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).”
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.11769/39018
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