Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1806
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dc.contributor.authorallLa Rosa, V.; Istituto di Archeologia, Università di Catania, Italyen
dc.date.accessioned2006-09-29T10:28:35Zen
dc.date.available2006-09-29T10:28:35Zen
dc.date.issued1995-11en
dc.identifier.urihttp://hdl.handle.net/2122/1806en
dc.description.abstractThe seismic destruction of the first Minoan palace at Phaistos is preliminarily confirmed. The hypothesis is then proposed that a change in the relationships a~nongth e powers in the Messarh plain was also produced by the different capacity of the Phaistos centre to react to the 1700 B.C. seismic effects, as compared to that of Knossos. This trend is thought to have continued after the second earthquake of the middle(?) of the XVII century B.C., indirectly confirming Knossian leadership in the island's entire central region during the age of the second palaces.en
dc.format.extent4774415 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.relation.ispartofseries5-6/38 (1995)en
dc.subjectSeismic archaeologyen
dc.subjectCreteen
dc.subjectMinoan civilizationen
dc.titleA hypothesis on earthquakes and political power in Minoan Creteen
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV05. General::05.09. Miscellaneous::05.09.99. General or miscellaneousen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorLa Rosa, V.en
dc.contributor.departmentIstituto di Archeologia, Università di Catania, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto di Archeologia, Università di Catania, Italy-
crisitem.classification.parent05. General-
Appears in Collections:Annals of Geophysics
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