File:Vesuv 9.jpg
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Deutsch: Der Berg ist heute 1281 m hoch. Er besteht aus den Resten eines früher wesentlich höheren, älteren Schichtvulkans, des Somma, dessen Spitze bei seinem letzten Ausbruch 79 n. Chr. zu einer Caldera eingestürzt ist, und dem im Inneren des Einsturzbeckens neugebildeten Kegel des „eigentlichen“ Vesuv. Aufnahme von 2017. |
| Date | |
| Source | Own work |
| Author | Colling-architektur |
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I, the copyright holder of this work, hereby publish it under the following license:
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 16:36, 22 April 2017 | | 5,184 × 3,456 (3.32 MB) | Colling-architektur (talk | contribs) | User created page with UploadWizard |
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