Devensian glacigenic sedimentation and landscape evolution in the Cardigan area of southwest Wales

Standard

Devensian glacigenic sedimentation and landscape evolution in the Cardigan area of southwest Wales. / Hambrey, Michael J.; Davies, J. R.; Glasser, Neil F.; Waters, Richard A.; Dowdeswell, Julian A.; Wilby, Philip R.; Wilson, David; Etienne, James L.

In: Journal of Quaternary Science, Vol. 16, No. 5, 07.2001, p. 455-482.

Research output: Contribution to journalArticlepeer-review

Harvard

Hambrey, MJ, Davies, JR, Glasser, NF, Waters, RA, Dowdeswell, JA, Wilby, PR, Wilson, D & Etienne, JL 2001, 'Devensian glacigenic sedimentation and landscape evolution in the Cardigan area of southwest Wales', Journal of Quaternary Science, vol. 16, no. 5, pp. 455-482. https://doi.org/10.1002/jqs.639

APA

Hambrey, M. J., Davies, J. R., Glasser, N. F., Waters, R. A., Dowdeswell, J. A., Wilby, P. R., Wilson, D., & Etienne, J. L. (2001). Devensian glacigenic sedimentation and landscape evolution in the Cardigan area of southwest Wales. Journal of Quaternary Science, 16(5), 455-482. https://doi.org/10.1002/jqs.639

Vancouver

Author

Hambrey, Michael J. ; Davies, J. R. ; Glasser, Neil F. ; Waters, Richard A. ; Dowdeswell, Julian A. ; Wilby, Philip R. ; Wilson, David ; Etienne, James L. / Devensian glacigenic sedimentation and landscape evolution in the Cardigan area of southwest Wales. In: Journal of Quaternary Science. 2001 ; Vol. 16, No. 5. pp. 455-482.

Bibtex - Download

@article{a5ed0d27655d4a7082f74d2c1914b056,
title = "Devensian glacigenic sedimentation and landscape evolution in the Cardigan area of southwest Wales",
abstract = "The depositional processes associated with late Devensian ice in areas bordering the Irish Sea basin have been the subject of considerable debate. Among the key areas around the Irish Sea, southwest Wales occupies a particularly crucial position because it is here that ice flowing from the north impinged upon the coast orthogonally and encroached inland. Two main hypotheses have emerged concerning deglaciation of the Irish Sea basin. The traditional hypothesis holds that sedimentation was ice-marginal or subglacial, whereas an alternative hypothesis that emerged in the 1980s argued that sedimentation was glaciomarine. Southwest Wales is well-placed to contribute to this debate. However, few detailed sedimentological studies, linked to topography, have been made previously in order to reconstruct glacial environments in this area. In this paper, evidence is presented from four boreholes drilled recently in the Cardigan area, combined with data from coastal and inland exposures in the lower Teifi valley and adjacent areas. A complex history of glaciation has emerged: (i) subglacial drainage channel formation in pre-Devensian time, (ii) deposition of iron-cemented breccias and conglomerates possibly during the last interglacial (or in the early/mid-Devensian interstadial), (iii) late Devensian ice advance across the region, during which a glaciolacustrine sequence over 75 m thick accumulated, within a glacial lake known as Llyn Teifi, (iv) a second high-level glaciolacustrine succession formed near Llandudoch, (v) outside the Teifi valley, ice-marginal, subglacial and glaciofluvial sediments were also laid down, providing a near-continuous cover of drift throughout the area. Glacial advance was characterized by reworking, deformation and sometimes erosion of the underlying sediments. The glaciomarine hypothesis is thus rejected for southwest Wales.",
author = "Hambrey, {Michael J.} and Davies, {J. R.} and Glasser, {Neil F.} and Waters, {Richard A.} and Dowdeswell, {Julian A.} and Wilby, {Philip R.} and David Wilson and Etienne, {James L.}",
note = "Hambrey, Michael, Davies, J.R., Glasser, N.F., Waters, R.A., (2001) 'Devensian glacigenic sedimentation and landscape evolution in the Cardigan area of southwest Wales', Journal of Quaternary Science 16(5) pp.455-482 RAE2008",
year = "2001",
month = jul,
doi = "10.1002/jqs.639",
language = "English",
volume = "16",
pages = "455--482",
journal = "Journal of Quaternary Science",
issn = "0267-8179",
publisher = "Wiley",
number = "5",

}

RIS (suitable for import to EndNote) - Download

TY - JOUR

T1 - Devensian glacigenic sedimentation and landscape evolution in the Cardigan area of southwest Wales

AU - Hambrey, Michael J.

AU - Davies, J. R.

AU - Glasser, Neil F.

AU - Waters, Richard A.

AU - Dowdeswell, Julian A.

AU - Wilby, Philip R.

AU - Wilson, David

AU - Etienne, James L.

N1 - Hambrey, Michael, Davies, J.R., Glasser, N.F., Waters, R.A., (2001) 'Devensian glacigenic sedimentation and landscape evolution in the Cardigan area of southwest Wales', Journal of Quaternary Science 16(5) pp.455-482 RAE2008

PY - 2001/7

Y1 - 2001/7

N2 - The depositional processes associated with late Devensian ice in areas bordering the Irish Sea basin have been the subject of considerable debate. Among the key areas around the Irish Sea, southwest Wales occupies a particularly crucial position because it is here that ice flowing from the north impinged upon the coast orthogonally and encroached inland. Two main hypotheses have emerged concerning deglaciation of the Irish Sea basin. The traditional hypothesis holds that sedimentation was ice-marginal or subglacial, whereas an alternative hypothesis that emerged in the 1980s argued that sedimentation was glaciomarine. Southwest Wales is well-placed to contribute to this debate. However, few detailed sedimentological studies, linked to topography, have been made previously in order to reconstruct glacial environments in this area. In this paper, evidence is presented from four boreholes drilled recently in the Cardigan area, combined with data from coastal and inland exposures in the lower Teifi valley and adjacent areas. A complex history of glaciation has emerged: (i) subglacial drainage channel formation in pre-Devensian time, (ii) deposition of iron-cemented breccias and conglomerates possibly during the last interglacial (or in the early/mid-Devensian interstadial), (iii) late Devensian ice advance across the region, during which a glaciolacustrine sequence over 75 m thick accumulated, within a glacial lake known as Llyn Teifi, (iv) a second high-level glaciolacustrine succession formed near Llandudoch, (v) outside the Teifi valley, ice-marginal, subglacial and glaciofluvial sediments were also laid down, providing a near-continuous cover of drift throughout the area. Glacial advance was characterized by reworking, deformation and sometimes erosion of the underlying sediments. The glaciomarine hypothesis is thus rejected for southwest Wales.

AB - The depositional processes associated with late Devensian ice in areas bordering the Irish Sea basin have been the subject of considerable debate. Among the key areas around the Irish Sea, southwest Wales occupies a particularly crucial position because it is here that ice flowing from the north impinged upon the coast orthogonally and encroached inland. Two main hypotheses have emerged concerning deglaciation of the Irish Sea basin. The traditional hypothesis holds that sedimentation was ice-marginal or subglacial, whereas an alternative hypothesis that emerged in the 1980s argued that sedimentation was glaciomarine. Southwest Wales is well-placed to contribute to this debate. However, few detailed sedimentological studies, linked to topography, have been made previously in order to reconstruct glacial environments in this area. In this paper, evidence is presented from four boreholes drilled recently in the Cardigan area, combined with data from coastal and inland exposures in the lower Teifi valley and adjacent areas. A complex history of glaciation has emerged: (i) subglacial drainage channel formation in pre-Devensian time, (ii) deposition of iron-cemented breccias and conglomerates possibly during the last interglacial (or in the early/mid-Devensian interstadial), (iii) late Devensian ice advance across the region, during which a glaciolacustrine sequence over 75 m thick accumulated, within a glacial lake known as Llyn Teifi, (iv) a second high-level glaciolacustrine succession formed near Llandudoch, (v) outside the Teifi valley, ice-marginal, subglacial and glaciofluvial sediments were also laid down, providing a near-continuous cover of drift throughout the area. Glacial advance was characterized by reworking, deformation and sometimes erosion of the underlying sediments. The glaciomarine hypothesis is thus rejected for southwest Wales.

U2 - 10.1002/jqs.639

DO - 10.1002/jqs.639

M3 - Article

VL - 16

SP - 455

EP - 482

JO - Journal of Quaternary Science

JF - Journal of Quaternary Science

SN - 0267-8179

IS - 5

ER -

View graph of relations
Citation formats