Middle Devensian ice-proximal gravels at Howe of Byth, Grampian region

A. M. Hall; G. Duller; J. Jarvis; A. G. Wintle

doi:10.1144/sjg31010061

Middle Devensian ice-proximal gravels at Howe of Byth, Grampian region

A. M. Hall, G. Duller, J. Jarvis, A. G. Wintle

Department of Geography and Earth Sciences

University of St Andrews

Research output: Contribution to journal › Article › peer-review

13 Citations (Scopus)

Abstract

These ice-proximal glaciofluvial gravels have given luminescence ages of 45 ± 4 and 37 ± 4 ka BP. The gravels were laid down by meltwater draining from an ice margin in the Moray Firth and provide the first firm evidence of extensive glaciation in NE Scotland during the Mid Devensian. -from Authors

Original language	English
Pages (from-to)	61-64
Number of pages	4
Journal	Scottish Journal of Geology
Volume	31
Issue number	1
DOIs	https://doi.org/10.1144/sjg31010061
Publication status	Published - 1995

Access to Document

10.1144/sjg31010061

Permanent link

Persistent link

Cite this

@article{b38c4a65f62d439c8942f641fc42433e,

title = "Middle Devensian ice-proximal gravels at Howe of Byth, Grampian region",

abstract = "These ice-proximal glaciofluvial gravels have given luminescence ages of 45 ± 4 and 37 ± 4 ka BP. The gravels were laid down by meltwater draining from an ice margin in the Moray Firth and provide the first firm evidence of extensive glaciation in NE Scotland during the Mid Devensian. -from Authors",

author = "Hall, {A. M.} and G. Duller and J. Jarvis and Wintle, {A. G.}",

year = "1995",

doi = "10.1144/sjg31010061",

language = "English",

volume = "31",

pages = "61--64",

journal = "Scottish Journal of Geology",

issn = "0036-9276",

publisher = "Geological Society of London",

number = "1",

}

TY - JOUR

T1 - Middle Devensian ice-proximal gravels at Howe of Byth, Grampian region

AU - Hall, A. M.

AU - Duller, G.

AU - Jarvis, J.

AU - Wintle, A. G.

PY - 1995

Y1 - 1995

N2 - These ice-proximal glaciofluvial gravels have given luminescence ages of 45 ± 4 and 37 ± 4 ka BP. The gravels were laid down by meltwater draining from an ice margin in the Moray Firth and provide the first firm evidence of extensive glaciation in NE Scotland during the Mid Devensian. -from Authors

AB - These ice-proximal glaciofluvial gravels have given luminescence ages of 45 ± 4 and 37 ± 4 ka BP. The gravels were laid down by meltwater draining from an ice margin in the Moray Firth and provide the first firm evidence of extensive glaciation in NE Scotland during the Mid Devensian. -from Authors

UR - http://www.scopus.com/inward/record.url?scp=0029541742&partnerID=8YFLogxK

U2 - 10.1144/sjg31010061

DO - 10.1144/sjg31010061

M3 - Article

AN - SCOPUS:0029541742

SN - 0036-9276

VL - 31

SP - 61

EP - 64

JO - Scottish Journal of Geology

JF - Scottish Journal of Geology

IS - 1

ER -

Middle Devensian ice-proximal gravels at Howe of Byth, Grampian region

Abstract

Access to Document

Permanent link

Other files and links

Fingerprint

Cite this