Title

Application of the Handysurf E-35B electronic profilometer for the study of weathering micro-relief in glacier forelands in SE Iceland

Journal title

Acta Geologica Polonica

Yearbook

2015

Volume

vol. 65

Issue

No 3

Authors

Dąbski, Maciej

Divisions of PAS

Nauki o Ziemi

Publisher

Komitet Nauk Geologicznych PAN ; Wydział Geologii UW

Date

2015[2015.01.01 AD - 2015.12.31 AD]

Identifier

DOI: 10.1515/agp-2015-0018 ; ISSN 0001-5709

Source

Acta Geologica Polonica; 2015; vol. 65; No 3

References

Winkler (2005), The Schmidt hammer as a relative - age dating technique : potential and limitations of its application on Holocene moraines in Mt Cook National Park Southern Alps New Zealand, New Zealand Journal of Geology and Geophysics, 48, 105, doi.org/10.1080/00288306.2005.9515102 ; Dąbski (2013), Time - dependant surface deterioration of glacially abraded basaltic boulders deposited by Fláajökull SE Iceland, Jökull, 63, 55. ; Kirkbridge (2001), Can lichenometry be used to date the Little Ice Age Glacier Maximum in Iceland, Climatic Change, 48, 151, doi.org/10.1023/A:1005654503481 ; Dąbski (2014), Rock surface micro roughness Schmidt hammer rebound and weathering rind thickness within LIA Skálafellsjökull foreland SE Iceland, Polish Polar Research, 35, 99, doi.org/10.2478/popore-2014-0008 ; Landvik (1994), The last glaciations of Germanialand and adjacent areas northeast Greenland, Journal of Quaternary Science, 9, 81, doi.org/10.1002/jqs.3390090108 ; Dąbski (2010), A commentary to Asynchronous Little Ice Age glacial maximum extent in southeast Iceland by Chenetet al a case of Fláajökull, Geomorphology Geomorphology, 120, 114. ; Matthews (1984), The status of the Little Ice Age is southern Norway : Relative - age dating of Neoglacial moraines with Schmidt hammer and lichenometry, Boreas, 13, 333, doi.org/10.1111/j.1502-3885.1984.tb01128.x ; Porter (1975), Weathering rinds as a relative - age criterion : Application to subdivision of glacial deposits in the Cascad Range, Geology, 3, 101, doi.org/10.1130/0091-7613(1975)3<101:WRAARC>2.0.CO;2 ; Dąbski (2012), Determining rock surface micro - roughness and search for new method of relative dating of glacial landforms ; a case study from Fláajökull and Biferten glacier ( Swiss Alps ) forefields Landform, Analysis, 21, 3. ; McCarroll (1991), The age and origin of Neoglacial moraines in Jotunheimen southern Norway : new evidence from weathering - based data, Boreas, 20, 283, doi.org/10.1111/j.1502-3885.1991.tb00156.x ; Viles (2001), Scale issues in weathering studies, Geomorphology, 41, 63, doi.org/10.1016/S0169-555X(01)00104-0 ; Nesje (1990), : Autochtonous block fields in southern Norway : implications for the geometry thickness and isostatic loading of the late Weischelian Scandinavian ice sheet, Journal of Quaternary Science, 5, 225, doi.org/10.1002/jqs.3390050305 ; Dąbski (2005), Small - scale Sorted Nets on Glacial Till Fláajökull ( Southeast Iceland ) and Elisbreen ( Northwest Spitsbergen ) and, Permafrost Periglacial Processes, 16, 305, doi.org/10.1002/ppp.527 ; Viles (1998), Weathering nanomorphologies : their experimental production and use as indicators of carbonate stone decay and Hydrology, Quarterly Journal of Engineering Geology, 31, 347, doi.org/10.1144/GSL.QJEG.1998.031.P4.08. ; Yoshida (2011), Weathering rind formation in buried terrace cobbles during periods of up to ka, Applied Geochemistry, 26, 1706, doi.org/10.1016/j.apgeochem.2011.04.027 ; Sigurðsson (1998), Glacier variations in Iceland From the database of the Icelandic Glaciological Society, Jökull, 45, 3. ; Nicholson (2009), Holocene microweathering rates and processes on ice - eroded bedrock Røldal area Hardangervidda southern Norway In and Periglacial and Paraglacial Processes and Environments London Special Publications, Geological Society, 320, 29, doi.org/10.1144/SP320.3 ; Chinn (1981), Use of rock weathering - rind thickness for Holocene absolute age - dating in New Zealand, Arctic and Alpine Research, 13, 33, doi.org/10.2307/1550624 ; Chenet (2011), A response to the commentary of M Dąbski about the paper Asynchronous Little Ice Age glacial maximum extent in southeast Iceland, Geomorphology Geomorphology, 114, 253. ; Ives (1978), The maximum extent of Laurentide ice sheet along the east coast of North America during the last glaciation, Arctic, 31, 24, doi.org/10.14430/arctic2638 ; Shakesby (2006), : The Schmidt hammer as a relative - age dating tool and its potential for calibrated - age dating in Holocene glaciated environments, Quaternary Science Reviews, 25, 2846, doi.org/10.1016/j.quascirev.2006.07.011 ; Dąbski (2007), Testing the size - frequency - based lichenometric dating curve on Fláajökull moraines and quantifying lichen population dynamics with respect to stone surface aspect, Jökull, 57, 21. ; Chenet (2010), Asynchronous Little Ice Age glacial maximum extent in southeast Iceland, Geomorphology, 114, 253, doi.org/10.1016/j.geomorph.2009.07.012 ; Etienne (2002), The role of biological weathering in periglacial areas : a study of weathering rinds in south Iceland, Geomorphology, 47, 75, doi.org/10.1016/S0169-555X(02)00142-3 ; Bradwell (2006), The Little Ice Age glacier maximum in Iceland and the North Atlantic Oscillation : evidence from Lambatungnajökull southeast Iceland, Boreas, 35, 61, doi.org/10.1080/03009480500359202 ; Matthews (2011), Holocene Chemical Weathering Surface Lowering and Rock Weakening Rates on Glacially Eroded Bedrock Surfaces in an Alpine Periglacial Environment Jotunheimen Southern Norway Permafrost and Periglacial, Processes, 22, 279. ; Evans (1999), A comparison of the lichenometric and Schmidt hammer dating techniques based on data from the proglacial areas of some Icelandic glaciers, Quaternary Science Reviews, 18, 13, doi.org/10.1016/S0277-3791(98)00098-5 ; Owen (2007), Rates of Holocene chemical weathering Little Ice Age glacial erosion and implications for Schmidt - hammer dating at a glacier - foreland boundary Fåbergstølsbreen southern Norway The, Holocene, 17, 829, doi.org/10.1177/0959683607081419 ; Viles (2012), Microbial geomorphology : A neglected link between life and landscape, Geomorphology, 157. ; Dominguez (2006), Early formation of gnammas ( weathering pits ) in a recently glaciated are of Torres del Paine southern Patagonia ( Chile ), Geomorphology, 76, 137, doi.org/10.1016/j.geomorph.2005.10.006 ; Kirkbride (2012), Correlation of Late Quaternary moraines : impact of climate variability glacier response and chronological resolution, Quaternary Science Reviews, 46, 1, doi.org/10.1016/j.quascirev.2012.04.002 ; McCarroll (1996), Rock surface roughness as an indicator of degree of rock surface weathering Surface Processes and, Earth Landforms, 21, 963, doi.org/10.1002/(SICI)1096-9837(199610)21:10<963::AID-ESP643>3.0.CO;2-J ; Carroll (1974), Relative age dating techniques and a late Quaternary chronology Arikaree Cirque Colorado, Geology, 2, 321, doi.org/10.1130/0091-7613(1974)2<321:RADTAA>2.0.CO;2 ; Bradwell (2013), Recent very rapid retreat of a temperate glacier in SE Iceland, Boreas, 42, 959. ; McCarroll (1993), The vertical extend of ice sheets in Nordjord western Norway : measuring degree of rock surface weathering, Boreas, 22, 255, doi.org/10.1111/j.1502-3885.1993.tb00185.x