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2 edition of Late Flandrian shoreline oscillations in the Severn estuary found in the catalog.

Late Flandrian shoreline oscillations in the Severn estuary

John R. L. Allen

Late Flandrian shoreline oscillations in the Severn estuary

the Rumney formation at its typesite (Cardiff area).

by John R. L. Allen

  • 18 Want to read
  • 25 Currently reading

Published by [s.n.] in [U.K.] .
Written in English


ID Numbers
Open LibraryOL15966708M

The Severn Estuary Partnership's 'Who Does What' guide provides information on many of these bodies. The Severn Estuary Partnership (SEP): The Severn Estuary Partnership (SEP) was established in as an independent Estuary-wide non-statutory initiative, led by Local Authorities, Statutory Agencies and Cardiff University. Severn Estuary SMP Review Notice This report was produced by Atkins Ltd for the Severn Estuary Coastal Group for the specific purpose of the Severn Estuary SMP2. This report may not be used by any person other than the Severn Estuary Coastal Group without the Severn Estuary Coastal Group ’s. express permission.

A comparison has been made of secular trends in sea-level from the twentieth century and late Holocene period, determined from tide gauge and geologic Vertical salt-marsh accretion since the Roman period in the Severn estuary, southwest Britain R. J. N., , Flandrian sea-level changes and vegetational history of the lower Thames. Holocene silts (salt marshes) and highest intertidal-supratidal peats are superbly exposed on a 15 kin coastal transect which reveals two laterally extensive units of annually banded silts (Beds 3, 7) associated with three transgressive-regressive silt-peat cycles (early sixth-early fourth millennium BC). Bed 3 in places is concordantly and gradationally related to peats above and below, but.

Allen, J.R.L. and Rae, J.E. Late Flandrian shoreline oscillations in the Severn Estuary: a geomorphological and stratigraphical reconnaissance. Philosophical Transactions of the Royal Society B, -   24,, articles and books. Periodicals Allen, J.R.L. Late Flandrian shoreline oscillations in the Severn Estuary: the Rumney Formation at its typesite (Cardiff area). J.E. Late Flandrian shoreline oscillations in the Severn Estuary: a geomorphological and stratigraphical reconnaissance. Philosophical Transactions of the.


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Late Flandrian shoreline oscillations in the Severn estuary by John R. L. Allen Download PDF EPUB FB2

The shore of the former tidal wetland northeast of Cardiff, called the Wentlooge Level and reclaimed during the Roman period, exposes a series of late Flandrian lithostratigraphic units dominated by estuarine clays. Chief among these are the (upper) Wentlooge Formation (up to m thick) and the Rumney Formation (up to m thick).

Allen J () Late Flandrian shoreline oscillations in the Severn Estuary: change and reclamation at Arlingham, Gloucestershire, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences,(), Online publication date: Mar LATE FLANDRIAN SHORELINE OSCILLATIONS IN THE SEVERN ESTUARY: A GEOMORPHOLOGICAL AND STRATIGRAPHICAL RECONNAISSANCE By J.

ALLEN, F.R.S., and J. RAE Department of Geology, The University, Reading, RG6 2AB, U.K. (Received 13 March ) [Plates ] CONTENTS PAGE 1. Introduction 2. Setting 3. Allen, Late Flandrian shoreline oscillations in the Severn Estuary: change and reclamation at Arlingham, Gloucestershire.

Philosophical Transactions of the Royal Society A Allen, The Severn Estuary in southwest Britain: its retreat under marine transgression and fine-sediment regime.

Late Flandrian Shoreline Oscillations in the Severn Estuary: A Geomorphological and Stratigraphical Reconnaissance. Philosophical Transactions of the Royal Society B: Biological Sciences • Darby SE, Leyland J, Kummu M, Räsänen TA, Lauri H. Relict Flandrian estuarine deposits in the Ythan valley are confined to an area in the lower valley around the present estuary.

They rest upon a discontinuous layer of peat over an irregular surface of sand and gravel, and consist for the most part of a grey silty clay, or carse deposit, which forms terraces or small areas of carseland. Late Flandrian shoreline oscillations in the Severn Estuary: a geomorphological and stratigraphical reconnaissance.

Philosophical Transactions of the Royal Society, London, B Andrews, J. T., Bowen, D. & Kidson, C. Amino-acid ratios and the correlation of raised beach deposits in south west England and Wales. The late Flandrian (Roman and post-Roman) muddy intertidal sediments of the well-mixed Severn Estuary display a spatially uniform temporal pattern of grain size-corrected trace-metal (Zn, Cu, Pb) abundances.

In the earlier deposits (chemozone I, pre-industrial) the metal content is low but steady. Over the period of chemozone II (industrial) the metals increase rapidly in abundance to a.

Books, pp. Brown and Allen - Recent finds of flintwork, Oldbury Flats Late Flandrian Shoreline Oscillations in the Severn Estuary: A Geomorphological and Stratigraphical Reconnaissance. The SMP2 for the Severn Estuary updates an earlier SMP1 () for the estuary. It aims to provide more certainty for landowners, residents and businesses; to know how the coast will be managed by regulators during the next years, so that they can plan ahead and make decisions about investments, homes, development and the management of.

J.R.L. Allen Late Flandrian shoreline oscillations in the Severn Estuary: the Rumney Formation at its typesite (Cardiff area) Philosophical Transactions of the Royal Society of London, B (), pp.

- Late Flandrian coastal change and tidal palaeochannel development at Hills Flats, Severn Estuary (SW Britain). Journal of the Geological Society, Vol. Issue. 1, p. ‘ Late Flandrian shoreline oscillations in the Severn Estuary: the Rumney Formation at its typesite (Cardiff area) ’.

Allen, J. and Rae, J. 'Late Flandrian shoreline oscillations in the Severn Estuary: a geomorphological and stratigraphical reconnaissance', Philosophical Transactions of the Royal Society of London, Series B,Coastal peat resouce database (Hazell, Page 1 of Extensive coastal flooding reported in the Severn Estuary in has been considered as evidence for a major tsunami (Bryant & Haslett ), although it is difficult to identify a potential.

Romano-British Wetland Reclamations at Longney, Gloucestershire, and Evidence for the Early Settlement of the Inner Severn Estuary - Volume 70 Issue 2 - J.

Allen, M. Fulford 5 Allen, J. and Rae, J. E., ‘ Late Flandrian shoreline oscillations in the Severn Estuary: a geomorphological and stratigraphical reconnaissance ’. Severn Estuary Shoreline Management Plan Review (SMP2) Notice.

This report was produced by Atkins Ltdfor the Severn Estuary Coastal Group (SECG) for the specific purpose of Severn Estuary Shoreline Management Plan Review.

This report may not be used by any person other than the SECG without the SECGs express permission. Allen, J R L, Late Flandrian Shoreline Oscillations in the Severn Estuary: The Rumney Formation at its Typesite, Phil Trans Roy Soc London, B,Allen, J R L, Reclamation and Sea Defence in Rumney Parish, Monmouthshire.

Allen, J R L. Late Flandrian shoreline oscillations in the Severn Estuary: the Rumney Formation at its typesite (Cardiff area). Philosophical Transactions of the Royal Society of London, Vol.B, Waters, R A and Lawrence, D J D. Geology of the South Wales Coalfield - Part III: the country around Cardiff.

Allen, J R L. Late Flandrian shoreline oscillations in the Severn Estuary: the Rumney Formation at its typesite (Cardiff area).

Philosophical Transactions of the Royal Society of London, Vol.B, Squirrell, H C and Downing, R A. Geology of the South Wales Coalfield, Part 1, the country around Newport (Monmouthshire).

Holocene transgressions and regressions on the Essex coast, Outer Thames Estuary. Late Flandrian shoreline oscillations in the Severn Estuary: The Rumney Formation at. Late Flandrian shoreline oscillations in The Severn Estuary: A geomorphological and stratigraphical reconnaissance.

Philosophical Transactions of the Royal Society of London, Series B,–Archaeology in the Severn Estuary 5 Title. The title of the publication or report. Title: Archaeology in the Severn Estuary 5 Gwent The Geoarchaeology of a Late Flandrian Tidal Palaeochannel.

the unconsolidated sediments at Caldicot Pill is a valuable record of local and regional changes in sea-level and shoreline position dating from.The Severn Estuary (Welsh: Aber Hafren) is the estuary of the River Severn, the longest river in Great is the confluence of four major rivers, being the Severn, Wye, Usk and Avon, and other smaller rivers.

Its high tidal range, approximately 50 feet (15 m), means that it has been at the centre of discussions in the UK regarding renewable energy.