Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study

Research output: Chapter in Book/Report/Conference proceeding › Book chapter › Research › peer-review

Standard

Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study. / Klint, K E S; Richardt, N; Krüger, Johannes.

The Mýrdalsjökull Ice Cap, Iceland. Glacial Processes, Sediments and Landforms on an Active Volcano. ed. / A Schomacker; Johannes Krüger; Kurt H Kjær. Amsterdam and Oxford : Elsevier, 2010. p. 145-158 (Developments in Quaternary Sciences, Vol. 13).

Research output: Chapter in Book/Report/Conference proceeding › Book chapter › Research › peer-review

Harvard

Klint, KES, Richardt, N & Krüger, J 2010, Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study. in A Schomacker, J Krüger & KH Kjær (eds), The Mýrdalsjökull Ice Cap, Iceland. Glacial Processes, Sediments and Landforms on an Active Volcano. Elsevier, Amsterdam and Oxford, Developments in Quaternary Sciences, vol. 13, pp. 145-158. https://doi.org/10.1016/S1571-0866(09)01309-8

APA

Klint, K. E. S., Richardt, N., & Krüger, J. (2010). Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study. In A. Schomacker, J. Krüger, & K. H. Kjær (Eds.), The Mýrdalsjökull Ice Cap, Iceland. Glacial Processes, Sediments and Landforms on an Active Volcano (pp. 145-158). Elsevier. Developments in Quaternary Sciences Vol. 13 https://doi.org/10.1016/S1571-0866(09)01309-8

Vancouver

Klint KES, Richardt N, Krüger J. Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study. In Schomacker A, Krüger J, Kjær KH, editors, The Mýrdalsjökull Ice Cap, Iceland. Glacial Processes, Sediments and Landforms on an Active Volcano. Amsterdam and Oxford: Elsevier. 2010. p. 145-158. (Developments in Quaternary Sciences, Vol. 13). https://doi.org/10.1016/S1571-0866(09)01309-8

Author

Klint, K E S ; Richardt, N ; Krüger, Johannes. / Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study. The Mýrdalsjökull Ice Cap, Iceland. Glacial Processes, Sediments and Landforms on an Active Volcano. editor / A Schomacker ; Johannes Krüger ; Kurt H Kjær. Amsterdam and Oxford : Elsevier, 2010. pp. 145-158 (Developments in Quaternary Sciences, Vol. 13).

Bibtex

@inbook{d378aaecbdb849659b5ed6a32572f0b8,
title = "Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of K{\"o}tluj{\"o}kull, Iceland – A Case Study",
abstract = "A geological section, 70 m long and 3–4 m high, cut into dead-ice moraine in front of K{\"o}tluj{\"o}kull, has been described. Five-sediment associations were recognized representing (1) proglacial glacio-fluvial sedimentation, (2) deposition and deformation in ice-marginal environment, (3) subglacial deformation and deposition from dynamically active ice, (4) subglacial deposition from stagnant ice and (5) supraglacial re-deposition in dead-ice environment during de-icing. This complete sedimentary sequence represents a single glacier advance-stagnation cycle.The melt-out till displays moderate consolidation, moderate content of fines and angular clasts, and a very strong clast fabric. The lodgement/deformation till displays strong to very strong consolidation, relatively high content of fines, low content of angular clasts, and a weak to strong clast fabric. The occurrence of water-escape structures below the basal till and complete lack of brittle deformations in the lodgement/deformation till suggest water-saturated subglacial conditions during the advance of K{\"o}tluj{\"o}kull.",
keywords = "Faculty of Science, K{\"o}tluj{\"o}kull",
author = "Klint, {K E S} and N Richardt and Johannes Kr{\"u}ger",
year = "2010",
doi = "10.1016/S1571-0866(09)01309-8",
language = "English",
series = "Developments in Quaternary Sciences",
publisher = "Elsevier",
pages = "145--158",
editor = "A Schomacker and Johannes Kr{\"u}ger and Kj{\ae}r, {Kurt H}",
booktitle = "The M{\'y}rdalsj{\"o}kull Ice Cap, Iceland. Glacial Processes, Sediments and Landforms on an Active Volcano",
address = "Netherlands",

}

RIS

TY - CHAP

T1 - Evidence for Subglacial Deformation and Deposition during a Complete Advance-Stagnation Cycle of Kötlujökull, Iceland – A Case Study

AU - Klint, K E S

AU - Richardt, N

AU - Krüger, Johannes

PY - 2010

Y1 - 2010

N2 - A geological section, 70 m long and 3–4 m high, cut into dead-ice moraine in front of Kötlujökull, has been described. Five-sediment associations were recognized representing (1) proglacial glacio-fluvial sedimentation, (2) deposition and deformation in ice-marginal environment, (3) subglacial deformation and deposition from dynamically active ice, (4) subglacial deposition from stagnant ice and (5) supraglacial re-deposition in dead-ice environment during de-icing. This complete sedimentary sequence represents a single glacier advance-stagnation cycle.The melt-out till displays moderate consolidation, moderate content of fines and angular clasts, and a very strong clast fabric. The lodgement/deformation till displays strong to very strong consolidation, relatively high content of fines, low content of angular clasts, and a weak to strong clast fabric. The occurrence of water-escape structures below the basal till and complete lack of brittle deformations in the lodgement/deformation till suggest water-saturated subglacial conditions during the advance of Kötlujökull.

AB - A geological section, 70 m long and 3–4 m high, cut into dead-ice moraine in front of Kötlujökull, has been described. Five-sediment associations were recognized representing (1) proglacial glacio-fluvial sedimentation, (2) deposition and deformation in ice-marginal environment, (3) subglacial deformation and deposition from dynamically active ice, (4) subglacial deposition from stagnant ice and (5) supraglacial re-deposition in dead-ice environment during de-icing. This complete sedimentary sequence represents a single glacier advance-stagnation cycle.The melt-out till displays moderate consolidation, moderate content of fines and angular clasts, and a very strong clast fabric. The lodgement/deformation till displays strong to very strong consolidation, relatively high content of fines, low content of angular clasts, and a weak to strong clast fabric. The occurrence of water-escape structures below the basal till and complete lack of brittle deformations in the lodgement/deformation till suggest water-saturated subglacial conditions during the advance of Kötlujökull.

KW - Faculty of Science

KW - Kötlujökull

U2 - 10.1016/S1571-0866(09)01309-8

DO - 10.1016/S1571-0866(09)01309-8

M3 - Book chapter

T3 - Developments in Quaternary Sciences

SP - 145

EP - 158

BT - The Mýrdalsjökull Ice Cap, Iceland. Glacial Processes, Sediments and Landforms on an Active Volcano

A2 - Schomacker, A

A2 - Krüger, Johannes

A2 - Kjær, Kurt H

PB - Elsevier

CY - Amsterdam and Oxford

ER -

ID: 32640961