peninsula, Baffin Island, District of Franklin.
[Arthur S Dyke; John T Andrews; Gifford H Miller]. Blackadar, R.G. Precambrian geology of Boothia Peninsula, Somerset Island and Prince of Wales Island, District of Franklin; Geological Survey of Canada, Bulletin61 p. The District of Franklin was a regional administrative district of Canada's Northwest district consisted of the Canadian high Arctic Islands, notably Ellesmere Island, Baffin Island, and Victoria district also contained the mainland Melville Peninsula and Boothia Peninsula.
English navigators Martin Frobisher and Henry Hudson were the first Europeans known to have. The Penny Ice Cap on the Cumberland Peninsula of Baffin Island, N.W.T., Canada, was studied during the summer of This ice cap has an area of some sq.
and rests on a m. high. CHRONOLOGY OF QUATERNARY LANDFORMS, QIVITU PENINSULA, NORTHERN CUMBERLAND PENINSULA, BAFFIN ISLAND, N.W.T., CANADA [Alan R Nelson] on Author: Alan R Nelson. Gifford H. Miller Late Quaternary glacial and climatic history of northern Cumberland Peninsula, Baffin Island, N.W.T., Canada.
"Part IX in a series dealing with the Quaternary history of northern Cumberland Peninsula, Baffin Island, N.W.T., Canada." Quaternary Research, 3(4): DOI: /(73) John T. Andrews Late Quaternary marine sediment accumulation in fiord-shelf-deep-sea transects, Baffin Island to Baffin Bay.
Quaternary Science Reviews, 6: DOI: /(87) John T. Andrews Part one: Southeastern Baffin Island. In INQUA Excursion Guide Book C-2, INQUA 87 Canada, XII International Congress. Quaternary Glacial and Marine Stratigraphy of the Qivitu Peninsula, Northern Cumberland Peninsula, Baffin Island, Canada A.
by: Sediment diatom and chemical analyses of cores from three poorly buffered extra-glacial lakes on the northeastern margin of the Canadian Shield (Cumberland Peninsula, Baffin Island) record interactions between aquatic and terrestrial spheres that were influenced by late Quaternary climatic conditions.
Although differences exist between each of the lakes, notably with regards to the intensity Cited by: Nelson, A.R. () ‘Quaternary glacial and marine stratigraphy of the Qivitu Peninsula, northern Cumberland Peninsula, Baffin Island, Canada’, PhD dissertation, Cited by: THE ICE-CORED MORAINES OF AKUDNIRMUIT GLACIER, CUMBERLAND PENINSULA, BAFFIN ISLAND, N.W.T., CANADA [Paul E Carrara] on *FREE* shipping on qualifying : Paul E Carrara.
Quaternary Geology of Cumberland Peninsula, Baffin Island, District of Franklin. Ottawa, Canada: Geological Survey of Canada, Ottawa, Canada: Geological Survey of Canada, ISBN 0. QUATERNARY RESEARCH 3, () Late Quaternary Glacial and Climatic History of Northern Cumberland Peninsula, Baffin Island, N.W.T., Canada' GIFFORD H.
MILLER Received Ma Radiocarbon dates on molluscs in marine facies associated with glacial deposits in northern Cumberland Peninsula indicate both main fiord (Laurentide) ice and local glaciers remained at their late Wisconsin Cited by: Tasikutaaq Lake, on Cumberland Peninsula, Baffin Island, receives inflow and fine sediment from a km 2 drainage basin, 21% of which is glacier covered.
During the summer of the lake remained essentially isothermal between about 4 and 6 ° by: The climatic mechanisms driving the shift from the Medieval Warm Period (MWP) to the Little Ice Age (LIA) in the North Atlantic region are debated. We use cosmogenic beryllium dating to develop a moraine chronology with century-scale resolution over the last millennium and show that alpine glaciers in Baffin Island and western Greenland were at or near their maximum LIA configurations Cited by: Lower Paleozoic Geology of Foxe Basin, Northeastern Melville Peninsula, and Parts of Northern and Central Baffin Island.
(IN Structural Geology, Stratigraphy and Paleontology) (Geological Survey of Canada PaperPart A. Report of Activities. Part A. April to Octoberp. by Trettin, H. and a great selection of related books, art and collectibles available now at 8 JOHN T. ANDREWS, OLIVIA T. GIBB, ANNE E. JENNINGS, QUENTIN SIMON, Variations in the provenance of sediment from ice sheets surrounding Baffin Bay during MIS 2 and 3 and export to the Labrador Shelf Sea: site HU Davis Strait, Journal of Quaternary Science,29, 1, 3Wiley Online Library.
Media in category "Geology of Baffin Island" The following 8 files are in this category, out of 8 total. Aerial photograph of a cliff on Baffin 1, × 2,; MB. We measured Baffin Island and Icelandic rocks where plume water was trapped inside the rocks, rather than being degassed into the atmosphere.
Credit: Magnús Tumi Guðmundsson Analysis of lava from deep within Earth’s mantle suggests that water-soaked dust grains present early in the solar system, as the planets were just beginning to form. This book is the second of three volumes in which the recent knowledge of the extent and chronology of Quaternary glaciations has been compiled on a global scale.
This information is seen as a fundamental requirement, not only for the glacial community, but for the wider user-community of general Quaternary workers. In particular the need for accurate ice-front positions is a basic requirement.
Quaternary Geology, Waterton Lakes National Park, Alberta Geological Survey of Canada, "A" Series Map A,1 p. Cumming, L.M., Geology of the l'Anse aux Meadows National Historic Park, northern Newfoundland Report of activities part A, April to OctoberGeological Survey of Canada, Paper no.
A,4 p. The Quaternary history of northern Cumberland Peninsula, east Baffin Island, N.W.T., Part X: Radiocarbon date list. Arctic and Alpine Research, 4: Google ScholarCited by: In the eastern Arctic, a similar expansion of the 18 ka ice margin offshore of Baffin Island is suggested by geomorphology, cosmogenic nuclide dating and marine-based work.
Extensive cosmogenic work and mapping of glacial features on Baffin Island initiated this idea (e.g. Briner et al., ; Miller et al., ).Author: April S. Dalton, April S. Dalton, Martin Margold, Chris R. Stokes, Lev Tarasov, Arthur S. Dyke, Arth.
Lying off the northeastern coast of Baffin Island, Bylot Island is almost completely covered in an ice cap, which is pierced by mountain peaks and ridges. Hall Peninsula and the promontory west of Frobisher Bay are lowlands of Precambrian gneiss rock. The terrain is rough and rocky, with hills near the coast.
This book is the last of three volumes in which the recent knowledge of the extent and chronology of Quaternary glaciations has been compiled on a global scale. This information is seen as a fundamental requirement, not only for the glacial community, but for the wider user-community of general Quaternary workers.
In particular the need for accurate ice-front positions is a basic requirement. The Baffin Bay 10 Be production rate comprises three independent and statistically indistinguishable calibration data sets that span the last ~ to years: two from Disko Bugt in western Greenland and one from Clyde Inlet, Baffin Island.
Combined, these independent data sets result in a regional production rate with % by: The history and topography of Dauphin, Cumberland, Franklin, Bedford, Adams, and Perry counties [Pennsylvania] by Rupp, Israel Daniel, Pages: Location map for the Antarctic Peninsula, showing minimum ages for ice retreat.
LGM-extent of ice in the Antarctic Peninsula region – terrestrial evidence. The Antarctic Peninsula (Fig. 2 and Fig. 5) ice sheet is a part of the marine-based WAIS, where sea level is a major control on ice volume.
Sugden & Clapperton () suggested, on the. SURFICIAL GEOLOGY AND AGGREGATE STUDIES IN THE BOREAL PLAINS OF NORTHEAST BRITISH COLUMBIA Victor M. Levson1, Travis Ferbey1, Adrian Hickin1, Jan Bednarski2, Rod Smith2, Tania Demchuk1, Michelle Trommelen1, Ben Kerr1 and Amber Church1 ABSTRACT This paper summarizes the results of several studies conducted as part of the northeast British Columbia.
idly, initiating deglaciation of the Foxe Peninsula. This resulted in the highest and oldest glaciomarine features observed on the peninsula: ice contact deltas at m with related radio-carbon ages of ca.
14C ka BP ( cal ka BP). As deglaciation progressed. In the s, explorers and whalers returned home from the Arctic described a cold, desolate world, one that could swallow up expeditions without leaving a trace.
But this did not describe the Arctic of the Inuit, who called this world their home. Today Karen Routledge tells the story of Baffin Island’s Inuit community as they.
Map of events of Franklin's northwest passage expedition. Picture right - A satellite picture of part of the above area taken on the 27th of June This is early in he season still for ice melt and break-up, it gives an indication of the degree to which the area amongst the islands is choked with ice making shipping movements difficult to say the least.
Flow and retreat of the Late Quaternary Pine Island‐Thwaites palaeo‐ice stream, West Antarctica Alastair G. Graham,1 Robert D.
Larter,1 Karsten Gohl,2 Julian A. Dowdeswell,3 Claus‐Dieter Hillenbrand,1 James A. Smith,1 Jeffrey Evans,4 Gerhard Kuhn,2 and Tara Deen1 Received 10 August ; revised 30 March ; accepted 8 April ; published 19 August Cited by: From a regional point of view the N extension is distinct in orientation from the approximately N‐S trend of plate separation between North America and Greenland in the Baffin Bay during the Eocene.
However, the extension recorded in the margin is nearly perpendicular to the obliquely spreading Eocene accretion axis in the Baffin by: Blue Box Seminar.
Friday, March 4, p.m. SN Postglacial Sea-Level Lowstand and Fjord-floor Morphology Around Cumberland Peninsula, Baffin Island, Nunavut, presented by Johnathan Carter. The Cumberland Peninsula of eastern Baffin Island differs from the majority of the coastal Canadian Arctic in two main respects.
Darter, J.,Compilation of a late-Quaternary sea level curve: Thirteenth Keck Research Symposium in Geology Proceedings, p. Hampton, C.,Deformation of the Western Edge of the North American Plate in Proximity to the San Andreas Fault in North-Central California as Recorded in Late Quaternary Marine Terraces.
Surficial geology, Beekman Peninsula, Baffin Island, Nunavut, NTS 25P and NTS 15M (part); Tremblay, T. Canada-Nunavut Geoscience Office Open File Map, 1 sheet (Open Access) (NRCan Cont.# ). Geology of National Parks / Edition 3 available in Hardcover, Paperback.
Add to Wishlist. ISBN ISBN Pub. Date: 01/01/ Publisher: Kendall/Hunt Publishing Company. Geology of National Parks / Edition 3. Publish your book with B&N. Learn : $ MARiNe GeoscieNce PRoGRAMMe ReseARch RePoRt RR/11/03 An overview of the lithostratigraphical framework for the Quaternary deposits on the United Kingdom continental shelf M s stoker, P s Balson, D long and D R tappin the National Grid and other ordnance survey data are used with the permission of the controller of her Majesty’s stationery office.
Cumberland Island National Seashore, Georgia, – By Daniel L. Calhoun and Jeffrey W. Riley. Abstract. Much research has been conducted to better understand erosion and accretion processes for the seaward zones of coastal barrier islands; however, at Cumberland Island National Seashore, Georgia, the greater management concernAuthor: Daniel L.
Calhoun, Jeffrey W. Riley. Scottish Over-Winter Whaling at Cumberland Gulf, Baffin Island, Chesley W. Sanger!
Introduction Commercial whaling evolved through stages, each of which began with dis covery and hopeful enterprise; passed through a phase of rapid expansion, in tense competition and ruthless exploitation; and ended in declining resources.Quaternary stratigraphy and glacial history of the Peace River valley, northeast British Columbia1 Gregory M.D.
Hartman and John J. Clague Abstract: Two Cordilleran and three Laurentide glacial advances are recorded in Quaternary sediments and landforms in the Peace River valley, northeast British by: William Baffin. English Navigator, Ship Pilot, and Explorer. While searching for the elusive Northwest Passage, William Baffin made important discoveries about the geography of the northern reaches of the New two of his most noteworthy expeditions—both with explorer Robert Bylot as commander—Baffin searched the waters now known as Hudson Bay or Baffin Bay for.