Serveur d'exploration Nissiros

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Hydrothermal euptions of Nisyros (Dodecanese, Greece). Past events and present hazard

Identifieur interne : 000383 ( Main/Exploration ); précédent : 000382; suivant : 000384

Hydrothermal euptions of Nisyros (Dodecanese, Greece). Past events and present hazard

Auteurs : L. Marini [Italie] ; C. Principe ; G. Chiodini ; R. Cioni ; M. Fytikas ; G. Marinelli

Source :

RBID : Pascal:93-0461020

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English descriptors

Abstract

The detailed analysis of the craters of hydrothermal eruptions and related products present on Nisyros Island demonstrates the ephemerality of these morphological forms. In other words, the mere recognizable existence of the craters and associated deposits implies recency of hydrothermal activity. The minimum temperature required to cause the explosive phenomenon and, possibly, the depth of the reservoir (which can be evaluated on the basis of the correlation between the diameter of the crater and the depth of explosion as proposed by Fytikas and Marinelli, 1976) are therefore closely representative of the current hydrothermal circulation. Both field evidence and historical records indicate that all the deposits of hydrothermal eruption recognized on Nisyros Island were emplaced as debris flows


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<term>aquifers</term>
<term>calderas</term>
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<term>Grèce</term>
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<term>Coulée clastique</term>
<term>Projection</term>
<term>Effondrement</term>
<term>Erosion</term>
<term>Vapeur eau</term>
<term>Nappe eau</term>
<term>Caldeira</term>
<term>Aquiclude</term>
<term>Historique</term>
<term>Séisme volcanique</term>
<term>Fracturation</term>
<term>Risque volcanique</term>
<term>Fumerolle</term>
<term>Départ gaz</term>
<term>Condition pression température</term>
<term>Ponce</term>
<term>Coulée lave</term>
<term>Système géothermique</term>
<term>Puits eau</term>
<term>Ile Nisyros</term>
<term>Circulation hydrothermale</term>
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