In the introduction, the evolution of Etna’s activity is erroneously described in terms of Ma instead of ka. The sentences should read: “Its activity began at ~500 ka with fissure-fed, undersea eruptions of tholeiitic lava, and became sub-aerial at ~320 ka following regional uplift. From ~110 ka, eruptions started to occur mostly through a central conduit exhibiting both explosive and effusive activity (e.g., Rittmann 1973; Romano et al. 1979; Romano 1982; Chester et al. 1985; Gillot et al. 1994; Branca et al. 2008).”
Erratum to: Chronicle of the 1865, NE flank eruption of Mt. Etna and geomorphologic survey of the Mts. Sartorius area
IMPOSA, Sebastiano;
2011-01-01
Abstract
In the introduction, the evolution of Etna’s activity is erroneously described in terms of Ma instead of ka. The sentences should read: “Its activity began at ~500 ka with fissure-fed, undersea eruptions of tholeiitic lava, and became sub-aerial at ~320 ka following regional uplift. From ~110 ka, eruptions started to occur mostly through a central conduit exhibiting both explosive and effusive activity (e.g., Rittmann 1973; Romano et al. 1979; Romano 1982; Chester et al. 1985; Gillot et al. 1994; Branca et al. 2008).”File in questo prodotto:
File | Dimensione | Formato | |
---|---|---|---|
2011 erratum Bull Volcanol.pdf
solo gestori archivio
Tipologia:
Versione Editoriale (PDF)
Licenza:
NON PUBBLICO - Accesso privato/ristretto
Dimensione
40.44 kB
Formato
Adobe PDF
|
40.44 kB | Adobe PDF | Visualizza/Apri |
I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.