Get our newsletter!
Check out our volcano tours on VolcanoAdventures.com!
Volcanoes & Earthquakes - new app for Android
Volcanoes & Earthquakes - app for iPhone & iPad

Guaranteed tours:
4-11 Aug 2019: Nyiragongo Lava Lake & Mountain Gorillas - DR Congo
12-30 Aug 2019: Kamchatka - Land of Colors - Kamchatka (Russia)
13-29 Aug 2019: Volcanoes of Java - Java (Indonesia)
14-17 Aug 2019: Krakatau Volcano Special - Krakatau volcano (Indonesia)
1-19 Sep 2019: Kamchatka - Land of Colors - Kamchatka (Russia)
3-18 Sep 2019: From Krakatau to Bali - Java (Indonesia)
21-28 Sep 2019: Pearl of the Aegean - Santorini - Santorini Island, Griekenland
12-20 Oct 2019: From Stromboli to Etna - Eolian Islands + Etna volcano (Italy)
: ruimten beschikbaar / : gegarandeerd / : enkele spaties links / : geboekt uit
Willekeurige foto 's
News

Geen nieuws in deze lijst:

 

Upolu vulkaan

Shield volcano 1100 m / 3,609 ft
Samoa, Samoan Islands, -13.94°S / -171.72°W
Current status: normal or dormant (1 out of 5) | Reports
Upolu vulkaan boeken
Typical eruption style: niet gespecifieerd
Upolu vulkaanuitbarstingen: unknown, no recent eruptionsGeen recente aardbevingen
TijdMag. / DiepteAfstandLocatie

Background:

The massive, basaltic shield volcano forming 75-km-long Upolu Island in Samoa is elongated in an E-W direction and was constructed during two periods of extensive eruptions during the Pliocene and Pleistocene. The most extensive activity during the Pleistocene took place along a 20-km segment along the central axis of the island. Following a lengthy period of erosion, the latest lava flows, at least three of which were estimated to be as young as a few hundred to a few thousand years old, were erupted from vents near the crest of the island at its center and western side (Stearns, 1944). One of the youngest flows reached the north-central coast along a roughly 1.5-km-wide front east of Vailele Bay, and another traveled down the Lefaga River channel and reached the SW coast at Lefaga Bay. Apolima Island off the western tip of Upolu is a Holocene tuff cone too young to be fringed by a coral reef, and other reef-free areas along the coastline may be formed by Holocene lava flows.
---
Smithsonian / GVP volcano information


Meest recente satellietbeelden

 

Meer op VolcanoDiscovery:

Copyrights: VolcanoDiscovery en andere bronnen zoals.
Materiaalgebruik: Most texts and images, in particular photographs, on this website are protected by copyright. Further reproduction and use of without authorization is usually not consented. If you are not sure or need licensing rights for photographs, for example for publications and commercial use, please contact us.