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Statements

Subject Item
dbr:Garth_tsunami
rdfs:label
Tsunami de Garth Garth tsunami
rdfs:comment
The Garth tsunami is a likely prehistoric tsunami off the Shetland Islands that may have occurred 5,500 years ago (3,500 BCE). Its origin is unknown; impact events, earthquakes, and submarine landslides similar to the Storegga Slide 8,100 years ago (6,100 BCE) have been proposed as factors contributing to the event. Evidence suggests a run-up of more than 10 metres (33 ft) in the Shetland Islands. It probably had great impact on coastal communities in the region; mass burials dating approximately to that time in the Shetland and Orkney Islands have been interpreted to host its fatalities. Le tsunami de Garth est un tsunami préhistorique qui s'est produit sur les iles Shetland vers 3500 av. J.-C., durant le Néolithique britannique. Son origine est incertaine mais des pistes comme l'impact d'une météorite, un séisme ou un glissement de terrain sous-marin similaire aux glissements de terrain de Storegga ont été proposés comme causes de cet évènement.
dcterms:subject
dbc:4th_millennium_BC dbc:Historical_geology dbc:Natural_disasters_in_Norway dbc:Natural_disasters_in_Scotland dbc:Tsunamis
dbo:wikiPageID
63143821
dbo:wikiPageRevisionID
1119483073
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n6:Bw6mr wikidata:Q85762783 dbpedia-vi:Sóng_thần_Garth dbpedia-fr:Tsunami_de_Garth dbpedia-fa:سونامی_گارث
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dbo:abstract
Le tsunami de Garth est un tsunami préhistorique qui s'est produit sur les iles Shetland vers 3500 av. J.-C., durant le Néolithique britannique. Son origine est incertaine mais des pistes comme l'impact d'une météorite, un séisme ou un glissement de terrain sous-marin similaire aux glissements de terrain de Storegga ont été proposés comme causes de cet évènement. The Garth tsunami is a likely prehistoric tsunami off the Shetland Islands that may have occurred 5,500 years ago (3,500 BCE). Its origin is unknown; impact events, earthquakes, and submarine landslides similar to the Storegga Slide 8,100 years ago (6,100 BCE) have been proposed as factors contributing to the event. Evidence suggests a run-up of more than 10 metres (33 ft) in the Shetland Islands. It probably had great impact on coastal communities in the region; mass burials dating approximately to that time in the Shetland and Orkney Islands have been interpreted to host its fatalities.
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