Get our newsletter!
Check out the volcano tours offered by Volcano-Adventures!
Volcanoes & Earthquakes - new app for Android
Guaranteed tours:
23 Aug - 5 Sep 2017: Volcano Special: Ibu - Dukono - Lokon - Halmahera (Indonesia)
5-20 Sep 2017: From Krakatau to Bali - Java (Indonesia)
16-23 Sep 2017: Pearl of the Aegean - Santorini - Santorini Island, Greece
20-24 Sep 2017: Sinabung Volcano Special - Sumatra (Indonesia)
20-25 Sep 2017: Sinabung Volcano Special - Sumatra (Indonesia)
23-28 Sep 2017: Aegean's Hidden Gem: Isle of Milos - Milos Island (Greece)
1-16 Oct 2017: From Krakatau to Bali - Java (Indonesia)
7-14 Oct 2017: Pearl of the Aegean - Santorini - Santorini Island, Greece
13-27 Oct 2017: Volcanoes of Italy - the Grand Tour - Southern Italy
16-19 Oct 2017: Indonesia Specials - Java-Komodo-Bali (Indonesia)
: spaces available / : guaranteed / : few spaces left / : booked out
Random pictures
News

no news in this list.

 

Lastarria volcano

stratovolcano 5697 m / 18,691 ft
Northern Chile, Bolivia and Argentina, South America, -25.17°S / -68.5°W
Current status: dormant (1 out of 5)
Lastarria volcano books
Typical eruption style: explosive
Lastarria volcano eruptions: unknown, but probably in historic times No recent earthquakes
TimeMag. / DepthDistanceLocation
Lastarria is a stratovolcano on the Argentina/Chile border. The volcano contains 5 nested summit craters. The youngest part of the volcano is a lava dome overlapping the northern crater.
A large prehistoric debris avalanche deposit is located on the SE flank and younger deposits of pyroclastic flows form an apron around the the northern base of the volcano.
There are no known historical eruptions, but the young morphology of some deposits suggest that Lastarria has been active during historical time. There is intense fumarolic activity on the rim and flanks of the northern summit crater and its NW flank, and sulfur flows have occurred by melting of extensive sulfur deposits in the summit region.

Background:

Negriales lava field is a large andesitic-dacitic flow on the western flanks and was erupted from a single vent on the SW-flank of Lastarria volcano.
The petrography of the Lastarria complex ranges from pyroxene-rich andesites to pyroxene-amphibole bearing dacites.

Inflation of the Lastarria-Cordon del Azufre complex
Satellite radar measurements have shown that an area of 45x37 km of the Lastarria-Cordon del Azufre complexis undergoing long-term wavelength cycles of ground deformation (inflation and deflation) at maximum rates of 2.5 cm/year. It is believed that this geothermal activity is caused by a pressurized, and partially sealed fluid system similar, but smaller to the very active hydrothermal systems at Yellowstone, Long Valley caldera, or the Campi Flegrei in Italy.

Lastarria debris avalanche
A pre-historic flank collapse occurred on the SE flank of Lastarria volcano. The collapse generated a debris avalanche that climbed and surpassed an older 125 m high scoria cone east of Lastarria. The avalanche had an unusually high velocity of 300 km/hr. Near Lastarria, the detached mass was fluidized and disintegrated, unlike the historic 1980 avalanche of Mt St Helens, which consisted of large coherent blocks, composed of parts of the original mountain flank (interleaved lavas and pyroclastic layers).

Sulfur flows
Lastarria volcano is one of the few locations in the world where sulfur flows have been documents (another example with recent flows is Ijen volcano, East Java). Sulfur usually flows as a Newtonian fluid, but the presence of gas bubbles and crystals at the Lastarria sulfur flows indicated it may have behaved as a Bingham fluid.

---
Sources:
- Smithsonian / GVP Lastarria volcano information
- José A. Naranjo (1992) "Chemistry and petrological evolution of the Lastarria volcanic complex in the north Chilean Andes", Geol. Magazine v 129, pp 723-740
- Froger et al (2007) "Two scales of inflation at Lastarria-Cordon del Azufre volcanic complex, central Andes, revealed from ASAR-ENVISAT interferometric data", Earth and Planetary Science Letters, V. 255 (1-2), pp 148-163
- José Antonio Naranjo and Peter Francis (1987) "High velocity debris avalanche at Lastarria volcano in the north Chilean Andes", Bull. Volc., v. 49 (2), pp 509-514


Latest satellite images

More on VolcanoDiscovery:

Copyrights: VolcanoDiscovery and other sources as noted.
Use of material: Text and images on this webpage are copyrighted. Further reproduction and use without authorization is not consented. If you need licensing rights for photographs, for example for publications and commercial use, please contact us.