Relevant bibliographies by topics / British Ice Sheet

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'British Ice Sheet'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "British Ice Sheet"

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Gandy, Niall, Lauren J. Gregoire, Jeremy C. Ely, et al. "Marine ice sheet instability and ice shelf buttressing of the Minch Ice Stream, northwest Scotland." Cryosphere 12, no. 11 (2018): 3635–51. http://dx.doi.org/10.5194/tc-12-3635-2018.

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Abstract. Uncertainties in future sea level projections are dominated by our limited understanding of the dynamical processes that control instabilities of marine ice sheets. The last deglaciation of the British–Irish Ice Sheet offers a valuable example to examine these processes. The Minch Ice Stream, which drained a large proportion of ice from the northwest sector of the British–Irish Ice Sheet during the last deglaciation, is constrained with abundant empirical data which can be used to inform, validate, and analyse numerical ice sheet simulations. We use BISICLES, a higher-order ice sheet
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Hartman, Gregory M. D., John J. Clague, René W. Barendregt, and Alberto V. Reyes. "Late Wisconsinan Cordilleran and Laurentide glaciation of the Peace River Valley east of the Rocky Mountains, British Columbia." Canadian Journal of Earth Sciences 55, no. 12 (2018): 1324–38. http://dx.doi.org/10.1139/cjes-2018-0015.

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In the past, researchers have disagreed over the maximum extent of the Cordilleran Ice Sheet in the Peace River valley during the Late Wisconsinan. Some workers argued that Cordilleran ice reached beyond the Rocky Mountains and briefly coalesced with the Laurentide Ice Sheet on the westernmost Interior Plains. In contrast, others asserted that Cordilleran ice did not reach beyond the eastern front of the Rocky Mountains. Stratigraphic interpretation of three sections within a Middle Wisconsinan paleovalley and re-examination of a previously published regional stratigraphic framework show that
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Ryder, June M., and Denny Maynard. "The Cordilleran Ice Sheet in Northern British Colombia." Géographie physique et Quaternaire 45, no. 3 (2007): 355–63. http://dx.doi.org/10.7202/032881ar.

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ABSTRACT Dates from lavas associated with tills and erratics indicate that ice-sheet glaciations occurred between 4 and 0.6 Ma BP. The few radiocarbon dates that are available suggest that the chronology of the Late Wisconsinan (Fraser Glaciation) ice sheet of northern British Columbia was similar to that of the southern part of the province. During what may have been a long, early phase of this glaciation, Glacial Lake Stikine was dammed by advancing valley glaciers in the Coast Mountains, and alpine glaciers developed on the intermontane plateau. At the climax of Fraser Glaciation, ice-flow
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Hughes, Anna L. C., Chris D. Clark, and Colm J. Jordan. "Subglacial bedforms of the last British Ice Sheet." Journal of Maps 6, no. 1 (2010): 543–63. http://dx.doi.org/10.4113/jom.2010.1111.

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Lindstrom, Dean R. "A Eurasian Ice-Sheet Study Using A Combined Ice-Sheet/ Ice-Shelf Numerical Model." Annals of Glaciology 14 (1990): 345. http://dx.doi.org/10.1017/s0260305500009125.

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A numerical model which simultaneously computes grounded and ice-shelf flow was used to develop an equilibrium ice-sheet–ice-shelf system over Eurasia and the Arctic region. Present-day net accumulation rates and mean annual and July temperature values were used as base values for climatic variable specifications. The values were adjusted during the model run to account for changes in the ice-surface elevation and atmospheric CO2 concentration. The model-determined equilibrium ice-sheet configuration was used as input for additional runs to observe what effect removing the Arctic ice shelf and
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Lindstrom, Dean R. "A Eurasian Ice-Sheet Study Using A Combined Ice-Sheet/ Ice-Shelf Numerical Model." Annals of Glaciology 14 (1990): 345. http://dx.doi.org/10.3189/s0260305500009125.

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A numerical model which simultaneously computes grounded and ice-shelf flow was used to develop an equilibrium ice-sheet–ice-shelf system over Eurasia and the Arctic region. Present-day net accumulation rates and mean annual and July temperature values were used as base values for climatic variable specifications. The values were adjusted during the model run to account for changes in the ice-surface elevation and atmospheric CO2 concentration. The model-determined equilibrium ice-sheet configuration was used as input for additional runs to observe what effect removing the Arctic ice shelf and
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Boulton, G. S. "The origin of till sequences by subglacial sediment deformation beneath mid-latitude ice sheets." Annals of Glaciology 22 (1996): 75–84. http://dx.doi.org/10.3189/1996aog22-1-75-84.

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A theory of erosion and deposition as a consequence of subglacial sediment deformation over beds of unlithified sediment is reviewed and applied to large-scale till sequences formed on the southern flanks of the North American and British and European ice sheets during the last glacial cycle. The distribution of till thickness, till lithology in relation to source materials and intra-till erosion surfaces along a flowline in the Michigan lobe of the North American ice sheet are shown to be compatible with the deformational theory but not with other modes of till genesis. It is then demonstrate
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Boulton, G. S. "The origin of till sequences by subglacial sediment deformation beneath mid-latitude ice sheets." Annals of Glaciology 22 (1996): 75–84. http://dx.doi.org/10.1017/s026030550001524x.

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A theory of erosion and deposition as a consequence of subglacial sediment deformation over beds of unlithified sediment is reviewed and applied to large-scale till sequences formed on the southern flanks of the North American and British and European ice sheets during the last glacial cycle. The distribution of till thickness, till lithology in relation to source materials and intra-till erosion surfaces along a flowline in the Michigan lobe of the North American ice sheet are shown to be compatible with the deformational theory but not with other modes of till genesis. It is then demonstrate
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Ely, Jeremy C., Chris D. Clark, David Small, and Richard C. A. Hindmarsh. "ATAT 1.1, the Automated Timing Accordance Tool for comparing ice-sheet model output with geochronological data." Geoscientific Model Development 12, no. 3 (2019): 933–53. http://dx.doi.org/10.5194/gmd-12-933-2019.

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Abstract. Earth's extant ice sheets are of great societal importance given their ongoing and potential future contributions to sea-level rise. Numerical models of ice sheets are designed to simulate ice-sheet behaviour in response to climate changes but to be improved require validation against observations. The direct observational record of extant ice sheets is limited to a few recent decades, but there is a large and growing body of geochronological evidence spanning millennia constraining the behaviour of palaeo-ice sheets. Hindcasts can be used to improve model formulations and study inte
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Clague, John J. "Quaternary stratigraphy and history, Williams Lake, British Columbia." Canadian Journal of Earth Sciences 24, no. 1 (1987): 147–58. http://dx.doi.org/10.1139/e87-012.

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Thick valley-fill sediments in the vicinity of Williams Lake, British Columbia, provide a detailed record of the late Quaternary history of an area near the centre of the former Cordilleran Ice Sheet. Stratigraphic units assigned to the late Wisconsinan Fraser Glaciation, the preceding (penultimate) glaciation, and the present interglaciation are described. Especially noteworthy are (1) thick units of sand and gravel deposited by braided streams, perhaps during periods of ice-sheet growth; and (2) complex glaciolacustrine sediments that accumulated in ice-dammed lakes during periods of deglaci
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Dissertations / Theses on the topic "British Ice Sheet"

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Davies, Bethan Joan. "British and Fennoscandian ice-sheet interactions during the Quaternary." Thesis, Durham University, 2008. http://etheses.dur.ac.uk/2225/.

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Northeastern England and the North Sea Basin is a critical location to examine the influence of glaciation in the northern Hemisphere during the Quaternary. This region was a zone of confluence between the British and Fennoscandian Ice Sheets, and harboured several dynamic ice lobes sourced from northern Scotland, the Cheviots, the Lake District and the Southern Uplands. The region thus has some of the most complex exposures of Middle to Late Pleistocene sediments in Britain, with both interglacial and glacial sediments deposited in terrestrial and marine settings, and being sourced from both
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Livingstone, Stephen John. "Reconstructing ice dynamics in the central sector of the last British-Irish Ice Sheet." Thesis, Durham University, 2010. http://etheses.dur.ac.uk/195/.

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The central sector (NW England and Scottish borders) of the last British-Irish Ice Sheet exhibits a palimpsest glacial geological and geomorphological signature characteristic of multi-phase ice flow and ice-marginal fluctuations. Despite its influential position at the heart of the British-Irish Ice Sheet, sourced from major ice dispersal centres of the northern Pennines, Lake District and Southern Uplands, and drained via fast-flowing outlets such as the Irish Sea Ice Stream, the region remains poorly constrained, both temporally and in terms of ice-flow dynamics. The principle goal of this
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McCarron, Stephen Gerard. "Late Devensian glaciation of the north of Ireland." Thesis, University of Ulster, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.268575.

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Hughes, Anna L. C. "The last British Ice Sheet : a reconstruction based on glacial landforms." Thesis, University of Sheffield, 2008. http://etheses.whiterose.ac.uk/16363/.

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The last British Ice Sheet has been a focus of research for over a century, and yet we have only a generalised picture of its extent and internal geometry. This is a remarkable situation compared to knowledge of the larger former ice sheets of North America and Fennoscandia. The central tenet of this thesis is that the glacial landform record has been neglected as a source of spatial information, hindering our attempts to reconstruct the characteristics of the ice sheet. This motivated systematic mapping of glacial landforms (subglacial bedforms, moraines, eskers, and meltwater channels) for t
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Finlayson, Andrew. "Geomorphology and dynamics of the British-Irish Ice Sheet in western Scotland." Thesis, University of Edinburgh, 2014. http://hdl.handle.net/1842/8965.

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Predicting the long-term behaviour of present-day ice sheets is hampered by the short timescales of our observations and restricted knowledge of the subglacial environment. Studying palaeoice sheets can help by revealing the nature and amplitude of past centennial- to millennial-scale ice sheet change. This thesis uses glacial sediments and landforms to examine the evolution of the partly marine-based British-Irish Ice Sheet (BIIS) and its bed, in western Scotland. Three zones of the former BIIS are considered: ranging from a mountain ice cap, to a core area of the ice sheet, to a peripheral m
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Small, David. "The deglaciation of the northwest sector of the last British-Irish ice sheet : integrating onshore and offshore data relating to chronology and behaviour." Thesis, University of St Andrews, 2013. http://hdl.handle.net/10023/3410.

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It is now accepted that the last British-Irish Ice Sheet (BIIS) was highly dynamic and drained by numerous fast flowing ice streams. This dynamic nature combined with its maritime location made the BIIS sensitive to the rapid climate change that characterised the Last Glacial Interglacial Transition. Gaining an understanding of the behaviour of the BIIS at this time is important to explore the nature of forcing between ice sheets and climate. This thesis presents new chronological data relating to the deglaciation of the northwest sector of the BIIS (NW-BIIS) from onshore dating of moraines us
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Sacchetti, Fabio. "Late Quaternary sedimentation associated with the British-Irish Ice Sheet on the NW Irish continental slope: a marine geological and geophysical investigation." Thesis, University of Manchester, 2012. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.646396.

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This research demonstrates the impact that glaciations had on the geomorphology and sediment deposition of the NW Irish continental margin, including both sides of the Rockall Trough and the Rockall Bank. A modern hydrographic, geophysical and sedimentological approach is used to analyse and interpret new and historical datasets, including multi beam, sidescan sonar, seismic and core data. New methodologies such as CUBE and Geocoder algorithms for multi beam bathymetry and backscatter data processing, 3D visualisations, ArcGIS Spatial and Hydrological Analysis and digital X-Ray scanning are us
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Weilbach, Kasper. "Extent, timing and nature of retreat of the British-Irish Ice Sheet offshore of north-western Ireland during and following the Last Glacial Maximum." Thesis, Durham University, 2018. http://etheses.dur.ac.uk/12655/.

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There has been a long history of research that has attempted to reconstruct the extent and dynamics of the British-Irish Ice Sheet (BIIS) during the last glacial cycle. Early reconstructions of ice extent in Ireland were based on terrestrial evidence, and advocated a relatively restricted ice sheet during the Last Glacial Maximum (LGM) that did not cover the whole of the island. More recent investigations from the continental shelf around Britain and Ireland reveal evidence for a much larger ice sheet, confluent with the Fennoscandian Ice Sheet in the North Sea and extending westwards onto the
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Leigh, Sasha Naomi Bharier. "A study of the dynamics of the British Ice Sheet during Marine Isotope Stages 2 and 3, focusing on Heinrich Events 2 and 4 and their relationship to the North Atlantic glaciological and climatological conditions /." St Andrews, 2007. http://hdl.handle.net/10023/525.

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Hibbert, Fiona Danielle. "Dynamics of the British Ice Sheet and prevailing hydrographic conditions for the last 175,000 years : an investigation of marine sediment core MD04-2822 from the Rockall Trough." Thesis, University of St Andrews, 2011. http://hdl.handle.net/10023/3136.

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This study presents a stratigraphic investigation of the marine sediment core MD04-2822 from the Rockall Trough (56° 50.54' N, 11° 22.96' W; 2344 m water depth). This core is currently the only available high resolution record for the calibration of Late Quaternary sedimentary sequences of the British (Hebridean) margin. It therefore offers an unprecedented archive of changing sedimentological and climatological conditions for the last 175,000 years. The high resolution, multi-proxy records have enabled surface and deep water conditions within the Rockall Trough to be reconstructed. In additio
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Books on the topic "British Ice Sheet"

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International Symposium on Representation of the Cryosphere in Climate and Hydrological Models (1996 Victoria, B.C.). Papers from the International Symposium on Representation of the Cryosphere in Climate and Hydrological Models held at Victoria, British Columbia, Canada, 12-15 August 1996. Edited by Walsh J. E. International Glaciological Society, 1997.

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D, Waddington Edwin, Walder Joseph S, International Association of Hydrological Sciences., and International Union of Geodesy and Geophysics. General Assembly,, eds. The physical basis of ice sheet modelling: Proceedings of an international symposium held during the XIXth General Assembly of the International Union of Geodesy and Geophysics at Vancouver, British Columbia, Canada, 9-22 August 1987. IAHS Press, 1987.

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Book chapters on the topic "British Ice Sheet"

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Brennand, Tracy A., Olav B. Lian, and Andrew J. Perkins. "The life and times of the Cordilleran Ice Sheet around the southern Fraser Plateau, British Columbia." In Trials and Tribulations of Life on an Active Subduction Zone: Field Trips in and around Vancouver, Canada. Geological Society of America, 2014. http://dx.doi.org/10.1130/2014.0038(06).

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Lee, Jonathan R., James Rose, Richard J. O. Hamblin, et al. "The Glacial History of the British Isles during the Early and Middle Pleistocene: Implications for the long-term development of the British Ice Sheet." In Developments in Quaternary Sciences. Elsevier, 2011. http://dx.doi.org/10.1016/b978-0-444-53447-7.00006-4.

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Holman, J. Alan. "Herpetological Population Adjustments in the Pleistocene of Britain and Europe." In Pleistocene Amphibians and Reptiles in Britain and Europe. Oxford University Press, 1998. http://dx.doi.org/10.1093/oso/9780195112320.003.0011.

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Compared to herpetological population adjustment patterns in North America (sec Holman, 1995c), the patterns in Britain and central and northern Europe seem to be rather straightforward. Basically, (1) very few herpetological species were present in ice-free areas during full glacial times, and (2) formerly glaciated areas were reinvaded by species from the south during warming cycles. Moreover, during climatic optimal warm times, several southern species existed well north of their present ranges. The invasion of southern Europe by northern populations in cold times is taken for granted (e.g., Rocek, 1995), although, as addressed in this chapter, it is difficult to document this in the fossil record. As indicated by geological and fossil evidence, the British Islands were connected to continental Europe during much of the Pleistocene. Although sea level changes in the British late Pleistocene arc a subject of some controversy (Stuart, 1982), it is generally agreed that Britain first separated from Ireland and then from the continent early in the Holocene. The classic idea is that the very depauperate British heretofauna of the cold part of the Devensian (last glacial stage) became somewhat, but not fully enriched by herpetological species during a warming trend that began about 10,000 ybp and lasted until about 8,500 ybp. The fact that Ireland has a much poorer modern herpetofauna (Triturus vulgaris, the rare Bufo calamita, Rana temporaria, and Lacerta vivipara) than Britain, which has six native species of amphibians and six native species of reptiles (Fra/,er, 1983; Smith, 1964), is attributed to Ireland's early separation from Britain. The Irish herpetofauna suggests that this separation occurred rather soon after the final withdrawal of the Devensian (last glacial) ice sheet. One of the most common questions asked about snakes, especially near St. Patrick's Day, is, "Have there ever been any snakes in Ireland?" No fossil snakes have ever been found in Ireland. But since Ireland lacks a terrestrial fossil record during most of the time that snakes have existed, it would seem that snakes could have lived in Ireland during some part of geological time. As far as I am aware, the few Pleistocene deposits containing herpetological remains in Ireland represent very late Devensian (last glacial) times.
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Alexander, Earl B., Roger G. Coleman, Todd Keeler-Wolfe, and Susan P. Harrison. "Northern Cascade-Fraser River, Domain 7." In Serpentine Geoecology of Western North America. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780195165081.003.0025.

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The Northern Cascade–Fraser River domain conforms to the Northern Cascade Mountains physiographic province in northwestern Washington and southern British Columbia, the San Juan Islands between the southern tip of Vancouver Island and the Northern Cascade Mountains, and much of the Interior Plateau province of British Columbia. The thread that connects these areas is the north–south Straight Creek–Fraser River fault system that runs through the Northern Cascade Mountains and northward along the Fraser River. The localities of domain 7 are along faults that branch off from this major fault system. The Northern Cascade Mountains are indeed mountainous, and the Interior Plateau of British Columbia is an area of dissected plateaus and scattered mountains. The Fraser River flows northwest in the Rocky Mountain Trench, which separates the North American craton on the northeast from accreted terranes on the southwest; then it turns around the northwest end of the Cariboo Mountains to the Interior Plateau. In the Interior Plateau, the Fraser River flows from Prince George south about 500 km to the Northern Cascade Mountains before turning westward toward the Pacific Coast. The northern part of domain 7 is in that part of the Fraser River basin, including tributaries northwest of Prince George, which is in the Interior Plateau province. Low, hilly terrain dominates the San Juan Islands. All of these areas in domain 7, except the Ingalls complex on southeast margin of the Northern Cascade Mountains, were covered by the Cordilleran ice sheet during the last stage of the Pleistocene glaciation, leaving <15 ka years for soil development on the current ground surfaces. Although alpine glaciers formed in the southeastern margin of the Northern Cascade Mountains, they did not cover all of the soils, allowing some of them longer time for development. Elevations in domain 7 range from sea level on San Juan Islands to mostly in the 600–1500 m range on the Interior Plateau of British Columbia, and up to 4392 m on Mt. Rainier in the Northern Cascade Mountains.
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Orr, David W. "Conservation and Conservatism." In The Nature of Design. Oxford University Press, 2002. http://dx.doi.org/10.1093/oso/9780195148558.003.0017.

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The philosophy of free-market conservatism has swept the political field virtually everywhere, and virtually everywhere conservatives have been, in varying degrees, hostile to the cause of conservation. This is a problem of great consequence for the long-term human prospect because of the sheer political power of conservative governments. Conservatism and conservation share more than a common linguistic heritage. Consistently applied they are, in fact, natural allies. To make such a case, however, it is necessary first to say what conservatism is. Conservative philosopher Russell Kirk (1982, xv–xvii) proposes six “first principles” of conservatism. Accordingly, true conservatives:… • believe in a transcendent moral order • prefer social continuity (i.e., the “devil they know to the devil they don’t know”) • believe in “the wisdom of our ancestors” • are guided by prudence • “feel affection for the proliferating intricacy of long-established social institutions” • believe that “human nature suffers irremediably from certain faults.”… For Kirk the essence of conservatism is the “love of order” (1982, xxxvi). Eighteenth-century British philosopher and statesman Edmund Burke, the founding father of modern conservatism and as much admired as he is unread, defined the goal of order more specifically as one which harmonized the distant past with the distant future. To this end Burke thought in terms of a contract, but not one about “things subservient only to the gross animal existence of a temporary and perishable nature.” Burke’s societal contract was not, in other words, about tax breaks for those who don’t need them, but about a partnership promoting science, art, virtue, and perfection, none of which could be achieved by a single generation without veneration for the past and a healthy regard for those to follow. Burke’s contract, therefore, was between “those who are living, those who are dead, and those who are to be born . . . linking the lower with the higher natures, connecting the visible and invisible world” ([1790] 1986, 194–195). The role of government, those “possessing any portion of power,” in Burke’s words, “ought to be strongly and awefully impressed with an idea that they act in trust” (ibid., 190).
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Conference papers on the topic "British Ice Sheet"

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Brennand, Tracy A., Jonathan E. Cripps, and Andrew J. Perkins. "DEGLACIAL STYLE, PATTERN AND TIMING OF THE CORDILLERAN ICE SHEET, SOUTH-CENTRAL INTERIOR BRITISH COLUMBIA." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-305052.

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Riedel, Jon. "RETREAT OF THE LAST CORDILLERAN ICE SHEET FROM THE NORTH CASCADE RANGE, WASHINGTON AND BRITISH COLUMBIA." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-305646.

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Jackson, Lionel E., Brent C. Ward, and Derek Turner. "GEOTECHNICAL DRILLING IN A BURIED FJORD PROVIDES EVIDENCE OF MULTIPLE ISOSTATIC MOATS MARGINAL TO COAST MOUNTAINS, SW BRITISH COLUMBIA, CANADA DURING CORDILLERAN ICE SHEET GROWTH, MARINE ISOTOPE STAGES 4 TO 2." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-337621.

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Reports on the topic "British Ice Sheet"

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Huntley, D. H., and B. E. Broster. Glacier flow patterns of the Cordilleran Ice Sheet during the Fraser Glaciation, Taseko Lakes map area, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/134203.

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Ryder, J. M., and J. J. Clague. Quaternary Stratigraphy and History, area of Cordilleran Ice Sheet - British Columbia [Chapter 1: Quaternary Geology of the Canadian Cordillera]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127935.

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