Log in

Relevant bibliographies by topics / Glaciations du Quaternaire / Journal articles

To see the other types of publications on this topic, follow the link: Glaciations du Quaternaire.

Journal articles on the topic 'Glaciations du Quaternaire'

Author: Grafiati

Published: 4 June 2021

Last updated: 2 February 2022

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Consult the top 50 journal articles for your research on the topic 'Glaciations du Quaternaire.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Browse journal articles on a wide variety of disciplines and organise your bibliography correctly.

1

Delmas, Magali, Marc Calvet, Yanni Gunnell, Régis Braucher, and Didier Bourlès. "Les glaciations quaternaires dans les Pyrénées ariégeoises : approche historiographique, données paléogéographiques et chronologiques nouvelles." Quaternaire, no. 23/1 (March 1, 2012): 61–85. http://dx.doi.org/10.4000/quaternaire.6091.

Full text

APA, Harvard, Vancouver, ISO, and other styles

2

Lebuis, J., and P. P. David. "La stratigraphie et les événements du Quaternaire de la partie occidentale de la Gaspésie, Québec." Dynamique et paléogéographie de l’inlandsis laurentidien 31, no. 3-4 (2011): 275–96. http://dx.doi.org/10.7202/1000278ar.

Full text

Abstract:

Une cartographie des dépôts meubles de la Gaspésie a permis d’identifier des unités lithostratigraphiques dont les noms formels sont proposés. Il existe des preuves pour deux glaciations distinctes représentées par des tills séparés par des intervalles de sédiments glacio-lacustres. La dernière glaciation a subi une inversion du sens de l’écoulement glaciaire et a permis la mise en place d’un troisième till, auquel est associé un diamicton glacio-marin déposé lors du vêlage des glaciers dans l’estuaire du Saint-Laurent. Enfin un quatrième till est dû à l’activité de calottes glaciaires confiné

APA, Harvard, Vancouver, ISO, and other styles

3

Hétu, Bernard, and James T. Gray. "Le modelé glaciaire du centre de la Gaspésie septentrionale, Québec." Géographie physique et Quaternaire 39, no. 1 (2007): 47–66. http://dx.doi.org/10.7202/032584ar.

Full text

Abstract:

RÉSUMÉLe relief du centre de la Gaspésie septentrionale a grandement été modifié au cours des événements glaciaires du Quaternaire, mais l'érosion glaciaire s'est montrée très sélective. Les éléments du paysage les plus touchés sont les vallées et, dans une moindre mesure, les escarpements séparant les plateaux. Les vallées ont été surcreusées dans leur partie aval, parfois même sous le niveau de la mer. De plus, elles ont été calibrées et élargies, ce qui s'est traduit par l'apparition de parois abruptes, d'éperons tronqués et de vallées affluentes suspendues. Par ailleurs, la majorité des va

APA, Harvard, Vancouver, ISO, and other styles

4

Stauch, Georg, and Frank Lehmkuhl. "Quaternary glaciations in the Verkhoyansk Mountains, Northeast Siberia." Quaternary Research 74, no. 1 (2010): 145–55. http://dx.doi.org/10.1016/j.yqres.2010.04.003.

Full text

Abstract:

AbstractGeomorphological mapping revealed five terminal moraines in the central Verkhoyansk Mountains. The youngest terminal moraine (I) was formed at least 50 ka ago according to new IRSL (infrared optically stimulated luminescence) dates. Older terminal moraines in the western foreland of the mountains are much more extensive in size. Although the smallest of these older moraines, moraine II, has not been dated, moraine III is 80 to 90 ka, moraine IV is 100 to 120 ka, and the outermost moraine V was deposited around 135 ka. This glaciation history is comparable to that of the Barents and Kar

APA, Harvard, Vancouver, ISO, and other styles

5

Fulton, R. J., E. Irving, and P. M. Wheadon. "Stratigraphy and paleomagnetism of Brunhes and Matuyama (>790 ka) Quaternary deposits at Merritt, British Columbia." Canadian Journal of Earth Sciences 29, no. 1 (1992): 76–92. http://dx.doi.org/10.1139/e92-009.

Full text

Abstract:

A succession of Quaternary deposits in the Merritt basin of south-central British Columbia contains evidence for four glaciations and two interglaciations. Paleomagnetic signatures in these sediments are of three types: normal polarity, proposed to have been acquired during the Brunhes Normal Polarity Chron; reversed polarity, proposed to have been acquired during the Matuyama Reversed Polarity Chron; and reversed polarity (Matuyama age) all but obscured by a normally magnetized overprint (Brunhes age).Reversely magnetized deposits at the base of the succession include glacial lacustrine depos

APA, Harvard, Vancouver, ISO, and other styles

6

Ramadhin, Christine, and Chuixiang Yi. "ESD Ideas: Why are glaciations slower than deglaciations?" Earth System Dynamics 11, no. 1 (2020): 13–16. http://dx.doi.org/10.5194/esd-11-13-2020.

Full text

Abstract:

Abstract. The Earth's climate during the Quaternary is dominated by short warm interglacials and longer cold glaciations paced by external forcings such as changes in insolation. Although not observed in the solar radiation changes, the time series of the cycles display asymmetry since transitions to full glacial conditions are slower than the termination of glaciations. Here an idea is proposed for the slower transition by identifying and describing two negative sea ice feedbacks dominant during the glaciation process that could serve as a control on the intermediate stage and decrease the pa

APA, Harvard, Vancouver, ISO, and other styles

7

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.

Full text

Abstract:

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

APA, Harvard, Vancouver, ISO, and other styles

8

Barendregt, R. W., J. S. Vincent, E. Irving, and J. Baker. "Magnetostratigraphy of Quaternary and late Tertiary sediments on Banks Island, Canadian Arctic Archipelago." Canadian Journal of Earth Sciences 35, no. 2 (1998): 147–61. http://dx.doi.org/10.1139/e97-094.

Full text

Abstract:

Sediments approximately 50 m thick from Banks Island (Canadian Arctic Archipelago) contain one of the longest terrestrial records of Pleistocene climate changes in North America. Samples have been obtained from 126 horizons distributed among four localitites, of which 116 horizons yielded acceptable paleomagnetic data. In sediments of the Matuyama Reversed Zone, there are recorded at least two and possibly as many as five full continental glaciations, two interglacial intervals, and a nonglacial interval at the beginning which is considered preglacial. Subzones attributable to the Olduvai and

APA, Harvard, Vancouver, ISO, and other styles

9

Locke, William W. "The late Quaternary geomorphic and paleoclimatic history of the Cape Dyer area, easternmost Baffin Island, N.W.T." Canadian Journal of Earth Sciences 24, no. 6 (1987): 1185–98. http://dx.doi.org/10.1139/e87-114.

Full text

Abstract:

The Cape Dyer area of easternmost Baffin Island was isolated from the Laurentide Ice Sheet by the fiords of Cumberland Peninsula. Accordingly, the glacial chronology at Cape Dyer is that of local ice only and is indicative of the local climate throughout the late Quaternary. Six drift units, representing three periods of restricted glaciation and three of expanded glaciation, are present. Beyond the most distal drift is an area that has not been modified by glaciation.The expanded glaciations were dated through correlation on the bases of moraine morphology, soil development, and amino-acid ra

APA, Harvard, Vancouver, ISO, and other styles

10

DOTSENKO, Valeriy, and Ibragim KERIMOV. "ABOUT THE REASONS OF CLIMATE WARMING BASED ON STUDYING THE HISTORY OF QUATERNARY GLACIOSES OF THE CAUCASUS (ON THE EXAMPLE OF THE INTERDURCHIE TEREK AND THE ANDIAN KOISU)." Sustainable Development of Mountain Territories 12, no. 3 (2020): 461–71. http://dx.doi.org/10.21177/1998-4502-2020-12-3-461-471.

Full text

Abstract:

The Greater Caucasus experienced repeated glaciation during the Quaternary (early, middle, upper Pleistocene, late Glacial, and late Holocene), which occurred under changing climatic conditions and differentiated tectonic movements. These glaciations, of course, are associated with changes in terrain, the formation of new deposits, transgressions and regressions of the Caspian Sea, changes in vegetation and soil types, so the problem of glaciation affects all earth Sciences to varying degrees. The study of Quaternary glaciation, especially Holocene glaciation, is currently relevant for underst

APA, Harvard, Vancouver, ISO, and other styles

11

Tidey, Emily J., and Christina L. Hulbe. "Bathymetry and glacial geomorphology in the sub-Antarctic Auckland Islands." Antarctic Science 30, no. 6 (2018): 357–70. http://dx.doi.org/10.1017/s0954102018000342.

Full text

Abstract:

AbstractNew high-resolution multibeam swath bathymetry along the east coast of the Auckland Islands is combined with subaerial topography and evaluated in the context of Quaternary glaciation of the islands. The marine geomorphology represents a mixture of past and current processes so that submerged glacial features are more evident in some areas than others. Fjords in the central and southern parts of the coastline are characterized by well-preserved terminal moraines and other glacial features while fjords to the north tend to have more subdued glacial features and a smoother seabed. This i

APA, Harvard, Vancouver, ISO, and other styles

12

Petley, D. J. "Report on Session 2b." Geological Society, London, Engineering Geology Special Publications 7, no. 1 (1991): 409–14. http://dx.doi.org/10.1144/gsl.eng.1991.007.01.37.

Full text

Abstract:

IntroductionNo part of geological time has had a more profound influence on the engineering characteristics of soils and rocks than the Quaternary period. Large areas of the earth’s surface are covered by superficial deposits of Quaternary age, and almost all surface soils and rocks affected by the changeds in climate which occurred in the Quaternary retain characteristics which have implications for engineering works at the present time.During the Quaternary period, at least five major glaciations occurred. During each glaciation, as the climate became colder, ice sheets spread from the poles

APA, Harvard, Vancouver, ISO, and other styles

13

Burbank, Douglas W., and Kang Jian Cheng. "Relative dating of Quaternary moraines, Rongbuk valley, Mount Everest, Tibet: Implications for an ice sheet on the Tibetan Plateau." Quaternary Research 36, no. 1 (1991): 1–18. http://dx.doi.org/10.1016/0033-5894(91)90013-u.

Full text

Abstract:

AbstractRelative-dating studies applied to high-altitude moraines (5000–5500 m) in the Rongbuk valley on the northern flank of Mt. Everest reveal strong contrasts in the weathering characteristics of the boulders exposed along moraine crests. These differences serve to define three intervals of major Pleistocene glaciation that, on the basis of the degree of weathering, are interpreted to extend back to at least the penultimate glaciation and probably encompass at least one still older glaciation. Either interpretation indicates that some of these moraines are considerably older than their pre

APA, Harvard, Vancouver, ISO, and other styles

14

May, Jan-Hendrik, Jana Zech, Roland Zech, et al. "Reconstruction of a complex late Quaternary glacial landscape in the Cordillera de Cochabamba (Bolivia) based on a morphostratigraphic and multiple dating approach." Quaternary Research 76, no. 1 (2011): 106–18. http://dx.doi.org/10.1016/j.yqres.2011.05.003.

Full text

Abstract:

AbstractAlthough glacial landscapes have previously been used for the reconstruction of late Quaternary glaciations in the Central Andes, only few data exist for the Eastern Cordillera in Bolivia. Here, we present results from detailed morphostratigraphic mapping and new data of surface exposure dating (SED), optically stimulated luminescence (OSL), and radiocarbon dating (14C) from the Huara Loma Valley, Cordillera de Cochabamba (Bolivia). Discrepancies between individual dating methods could be addressed within the context of a solid geomorphic framework. We identified two major glaciations.

APA, Harvard, Vancouver, ISO, and other styles

15

CONCHON, O. "Quaternary glaciations in Corsica." Quaternary Science Reviews 5 (1986): 429–32. http://dx.doi.org/10.1016/s0277-3791(86)80036-1.

Full text

APA, Harvard, Vancouver, ISO, and other styles

16

Rosqvist, Gunhild. "Quaternary glaciations in Africa." Quaternary Science Reviews 9, no. 2-3 (1990): 281–97. http://dx.doi.org/10.1016/0277-3791(90)90023-4.

Full text

APA, Harvard, Vancouver, ISO, and other styles

17

Andriashek, Laurence D., and René W. Barendregt. "Evidence for Early Pleistocene glaciation from borecore stratigraphy in north-central Alberta, Canada." Canadian Journal of Earth Sciences 54, no. 4 (2017): 445–60. http://dx.doi.org/10.1139/cjes-2016-0175.

Full text

Abstract:

Pleistocene sediments collected in north-central Alberta, Canada, were subsampled and studied for paleomagnetic remanence characteristics. A magnetostratigraphy has been established for sediments previously assumed to represent multiple continental (Laurentide) glaciations but for which no geochronology was available. Based on the Quaternary record elsewhere in Alberta and Saskatchewan, it was thought that some of these sediments were deposited during pre-late Wisconsinan glaciations. The Quaternary sedimentary successions of north-central Alberta have a thickness up to 300 m within buried val

APA, Harvard, Vancouver, ISO, and other styles

18

Clague, John J. "The Quaternary stratigraphic record of British Columbia—evidence for episodic sedimentation and erosion controlled by glaciation." Canadian Journal of Earth Sciences 23, no. 6 (1986): 885–94. http://dx.doi.org/10.1139/e86-090.

Full text

Abstract:

The terrestrial Quaternary stratigraphic record of British Columbia is largely a product of brief depositional events separated by long periods of nondeposition and erosion. Thick, stratified Quaternary sediments are present mainly in valleys and coastal lowlands and accumulated during periods of growth and decay of the Cordilleran Ice Sheet. At glacial maxima, till was deposited over large areas of low and moderate relief. However, at the same time, much of the landscape was eroded by glaciers.Sedimentation has been more restricted and has occurred at lower rates during nonglacial periods tha

APA, Harvard, Vancouver, ISO, and other styles

19

Böse, Margot. "Quaternary glaciations of northern Europe." Quaternary International 279-280 (November 2012): 61. http://dx.doi.org/10.1016/j.quaint.2012.07.268.

Full text

APA, Harvard, Vancouver, ISO, and other styles

20

Sarikaya, Mehmet Akif. "Late Quaternary glaciations in Turkey." Quaternary International 279-280 (November 2012): 427. http://dx.doi.org/10.1016/j.quaint.2012.08.1384.

Full text

APA, Harvard, Vancouver, ISO, and other styles

21

Böse, Margot, Christopher Lüthgens, Jonathan R. Lee, and James Rose. "Quaternary glaciations of northern Europe." Quaternary Science Reviews 44 (June 2012): 1–25. http://dx.doi.org/10.1016/j.quascirev.2012.04.017.

Full text

APA, Harvard, Vancouver, ISO, and other styles

22

Brown, Iain M. "Quaternary glaciations of New Guinea." Quaternary Science Reviews 9, no. 2-3 (1990): 273–80. http://dx.doi.org/10.1016/0277-3791(90)90022-3.

Full text

APA, Harvard, Vancouver, ISO, and other styles

23

van Vliet-Lanoë, Brigitte. "Le prélude au Quaternaire : les modalités d'entrée en glaciation (65 Ma - 2,2 Ma)." Quaternaire, no. 18/2 (June 1, 2007): 111–28. http://dx.doi.org/10.4000/quaternaire.1006.

Full text

APA, Harvard, Vancouver, ISO, and other styles

24

Zech, Wolfgang, Rupert Bäumler, Oksana Savoskul, Anatoli Ni, and Maxim Petrov. "Bodengeographische Beobachtungen zur pleistozänen und holozänen Vergletscherung des Westlichen Tienshan (Usbekistan)." E&G Quaternary Science Journal 46, no. 1 (1996): 144–51. http://dx.doi.org/10.3285/eg.46.1.11.

Full text

Abstract:

Abstract. Soil geographic studies were carried out in the Oigaing valley between Ugamsky and Pskemsky range NE of Tashkent (W-Tienshan, Republic of Uzbekistan) with special regard to the Pleistocene and Holocene glaciation. Clear end moraines of the last main glaciation are preserved at the junction of Maidan and Oigaing river at 1500-1600 m a.s.l. They show intensively weathered soils with a depth of more than 80 cm. Similar deposits ol presumably Pleistocene or late glacial origin are also located upvalley at the embouchure of numerous side valleys (Beschtor, Tekesch, Aütor) into the main va

APA, Harvard, Vancouver, ISO, and other styles

25

Wang, Xiaoli, Jiangyong Qu, Naifa Liu, Xinkang Bao, and Sen Song. "Limited gene flow and partial isolation phylogeography of Himalayan snowcock Tetraogallus himalayensis based on part mitochondrial D-loop sequences." Current Zoology 57, no. 6 (2011): 758–67. http://dx.doi.org/10.1093/czoolo/57.6.758.

Full text

Abstract:

Abstract Himalayan snowcock Tetraogallus himalayensis are distributed in alpine and subalpine areas in China. We used mitochondrial DNA control-region data to investigate the origin and past demographic change in sixty-seven Himalayan snowcock T. himalayensis. The fragments of 1155 nucleotides from the control region of mitochondrial DNA were sequenced, and 57 polymorphic positions defined 37 haplotypes. A high level of genetic diversity was detected in all populations sampled and may be associated isolation of the mountains and habitat fragmentation and deterioration from Quaternary glaciatio

APA, Harvard, Vancouver, ISO, and other styles

26

SHI, Y. "Quaternary glaciation in China." Quaternary Science Reviews 5 (1986): 503–7. http://dx.doi.org/10.1016/s0277-3791(86)80044-0.

Full text

APA, Harvard, Vancouver, ISO, and other styles

27

Rother, H., and J. Shulmeister. "Synoptic climate change as a driver of late Quaternary glaciations in the mid-latitudes of the Southern Hemisphere." Climate of the Past 2, no. 1 (2006): 11–19. http://dx.doi.org/10.5194/cp-2-11-2006.

Full text

Abstract:

Abstract. The relative timing of late Quaternary glacial advances in mid-latitude (40-55° S) mountain belts of the Southern Hemisphere (SH) has become a critical focus in the debate on global climate teleconnections. On the basis of glacial data from New Zealand (NZ) and southern South America it has been argued that interhemispheric synchrony or asynchrony of Quaternary glacial events is due to Northern Hemisphere (NH) forcing of SH climate through either the ocean or atmosphere systems. Here we present a glacial snow-mass balance model that demonstrates that large scale glaciation in the tem

APA, Harvard, Vancouver, ISO, and other styles

28

Scapozza, Cristian. "Evidence of paraglacial and paraperiglacial crisis in Alpine sediment transfer since the last glaciation (Ticino, Switzerland)." Quaternaire, no. 27/2 (June 1, 2016): 139–55. http://dx.doi.org/10.4000/quaternaire.7805.

Full text

APA, Harvard, Vancouver, ISO, and other styles

29

Paillard, Didier. "Quaternary glaciations: from observations to theories." Quaternary Science Reviews 107 (January 2015): 11–24. http://dx.doi.org/10.1016/j.quascirev.2014.10.002.

Full text

APA, Harvard, Vancouver, ISO, and other styles

30

Paillard, D. "On Quaternary glaciations, observations and theories." Quaternary Science Reviews 120 (July 2015): 128–32. http://dx.doi.org/10.1016/j.quascirev.2015.05.017.

Full text

APA, Harvard, Vancouver, ISO, and other styles

31

Stauch, G., and L. Gualtieri. "Late Quaternary glaciations in northeastern Russia." Journal of Quaternary Science 23, no. 6-7 (2008): 545–58. http://dx.doi.org/10.1002/jqs.1211.

Full text

APA, Harvard, Vancouver, ISO, and other styles

32

Ingólfsson, Ó. "Fingerprints of Quaternary glaciations on Svalbard." Geological Society, London, Special Publications 354, no. 1 (2011): 15–31. http://dx.doi.org/10.1144/sp354.2.

Full text

APA, Harvard, Vancouver, ISO, and other styles

33

Ghil, M., A. Mullhaupt, and P. Pestiaux. "Deep water formation and Quaternary glaciations." Climate Dynamics 2, no. 1 (1987): 1–10. http://dx.doi.org/10.1007/bf01088850.

Full text

APA, Harvard, Vancouver, ISO, and other styles

34

Rabassa, Jorge, and Chalmers M. Clapperton. "Quaternary glaciations of the southern Andes." Quaternary Science Reviews 9, no. 2-3 (1990): 153–74. http://dx.doi.org/10.1016/0277-3791(90)90016-4.

Full text

APA, Harvard, Vancouver, ISO, and other styles

35

Jansson, Peter, Cecilia Richardson, and Stig Jonsson. "Assessment of requirements for cirque formation in northern Sweden." Annals of Glaciology 28 (1999): 16–22. http://dx.doi.org/10.3189/172756499781821959.

Full text

Abstract:

AbstractCirques in the Rassepautasjtjåkka massif currently lack glaciers and the geomorphology indicates that no glaciers occupied the cirques during the Holocene. The current climatic conditions in the cirques can be assessed using available climatic data; air temperature at Rassepautasjtjåkka, summer and winter balances of adjacent glaciers, and general precipitation patterns in northern Sweden. The data suggest that either a significant change in precipitation and wind regime or a moderate change in temperature is required to initiate a cirque glacier in the massif. Formation of a wet-based

APA, Harvard, Vancouver, ISO, and other styles

36

Jeppsson, Lennart, and Mikael Calner. "The Silurian Mulde Event and a scenario for secundo–secundo events." Transactions of the Royal Society of Edinburgh: Earth Sciences 93, no. 2 (2002): 135–54. http://dx.doi.org/10.1017/s0263593300000377.

Full text

Abstract:

ABSTRACTGraphic correlation using graptolites and conodonts provides a high-resolution timescale for correlating from coastal to deep oceanic sections and, thereby, also a detailed record of the sequence of changes during the Mulde Secundo-Secundo Event. That interval includes sedimentary facies otherwise unknown in older Wenlock to early Ludlow strata on Gotland. The identified sequence of changes includes a detailed record of, in order: two extinctions (Datum points 1 and 1·5); widespread deposition of carbon-rich sediments extensive enough to cause a δ13C increase of c. 4.8‰, the onset, max

APA, Harvard, Vancouver, ISO, and other styles

37

Sosa-Pivatto, María, Gonzalo A. Camps, Matías C. Baranzelli, Anahí Espíndola, Alicia N. Sérsic, and Andrea Cosacov. "Connection, isolation and reconnection: Quaternary climatic oscillations and the Andes shaped the phylogeographical patterns of the Patagonian bee Centris cineraria (Apidae)." Biological Journal of the Linnean Society 131, no. 2 (2020): 396–416. http://dx.doi.org/10.1093/biolinnean/blaa116.

Full text

Abstract:

Abstract The joint effect of the Andes as a geographical barrier and the Quaternary glaciations as promoters of genetic divergence remains virtually unexplored in southern South America. To help fill this knowledge gap, in this study we investigated the demographic history of Centris cineraria, a solitary bee mainly distributed in Patagonia. We used mitochondrial and nuclear markers and performed phylogeographical and dating analyses, adjusted spatio-temporal diffusion and species distribution models, and used Approximate Bayesian Computation to identify likely historical demographic scenarios

APA, Harvard, Vancouver, ISO, and other styles

38

Barr, Iestyn D., and Chris D. Clark. "Late Quaternary glaciations in Far NE Russia; combining moraines, topography and chronology to assess regional and global glaciation synchrony." Quaternary Science Reviews 53 (October 2012): 72–87. http://dx.doi.org/10.1016/j.quascirev.2012.08.004.

Full text

APA, Harvard, Vancouver, ISO, and other styles

39

Owen, Lewis A., Ruth Robinson, Douglas I. Benn, et al. "Quaternary glaciation of Mount Everest." Quaternary Science Reviews 28, no. 15-16 (2009): 1412–33. http://dx.doi.org/10.1016/j.quascirev.2009.02.010.

Full text

APA, Harvard, Vancouver, ISO, and other styles

40

Sizov, Oleg, Anna Volvakh, Anatoly Molodkov, Andrey Vishnevskiy, Andrey Soromotin, and Evgeny Abakumov. "Lithological and geomorphological indicators of glacial genesis in the upper Quaternary strata, Nadym River basin, Western Siberia." Solid Earth 11, no. 6 (2020): 2047–74. http://dx.doi.org/10.5194/se-11-2047-2020.

Full text

Abstract:

Abstract. Analysing the genesis of Quaternary sediments is important for understanding the glaciation history and development of marine sediments in the northern part of Western Siberia. The problem is relevant since there is no consistent concept of the Quaternary sediment genesis in the north of Western Siberia. The formation of sediments is associated with marine, glacial and interglacial sedimentation conditions. The research objective is to identify the persistent features characterising the conditions of sedimentation and relief formation using the Nadym River basin as an example. The be

APA, Harvard, Vancouver, ISO, and other styles

41

Ludwikowska-Kędzia, Małgorzata, Halina Pawelec, and Grzegorz Adamiec. "Sedimentological interpretation and stratigraphical position of glacigenic deposits in the Napęków area (Holy Cross Mountains, Poland)." Geologos 21, no. 4 (2015): 261–84. http://dx.doi.org/10.1515/logos-2015-0018.

Full text

Abstract:

AbstractThe identification of depositional conditions and stratigraphical position of glacigenic deposits in the Napęków area is important for the genetic and stratigraphical interpretation of Quaternary deposits in the central part of the Holy Cross Mountains, as well as for a revision of the course and extent of Middle Polish (Saalian) glaciations. These deposits comprise a series of diamictons which occur between sandy-gravelly deposits. Based on results of macro- and microscopic sedimentological investigations, analysis of heavy mineral composition, roundness and frosting of quartz grains,

APA, Harvard, Vancouver, ISO, and other styles

42

Dauvillier, A. "Note sur la liaison continentale Amérique du Sud-Antarctique." Cahiers de géographie du Québec 17, no. 41 (2005): 339–42. http://dx.doi.org/10.7202/021122ar.

Full text

APA, Harvard, Vancouver, ISO, and other styles

43

Bobrowsky, Peter, and Nathaniel W. Rutter. "The Quaternary Geologic History of the Canadian Rocky Mountains." Géographie physique et Quaternaire 46, no. 1 (2007): 5–50. http://dx.doi.org/10.7202/032887ar.

Full text

Abstract:

ABSTRACT The Canadian Rocky Mountains figured prominently during the glacial history of western Canada. First as a western limit or boundary to the Laurentide Ice Sheet, second as an eastern margin of the Cordilleran Ice Sheet, and finally as a centre of local Montane ice. Throughout the Quaternary, complex interactions of glacier ice from these three ice sources markedly changed the physical form of the Rocky Mountains, Trench and Foothills areas. Investigations into the Quaternary history of this region have been ongoing since the beginning of the last century. Since about 1950, the number o

APA, Harvard, Vancouver, ISO, and other styles

44

Shanahan, Timothy M., and Marek Zreda. "Chronology of Quaternary glaciations in East Africa." Earth and Planetary Science Letters 177, no. 1-2 (2000): 23–42. http://dx.doi.org/10.1016/s0012-821x(00)00029-7.

Full text

APA, Harvard, Vancouver, ISO, and other styles

45

Akcar, Naki. "Quaternary Glaciations at Uludag Mountain (NW Turkey)." Quaternary International 279-280 (November 2012): 13. http://dx.doi.org/10.1016/j.quaint.2012.07.051.

Full text

APA, Harvard, Vancouver, ISO, and other styles

46

Sarıkaya, Mehmet Akif, and Attila Çiner. "Late Quaternary glaciations in the eastern Mediterranean." Geological Society, London, Special Publications 433, no. 1 (2015): 289–305. http://dx.doi.org/10.1144/sp433.4.

Full text

APA, Harvard, Vancouver, ISO, and other styles

47

MANN, DANIEL H., RONALD S. SLETTEN, and RICHARD E. REANIER. "Quaternary glaciations of the Rongbuk Valley, Tibet." Journal of Quaternary Science 11, no. 4 (1996): 267–80. http://dx.doi.org/10.1002/(sici)1099-1417(199607/08)11:4<267::aid-jqs242>3.0.co;2-v.

Full text

APA, Harvard, Vancouver, ISO, and other styles

48

Veyret, Y. "Quaternary glaciations in the French Massif Central." Quaternary Science Reviews 5 (January 1986): 395–96. http://dx.doi.org/10.1016/0277-3791(86)90202-7.

Full text

APA, Harvard, Vancouver, ISO, and other styles

49

Bednarski, Jan. "Late Quaternary glacial and sea-level events, Clements Markham Inlet, northern Ellesmere Island, Arctic Canada." Canadian Journal of Earth Sciences 23, no. 9 (1986): 1343–55. http://dx.doi.org/10.1139/e86-129.

Full text

Abstract:

Clements Markham Inlet cuts into the Grant Land Mountains of the northernmost coast of Ellesmere Island. The head of the inlet is bounded on three sides by mountain ice caps that surround lowlands mantled by extensive raised marine deposits. Fieldwork and mapping of late Quaternary sediments were used to determine the limits of past glaciations and the nature of ice retreat from the inlet head. Forty-five radiocarbon dates on driftwood and marine shells provide a deglacial chronology and document related sea-level adjustments.High-level ice-marginal meltwater channels and mountain summit errat

APA, Harvard, Vancouver, ISO, and other styles

50

Broster, Bruce E., and John J. Clague. "Advance and retreat glacigenic deformation at Williams Lake, British Columbia." Canadian Journal of Earth Sciences 24, no. 7 (1987): 1421–30. http://dx.doi.org/10.1139/e87-134.

Full text

Abstract:

Glacigenic deformation structures at Williams Lake, British Columbia, occur within stratified Quaternary sediments that both overlie and underlie lodgement till of the last (Fraser = Late Wisconsinan) glaciation. The main structures in sediments below the lodgement till are faults, joints, and clastic dikes produced by glacier overriding during Late Wisconsinan time. The orientation of these structures is closely related to the direction of glacier flow at Williams Lake. Their character and stratigraphic position suggest that the substrate in this area was partly frozen and partly unfrozen whe

APA, Harvard, Vancouver, ISO, and other styles

We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!