Articles | Volume 5, issue 2
https://doi.org/10.5194/se-5-683-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/se-5-683-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
21 Jul 2014
Research article |
| 21 Jul 2014
Maskevarri Ráhppát in Finnmark, northern Norway – is it an earthquake-induced landform complex?
R. Sutinen
Geological Survey of Finland, P. O. Box 77, 96101 Rovaniemi, Finland
I. Aro
Geological Survey of Finland, P. O. Box 77, 96101 Rovaniemi, Finland
P. Närhi
Geological Survey of Finland, P. O. Box 77, 96101 Rovaniemi, Finland
M. Piekkari
Geological Survey of Finland, P. O. Box 77, 96101 Rovaniemi, Finland
M. Middleton
Geological Survey of Finland, P. O. Box 77, 96101 Rovaniemi, Finland
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Solid Earth, 14, 333–351, https://doi.org/10.5194/se-14-333-2023, https://doi.org/10.5194/se-14-333-2023, 2023
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We discuss collapse sinkholes occuring since 2004 on the sports field of Münsterdorf, a village north of Hamburg. The sinkholes, 2–5 m in size and about 3–5 m deep, develop in peri-glacial sand, with a likely origin in the Cretaceous chalk, present at about 20 m depth. The area has been analyzed with geophysical and direct-push-based methods, from which material properties of the subsurface have been derived. The properties have been used for mechanical models, predicting the subsidence.
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Solid Earth, 13, 1631–1647, https://doi.org/10.5194/se-13-1631-2022, https://doi.org/10.5194/se-13-1631-2022, 2022
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We studied the mobility and sedimentary characteristics of rock avalanches influenced by initial discontinuity sets with experimental methods. In the experiments, we set different initial configurations of blocks. The results revealed that the mobility and surface structures of the mass flows differed significantly. In the mass deposits, the block orientations were affected by their initial configurations and the motion processes of the mass flows.
Marianne Métois, Jean-Emmanuel Martelat, Jérémy Billant, Muriel Andreani, Javier Escartín, Frédérique Leclerc, and the ICAP team
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We use the Minerve virtual reality software to bring undergraduate students to an unusual field trip at 1200 m below sea level in the Lesser Antilles area. This region is located above an active subduction zone responsible for intense volcanic and seismic activity. In particular, we focus on the Roseau submarine fault that ruptured during the Mw 6.3 Les Saintes earthquake and presented a fresh scarp that the students can analyze and map in VR. They compile their results in a GIS project.
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François Clapuyt, Veerle Vanacker, Marcus Christl, Kristof Van Oost, and Fritz Schlunegger
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Using state-of-the-art geomorphic techniques, we quantified a 2-order of magnitude discrepancy between annual, decadal, and millennial sediment fluxes of a landslide-affected mountainous river catchment in the Swiss Alps. Our results illustrate that the impact of a single sediment pulse is strongly attenuated at larger spatial and temporal scales by sediment transport. The accumulation of multiple sediment pulses has rather a measurable impact on the regional pattern of sediment fluxes.
Robert A. Watson, Eoghan P. Holohan, Djamil Al-Halbouni, Leila Saberi, Ali Sawarieh, Damien Closson, Hussam Alrshdan, Najib Abou Karaki, Christian Siebert, Thomas R. Walter, and Torsten Dahm
Solid Earth, 10, 1451–1468, https://doi.org/10.5194/se-10-1451-2019, https://doi.org/10.5194/se-10-1451-2019, 2019
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The fall of the Dead Sea level since the 1960s has provoked the formation of over 6000 sinkholes, a major hazard to local economy and infrastructure. In this context, we study the evolution of subsidence phenomena at three area scales at the Dead Sea’s eastern shore from 1967–2017. Our results yield the most detailed insights to date into the spatio-temporal development of sinkholes and larger depressions (uvalas) in an evaporite karst setting and emphasize a link to the falling Dead Sea level.
Djamil Al-Halbouni, Eoghan P. Holohan, Abbas Taheri, Robert A. Watson, Ulrich Polom, Martin P. J. Schöpfer, Sacha Emam, and Torsten Dahm
Solid Earth, 10, 1219–1241, https://doi.org/10.5194/se-10-1219-2019, https://doi.org/10.5194/se-10-1219-2019, 2019
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A 2-D numerical modelling approach to simulate the mechanical formation of sinkhole cluster inside large-scale karstic depressions is presented. Different multiple cavity growth scenarios at depth are compared regarding the mechanical process and collapse style. The outcomes of the models are compared to results from remote sensing and geophysics for an active sinkhole area in the Dead Sea region.
Michael Hodge, Juliet Biggs, Åke Fagereng, Austin Elliott, Hassan Mdala, and Felix Mphepo
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Bruno Cagnoli and Antonio Piersanti
Solid Earth, 8, 177–188, https://doi.org/10.5194/se-8-177-2017, https://doi.org/10.5194/se-8-177-2017, 2017
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The purpose of our research is to understand the mechanisms that determine the mobility of granular flows of rock fragments. Since rock avalanches and pyroclastic flows are too dangerous to be studied at close range, we use numerical simulations and laboratory experiments. We focus on the fundamentals upon which new numerical models will be built to predict the behaviors of natural flows. These fundamentals include the effects of grain size, flow volume and channel width.
Alexis Nutz and Mathieu Schuster
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Enric Vázquez-Suñé, Miguel Ángel Marazuela, Violeta Velasco, Marc Diviu, Andrés Pérez-Estaún, and Joaquina Álvarez-Marrón
Solid Earth, 7, 1317–1329, https://doi.org/10.5194/se-7-1317-2016, https://doi.org/10.5194/se-7-1317-2016, 2016
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This study shows the need for a symbiotic relationship between government and research groups for efficient management of geologic data in urban environments. Through its implementation, both the city administration and private companies benefit from the feedback of geologic knowledge acquired during this process, thereby substantially reducing the cost of construction projects and facilitating the development of aquifer management plans.
Abdulvahed Khaledi Darvishan, Vafa Homayounfar, and Seyed Hamidreza Sadeghi
Solid Earth, 7, 1293–1302, https://doi.org/10.5194/se-7-1293-2016, https://doi.org/10.5194/se-7-1293-2016, 2016
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Different stages of soil removal, transfer, preparation and placement in laboratory plots cause significant changes in soil structure and, subsequently, the results of runoff, sediment concentration and soil loss. The increasing rates of runoff coefficient, sediment concentration and soil loss due to the study soil preparation method for laboratory soil erosion plots were 179, 183 and 1050 % (2.79, 2.83 and 11.50 times), respectively.
Jozef Gallik and Lenka Bolešová
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Technology is moving ahead very fast, and so researchers have new possibilities for their research. We tried to demonstrate benefits of using remote-sensing technology (Phantom 1 drone) such as its accuracy in the terrain, easy access to hardly accessible areas, and the possibility to collect data even during unfavourable weather conditions. The high mountainous environment provided us great conditions for testing the drone as a device for very easy and accurate mapping of natural phenomena.
Mohammad Hassan Sadeghravesh, Hassan Khosravi, and Soudeh Ghasemian
Solid Earth, 7, 673–683, https://doi.org/10.5194/se-7-673-2016, https://doi.org/10.5194/se-7-673-2016, 2016
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Select appropriate strategies according to all effective criteria in combating desertification process can be so useful in controlling and rehabilitation of degraded lands, and avoid degradation in vulnerable fields. This study provides systematic and optimal strategies of combating desertification by group decision-making model. To this end, in the framework of Multi Attribute Decision Making (MADM) and by using Delphi model (Delphi), the preferences of indexes were obtained.
Guang Jie Luo, Shi Jie Wang, Xiao Yong Bai, Xiu Ming Liu, and An Yun Cheng
Solid Earth, 7, 457–468, https://doi.org/10.5194/se-7-457-2016, https://doi.org/10.5194/se-7-457-2016, 2016
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For accurately reflecting the eco-hydrological process of the dual structure of the surface and subsurface, we propose a new method for the extraction of small watersheds in karst regions. In this study, we think that the minimum karst watershed has an exit at the corrosion–erosion datum, and the further karst sub-watershed division may cause an eco-hydrological fault. The watersheds delineated by our method accurately reflect the hydrological process in the Sancha River.
J. Rodrigo Comino, C. Brings, T. Lassu, T. Iserloh, J. M. Senciales, J. F. Martínez Murillo, J. D. Ruiz Sinoga, M. Seeger, and J. B. Ries
Solid Earth, 6, 823–837, https://doi.org/10.5194/se-6-823-2015, https://doi.org/10.5194/se-6-823-2015, 2015
M. Arian and Z. Aram
Solid Earth, 5, 1277–1291, https://doi.org/10.5194/se-5-1277-2014, https://doi.org/10.5194/se-5-1277-2014, 2014
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The Kermanshah area in the High Zagros, Iran (the collision of the Arabian and Eurasian plates) has been affected by four classes of tectonic variation. These regions were identified as very high, high, moderate and low relative tectonic activity by calculation and analysis of six geomorphic indices.
A. Gómez-Ortiz, M. Oliva, F. Salvador-Franch, M. Salvà-Catarineu, D. Palacios, J. J. de Sanjosé-Blasco, L. M. Tanarro-García, J. Galindo-Zaldívar, and C. Sanz de Galdeano
Solid Earth, 5, 979–993, https://doi.org/10.5194/se-5-979-2014, https://doi.org/10.5194/se-5-979-2014, 2014
M. Oliva, G. Vieira, P. Pina, P. Pereira, M. Neves, and M. C. Freitas
Solid Earth, 5, 901–914, https://doi.org/10.5194/se-5-901-2014, https://doi.org/10.5194/se-5-901-2014, 2014
Y. Liu, F. Métivier, J. Gaillardet, B. Ye, P. Meunier, C. Narteau, E. Lajeunesse, T. Han, and L. Malverti
Solid Earth, 2, 283–301, https://doi.org/10.5194/se-2-283-2011, https://doi.org/10.5194/se-2-283-2011, 2011
H. C. Ho
Solid Earth, 2, 155–158, https://doi.org/10.5194/se-2-155-2011, https://doi.org/10.5194/se-2-155-2011, 2011
A. Limare, M. Tal, M. D. Reitz, E. Lajeunesse, and F. Métivier
Solid Earth, 2, 143–154, https://doi.org/10.5194/se-2-143-2011, https://doi.org/10.5194/se-2-143-2011, 2011
Cited articles
Andersen, B. G., Mangerud, J., Sørensen, R., Reite, A., Sveian, H., Thoresen, M., and Bergström, B.: Younger Dryas ice-marginal deposits in Norway, Quaternary Int., 28, 147–169, 1995.
Arvidsson, R.: Fennoscandian earthquakes: whole crustal rupturing related to postglacial rebound, Science, 274, 744–746, 1996.
Banerjee, I. and McDonald, B. C.: Nature of esker sedimentation, Special Publications of the Society of Economic Paleontologists and Mineralogists, Tulsa, 23, 132–154, 1975.
Bennett, M. R., Huddard, D., Waller, R. I., Cassidy, N., Tomio, A., Zukowskyj, P., Midglet, G., Cook, S. J., Gonzales, S., and Glasser, N. F.: Sedimentary and tectonic architecture of a large push moraine: a case study from Hagafellsjökull-Eystri, Iceland, Sediment. Geol., 172, 269–292, 2004.
Blikra, L. H. and Christiansen, H. H.: A field-based model of permafrost-controlled rockslide deformation in northern Norway, Geomorphology, 208, 34–49, 2014.
Boulton, G. S., van der Meer, J. J. M., Beets, D. J., Hart, J. K., and Ruegg, G. H. J.: The sedimentary and structural evolution of a recent push moraine complex: Holmstrømbreen, Spitsbergen, Quaternary Sci. Rev., 18, 339–371, 1999.
Bøe, R., Longva, O., Lepland, A., Blikra, L. H., Sønstegaard, E., Haflidason, H., Bryn, P., and Lien, R.: Postglacial mass movements and their causes in flords and lakes in western Norway, Norw. J. Geol., 84, 35–55, 2004.
Brandes, C., Winseman, J., Roskosch, J., Meinsen, J., Tanner, D. C., Frechen, M., Steffen, H., and Wu, P.: Activity along the Osning Thrust in Central Europe during the Lateglacial: ice-sheet and lithosphere interactions, Quaternary Sci. Rev., 38, 49–62, 2012.
Brandes, C. and Winsemann, J.: Soft-sediment deformation structures in NW germany caused by late Pleistocene seismicity, Int. J. Earth Sci., 102, 2255–2274, https://doi.org/10.1007/s00531-013-0914-4, 2013.
Clark, P. U. and Walder, J. S.: Subglacial drainage, eskers, and deforming beds beneath the Laurentide and Eurasian ice sheets, Geol. Soc. Am. Bull., 106, 304–314, 1994.
Dehls, J. F., Olesen, O., Olsen, L., and Blikra, L. H.: Neotectonic faulting in northern Norway, the Stuoragurra and Nordmannvikdalen faults, Quaternary Sci. Rev., 19, 1447–1460, 2000.
Ekström, G. Nettles, M., and Tsai, V. C.: Seasonality and increasing frequency of Greenland glacial earthquakes, Science, 311, 1756–1758, 2006.
Evans, J. A., Young, N. J. P., and ÓCofaigh, C.: Glacial geomorphology of terrestrial-terminating fast flow lobes/ice stream margins in the southwest Laurentide Ice Sheet, Geomorphology, 204, 86–113, 2014.
Friedman, S. P.: Soil properties influencing apparent electrical conductivity; a review, Comput. Electron. Agr., 46, 45–70, 2005.
Grachev, A. M. and Severinghaus, J. P.: A revised +10 ± 4 °C magnitude of the abrupt change in Greenland temperature at the Younger Dryas termination using published GISP2 gas isotope data and air thermal diffusion constants, Quaternary Sci. Rev., 24, 513–519, 2005.
Graham, D. J. and Midgley, N. G.: Moraine mound formation by englacial thrusting: the Younger Dryas moraines of Cwm Idwal, North Wales, in: Deformation of Glacial materials, edited by: Maltman, A. J., Hubbard, B., and Hambrey, M. J., Geological Society, London, Spec. Publ., 176, 321–336, 2000.
Grunblatt, J. and Atwood, D.: Mapping lakes for winter liquid water availability using SAR on the North Slope of Alaska, Int. J. Appl. Earth Obs., 27, 63–69, 2014.
Hoppe, G.: Hummocky moraine regions with special reference to the interior of Norrbotten, Geogr. Ann., 34, 1–72, 1952.
Jakobsson, M., Björk, S., O'Regan, M., Flodén, T., Greenwood, S. L., Swärd, H., Lif, A., Ampel, L., Koyi, H., and Skelton, A.: Major earthquake at the Pleistocene-Holocene transition in Lake Vättern, southern Sweden, Geology, 42, 379–382, https://doi.org/10.1130/G35499.1, 2014.
Johnson, M., Benediktsson, Í.Ö., and Björklund, L.: The Ledsjö end moraine – a subaquatic push moraine composed of glaciomarine clay in central Sweden, P. Geologist. Assoc., 124, 738–752, 2013.
Jones, B. M., Grosse, G., Hinkel, K. M., Arp, C. D., Walker, S., Beck, R. A., and Galloway, J. P.: Assessment of pingo distribution and morphometry using an IfSAR derived digital surface model, western Arctic Coastal Plain, Northern Alaska, Geomorphology, 138, 1–14, 2012.
Kujansuu, R.: Nuorista siirroksista Lapissa. Summary: Recent faults in Lapland, Geologi, 16, 30–36, 1964.
Kukkonen, I., Olesen, O., Ask, M. V. S., and PFDP Working Group: Postglacial faults in Fennoscandia: Targets for scientific drilling, GFF, 132, 71–81, 2010.
Lagerbäck, R.: Late Quaternary faulting and paleoseismicity in northern Fennoscandia with particular reference to the Landsjärv area, northern Sweden. Geol. För. i Stockholm Förh., 112, 333–354, 1990.
Lagerbäck, R. and Sundh, M.: Early Hololocene faulting and paleoseismicity in northern Sweden, Sver. Geol. Unders., C836, 80 pp., 2008.
Lilleøren, K. S., Etzelmüller, B., Schuler, T. V., Gisnås, K., and Humlum, O.: The relative age of mountain permafrost – estimation of Holocene permafrost limits in Norway, Global Planet. Change, 92–93, 209–223, 2012.
Lund, B.: Effects of deglaciation on the crustal stress field and implications for endglacial faulting: A parametric study of simple Earth and ice models, SKBF/KBS Technical Report 05-04, Swedish Nuclear Fuel and Waste Management Co, Stockholm, 68 pp., 2005.
Lund, B., Schmidt, P., and Hieronymus, C.: Stress evolution and fault stability during the Weichselian glacial cycle, SKBF/KBS Technical Report 09-15, Swedish Nuclear Fuel and Waste Management Co, Stockholm, 106 pp., 2009.
Lundqvist, J.: The Younger Dryas Ice-Marginal Zone in Sweden, Quaternary Int., 28, 171–176, 1995.
Lundqvist, J. and Lagerbäck, R.: The Pärve Fault: A late-glacial fault in the Precambrian of Swedish Lapland, Geol. För. i Stockholm Förh., 98, 45–51, 1976.
Morgenstern, A., Ulrich, M., Günther, F., Roesslr, S., Fedorova, I. V., Rudaya, N. A., Wettrrich, S., Boike, J., and Schirrmaister, L.: Evolution of thermokarst in East Siberian ice-rich permafrost: A case study, Geomorphology, 201, 262–379, 2013.
Nettles, M. and Ekström, G.: Glacial earthquakes in Greenland and Antarctica, Annu. Rev. Earth Pl. Sc., 38, 467–491, 2010.
Neuzil, C. E.: Hydromechanical effects of continental glaciations on groundwater system, Geofluids, 12, 22–37, 2012.
Nordkalott Project: Geological map, Northern Fennoscandia, 1.1 mill. Geological Surveys of Finland, Norway and Sweden, 1986.
Norton, K. P. and Hampel, A.: Postglacial rebound promotes glacial re-advances – a case study from the European Alps, Terra Nova, 22, 297–302, 2010.
Olesen, O., Blikra, L. H., Braathen, A., Dehls, J. F., Olsen, L., Rise, L., Roberts, D., Riis, F., Faleide, J. I., and Anda, E.: Neotectonic deformation in Norway and its implications: a review, Norw. J. Geol., 84, 3–34, 2004.
Olsen, L., Riiber, A., and Sørensen, K.: Finnmark County, Map of Quaternary Geology, scale 1 : 500,000 with description, Geol. Surv. Norway, 1996.
Ottesen, D., Stokes, C. R., Rise, L., and Olsen, L.: Ice-sheet dynamics and ice streaming along the coastal parts of the northern Norway, Quaternary Sci. Rev., 27, 922–940, 2008.
Peteet, D. M.: Younger Dryas, in: Encyclopedia of Paleoclimatolgy and Ancient Environments, edited by: Gornitz, V., Encyclopedia of Earth Sciences Series, Springer, 993–996, 2009.
Rampton, V. N.: Large-scale effects of subglacial meltwater flow in the southern Slave Province, Northwest Territories, Canada, Can. J. Earth Sci., 37, 81–93, 2000.
Renssen, H. and Isarin, R. F. B.: The two major warming phases of the last deglaciation at 14.7 and 11.5 ka cal BP in Europe: climatic reconstructions and AGCM experiments, Global Planet. Change, 30, 117–153, 2001.
Roberts, D., Olesen, O., and Karpuz, M. R.: Seismo- and neotectonics in Finnmark, Kola Peninsula and the southern Barents Sea. Part 1. Geological and neotectonic framework, Tectonophysics, 270, 1–13, 1997.
Seppälä, M.: Synthesis of studies of palsa formation underlining the importance of local environmental and physical characteristics, Quaternary Res., 75, 366–370, 2011.
Smith, C. A., Sundh, M., and Mikko, H.: Surficial geology indicates early Holocene faulting and seismicity, central Sweden, Int. J. Earth Sci., in preparation, 2014.
Sollid, J. L. and Sorbel, L.: Influence of temperature conditions in formation of end moraines Fennoscandia and Svalbard, Boreas 17, 553–558, 1988.
Sollid, J. L., Andersen, S., Hamre, N., Kjeldsen, O., Salviksen, O., Sturød, S., Tveitå, T., and Wilhelmsen, A.: Deglaciation of Finmark, North Norway, Norsk Geografisk Tidsskrift, 27, 233–325, 1973.
Stewart, I. S., Sauber, J., and Rose, J.: Glacio-seismotectonics, ice sheets, crustal deformation and seismicity, Quaternary Sci. Rev., 19, 1367–1389, 2000.
Sutinen, R., Piekkari, M., and Middleton, M.: Glacial geomorphology in Utsjoki, Finnish Lapland proposes Younger Dryas fault-instability, Global Planet. Change, 69, 16–28, 2009a.
Sutinen, R., Middleton, M., Liwata, P., Piekkari, M., and Hyvönen, E.: Sediment anisotropy coincides with moraine ridge trend in south-central Finnish Lapland, Boreas, 38, 638–646, 2009b.
Sutinen, R., Jakonen, M., Piekkari, M., Haavikko, P., Närhi, P. and Middleton, M.: Electrical-sedimentary anisotropy of Rogen moraine, Lake Rogen area, Sweden, Sediment. Geol., 232, 181–189, 2010a.
Sutinen, R., Hyvönen, E., Närhi, P., Haavikko, P., Piekkari, M., and Middleton, M.: Sedimentary anisotropy diverges from flute trends in south-east Finnish Lapland, Sediment. Geol., 232, 190–197, 2010b.
Sutinen, R., Hyvönen, E., and Kukkonen, I.: LiDAR detection of paleolandslides in the vicinity of the Suasselkä postglacial fault, Finnish Lapland, Int. J. Appl. Earth Obs., 27, 91–99, 2014a.
Sutinen, R., Hyvönen, E., Middleton, M., and Ruskeeniemi, T.: Airborne LiDAR detection of postglacial faults and Pulju moraine in Palojärvi, Finnish Lapland, Global Planet. Change, 115, 24–32, 2014b.
Svendsen, J. I., Astakhov, V. I., Bolshiyanov, D. Yu., Demidov, I., Dowdeswell, J. A., Gataullin, V., Hjort, C., Hubberten, H. W., Larsen, E., Mangerud, J., Melles, M., Möller, P., Saarnisto, M., and Siegert, M. J.: Maximum extent of the Eurasian ice sheets in the Barents and Kara Sea region during the Weichselian, Boreas, 28, 234–242, 1999.
Tabuchi, H. and Seppälä, M.: Surface temperature inversion in the palsa and pounu fields of northern Finland, Polar Sci., 6, 237–251, 2012.
Tanner, V.: Studier over kvartärsystemet i Fennoskandias nordliga delar IV. Bulletin de la commission Géologique de Finlande, 88, 594 pp., 1930.
Taylor, R. W. and Fleming, A. H.: Characterizing jointed systems by azhimuthal resistivity surveys, Ground Water, 26, 464–474, 1988.
Utting, D. J., Ward, B. C., and Little, E. C.: Genesis of hummocks in glaciofluvial corridors near the Keewatin Ice Divide, Canada, Boreas, 38, 471–481, 2009.
Vorren, T. and Plassen, L.: Deglaciation and palaeoclimate of the Andflord-Vågsfjord area, North Norway, Boreas, 31, 97–125, 2002.
West, M. E., Larsen, C. F., Truffer, M., O'Neel, S., and LeBlanc, L.: Glacier microseismicity, Geology, 38, 319–322, 2010.
Wetterich, S., Grosse, G., Schirrmeister, L., Andreev, A. A., Bobrov, A. A., Kienast, F., Bigelow, N. H., and Edwards, M. E.: Late Quaternary environmental and landscape dynamics revealed by a pingo sequence on the northern Seward Peninsula, Alaska, Quaternary Sci. Rev., 39, 26–44, 2012.
Wu, P., Johnston, P., and Lambeck, K.: Postglacial rebound and fault instability in Fennoscandia, Geophys. J. Int., 139, 657–670, 1999.
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