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News
Sunday, Oct 20, 2019
The Alaska Volcano Observatory (AVO) recorded small explosion signals from the volcano via its infrasound network located at Sand Point and on the local seismic network yesterday. ... [Leer más]
Thursday, Jun 13, 2019
The elevated seismic activity observed in mid May has again declined to background levels. TRhe Alaska Volcano Observatory lowered the Aviation Color Code and Alert Level to GREEN/NORMAL. [Leer más]
Map of Pavlov volcano and the Emmons Lake volcanic center on the Alaksa Peninsula. (Image Creator: Waythomas, Chris /Image courtesy of AVO/USGS)
Map of Pavlov volcano and the Emmons Lake volcanic center on the Alaksa Peninsula. (Image Creator: Waythomas, Chris /Image courtesy of AVO/USGS)
 

Pavlof volcano

Stratovolcano 2519 m / 8,264 ft
Alaska Peninsula, USA, 55.42°N / -161.89°W
Current status: restless (2 out of 5)
Pavlof webcams / datos en tiempo real | Reports
Pavlof volcano books
Last update: 20 Oct 2019 (possible small explosions, seismic unrest)
Typical eruption style: Explosivos.
Erupciones del volcán Pavlof: 1762(?), 1790(?), 1817, 1825(?), 1838(?), 1844, 1846, 1852(?), 1866(?), 1880, 1886, 1892, 1894, 1901, 1903(?), 1906, 1914, 1917, 1922, 1924, 1929, 1936, 1950, 1951, 1953, 1958, 1960, 1966, 1973, 1974(?), 1975, 1980(Mar-May), 1980 (Jul)(?), 1980 (Nov), 1981, 1983 (Jul), 1983 (Nov-Dec), 1983, 1986, 1990, 1996, 2007 (Aug), 2013, 2014, 2016 No hay terremotos recientes
Fecha / HoraRevista / ProfundidadDistanciaUbicación
Pavlov is the most active volcano of the Aleutian arc.

Background:

The 2519-m-high, largely snow-capped Holocene stratovolcano was constructed along a line of vents extending NE from the Emmons Lake caldera.
Pavlof and its twin volcano to the NE, 2142-m-high Pavlof Sister, form a dramatic pair of symmetrical, glacier-covered stratovolcanoes that tower above Pavlof and Volcano bays. A third cone, Little Pavolf, is a smaller volcano on the SW flank of Pavlof volcano, near the rim of Emmons Lake caldera. Unlike Pavlof Sister, Pavlof has been frequently active in historical time, typically producing strombolian to vulcanian explosive eruptions from the summit vents and occasional lava flows. The active vents lie near the summit on the north and east sides. The largest historical eruption of Pavlof took place in 1911, at the end of a 5-year-long eruptive episode; a fissure opened on the northern flank of the volcano, ejecting large blocks and issuing lava flows.
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Source: GVP (Global Volcanism Program), Pavlov information


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