The Santorini eruption and its consequences
Identifieur interne : 000541 ( Main/Exploration ); précédent : 000540; suivant : 000542The Santorini eruption and its consequences
Auteurs : R. S. J SparksSource :
- Endeavour [ 0160-9327 ] ; 1979.
Descripteurs français
- Wicri :
- topic : Crète.
English descriptors
- KwdEn :
- Aegean world, Akrotiri, Cold water, Congress volcano thera, Crete, Destructive effects, Direct evidence, Eastern mediterranean, Eruption, Eruption column, Explosive activity, Geological evidence, Geological record, Great thicknesses, Ignimbrite, Ignimbrite phase, Kilometre, Lava fragments, Magma, Minoan, Minoan civilisation, Pottery chronology, Pottery styles, Pyroclastic flows, Rhode island, Santorini, Santorini eruption, Sediment cores, Shock waves, Significant proportion, Square kilometres, Tidal waves, Volcanic, Volcanic theory, Volcano.
- Teeft :
- Aegean world, Akrotiri, Cold water, Congress volcano thera, Crete, Destructive effects, Direct evidence, Eastern mediterranean, Eruption, Eruption column, Explosive activity, Geological evidence, Geological record, Great thicknesses, Ignimbrite, Ignimbrite phase, Kilometre, Lava fragments, Magma, Minoan, Minoan civilisation, Pottery chronology, Pottery styles, Pyroclastic flows, Rhode island, Santorini, Santorini eruption, Sediment cores, Shock waves, Significant proportion, Square kilometres, Tidal waves, Volcanic, Volcanic theory, Volcano.
Abstract
Abstract: In the late Bronze Age, sometime between 1500 and 1450 BC, a paroxysmal explosive eruption of the volcano Santorini took place in the Aegean Sea. Many scientists now link the rapid decline of the Minoan Civilisation centred on Crete with the destructive effects of this catastrophic eruption. The geological record indicates that one or two eruptions of comparable magnitude may occur every 1000 years. In our present-day world with its rapidly expanding population and economy the catastrophic effects of such an eruption occurring today should be seriously considered.
Url:
DOI: 10.1016/0160-9327(79)90006-1
Affiliations:
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Le document en format XML
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J Sparks</name></author></analytic><monogr></monogr><series><title level="j">Endeavour</title><title level="j" type="abbrev">ENDE</title><idno type="ISSN">0160-9327</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1979">1979</date><biblScope unit="volume">3</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="27">27</biblScope><biblScope unit="page" to="31">31</biblScope></imprint><idno type="ISSN">0160-9327</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0160-9327</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Aegean world</term><term>Akrotiri</term><term>Cold water</term><term>Congress volcano thera</term><term>Crete</term><term>Destructive effects</term><term>Direct evidence</term><term>Eastern mediterranean</term><term>Eruption</term><term>Eruption column</term><term>Explosive activity</term><term>Geological evidence</term><term>Geological record</term><term>Great thicknesses</term><term>Ignimbrite</term><term>Ignimbrite phase</term><term>Kilometre</term><term>Lava fragments</term><term>Magma</term><term>Minoan</term><term>Minoan civilisation</term><term>Pottery chronology</term><term>Pottery styles</term><term>Pyroclastic flows</term><term>Rhode island</term><term>Santorini</term><term>Santorini eruption</term><term>Sediment cores</term><term>Shock waves</term><term>Significant proportion</term><term>Square kilometres</term><term>Tidal waves</term><term>Volcanic</term><term>Volcanic theory</term><term>Volcano</term></keywords><keywords scheme="Teeft" xml:lang="en"><term>Aegean world</term><term>Akrotiri</term><term>Cold water</term><term>Congress volcano thera</term><term>Crete</term><term>Destructive effects</term><term>Direct evidence</term><term>Eastern mediterranean</term><term>Eruption</term><term>Eruption column</term><term>Explosive activity</term><term>Geological evidence</term><term>Geological record</term><term>Great thicknesses</term><term>Ignimbrite</term><term>Ignimbrite phase</term><term>Kilometre</term><term>Lava fragments</term><term>Magma</term><term>Minoan</term><term>Minoan civilisation</term><term>Pottery chronology</term><term>Pottery styles</term><term>Pyroclastic flows</term><term>Rhode island</term><term>Santorini</term><term>Santorini eruption</term><term>Sediment cores</term><term>Shock waves</term><term>Significant proportion</term><term>Square kilometres</term><term>Tidal waves</term><term>Volcanic</term><term>Volcanic theory</term><term>Volcano</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Crète</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: In the late Bronze Age, sometime between 1500 and 1450 BC, a paroxysmal explosive eruption of the volcano Santorini took place in the Aegean Sea. Many scientists now link the rapid decline of the Minoan Civilisation centred on Crete with the destructive effects of this catastrophic eruption. The geological record indicates that one or two eruptions of comparable magnitude may occur every 1000 years. In our present-day world with its rapidly expanding population and economy the catastrophic effects of such an eruption occurring today should be seriously considered.</div></front></TEI><affiliations><list></list><tree><noCountry><name sortKey="Sparks, R S J" sort="Sparks, R S J" uniqKey="Sparks R" first="R. S. J" last="Sparks">R. S. J Sparks</name></noCountry></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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