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Academic literature on the topic 'Glaciation'

Author: Grafiati

Published: 4 June 2021

Last updated: 15 June 2025

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Journal articles on the topic "Glaciation"

1

Arnscheidt, Constantin W., and Daniel H. Rothman. "Routes to global glaciation." Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences 476, no. 2239 (2020): 20200303. http://dx.doi.org/10.1098/rspa.2020.0303.

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Theory and observation suggest that Earth and Earth-like planets can undergo runaway low-latitude glaciation when changes in solar heating or in the carbon cycle exceed a critical threshold. Here, we use a simple dynamical-system representation of the ice–albedo feedback and the carbonate–silicate cycle to show that glaciation is also triggered when solar heating changes faster than a critical rate. Such ‘rate-induced glaciations’ remain accessible far from the outer edge of the habitable zone, because the warm climate state retains long-term stability. In contrast, glaciations induced by changes in the carbon cycle require the warm climate state to become unstable, constraining the kinds of perturbations that could have caused global glaciation in Earth’s past. We show that glaciations can occur when Earth’s climate transitions between two warm stable states; this property of the Earth system could help explain why major events in the development of life have been accompanied by glaciations.

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Duk-Rodkin, Alejandra, and Owen L. Hughes. "Pleistocene Montane Glaciations in the Mackenzie Mountains, Northwest Territories." Géographie physique et Quaternaire 46, no. 1 (2007): 69–83. http://dx.doi.org/10.7202/032889ar.

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ABSTRACT During the Pleistocene the Mackenzie Mountains were affected by a series of glaciations. Through all the glaciations a single pattern seems to have been repeated: a Cordilleran ice sheet formed to the west of the continental divide and montane valley glaciers formed to the east. The montane glaciers in the Mackenzie Mountains emanated from two differents sources: a) a glacial divide, lying generally along the topographic divide between Pacific and Arctic drainage, and dividing the westerly flowing Cordilleran Ice Sheet from easterly and northerly flowing montane glaciers, b) local peaks in the Canyon Ranges. There were two well defined glacial advances in this mountain region: lllinoian, Late Wisconsinan, and one or more less defined pre-lllinoian glaciation(s). lllinoian and Late Wisconsinan glaciations are herein named Mountain River and Gayna River glaciations respectively. These advances are usually identifiable in valleys by frontal and segments of lateral moraines and glacial erosional features. Pre-lllinoian glaciation(s) have been recognized so far only in stratigraphie sections. The older advances were more extensive than the Gayna River advance; associated deposits occur higher on the valley sides and further down the valley than those associated with Gayna River Glaciation. During Mountain River Glaciation some of the montane glaciers in the Canyon Ranges merged to form piedmont glaciers. In contrast, during Gayna River Glaciation, the local glaciers consisted of single tongues, and these were mostly restricted to tributary valleys that had northward facing cirques.

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Lindner, Leszek, and Jan Dzierżek. "Pleistocene deposits in the western part of the Holy Cross Mountains." Studia Quaternaria 36, no. 2 (2019): 75–85. http://dx.doi.org/10.24425/sq.2019.126381.

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The paper presents characteristics of the Pleistocene sediments in the western part of the Holy Cross Mountains. They are subdivided into four complexes and their stratigraphic setting is referred to the updated scheme for the Pleistocene of Poland. The Preglacial Complex includes fluvial sediments characteristic for its lack of Scandinavian material. Sediments of three main glaciations (Nidanian, Sanian 1 and Sanian 2) within the South Polish Complex, are referred also as the South Polish Glaciations. The oldest of these glaciations (Nidanian) is separated from the middle glaciation (Sanian 1) by sediments of the Podlasian Interglacial, represented by clay at the Kozi Grzbiet Cave that contains faunal remains and record of the Brunhes/Matuyama palaeomagnetic boundary. During the middle (Sanian 1) and youngest glaciation (Sanian 2), the Holy Cross Mountains were almost completely covered by the Scandinavian ice sheet, forming glacial deposits separated by fluvial series of the Ferdynandovian Interglacial. The Middle Polish Complex begins with sediments of the Mazovian Interglacial, represented by a pollen record from the Zakrucze site. They are followed by deposits of periglacial and fluvial origin of the Liwiecian Glaciation, Zbójnian Interglacial, Krznanian Glaciation and Lublinian Interglacial. The following glaciation (Odranian) is represented by the youngest glacial deposits that document presence of the Scandinavian ice-sheet in the westernmost part of the Holy Cross Mountains. The North Polish Complex is composed of a climatic warming (Eemian Interglacial) and cooling (Vistulian Glaciation), and is represented by valley and periglacial deposits. The last cooling of the Pleistocene is recorded in faunal remains in the Raj Cave.

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Tsai, Cheng-Lung, Kôhei Kubota, Hong-Thai Pham, and Wen-Bin Yeh. "Ancestral Haplotype Retention and Population Expansion Determine the Complicated Population Genetic Structure of the Hilly Lineage of Neolucanus swinhoei Complex (Coleoptera, Lucanidae) on the Subtropical Taiwan Island." Insects 12, no. 3 (2021): 227. http://dx.doi.org/10.3390/insects12030227.

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The present study demonstrates that the complicated genetic structure of the hilly lineage of the Neolucanus swinhoei complex was driven by its biological features and habitat requirements as well as hindrance by the CMR during periodical Pleistocene glaciations. The results revealed a tendency of geographical differentiation and major and sub- lineage divergences before and after the Riss glaciation, followed by stable population growth during Würm glaciation. At least four refugia were inferred for N. swinhoei during the Riss–Würm glaciations. The ancestral haplotype retention in the cytochrome oxidase subunit I (COI) gene and compensated substitution in 16S rRNA gene is a possible evolutionary scenario resulting in the inconsistent evolution pattern between COI and 16S rRNA gene coupled with the long-distance dispersal of N. swinhoei. Although the CMR did hinder the dispersal of N. swinhoei, its ancestors may have dispersed to eastern Taiwan through the northern and southern low mountains of the CMR before the Riss glaciation. Our finding suggests that the population growth in the Würm glaciation led a dispersal back to western Taiwan, which is contrast to the more common dispersal scenario from western Taiwan to eastern populations proposed in other studies.

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Barrows, Timothy T., John O. Stone, L. Keith Fifield, and Richard G. Cresswell. "Late Pleistocene Glaciation of the Kosciuszko Massif, Snowy Mountains, Australia." Quaternary Research 55, no. 2 (2001): 179–89. http://dx.doi.org/10.1006/qres.2001.2216.

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AbstractLate Pleistocene glaciation of the Australian mainland was restricted to a small area of the southeastern highlands. Geomorphic mapping of the area and exposure dating using thein situproduced cosmogenic isotope10Be provides evidence for at least two distinct glaciations. The Early Kosciuszko glaciation consisted of a single glacier advance before 59,300 ± 5400 years ago (Snowy River Advance). The Late Kosciuszko glaciation comprised three glacier advances 32,000 ± 2500 (Headley Tarn Advance), 19,100 ± 1600 (Blue Lake Advance), and 16,800 ± 1400 years ago (Mt. Twynam Advance). The Early Kosciuszko glaciation was the most extensive and the Late Kosciuszko advances were progressively less extensive. These periods of glaciation in the highlands correspond to episodes of periglacial activity and peaks in lake levels and river discharge at lower elevations in southeastern Australia. Glacier advances on the Kosciuszko Massif correlate with advances in Tasmania, South America, and New Zealand and are broadly representative of hemispheric climate changes during the last glacial cycle.

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Humlum, Ole, Hanne H. Cristiansen, Lis E. Mortensen, Finlay M. Stuart, and John O. Stone. "Weichselian Glaciation of the Faroe Islands." Bulletin of the Geological Society of Denmark 72 (February 23, 2023): 19–100. http://dx.doi.org/10.37570/bgsd-2023-72-02.

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This paper presents a new complete field mapping of glacial landscapes, landforms and sediments in the Faroe Islands, supplemented by observations from bathymetric maps of the Faroe Shelf. In addition, previous investigations of Quaternary and espe-cially the Weichselian glaciation of the archipelago are reviewed. New cosmogenic nuclide exposure ages indicate that the last extensive glaciation of the Faroe Islands occurred during the Late Weichselian, most likely during the Last Glacial Maximum (LGM; c. 26.5–19.0 cal. ka BP), although a Younger Dryas (c. 12.9–11.7 cal. ka BP) age cannot be entirely excluded. Geomorphological mapping provides a background for reconstructing the extent and type of the glaciation of the Faroe Islands. The reconstructed Weichselian glaciation appears to have had the character of an exten-sive valley glaciation, with several marine glacier termini. The present glaciation of southern Spitsbergen, Svalbard, represents a modern analogue of the reconstructed Weichselian glaciation in the Faroe Islands. The lack of raised coastal features in the Faroe Islands, also at protected sites, suggests that postglacial isostatic uplift was smaller than post-LGM eustatic sea level rise. Numerical glacier reconstructions carried out for different extents of the last extensive Faroese glaciation suggest that such limited postglacial isostatic crustal uplift requires that the Faroe Shelf was not extensively glaciated during the Late Weichselian, but it doubtless was so during at least one of the previous Quaternary glaciations.

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Fitzsimons, Sean J., and Eric A. Colhoun. "Pleistocene glaciation of the King Valley, Western Tasmania, Australia." Quaternary Research 36, no. 2 (1991): 135–56. http://dx.doi.org/10.1016/0033-5894(91)90022-w.

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AbstractAnalysis of the geomorphology, geology, and palynology of deposits in the King Valley permits the identification of four glaciations and two interglaciations and has led to a revision of the Pleistocene stratigraphy of the West Coast Range. The oldest late-Cenozoic deposits in the valley appear to predate glaciation, contain extinct pollen types, and are probably of late-Tertiary age. Overlying deposits of the Linda Glaciation show intense chemical weathering and have a reversed detrital remanent magnetization indicating deposition before 730,000 yr B.P. The highly weathered tills are conformably overlain by organic deposits of the Regency Interglaciation which show a transition from montane scrub rainforest to lowland temperate rainforest. Deposits formed during the later Moore Glaciation record advances of the King Glacier and glaciers from the West Coast Range. A pollen-bearing fluvial deposit records an interstade during this glaciation. On the basis of weathering rinds, amino acid dating, and palaeomagnetism the deposits are estimated to have formed between 730,000 and 390,000 yr B.P. The Moore Glaciation deposits are overlain by sediments of the Henty Glaciation which are believed to predate 130,000 yr B.P. These deposits record multiple advances of the King Glacier and the development of a large lake during an interstade. Deposits of the subsequent Pieman Interglaciation consist of organic fine sands and silts that record a lowland scrub rainforest. Deposits of the last (Margaret) glaciation are restricted to small areas in the northern part of the valley. Although the most recent ice advance culminated after 19,000 yr B.P., evidence of older deposits of the Margaret Glaciation suggests that an early last-glaciation ice advance may have occurred. When combined with earlier studies, the recent work in the King Valley has provided one of the more complete records of Pleistocene glaciation in the Southern Hemisphere. Comparison of the deposits with the record of glaciation in southern South America and Westland, New Zealand, suggests some similarities exist between pre-last-glaciation events and indicates that glacial events in Southern Hemisphere middle latitude areas were synchronous during the last glaciation.

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Duk-Rodkin, Alejandra, and Owen L. Hughes. "Age Relationships of Laurentide and Montane Glaciations, Mackenzie Mountains, Northwest Territories." Géographie physique et Quaternaire 45, no. 1 (2007): 79–90. http://dx.doi.org/10.7202/032847ar.

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ABSTRACT The Mackenzie Mountains were glaciated repeatedly by large valley glaciers that emanated from the Backbone Ranges, and by much smaller valley glaciers that emanated from peaks in the Canyon Ranges. During the Late Wisconsinan the Laurentide Ice Sheet reached its all-time maximum position. The ice sheet pressed against the Canyon Ranges and moved up major valleys causing the diversion of mountain waters and organizing a complex meltwater system that drained across mountain interfluve areas towards the northwest. Two ages of moraines deposited by montane glaciers occur widely in the Mackenzie Mountains. Near the mountain front certain of the older moraines have been truncated by the Laurentide Ice Sheet, and others have been incised by meltwater streams emanating from the Laurentide ice margin, indicating that these older moraines predate the maximum Laurentide advance. Locally, certain of the younger montane moraines breach moraines and other ice marginal features of the Laurentide maximum, indicating that the younger montane glaciation post-dated the Laurentide maximum. Some large montane glaciers extended out from the mountains to merge with the retreating Laurentide Ice Sheet. There are several localities that display the age relationships between montane and Laurentide glaciations such as Dark Rock Creek, Durkan-Lukas Valley, Little Bear River and Katherine Creek. The older of the local montane glaciations is correlated tentatively with Reid Glaciation (lllinoian?) of central Yukon, and the younger with the Late Wisconsinan McConnell Glaciation. The Laurentide Glaciation is correlated with Hungry Creek Glaciation of Bonnet Plume Depression, which probably culminated about 30,000 years ago or somewhat later.

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Fairburn, William A., and Mark D. Bateman. "Possible new evidence for Mid-Pleistocene glaciation in the Vale of Pickering, North Yorkshire, UK." Proceedings of the Yorkshire Geological Society 63, no. 4 (2021): pygs2020–019. http://dx.doi.org/10.1144/pygs2020-019.

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Whilst the Late Devensian glaciation (MIS2) of the Vale of Pickering is well-documented, earlier glaciations within it are not. A proposed limited glaciation in the Mid-Pleistocene, thought to be of Marine Isotope Stage 8 (MIS) age is not well constrained. This paper aims to obtain preliminary ages for two of the most prominent geomorphic features in the Vale of Pickering to see if they related to pre-Devensian glaciations. New luminescence dating by infra-red stimulation of feldspars from sand accumulations near the summit of Gallows Hill, part of the Wykeham Moraine, and from a section through poorly sorted fluvial sand and gravel on the flanks of the Hutton Buscel Terrace in Yedman Dale gave ages of 176 ± 14 ka and 156 ± 12 ka, respectively. Evidence suggests they represent a glacial incursion (MIS 6) into the Vale of Pickering blocking its eastern end and forming a pre-Devensian Glacial Lake Pickering. Whilst they could be older, this style of glaciation is very different to the limited plateau ice-field proposed for MIS 8 at the western end of the Vale of Pickering. Taken at face value, these preliminary ages suggest that the Vale of Pickering was partially glaciated in MIS 6 as part of a wider ice sheet and contemporary with the Saalian glaciation in Europe.

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Dortch, Jason M., Lewis A. Owen, and Marc W. Caffee. "Quaternary glaciation in the Nubra and Shyok valley confluence, northernmost Ladakh, India." Quaternary Research 74, no. 1 (2010): 132–44. http://dx.doi.org/10.1016/j.yqres.2010.04.013.

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AbstractThree glacial stages (Deshkit 1, Deshkit 2 and Dishkit 3 glacial stages) are identified in the Nubra and Shyok valleys in northernmost Ladakh, northwest India, on the basis of geomorphic field mapping, remote sensing, and 10Be terrestrial cosmogenic nuclide surface exposure dating. The glacial stages date to ∼ 45 ka (Deshkit 1 glacial stage), ∼ 81 ka (Deshkit 2 glacial stage) and ∼ 144 ka (Deshkit 3 glacial stage). A mean equilibrium line altitude depression of ∼ 290 m for the Deshkit 1 glacial stage was calculated using the area accumulation ratio, toe-to-headwall ratio, area–altitude, and area–altitude balance ratio methods. Comparison of glaciation in the Nubra and Shyok valleys with glaciations in the adjacent Central Karakoram of northern Pakistan and northern side of the Ladakh Range of northern India indicates that glaciation was synchronous on Milankovitch timescales across the region during MIS-6, but differed greatly in extent, with more extensive glaciation in the Karakoram than the morphostratigraphically equivalent glaciation on the northern slopes of the Ladakh Range. This highlights the strong contrast in the extent of glaciation across ranges in the Himalaya–Tibetan orogen, necessitating caution when correlating glacial successions within and between mountain ranges.

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Dissertations / Theses on the topic "Glaciation"

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Holden, W. G. "The glaciation of central Ayrshire." Thesis, University of Glasgow, 1997. http://theses.gla.ac.uk/1585/.

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Ross, Hamish. "The last glaciation of Shetland." Thesis, University of St Andrews, 1997. http://hdl.handle.net/10023/15278.

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Evidence of the last glaciation of the Shetland Islands, UK, is re-examined and combined with new data on terrestrial glacigenic deposits and recent offshore data from the continental shelf to produce a dynamic, integrated model of the history of the whole ice cap. It is shown that evidence which has previously been attributed to last glacial, or earlier, Scandinavian ice incursion, might be explained by the eastwards migration of local ice sheds. At its maximum, the ice sheet reached the continental shelf edge to the west of the islands, at least 75 km east, at least 50 km north and might be seen as a peninsular extension of the Scottish ice sheet to the south. The changing patterns of ice flow during deglaciation are reconstructed, implying an early phase of deglaciation at the west and northwest margins (possibly accounting for the suggested eastern migration of the ice shed), followed by retreat at more northern, then eastern, then southern margins. It is suggested that the above pattern reflects tidewater calving controlled by bathymmetric variation around the ice sheet. During a later phase of deglaciation, the margin of the ice cap may have grounded at around the current -100m bathymmetric contour and from there retreated terrestrially. The importance of topographic control on patterns of deglaciation as ice retreated towards the island group is clearly established. Some minor moraines in parts of Shetland are due to active ice margins but their age is unknown. Radiocarbon dates reported here show that the last glaciation was Late Weichselian and that the maximum northern extent was at least 50 km north of the islands. The concepts of an eastwards migrating ice shed and an early, extensive ice cap retreating to a grounding point, could have parallels elsewhere in Scotland during the last glaciation. The methodology applied in this study of Shetland - integrating onshore and offshore data, and developing a dynamic picture of the whole ice cap - needs to be applied to the last Scottish ice sheet also.

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Rae, Alaric Campbell. "Late Quaternary glaciation in Southwest Ireland." Thesis, Coventry University, 2004. http://curve.coventry.ac.uk/open/items/03055be6-aad0-4313-d72e-1dac2156f221/1.

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During the last main phase of glaciations (26-13kaBP) an ice cap developed in south west Ireland and ice, from a dispersal centre in the vicinity of Kenmare, flowed north and diverged on the southern slopes of the Macgillycuddy’s Reeks. On these slopes, a weathering limit separates ice-moulded bedrock, on low ground, from frost-weathered terrain above. Assessment of bedrock dilation joint characteristics, Schmidt hammer R-value data, clay-sized mineral contents and magnetic properties of basal soil samples confirms significant contrasts in the degree of weathering above and below this limit. The weathering limit declines in altitude along former ice flow-lines and is confluent with morainic deposits on the eastern side of the Gap of Dunloe and on the western slopes of Skregbeg. This evidence supports the assertion that the high-level weathering limit is a periglacial trimline that marks the former maximum upper limit of the body of ice, which occupied this area of southwest Ireland during the LGM. This evidence, however, does not confute the notion that cold based, non-erosive plateau ice may have covered some or all of the upland surfaces that occur above the recorded weathering limits. Reconstruction of the former ice surface profile from periglacial trimline limits along three former flow lines yielded mean estimates for basal shear stress that ranged from 104.2 to 125.9 kPa. Although these values are high, they are within the range deemed normal for glaciers and ice sheets. The values suggest that the reconstructed areas of the ice cap were warm based and flowing on a bedrock substrate. This is supported by the geomorphological evidence of these areas, which shows that a landform – sediment association has developed consisting of zones of glacial scour and a thin, discontinuous drift cover. This contrasts with the glacial geomorphology of northern parts of the study area, where drift cover is largely continuous, and extensive in valley bottoms and on surrounding hillsides, and is associated with large lateral moraines.

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Poussart, Pascale Francine. "Late Ordovician glaciation, modelling experiments of a paradox." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp01/MQ37415.pdf.

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Kilfeather, Aoibheann Aoife. "Glaciation, deformation and till porosity : County Laois, Ireland." Thesis, Queen Mary, University of London, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.413647.

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Carr, Simon James. "The last glaciation of the North Sea Basin." Thesis, University of London, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.266821.

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Mitchell, W. A. "Glaciation of upper Wensleydale and adjoining watershed regions." Thesis, Royal Holloway, University of London, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.322134.

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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, Philip David. "Quaternary glaciation in the Pindus Mountains, Northwest Greece." Thesis, University of Cambridge, 2004. https://www.repository.cam.ac.uk/handle/1810/273442.

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Geomorphological and geological evidence for former Quaternary glaciation has been mapped n the Pindus Mountains of Northwest Greece. the dynamics and chronology of glaciation in this area has been established through sedimentological analysis, soil analysis and Uranium-series dating. Four glacial events are recorded in the sedimentological and geomorphological records. The more extensive recorded glaciation pre-dates 350,000 years BP and was characterised by extensive valley glaciers and ice-fields. A second glaciation occurred prior to the last interglacial, before <i>ca</i>. 127,000 years BP, and was characterised by glaciers that reached mid-valley positions. the height of the last glacial stage in Greece (30-20,000 <sup>14</sup>C years BP) is recorded by small cirque glacier moraines and relict periglacial rock glaciers. evidence for a fourth glacial phase is recorded only in the highest cirques of Mount Smolikas (2637 m a.s.l.), the highest peak in the Pindus Mountains. This phase of glaciation is likely to have occurred during the Late-glacial Substage (14-10,000 <sup>14</sup>C years BP). All of the glaciers during the different glacial stages were reconstructed and used alongside periglacial rock glaciers to determine palaeoclimate. During the glacial maximum of the last glacial stage mean annual temperatures were <i>ca</i>. 8-9°C lower than at present, and mean annual precipitation greater than 2000 mm - similar to modern values. Earlier glacial maxima are likely to have been colder but with mean annual precipitation still greater than 2000 mm. Maximum glacier extent in the Pindus Mountains is likely to have preceded the most severe arid phase of glacial cycles indicated in the pollen record and also global glacial maxima. this was because of the small size of the former Pindus glaciers and their rapid response to climate change, as well as the increased prevalence of aridity around the global glacial maxima. The glacial sequence in the Pindus Mountains represents the longest and best-dated recognised record of glaciation in the Mediterranean region and provides a stratigraphical framework for Quaternary cold-stage climates in Greece.

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Midgley, Nicholas Goulden. "Moraine-mound development in Britain and Svalbard : the development of 'hummocky moraine'." Thesis, Liverpool John Moores University, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.247350.

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Books on the topic "Glaciation"

1

King, Cuchlaine A. M. Glaciation. Nelson, 1992.

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A, Evans David J., ed. Glaciers & glaciation. Arnold, 1998.

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Cooper, Max P., and John E. Mylroie. Glaciation and Speleogenesis. Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-16534-9.

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Kuhle, Matthias. The Glaciation of High Asia. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-77566-1.

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1936-, Hamilton Thomas D., Reed Katherine M, Thorson Robert M. 1951-, Alaska Geological Society, and Alaska Quaternary Center, eds. Glaciation in Alaska: The geologic record. Alaska Geological Society, 1986.

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1936-, Hamilton Thomas D., and Alaska Geological Society, eds. Glaciation in Alaska: The geologic record. Alaska Geological Society, 1986.

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Hambrey, M. J. Late Precambrian glaciation of central East Greenland. Nyt Nordisk Forlag, 1987.

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1936-, Figge Udo Ludwig, ed. Language in the Würm glaciation: Acta colloquii. Brockmeyer, 1995.

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McCarron, Stephen G. Late Devensian glaciation of the North of Ireland. The Author], 2000.

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Geological Survey (U.S.), ed. Glaciers and glaciation in Glacier National Park, Montana. U.S. Geological Survey, 1993.

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Book chapters on the topic "Glaciation"

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Pinti, Daniele L. "Glaciation." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_649-3.

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Pinti, Daniele L. "Glaciation." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_649.

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Pinti, Daniele L. "Glaciation." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_649.

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Pinti, Daniele L. "Glaciation." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2023. http://dx.doi.org/10.1007/978-3-662-65093-6_649.

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Pinti, Daniele L. "Glaciation." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-642-27833-4_649-4.

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Bekker, Andrey. "Huronian Glaciation." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_742-4.

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Bekker, Andrey. "Huronian Glaciation." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_742.

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Ehlers, Jürgen, and Philip Gibbard. "Quaternary Glaciation." In Encyclopedia of Earth Sciences Series. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_423.

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Bekker, Andrey. "Huronian Glaciation." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_742.

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Bekker, Andrey. "Huronian Glaciation." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2023. http://dx.doi.org/10.1007/978-3-662-65093-6_742.

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Conference papers on the topic "Glaciation"

1

Pu, Judy P., Samuel A. Bowring, Jahandar Ramezani, et al. "GEOCHRONOLOGY OF THE GASKIERS GLACIATION." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286652.

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2

Rodbell, Donald, Robert G. Hatfield, Mark Abbott, et al. "700,000 YEARS OF TROPICAL ANDEAN GLACIATION." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-380841.

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3

Schanz, Sarah A., David R. Montgomery, Brian D. Collins, and Alison R. Duvall. "GLACIATION THROUGH THE LENS OF STRATH TERRACES." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-319251.

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4

Keller, C. Brenhin, and Kalin McDannell. "GEOCHEMICAL AND PHYSICAL CONSEQUENCES OF PROTEROZOIC GLACIATION." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-382600.

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5

Owen, Lewis A. "QUATERNARY GLACIATION OF TIBET AND THE BORDERING MOUNTAINS." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-297498.

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6

Clark, Peter. "KEN PIERCE'S BENCHMARK CONTRIBUTIONS TO WESTERN U.S. GLACIATION." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-383719.

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7

Jackson, Margaret S., Meredith A. Kelly, James M. Russell, et al. "HOLOCENE GLACIATION IN THE AFRICAN AND SOUTH AMERICAN TROPICS." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328035.

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8

Vesely, Fernando. "LITHOLOGICAL INDICATORS OF GLACIATION: WHY DO THEY STILL MATTER?" In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-355729.

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9

Wiles, Gregory, Ben Gaglioti, Victoria Race, et al. "ADVANCES IN UNDERSTANDING HOLOCENE ALPINE GLACIATION, SOUTHERN COASTAL ALASKA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-333049.

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10

Anders, Alison, Cecilia Cullen, Joshua J. McDanel, et al. "HOW DO FLUVIAL NETWORKS BECOME RE-ESTABLISHED FOLLOWING GLACIATION?" In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-335344.

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Reports on the topic "Glaciation"

1

Clague, J. J. Chapter 12: Quaternary Glaciation and Sedimentation. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/134099.

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2

Clague, J. J. Chapitre 12: Glaciation et Sédimentation Quaternaires. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/134100.

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3

Pelletier, B. R., P. R. Hill, P. J. Mudie, and S. M. Blasco. Late Quaternary glaciation and sea level history. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/126961.

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4

King, L. H., and G. B. Fader. Wisconsinan Glaciation On the Continental Shelf - Southeast Atlantic Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/129963.

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5

King, L. H., and G. B. J. Fader. Wisconsinan glaciation of the Atlantic continental shelf of southeast Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/120601.

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6

Reger, R. D., and T. K. Bundtzen. Multiple glaciation and gold-placer formation, Valdez Creek Valley, western Clearwater Mountains, Alaska. Alaska Division of Geological & Geophysical Surveys, 1990. http://dx.doi.org/10.14509/2288.

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7

Plouffe, A. Ice flow and late glacial lakes of the Fraser Glaciation, central British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/208610.

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8

Huscroft, C., and A. Plouffe. Field investigations of glacial Lake Knewstubb of the Fraser Glaciation, central British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210155.

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9

Andrews, J. T. Nature of the Last Glaciation in Canada [Chapter 8: Quaternary Geodynamics in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131628.

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10

Andrews, J. T. Nature de la Dernière Glaciation au Canada [Chapitre 8: Géodynamique Quaternaires au Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131629.

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