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Dienstag, Jun 18, 2013
No changes in activity were reported by the Alaska Volcano Observatory. Seismic activity continues to decrease and no elevated surface temperatures were detected in satellite images during the past 24 hours. No plumes were visible in satellite images, while web camera images show mostly cloudy conditions. [mehr]
Montag, Jun 17, 2013
AVO reports no significant change in the seismicity at Pavlof in the past 24 hours: seismic tremor continues, but at lower amplitudes than previously. ... [mehr]
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)

Pavlov Vulkan

Schichtvulkan 2519 m / 8,264 ft
Alaska Peninsula, USA, 55.42°N / -161.89°W
Aktueller Status: Schwache Aktivität oder Ausbruchswarnung (3 von 5)
Pavlov Webcams / aktuelle Daten
Letztes Update: 18 Jun 2013
Typische Aktivität: Explosive.
Ausbrüche des Pavlov: 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)
Letzte Erdbeben in der Nähe: No recent earthquakes
ZeitMag. / TiefeDistanceOrt
Pavlov is the most active volcano of the Aleutian arc.

Beschreibung:

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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