DOCSLIB.ORG

Geomorphic Origin of a Lithalsa in the Great Slave Lowlands, Northwest Territories, Canada

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Geomorphic Origin of a Lithalsa in the Great Slave Lowlands, Northwest Territories, Canada Geomorphic origin of a lithalsa in the Great Slave Lowlands, Northwest Territories, Canada by Adrian J.R. Gaanderse A thesis submitted to the Faculty of Graduate and Postdoctoral Affairs in partial fulfillment of the requirements for the degree of Master of Science in Geography Carleton University Ottawa, Ontario © 2015, Adrian J.R. Gaanderse ii Abstract Lithalsas, mineral-based permafrost mounds with segregated ice in their cores, are found in the Great Slave Lowlands, Northwest Territories. They are formed in glaciolacustrine deposits of Glacial Lake McConnell and ancestral Great Slave Lake left as water levels receded during the Holocene to the present level of Great Slave Lake. Ground ice conditions were examined in one 700-m long lithalsa adjacent to Highway 3, 30 km west of Yellowknife. Samples obtained to depths of 8.4 m from 17 boreholes revealed domed layers of silts, sands, and clays in the lithalsa, with related layers appearing horizontally beneath an adjacent peatland. Segregated ice lenses over 0.1 m thick occurred in clays below 4 m depth. δ18O values of lithalsa ice indicate modern water sources for the ground ice. The ages of organic material recovered from the lithalsa imply permafrost aggradation initiated growth of the feature within the last 700 to 400 years. iii Acknowledgements I would firstly like to thank Steve Wolfe for his infectious enthusiasm for scientific research, as well as his continuous encouragement and confidence in me. It was deeply appreciated both in the field and throughout the writing process in Ottawa. Fieldwork would also not have been the same without our annual pike fishing excursions. Thanks Steve. Chris Burn’s constant support and attention to detail at Carleton University for the past four years is greatly valued. I’ve become a better writer, presenter and critical thinker because of his efforts. Thanks Chris. I’d like to also thank Steve Kokelj and Peter Morse for their contributions during lab analysis and writing. My field assistants Mark Ednie, Brendan O’Neill and Chris Stevens went the extra mile for me in Yellowknife. Thank you guys for all of your efforts. My long-standing friends from Ottawa, as well as new ones I had the pleasure of meeting at school along the way, were always ready to listen to my ups and downs throughout this degree, and I thank them for all of their support. Rachel Plewes assisted with some statistical portions of this thesis, and I thank her for her help. Finally, my parents and family have always been behind me no matter what I do in life, and this degree has been no different. Thank you for everything you’ve done to get me to where I am now. iv Table of Contents Abstract ............................................................................................................................... ii Acknowledgements ............................................................................................................ iii Table of Contents ............................................................................................................... iv List of Tables ..................................................................................................................... ix List of Figures ..................................................................................................................... x List of Appendices ........................................................................................................... xvi Chapter 1 Overview and objectives ............................................................................. 1 1.1 Introduction ......................................................................................................................... 1 1.2 Palsas and lithalsas ............................................................................................................. 2 1.3 Field area ............................................................................................................................. 3 1.4 Research objectives and hypotheses .................................................................................. 6 1.5 Thesis structure ................................................................................................................... 8 Chapter 2 Background.................................................................................................. 9 2.1 Water migration and ice segregation ................................................................................ 9 2.1.1 Darcy’s Law ................................................................................................................... 9 2.1.2 Cryosuction .................................................................................................................... 9 2.1.3 Water migration and unfrozen water content ............................................................... 10 2.1.4 Ice segregation ............................................................................................................. 12 2.1.5 Frost heave ................................................................................................................... 13 2.2 Palsas .................................................................................................................................. 13 2.2.1 Introduction .................................................................................................................. 13 2.2.2 Size and growth rate .................................................................................................... 14 2.2.3 Climatic conditions for development ........................................................................... 14 v 2.2.4 Thermal and nival offsets ............................................................................................ 15 2.2.5 Life cycle ..................................................................................................................... 16 2.3 Lithalsas ............................................................................................................................. 18 2.3.1 Introduction .................................................................................................................. 18 2.3.2 Regional and climatic settings for development .......................................................... 19 2.3.3 Development in mineral sediments .............................................................................. 19 2.3.4 Isotopic values within a lithalsa ................................................................................... 21 2.3.5 The potential development of a lithalsa from a palsa .................................................. 21 2.3.6 Internal composition .................................................................................................... 22 2.3.7 Degradation .................................................................................................................. 24 2.3.8 A criticism of aeolian erosion theory ........................................................................... 26 2.4 Palsas, lithalsas, and climate change ............................................................................... 27 2.5 Palsa and lithalsa age ........................................................................................................ 28 2.6 Potential for lithalsas near Yellowknife .......................................................................... 29 2.7 Stable isotopes as an indicator of ice lens water sources ............................................... 30 Chapter 3 Study region and methods ........................................................................ 33 3.1 Study area .......................................................................................................................... 33 3.1.1 Regional context .......................................................................................................... 33 3.1.2 Glacial Lake McConnell and Great Slave Lake .......................................................... 33 3.1.3 Climate ......................................................................................................................... 34 3.1.4 Permafrost conditions .................................................................................................. 35 3.1.5 Boundary Creek Study Area ........................................................................................ 36 3.1.6 Electrical resistivity ..................................................................................................... 40 3.2 Field methods ..................................................................................................................... 40 3.2.1 Creating a transect ....................................................................................................... 40 vi 3.2.2 Site descriptions ........................................................................................................... 42 3.2.3 Vegetation surveys ....................................................................................................... 42 3.2.4 The active layer ............................................................................................................ 42 3.2.5 Determining depth to bedrock ..................................................................................... 45 3.2.6 Boreholes ....................................................................................................................
Load more

Recommended publications
  • MG17 3 2010 Complete.Pdf 16363KB 26 May 2018
    MERCIAN Geologist VOLUME 17 PART 3 AUGUST 2010 East Midlands Geological Society Contents President Vice-President Mercian News 142 Tim Colman John Travis Geobrowser 143 The Record 146 Secretary Treasurer From the Archives 147 Janet Slatter Colin Bagshaw David G. Bate 149 Editorial Board Sir Henry Thomas de la Beche Tony Waltham Andy Howard and the founding of the British Geological Survey John Carney Tony Morris John N. Carney 166 Alan Filmer Gerry Slavin Magma mixing in the South Leicestershire Diorite: Council evidence from an Ordovician pluton at Croft Quarry Keith Ambrose Duncan Short Tim Colman 173 David Bate Gerry Slavin Gold in Britain: past , present and future Paul Guion Ian Sutton Stephen Gurney, Timothy Astin, Geoffrey Griffi ths 181 Richard Hamblin Neil Turner Origin and structure of Devensian depressions Sue Miles Geoff Warrington at Letton, Herefordshire Gerry Shaw Albert Horton 185 Correspondence Building stones of St Mary’s Church Society Secretary, 100 Main Street, at Colston Bassett, Nottinghamshire Long Whatton, Loughborough LE12 5DG Helen Boynton and Trevor Ford 195 01509 843297 [email protected] William W. Watts, pioneer Midlands geologist Mercian Geologist Editor, Reports 11 Selby Road, Nottingham NG2 7BP 0115 981 3833 [email protected] Members’ Evening, 2010: Shetland: John Aram 203 Mercian Geologist is printed by John Browns; Golcona Mine: John Jones 205 and published by the East Midlands Geological Society. James Hutton: Gerard Slavin, Gerry Shaw, Brenda Slavin 207 No part of this publication may be reproduced in printed or electronic form without prior consent of the Society. Charnian fossils: Helen Boynton 210 ISSN 0025 990X Wave Rock, Australia: Alan Filmer 211 © 2010 East Midlands Geological Society Registered Charity No.
    [Show full text]
  • Alphabetical Glossary of Geomorphology
    International Association of Geomorphologists Association Internationale des Géomorphologues ALPHABETICAL GLOSSARY OF GEOMORPHOLOGY Version 1.0 Prepared for the IAG by Andrew Goudie, July 2014 Suggestions for corrections and additions should be sent to [email protected] Abime A vertical shaft in karstic (limestone) areas Ablation The wasting and removal of material from a rock surface by weathering and erosion, or more specifically from a glacier surface by melting, erosion or calving Ablation till Glacial debris deposited when a glacier melts away Abrasion The mechanical wearing down, scraping, or grinding away of a rock surface by friction, ensuing from collision between particles during their transport in wind, ice, running water, waves or gravity. It is sometimes termed corrosion Abrasion notch An elongated cliff-base hollow (typically 1-2 m high and up to 3m recessed) cut out by abrasion, usually where breaking waves are armed with rock fragments Abrasion platform A smooth, seaward-sloping surface formed by abrasion, extending across a rocky shore and often continuing below low tide level as a broad, very gently sloping surface (plain of marine erosion) formed by long-continued abrasion Abrasion ramp A smooth, seaward-sloping segment formed by abrasion on a rocky shore, usually a few meters wide, close to the cliff base Abyss Either a deep part of the ocean or a ravine or deep gorge Abyssal hill A small hill that rises from the floor of an abyssal plain. They are the most abundant geomorphic structures on the planet Earth, covering more than 30% of the ocean floors Abyssal plain An underwater plain on the deep ocean floor, usually found at depths between 3000 and 6000 m.
    [Show full text]
  • New Ground Ice Maps for Canada Using a Paleogeographic Modelling Approach
    New ground ice maps for Canada using a paleogeographic modelling approach 5 H. Brendan O’Neill1, Stephen A. Wolfe1, Caroline Duchesne1 1Geological Survey of Canada, Natural Resources Canada, 601 Booth St. Ottawa, Canada Correspondence to: H. Brendan O’Neill: [email protected] The works published in this journal are distributed under the Creative Commons Attribution 4.0 License. This licence does not affect the Crown copyright work, which is re-usable under the Open Government Licence (OGL). The Creative Commons 10 Attribution 4.0 License and the OGL are interoperable and do not conflict with, reduce or limit each other. © Her Majesty the Queen in Right of Canada, as represented by the Minister of Natural Resources, 2018 1 Abstract Ground ice melt caused by climate-induced permafrost degradation may trigger significant ecological change, damage infrastructure, and alter biogeochemical cycles. The fundamental ground ice mapping for Canada is now >20 years old, and does not include significant new insights gained from recent field and remote sensing based studies. New modelling 5 incorporating paleogeography is presented in this paper to depict the distribution of three ground ice types (massive ice and icy sediments, segregated ice, and wedge ice) in northern Canada. The modelling uses an expert-system approach in a geographic information system (GIS), founded in conceptual principles gained from empirically-based research, to predict ground ice abundance in near-surface permafrost. Datasets of surficial geology, deglaciation, paleovegetation, glacial lake and marine limits, and modern permafrost distribution allow representations in the models of paleoclimatic shifts, tree line 10 migration, marine and glacial lake inundation, and terrestrial emergence, and their effect on ground ice abundance.
    [Show full text]
  • Palsas and Lithalsas
    Published in : Treatise on Geomorphology (2013), vol. 8, pp. 223–237 DOI: http://dx.doi.org/10.1016/B978-0-12-374739-6.00210-4 Status : Postprint (Author’s version) PALSAS AND LITHALSAS GLOSSARY Active layer: The top layer of ground subject to annual thawing and freezing in areas underlain by permafrost (Glossary of permafrost and related ground-ice terms, Technical memorandum, 142, National Research Council, Canada (1988)). Aggradational ice: Segregation ice formed in the lower part of the active layer and incorporated into the permafrost. Cryogenic structures: Distinct soil micromorphology resulting from the effects of freezing and mainly from the formation of segregation ice in the ground. Cryosuction: A suction of water in the ground to the freezing front in fine-grained material. Frost thrusting: Lateral movement of mineral soil in relation to freezing of water in the soil. Gelifluction: The slow downslope flow of unfrozen earth materials on a frozen substrate. Little ice age: A period of cooling and glacier expansion that covers a period extending from the sixteenth to the nineteenth centuries. Mud boils or frost boils: Small mounds of soil material formed by frost action and corresponding in section to cryoturbations. ABSTRACT Palsas and Iithalsas are mounds that contain lenses of segregation ice. They are islands of permafrost. These two kinds of mounds are very similar in shape, size, and origin. However, the palsas have a cover of peat which does not exist in Iithalsas. The formation of ice in the core of these mounds requires material in which capillary water undergoes slow freezing. The remnants of Iithalsas are depressions surrounded by ramparts, which does not exist after the melting of palsas.
    [Show full text]
  • Features Caused by Ground Ice Growth And
    Features caused by ground ice growth and decay in Late Pleistocene fluvial deposits, Paris Basin, France Pascal Bertran, Eric Andrieux, Mark Bateman, Marianne Font, Kevin Manchuel, Déborah Sicilia To cite this version: Pascal Bertran, Eric Andrieux, Mark Bateman, Marianne Font, Kevin Manchuel, et al.. Features caused by ground ice growth and decay in Late Pleistocene fluvial deposits, Paris Basin, France. Geomorphology, Elsevier, 2018, 310, pp.84 - 101. 10.1016/j.geomorph.2018.03.011. hal-01774864 HAL Id: hal-01774864 https://hal-normandie-univ.archives-ouvertes.fr/hal-01774864 Submitted on 17 Jul 2018 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Features caused by ground ice growth and decay in Late Pleistocene fluvial deposits, Paris Basin, France a,b,⁎ b,c c d e e Pascal Bertran , Eric Andrieux ,Mark Bateman , Marianne Font , Kevin Manchuel , Deborah Sicilia a Inrap, 140 avenue du Maréchal Leclerc, 33130 Bègles, France b PACEA, bâtiment B18, allée Geoffroy-Saint-Hilaire, 33615 Pessac, France c Geography Department, University of Sheffield, Winter Street, Sheffield S10 2TN, UK d M2C, UMR CNRS 6143, 24 rue des Tilleuls, 14000 Caen, France e EDF, TEGG/Service Géologique Géotechnique, 905 Avenue du Camp de Menthe, 13097 Aix-en-Provence, France 1.
    [Show full text]
  • The Shaping of the Arctic (Modified for Adeed)
    THE SHAPING OF THE ARCTIC (MODIFIED FOR ADEED) Overview: Permafrost is the foundation of the Arctic landscape. Students will study landscape features and the basic processes by which they are formed. Objectives: The student will: • view images of and identify common permafrost landscape features; • explain how common permafrost landscape features are formed; and • make a model of permafrost landscape features and share with classmates. Targeted Alaska Grade Level Expectations: [9] SA1.1 The student develops an understanding of the processes of science by asking questions, predicting, observing, describing, measuring, classifying, making generalizations, inferring, and communicating. [10] SA1.1 The student develops an understanding of the processes of science by asking questions, predicting, observing, describing, measuring, classifying, making generalizations, analyzing data, developing models, inferring, and communicating. [9] SD1.2 The student demonstrates an understanding of geochemical cycles by applying knowledge of the water cycle to explain changes in the Earth’s surface. [10] SD1.2 The student demonstrates an understanding of geochemical cycles by describing their interrelationships (i.e., water cycle, carbon cycle, oxygen cycle). Vocabulary: active layer – the layer of ground that is subject to annual thawing and freezing in areas underlain by permafrost beaded stream – a stream characterized by narrow reaches linking pools or small lakes continuous permafrost – permafrost occurring everywhere beneath an exposed land surface;
    [Show full text]
  • Chapter 6. Permafrost and Climate Change in Nunavik and Nunatsiavut: Importance for Municipal and Transportation Infrastructures
    Chapter 6. Permafrost and climate change in Nunavik and Nunatsiavut: Importance for municipal and transportation infrastructures Lead authors Michel Allard, Mickaël Lemay, Carl Barrette, Emmanuel L’Hérault, Denis Sarrazin Centre d’études nordiques (CEN), ArcticNet, Université Laval, Québec, QC Contributing authors T. Bell, and G. Doré Abstract Permafrost degradation is seriously affecting the natural environment. The landscape is changing through thermokarst that takes place mostly in the discontinuous permafrost zone and through thicker active layer depth and more frequent slope processes in the continuous zone. Northern residents are affected as vegeta- tion, water bodies and soil drainage are greatly modified, which has an impact on resources traditionally available for humans. The modern built environment is also affected. Transportation infrastructure is being studied and adaptive solutions are sought, applied and tested. To protect and optimize the major invest- ments required for extensive housing and construction, the urban planning of communities calls upon better permafrost maps and prediction of permafrost behavior. Final permafrost degradation around 0°C appears to be primarily under the influence of unfrozen water content and heat brought to the thawing interface by groundwater. This process is also effective in accelerating localized thawing under man-made infrastructures. Collection and organization of permafrost information in geographic information systems (GIS) allows for the integration of essential knowledge and provides a very useful tool for establishing situation diagnostics, sharing information with stakeholders and communities, and supporting multidisci- plinary decision making for land use planning. The principal adaptive measures lie in adapting foundation types to mapped permafrost conditions to ensure a prolonged service life of buildings.
    [Show full text]
  • Frozen Ground
    FROZEN GROUND The News Bulletin of the International Permafrost Association Number 25, December 2001 International Permafrost Association The International Permafrost Association, founded in 1983, has as its objectives fostering the dissemination of knowledge concerning permafrost and promoting cooperation among persons and national or international or- ganizations engaged in scientific investigation and engineering work on permafrost. Membership is through ad- hering national or multinational organizations or as individuals in countries where no Adhering Body exists. The IPA is governed by its officers and a Council consisting of representatives from 23 Adhering Bodies having inter- ests in some aspect of theoretical, basic and applied frozen ground research, including permafrost, seasonal frost, artificial freezing and periglacial phenomena. Committees, Working Groups, and Task Forces organize and coor- dinate research activities and special projects. The IPA became an Affiliated Organization of the International Union of Geological Sciences in July 1989. The Association’s primary responsibilities are convening International Permafrost Conferences and accomplishing special projects such as preparing maps, bibliographies, and glossaries. The first Conference was held in West Lafayette, Indiana, USA, 1963; the second in Yakutsk, Siberia, 1973; the third in Edmonton, Canada, 1978; the fourth in Fairbanks, Alaska, 1983; the fifth in Trondheim, Norway, 1988; the sixth in Beijing, China, 1993; and the seventh in Yellowknife, Canada, 1998. The eighth will be in Zurich, Switzerland in 2003. Field excursions are an integral part of each Conference, and are organized by the host country. Executive Committee 1998–2003 Council Members President Argentina Professor Hugh M. French, Canada Austria Vice Presidents Belgium Dr. Felix E. Are, Russia Professor Wilfried Haeberli, Switzerland Canada China Members Dr.
    [Show full text]
  • Vertical Movements of Frost Mounds in Sub-Arctic Permafrost Regions
    1 Vertical movements of frost mounds in sub-Arctic 2 permafrost regions analyzed using geodetic survey and 3 satellite interferometry 4 5 I.Beck 1,5 , R. Ludwig 2, M. Bernier 3, T. Strozzi 4 and J. Boike 1 6 7 [1]{Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Potsdam, 8 Germany} 9 [2] {Department of Geography, Ludwig-Maximilians University, Munich, Germany} 10 [3] {Centre Eau, Terre & Environnement, Institut national de la recherche scientifique, 11 Québec Canada} 12 [4]{GAMMA Remote Sensing Research and Consulting AG, Gümlingen, Switzerland} 13 [5]{ GIScience Research Group, Institute of Geography, Heidelberg University} 14 Correspondence to: I. Beck ([email protected]) 15 16 Abstract 17 Permafrost-affected soils cover about 450 – 45 % of Canada. The environment in such areas, 18 especially those located within the discontinuous permafrost zone, has been impacted more 19 than any other by recorded climatic changes. A number of changes, such as surface 20 subsidence and the degradation of frost mounds due to permafrost thawing have already been 21 observed at many locations. 22 We surveyed three frost mounds (lithalsas) in the sub-Arctic close to Umiujaq in, northern 23 Quebec , sub-Arctic , using a high-precision differential Global Positioning System (d-GPS) 24 technology during field visits in 2009, 2010 and 2011, thus obtaining detailed information on 25 their responses to the freezing and thawing that occurs during the course of the annual 26 temperature cycle. Seasonal pulsations were detected in the frost mounds and these responses 27 were shown to vary with the state of degradation and the land cover.
    [Show full text]
  • The Potential Lateral Growth of Lithalsas
    Published in : Quaternary Research (2011), vol. 75, pp. 371-377 DOI:10.1016/j.yqres.2011.01.001 Status : Postprint (Author’s version) THE POTENTIAL LATERAL GROWTH OF LITHALSAS Albert Pissart a, Fabrice Calmels b, Cécile Wastiaux a a Department of Geography, University of Liege, Liège, Belgium, b Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB T6G 2E3, Canada KEYWORDS: Lithalsa ; Hudson Bay ; Hautes-Fagnes ; Frost thrusting ABSTRACT The lithalsas in the Hudson Bay region of northern Quebec, Canada, are the closest modern analogs of ancient features that collapsed to form conspicuous circular depressions (“viviers”) common in the Hautes-Fagnes, a region in Belgium. Observations made in both regions are complementary and suggest that these mounds formed by frost heaving displacing soil not only upward, as previously assumed, but also laterally. This lateral displacement is consistent with diverse observations and inferences, which include (1) the simple rounded outline, either circular or oval, typical of both active and relic lithalsas; (2) evidence of local lateral extension inferred from exposures of the relic forms; (3) the relative inefficiency of solifluction in accumulating surface material to form the peripheral ramparts of remnant lithalsas due to the very gentle slopes of the mounds; and (4) the dip of ice lenses within a lithalsa in the Hudson Bay region, perhaps indicating that the freezing front dipped outward along its periphery. The growth of segregation ice is the primary driver for the vertical growth and lateral enlargement of a lithalsa. Published in : Quaternary Research (2011), vol. 75, pp. 371-377 DOI:10.1016/j.yqres.2011.01.001 Status : Postprint (Author’s version) Introduction The viviers of Hautes-Fagnes, Belgium, are perfectly preserved remnants of lithalsas (Pissart, 2000, 2003).
    [Show full text]
  • New Ground Ice Maps for Canada Using a Paleogeographic Modelling Approach
    The Cryosphere, 13, 753–773, 2019 https://doi.org/10.5194/tc-13-753-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. New ground ice maps for Canada using a paleogeographic modelling approach H. Brendan O’Neill, Stephen A. Wolfe, and Caroline Duchesne Geological Survey of Canada, Natural Resources Canada, 601 Booth St., Ottawa, Canada Correspondence: H. Brendan O’Neill ([email protected]) Received: 12 September 2018 – Discussion started: 20 September 2018 Revised: 29 January 2019 – Accepted: 1 February 2019 – Published: 5 March 2019 Abstract. Ground ice melt caused by climate-induced sults are generally comparable with the previous ground ice permafrost degradation may trigger significant ecological mapping for Canada. However, the model outputs are more change, damage infrastructure, and alter biogeochemical cy- spatially explicit and better reflect observed ground ice con- cles. The fundamental ground ice mapping for Canada is now ditions in many regions. Synthetic modelling products that > 20 years old and does not include significant new insights incorporated the previous ground ice information may there- gained from recent field- and remote-sensing-based studies. fore include inaccuracies. The presented modelling approach New modelling incorporating paleogeography is presented is a significant advance in permafrost mapping, but additional in this paper to depict the distribution of three ground ice field observations and volumetric ice estimates from more types (relict ice, segregated ice, and wedge ice) in northern areas in Canada are required to improve calibration and val- Canada. The modelling uses an expert-system approach in a idation of small-scale ground ice modelling.
    [Show full text]
  • Pingos, Palsas and Lithalsas: Comparison with the Martian Mounds
    Published in : Zeitschrift für Geomorphologie (2011), vol. 55, no 4, pp. 463–473 DOI:10.1127/0372-8854/2011/0051 Status : Postprint (Author’s version) Pingos, palsas and lithalsas: comparison with the Martian mounds Albert Pissart Professeur émérite à l’Université de Liège, 29, rue Lavaux, 4130 Esneux (Belgium). E-Mail: [email protected] KEYWORDS: Mars, pingos, lithalses, Canadian Arctic, Hautes-Fagnes. ABSTRACT On Mars, mounds similar to pingos were described for a long time. From the Canadian Arctic, some rare pingos which are neither of the Greenland type, nor of the Mackenzie type may be equivalent of some features on Mars. On the other hand, remnants of lithalsas looks very similar to “ring shaped features” described by de Pablo & Komatsu (2009) in the Utopia Basin. Published in : Zeitschrift für Geomorphologie (2011), vol. 55, no 4, pp. 463–473 DOI:10.1127/0372-8854/2011/0051 Status : Postprint (Author’s version) 1. Introduction The similarities between Martian mounds and pingos on Earth are so great that as soon as the first Viking images became available, it was proposed that pingos are present on Mars (see Rossbacher & Judson 1981). Now the periglacial origin of mounds on some parts of Mars seems largely accepted (de Pablo & Komatsu 2009, Burr et al. 2009). They have been compared extensively to periglacial mounds in the Arctic, starting more than 25 years ago (Lucchita 1981, Greeley 1985, Joens 1985, Witbeck & Underwood 1985). Recognizing periglacial mounds from satellite images is, however, a delicate matter. It is especially difficult on Mars images as we generally do not know the nature and structure of the substrate near the surface of this planet (de Pablo & Komatsu 2009).
    [Show full text]