This valley at the NW flank of the volcanic island of Stromboli was formed due to a sector collapse approx. 5000 years ago. It is the scene of sliding and jumping talus scree and partly incandescent pyroclastic fragments produced by frequent eruptions near the summit area.
- Location
- View on OpenStreetMap
- Created
- on Sunday 1 June 2003 by Martin Mergili
- Keywords
- active volcano, coastscape, stratovolcano, volcanism
- Visits and license
- 3720 visits, CC BY-NC-SA 4.0 DEED license