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Holocene 7 (1)
Title
The title of the publication or report
Title:
Holocene 7 (1)
Series
The series the publication or report is included in
Series:
The Holocene
Volume
Volume number and part
Volume:
7 (1)
Publication Type
The type of publication - report, monograph, journal article or chapter from a book
Publication Type:
Journal
Year of Publication
The year the book, article or report was published
Year of Publication:
1997
Note
Extra information on the publication or report.
Note:
Date Of Issue From: 1997
Source
Where the record has come from or which dataset it was orginally included in.
Source:
BIAB (The British & Irish Archaeological Bibliography (BIAB))
Relations
Other resources which are relevant to this publication or report
Relations:
URI:
http://hol.sagepub.com/content/7/1.toc
Created Date
The date the record of the pubication was first entered
Created Date:
20 Jan 2002
Please click on an Article link to go to the Article Details.
Article Title
Access Type
Author / Editor
Page
Start/End
Abstract
Holocene relative sea-level changes on the margin of a glacio-isostatically uplifted area: an example from northern Caithness, Scotland
Susan Dawson
59 - 77
Evidence from intercalated clastic and organic sediments in the lower Wick River valley indicates a rapid rise in sea-level, culminating between c. 6900 BP and c. 5900 BP. Following a subsequent regression, the sediments record two further marine transgressions beginning at c. 4400 BP and c. 1200 BP. There is also evidence of a tsunami (tidal-wave) event between c. 7300 BP and c. 7000 BP.
Modelling long-term anthropogenic erosion of a loess cover: South Downs, UK
David Favis-Mortlock
John Boardman
Martin G Bell
79 - 89
The Erosion-Productivity Impact Calculator (EPIC) model is used to simulate erosion on a hill slope in the Downs from 7000 BP to the present day. Results suggest that the major period of soil loss was between 4000 and 1800 BP, under conditions of gradually intensifying agriculture following permanent clearance.
Investigation of the environmental impact of remote volcanic activity on north Mayo, Ireland, during the mid-Holocene
Rosaleen B Dwyer
Fraser B Mitchell
113 - 118
Tephra deposits from peat bogs at Croaghaun East are dated by radiocarbon to around 4000 BP. Analysis of pollen, fungal spores, and testate amoebae from the peat is used to indicate the rate of environmental change around the time of tephra deposition. A change to wetter conditions is evinced, but the decline in pine trees (Pinus) is thought to have occurred c. 100 years before the eruption.
