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<article language="en">
	<journal>
		<journal_title>Natural Hazards and Earth System Science</journal_title>
		<journal_url>www.nat-hazards-earth-syst-sci.net</journal_url>
		<issn>1561-8633</issn>
		<eissn>1684-9981</eissn>
		<volume_number>8</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/nhess-8-587-2008</doi>
	<article_url>http://www.nat-hazards-earth-syst-sci.net/8/587/2008/</article_url>
	<abstract_html>http://www.nat-hazards-earth-syst-sci.net/8/587/2008/nhess-8-587-2008.html</abstract_html>
	<fulltext_pdf>http://www.nat-hazards-earth-syst-sci.net/8/587/2008/nhess-8-587-2008.pdf</fulltext_pdf>
	<start_page>587</start_page>
	<end_page>601</end_page>
	<publication_date>2008-06-30</publication_date>
	<article_title content_type="html">Historic tsunami in Britain since AD 1000: a review</article_title>
	<authors>
		<author numeration="1" affiliations="1,3">
			<name>S. K. Haslett</name>
			<email>simon.haslett@newport.ac.uk</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>E. A. Bryant</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Quaternary Research Centre, Department of Geography, School of Science and the Environment, Bath Spa University, Newton Park, Bath, BA2 9BN, UK</affiliation>
		<affiliation numeration="2" content_type="html">Science Faculty Office, University of Wollongong, Wollongong, NSW 2522, Australia</affiliation>
		<affiliation numeration="3" content_type="html">present address: CELT, University of Wales, Newport, Lodge Road, Caerleon, South Wales, NP18 3QT, UK</affiliation>
	</affiliations>
	<abstract content_type="html">The British coast is not considered at particular risk from
tsunami, a view that is supported by a number of recent government reports.
However, these reports largely ignore some written historic records that
suggest southern Britain has experienced a number of events over the past
1000 yrs. This study briefly assesses these records and recognises four
groups of events: 1) sea disturbance and coastal floods in southeast England
linked to earthquakes in the Dover Straits (e.g. 1382 and 1580), 2)
far-field tsunami reaching the coast of the British Isles, for example, from
earthquakes along the Azores-Gibraltar Fault Zone offshore Portugal (e.g.
1755), 3) tsunami associated with near-coastal low magnitude earthquakes
(e.g. 1884 and 1892), and 4) a flood event in AD 1014 that has been linked
to comet debris impact. The seismogenic events range from minor water
disturbance, through seismic seiching, to small and &quot;giant&quot; waves,
suggesting near-coastal, low-magnitude, shallow earthquakes may be capable
of triggering disturbance in relatively shallow water, as supported by
similar occurrences elsewhere, and that the British tsunami risk requires a
more careful evaluation.</abstract>
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</article>

