Pavlof Volcano Introduction
Pavlof is one of the most active volcanoes in North America. In the past 100 years, Pavlof has erupted at least 24 times and
may have erupted on several other occasions. The remote location and weather with limited visibility, combined with the fact that there are few local inhabitants, may have allowed some
eruptions to go unconfirmed. Today, daily satellite monitoring and real-time data from instruments around the volcano bring a
continuous stream of information to scientists.
Although there is very little human activity on the land immediately surrounding Pavlof, the sky above is heavily travelled. Each
day at least 20,000 international airline passengers and dozens of flights loaded with freight fly above the volcano. An eruption at Pavlof that puts large amounts of volcanic ash high into the atmosphere produces air traffic safety concerns and significant financial
losses as flights must be rerouted. This is why the volcano receives so much attention from scientists.
Related: Pavlof Eruption Photos from the Space Station
Pavlof Volcano: Plate Tectonic Setting
Pavlof is located near the western end of the Alaska Peninsula. The convergent boundary between the North American Plate and the
Pacific Plate is located to the south and east of Pavlof as shown in the map below. The North American Plate is moving in a southerly
direction and the Pacific Plate is moving towards the northwest.
|Map: Where is Pavlov Volcano?|
|Map showing the location of Pavlof Volcano near the end of the Alaska Peninsula. The boundary between the North American Plate and the Pacific Plate is shown by the gray toothed line. The Pacific Plate is to the south of the boundary, and the North American plate is to the north of this boundary. The A-B line shows the location of the cross section below.
At this location both plates consist of oceanic lithosphere. At the plate boundary, the Pacific Plate is forced under the North
American Plate to form the Aleutian Trench and a subduction zone. A diagram of this plate boundary situation is shown in the
simplified cross section below.
|Simplified plate tectonics cross section (A to B)|
|Simplified plate tectonics cross-section showing how Pavlof Volcano is located on the Alaska Peninsula. A subduction zone formed where the Pacific Plate descends beneath the North American Plate is directly below the volcano. Magma produced from the melting mantle and Pacific Plate rises to the surface and causes eruptions.
Pavlof Volcano: Eruptive History
The diagram below summarizes the eruptive frequency of Pavlov for which there is a written record.
The small number of eruptions in the early portion of this record reflects the remote location of the volcano, the lack of
local population and the poor weather conditions that limited observation. Eruption frequencies in
the 1700s, 1800s and early 1900s are underrepresented.
Some of the eruptions are marked as "questionable." At times it was impossible to attribute
an eruption to a specific volcano because vents are so numerous and close together in the Eammons
Lake Volcanic Center.
Most of Pavlof's eruptions have involved low energy ash releases, minor lava flows or minor lava fountaining. These
sometimes produce lahars when ash and lava melt portions of Pavlof's snow cap. Some of these lahars
have been large enough to reach the Pacific Ocean to the south or the Bering Sea to the north.
Occasionally, Pavlof produces a strong explosive eruption or a number of
smaller explosive events in a single eruptive episode.
The 1983, 1981, 1974/1975, 1936/1948, and 1906/1911 eruptions produced enough ejecta to be rated at level 3 on the Volcanic Explosivity Index. The 1762/1786 eruption has been rated at VEI 4. 
|Chart of the eruptive history of Pavlof Volcano by century. The greater
frequency of eruptions over the last two centuries can mainly be attributed to improved observation abilities and greater
interest in the volcano. Data in this chart is from the Alaska Volcano Observatory,
where more specific details for most of these eruptions are available for public view. Some of the eruptions extended in
time across two or more calendar years. 
Pavlof: Geology and Hazards
Although eruptions at Pavlof have been numerous, they have fortunately been small to moderate in size. They are often Strombolian
eruptions that produce local falls of tephra. Pavlof also produces ash plumes that can be carried hundreds of miles by the wind.
Pavlof has not been a deadly threat to people on the ground because very few people venture near the volcano. The nearest community is
Cold Bay, about 35 miles to the southwest. Other nearby communities include King Cove, Nelson Lagoon and Sand Point. All of these are
beyond the reach of lahars and pyroclastic flows; however, each of these communities has experienced ash falls from eruptions
Ash plumes are the most significant hazard associated with eruptions at Pavlof. They are a major hazard to local aircraft
and a threat to international air traffic when they reach significant height. This is why the volcano is monitored with instruments
and why satellite images of the volcano are examined daily.
Pavlof is usually covered by snow and ice. Eruptions can quickly melt significant amounts of snow and ice to produce volcanic mudflows
known as lahars. These lahars are fast-moving slurries. They can fill stream valleys with hot water, sand, gravel, boulders and volcanic
debris. They destroy stream habitat, which can be lost for many years after an eruption. They travel at very high speeds, and anyone in
stream valleys below the volcano when an eruption occurs must quickly move to high ground to escape the deadly flow.
Pavlof eruptions often produce pyroclastic flows. These are hot clouds of rock, gas and ash that sweep down the flanks of the volcano at
speeds of up to 100 miles per hour. They are dense enough to knock down trees and hot enough to incinerate everything in their path.
Lava flows are produced by many Pavlof eruptions. They are generally not a hazard to humans because they move slowly, their flow path is predictable,
and they generally do not travel far from the volcano.
Pavlof Volcano gets a lot of attention because it produces a small eruption every few years, making it one of the most active volcanoes
in North America. It has the ability to cause temporary air traffic disruptions, but it ranks far below a major threat to local populations
and the planet in general.
The eruptive history of the Emmons Lake Volcanic Center includes several large caldera-forming
eruptions. Between three and six major caldera-forming eruptions have occurred there in the past 400,000 years. Estimated dates of these major eruptions are around 294,000, 234,000, 123,000, 100,000, 30-50,000, and 26,000 years ago.
Some of these eruptions have been powerful enough to cover up to 1000 square miles with pyroclastic flows of dacite and rhyolite. In some eruptions they were hot enough to produce welded deposits at distances of up to 20 miles from the vent! Fortunately, these caldera-forming eruptions are extremely rare, and there is no indication that one will occur in the foreseeable future. 
Contributor: Hobart King
Find it on Geology.com
More from Geology.com
|Olivine is a rock-forming mineral found in the crust, the mantle, and in some meteorites.
|Mount Cleveland is an active volcano in the Aleutian Islands and a threat to air traffic.
|Metals are important mineral products used in manufacturing and construction projects.
|Ash Plume from Pavlof's 2007 Eruption
|Pavlof volcano and an eruption plume photographed from a commercial flight on August 30, 2007. The plume is about 17,000 feet tall. Little Pavlof is the smaller peak on Pavlof's right shoulder. Eruptions like this are a severe hazard to local and international air traffic. Photograph by Chris Waythomas, Alaska Volcano Observatory / U.S. Geological Survey.
| Photograph of the three Pavlofs. From left: Pavlof Sister, Pavlof, and Little Pavlof (small peak on the right shoulder of Pavlof) as observed from Trader Mountain in August 2005 by Chris Waythomas.  Pavlof Sister and Little Pavlof have not erupted during recorded history but have probably erupted within the past 10,000 years. Alaska Volcano Observatory image.
|Pavlof Volcano - 1996 Eruption
| A photo of Pavlof Volcano taken on November 13, 1996. This image shows Pavlof's steep stratovolcano geometry. This eruption began on September 15, 1996 and ended on January 3, 1997. It produced numerous steam and ash eruptions, strombolian eruptions, lava fountains and lava flows. USGS image by Elgin Cook.|
|Facts About Pavlof Volcano
||Near the end of the Alaska Peninsula
||55° 25′ 0" N 161° 53′ 15" W
||2,519 meters (8,264 feet)
|Pavlof Volcano - 2007 Eruption
| Photograph of Pavlof Volcano (erupting), Pavlof Sister (left) and Little Pavlof (small peak on the right shoulder of Pavlof) taken on August 29, 2007 by Guy Tygat. Alaska Volcano Observatory image.
|Lahar runout deposit produced during the 2007 eruption at Pavlof. It is a sandy matrix-support deposit with a mix of volcanic ejecta and stream pebbles. Image by Chris Waythomas. USGS image. Enlarge.
|Map showing the geographic extent and locations of pyroclastic flow, surge and blast hazards around Pavlof and neighboring volcanoes. USGS image. Enlarge. Additional maps of lahar, debris-avalanche, ash fallout and other hazards are part of the Preliminary Volcano-Hazard Assessment for the Emmons Lake Volcanic Center report and map set. 
|Video of a lahar produced during the 2007 eruption of Pavlof. In the video you can observe the front of the lahar sweeeping down the channel. Other larger lahars exceeded the capacity of the channel and produced the sediment-covered landscape around the channel. Filmed by pilot Jeff Linscott of JL Aviation. Alaska Volcano Observatory video.|
|USGS topographic map of Pavlof and surrounding volcanic features. Enlarge.|
|More Information About Pavlof