Logo link to homepage

Ukinrek Maars

Photo of this volcano
  • Country
  • Primary Volcano Type
  • Last Known Eruption
  •  
  • 57.8344°N
  • 156.5203°W

  • 91 m
    299 ft

  • 312131
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number
Most Recent Weekly Report: 12 May-18 May 2021 Citation IconCite this Report

On 12 May AVO changed the Aviation Color Code and Volcano Alert Level for Ukinrek-Maars to Green and Normal, respectively, reflecting that communication with seismic stations had been re-established, allowing for the location of earthquakes and detection of unrest.

Source: US Geological Survey Alaska Volcano Observatory (AVO)


Most Recent Bulletin Report: May 1998 (BGVN 23:05) Citation IconCite this Report

Earthquake swarm decreases in rate and intensity

During the last week of May, the anomalous seismic activity under SW Lake Becharof (BGVN 23:04) continued but at a decreased rate and intensity; magnitudes of 12 located earthquakes ranged from M 1.7 to 3.3. During 1-5 June, 20 earthquakes were located ranging from M 1.8 to 4.3. Activity decreased significantly during 6-12 June; only four earthquakes were located, all M > 3.0. Several overflights of the location by AVO scientists revealed no signs of volcanic activity or surface breakage. The area of seismicity was not monitored by real-time seismic instrumentation; however, a portable seismic instrument has recently been installed. AVO is in communication with local citizens and land managers who frequently overfly the area. There was no evidence of imminent hazard at the site.

Information Contacts: Alaska Volcano Observatory (AVO), a cooperative program of a) U.S. Geological Survey, 4200 University Drive, Anchorage, AK 99508-4667, USA (URL: http://www.avo.alaska.edu/), b) Geophysical Institute, University of Alaska, PO Box 757320, Fairbanks, AK 99775-7320, USA, and c) Alaska Division of Geological & Geophysical Surveys, 794 University Ave., Suite 200, Fairbanks, AK 99709, USA.

Weekly Reports - Index


2021: April | May


12 May-18 May 2021 Citation IconCite this Report

On 12 May AVO changed the Aviation Color Code and Volcano Alert Level for Ukinrek-Maars to Green and Normal, respectively, reflecting that communication with seismic stations had been re-established, allowing for the location of earthquakes and detection of unrest.

Source: US Geological Survey Alaska Volcano Observatory (AVO)


14 April-20 April 2021 Citation IconCite this Report

AVO reported a loss of operation and communication with seismic stations that monitor Ukinrek-Maars, likely caused by snow cover. Both the Aviation Color Code and the Volcano Alert Level were changed to Unassigned on 19 April, reflecting the inability to locate earthquakes to detect unrest. Monitoring will continue with the remaining seismic stations, regional infrasound networks, lightning detection, and satellite images.

Source: US Geological Survey Alaska Volcano Observatory (AVO)


Bulletin Reports - Index

Reports are organized chronologically and indexed below by Month/Year (Publication Volume:Number), and include a one-line summary. Click on the index link or scroll down to read the reports.

03/1977 (NSEB 02:03) Explosions send ash plume above 6 km height

04/1977 (NSEB 02:04) Two new maars formed NW of Peulik volcano after 30 March

05/1977 (NSEB 02:05) Periodic earthquake swarms near the new vents

04/1998 (BGVN 23:04) Tectonic earthquake swarm in the Ukinrek Maars area

05/1998 (BGVN 23:05) Earthquake swarm decreases in rate and intensity




Information is preliminary and subject to change. All times are local (unless otherwise noted)


March 1977 (NSEB 02:03) Citation IconCite this Report

Explosions send ash plume above 6 km height

On 30 March, explosions were reported at 1500 and 1720 from a vent 13 km [but see 2:4] NW of Peulik volcano. The latter explosion was viewed from close range from a Wien Air Alaska plane. Its crew reported that the dense, ash-laden eruption cloud rose higher than 6,000 m. Peulik, an 1,844-m stratovolcano with a dacite lava dome, last erupted in 1852. It is surrounded by several small olivine andesite scoria cones.

Information Contacts: T. Miller, USGS, Anchorage.


April 1977 (NSEB 02:04) Citation IconCite this Report

Two new maars formed NW of Peulik volcano after 30 March

Two new maars formed in tundra terrain, 15 km NW of Peulik volcano, between 30 March and 9 April. Explosions were first observed on 30 March from 70 km SW of the eruption site. Pilots who overflew the eruption at 1725 and 1800 reported a single vent, 20-30 m in diameter, that emitted white steam, then a dark, ash-laden cloud that rose 6,000-7,500 m. Fine ash fell 135 km ESE of the vent, and a sulfurous haze layer lay over Kodiak (250 km E of the vent) all day. More ash clouds were seen on 1 and 2 April.

On 2 April, the original crater had filled with water and become quiescent, and a new 60-m-diameter vent had formed 500 m to the E. By the early afternoon of 3 April, the E crater had grown to about 100 m in diameter and contained a yellowish-orange lava lake. Fragments up to 1 m across were being ejected to 300 m height. Later in the afternoon, 15-20-m lava fountains were observed.

An ash cloud rising more than 4,000 m deposited traces of ash 95 km to the N on 5 April, but by 6 April activity had declined to steam emission and some ash explosions, which sent tephra to more than 1,000 m above the lava lake. Similar activity, including 30-m orange-red lava fountains, was reported on 7 April. No further eruptions were reported until the early morning of 9 April, when violent explosions of incandescent material were seen 30 km away.

A team of volcanologists from the University of Alaska and Dartmouth College visited the eruption site 14-21 April. The W crater was oblong (150 x 65 m) and filled with lukewarm, slightly acidic water. The E crater was about 250 m in diameter and 100 m deep. About 2/3 of its floor was occupied by a lava dome up to 40 m high that was degassing and was coated with sulfur and hematite. Ground water emerged from the crater walls at 50-70 m depth and cascaded onto the dome, where it flashed to steam. Occasional ash puffs were created by the caving of the steep crater walls. Blocks and boulders of highly variable composition and various degrees of rounding, and olivine basalt bombs with lithic cores, decreased in size from 1.5 m in diameter near the crater rims to about 50 cm diameter a few hundred meters away. Fist-sized cinders fell as far as 2 km away. Stripped bark, and mud with imbedded scoria plastered against tree trunks 500 m from the vents, indicate at least minor base surge activity during 1 or more explosions of the E crater.

Two portable short-period seismograph systems, which operated from 15-20 April, recorded a high level of microearthquake activity and three distinct earthquake swarms of several hours duration. More than 1 event per minute was recorded during the swarms. Many of the smaller events were shallow, but some of the larger ones showed S-P times indicating hypocenter depths between a few km and 20 km. Some of the larger events were also recorded by a permanent University of Alaska seismic station 25 km N of the eruption site.

Information Contacts: J. Kienle, Univ. of Alaska.


May 1977 (NSEB 02:05) Citation IconCite this Report

Periodic earthquake swarms near the new vents

When visited in late May, the E vent was filling with water. A glow could be seen through fractures in the E vent dome, which had ceased growing and was degassing less vigorously than in mid-April. The vents are located on the Bruin Bay Fault. Its projected trend cuts an area of about 12 new hot springs that have formed about 3 km to the N in Becharof Lake. Periodic earthquake swarms continued to occur in the vicinity of the new vents. A third seismograph station was added in late May to the two installed in April.

Further References. Kienle, J., Kyle, P.R., Self, S., Motyka, R.J., and Lorenz, V., 1980, Ukinrek Maars, Alaska, I. April 1977 eruption sequence, petrology and tectonic setting: JVGR, v. 7, p. 11-38.

Kienle, J., and Swanson, S.E., 1983, Volcanism in the eastern Aleutian Arc: late Quaternary and Holocene centers, tectonic setting, and petrology: JVGR, v. 17, p. 393-432. (This reference also contains data on Augustine and Iliamna.)

Self, S., Kienle, J., and Huot, J.P., 1980, Ukinrek Maars, Alaska, II. Deposits and formation of the 1977 craters: JVGR, v. 17, p. 39-66.

Information Contacts: J. Kienle, Univ. of Alaska.


April 1998 (BGVN 23:04) Citation IconCite this Report

Tectonic earthquake swarm in the Ukinrek Maars area

During 8-9 May, a seismic swarm of tectonic earthquakes shook the middle Alaskan Peninsula region including the towns of King Salmon, Dillingham, Egegik, and Pilot Point. The swarm began with five earthquakes of M 5.2-4.7 occurring between 1630 and 2259. Dozens of earthquakes in the M 2.5-3.5 range were felt locally. The earthquakes continued through 9 May, but the number of earthquakes had decreased notably by the morning of 10 May. Felt earthquakes were still occurring at a rate of 1-2/day as of the afternoon of 12 May.

The earthquakes were clustered on the SW shore of Lake Becharof, approximately 10-20 km NW of the 1977 Ukinrek Maars volcanoes and near the S end of the Bruin Bay fault. The earthquakes were all very shallow (<7 km in depth). In the past, the few local seismic stations have been able to accurately locate earthquakes only of magnitudes greater than M 4. The recent expansion of Alaska Volcano Observatory (AVO) volcano seismic monitoring to include volcanoes in Katmai National Park, NE of Lake Becharof, and Aniakchak Volcano, to the SW, has allowed better detection and location of Becharof earthquakes.

AVO scientists traveled to King Salmon on 9 May for an overflight of the swarm location and vicinity. Their U.S. Fish and Wildlife Service (FWS) pilot had overflown the area the evening of 8 May after the first earthquakes. Nothing indicating any volcanic activity or surface breakage was seen on either flight. Some small slumping was noticed along the SW shoreline of Lake Becharof and some local discoloration by sediments was seen both likely resulting from ground shaking. Similarly, a slight change in the green coloration of the crater lake in the large maar at Ukinrek Maars was likely due to disturbed sediments. No evidence of any disturbance or unusual activity was seen at Peulik volcano. Peulik is heavily snow-covered and showed no sign of discoloration, deformation, or slumping. The area of seismicity is not monitored by real-time seismic instrumentation; scientists scouted for possible locations to establish a temporary seismic net. The net will allow scientists to determine if there is a volcanic component to the earthquake swarm and any potential volcanic hazard. AVO is also in communication with citizens of King Salmon, Egegik, Meshik, and Pilot Point, as well as the National Park Service and FWS pilots who frequently overfly the area.

The preliminary interpretation is that the swarm was of tectonic origin, although the occurrence of five M 4.7-5.2 earthquakes in such a short time with no clear mainshock may suggest a volcanic component. Considering the nature of the formation of Ukinrek Maars in 1977, where no volcano existed previously, intrusion of magma associated with tectonic movement is possible. There is no evidence of imminent volcanic hazard from this seismic swarm.

Background. The May 1998 swarm was the most energetic to date. There were no major seismic events detected in association with the 1977 Ukinrek Maars eruptions, except for a number of small events detected by a portable seismic net which was deployed by the University of Alaska at Fairbanks (UAF) and the U.S. Geological Survey (USGS) for several months following the 1977 eruptions. Ukinrek Maars formed 30 March-10 April, 1977 as a result of magmatic intrusion into water-saturated glacial till 2 km S of Gas Rocks on the S shore of Lake Becharof. During a 10-day period, violent explosions produced steam and ash plumes as high as 6.5 km and light ash fall as far as 160 km to the N. Since the Ukinrek Maars formed, CO2 gas has been continuously emitted from the vicinity of the maars, the Gas Rocks, and from beneath Lake Becharof.

Information Contacts: Alaska Volcano Observatory (AVO), a cooperative program of a) U.S. Geological Survey, 4200 University Drive, Anchorage, AK 99508-4667, USA (URL: http://www.avo.alaska.edu/), b) Geophysical Institute, University of Alaska, PO Box 757320, Fairbanks, AK 99775-7320, USA, and c) Alaska Division of Geological & Geophysical Surveys, 794 University Ave., Suite 200, Fairbanks, AK 99709, USA; Roger Hansen, Geophysical Institute, University of Alaska, PO Box 757320, Fairbanks, AK 99775 USA.


May 1998 (BGVN 23:05) Citation IconCite this Report

Earthquake swarm decreases in rate and intensity

During the last week of May, the anomalous seismic activity under SW Lake Becharof (BGVN 23:04) continued but at a decreased rate and intensity; magnitudes of 12 located earthquakes ranged from M 1.7 to 3.3. During 1-5 June, 20 earthquakes were located ranging from M 1.8 to 4.3. Activity decreased significantly during 6-12 June; only four earthquakes were located, all M > 3.0. Several overflights of the location by AVO scientists revealed no signs of volcanic activity or surface breakage. The area of seismicity was not monitored by real-time seismic instrumentation; however, a portable seismic instrument has recently been installed. AVO is in communication with local citizens and land managers who frequently overfly the area. There was no evidence of imminent hazard at the site.

Information Contacts: Alaska Volcano Observatory (AVO), a cooperative program of a) U.S. Geological Survey, 4200 University Drive, Anchorage, AK 99508-4667, USA (URL: http://www.avo.alaska.edu/), b) Geophysical Institute, University of Alaska, PO Box 757320, Fairbanks, AK 99775-7320, USA, and c) Alaska Division of Geological & Geophysical Surveys, 794 University Ave., Suite 200, Fairbanks, AK 99709, USA.

This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.

Eruptive History

There is data available for 2 confirmed Holocene eruptive periods.

1977 Mar 30 - 1977 Apr 9 Confirmed Eruption Max VEI: 3

Episode 1 | Eruption Episode West and East Ukinrek Maars
1977 Mar 30 - 1977 Apr 9 Evidence from Observations: Reported

List of 11 Events for Episode 1 at West and East Ukinrek Maars

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion
   - - - -    - - - - Phreatic activity
   - - - -    - - - - Pyroclastic flow
   - - - -    - - - - Lava fountains
   - - - -    - - - - Lava lake
   - - - -    - - - - Lava dome
   - - - -    - - - - Ash
   - - - -    - - - - Bombs
   - - - -    - - - - Blocks
   - - - -    - - - - Earthquakes (undefined) After.
1977 Mar 30    - - - - VEI (Explosivity Index)

0350 BCE (?) Confirmed Eruption  

Episode 1 | Eruption Episode Gas Rocks
0350 BCE (?) - Unknown Evidence from Isotopic: 14C (uncalibrated)

List of 2 Events for Episode 1 at Gas Rocks

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Phreatic activity
   - - - -    - - - - Ash
Deformation History

There is no Deformation History data available for Ukinrek Maars.

Emission History

There is no Emissions History data available for Ukinrek Maars.

Photo Gallery

The 300-m-wide East Maar is one of the two Ukinrek Maars, which were formed during an eruption in 1977 through glacial deposits on the Alaska Peninsula. This fresh maar, in contrast to older ones whose rims have been modified by slumping and erosion, has steep-sided walls. The explosions blasted through the pre-existing, light-colored glacial till forming the bottom half of the distant crater wall and then deposited the dark, bedded layers in the upper half of the crater wall as well as the dark blanket of blocks and ash surrounding the maar.

Copyrighted photo by Katia and Maurice Krafft, 1978.
The Ukinrek Maars were formed during an eruption in 1977 at a Bering Sea lowland area without previous volcanic activity. Powerful phreatomagmatic explosions formed the 170-m-wide West Maar and 300-m-wide East Maar. The maars were named from the Yupik Eskimo words for "two holes in the ground." Late in the 10-day-long eruption a lava dome formed in East Maar, seen here from the NW rim with Peulik volcano in the background. The dome is now submerged beneath a 60-m-deep lake.

Copyrighted photo by Katia and Maurice Krafft, 1978.
French volcanologist Katia Krafft observes blocky ejecta from the 1977 eruptions that formed Ukinrek Maars. The 10-day-long eruption produced two new maars, 170-m-wide West Maar and 300-m-wide East Maar. Phreatomagmatic explosions formed an ejecta blanket of ash and blocks that surrounded the new vents.

Copyrighted photo by Katia and Maurice Krafft, 1978.
Phreatomagmatic eruptions produced when magma came in contact with groundwater eject an ash plume at the Ukinrek Maars on the Alaska Peninsula. This photo from the south on 5 April 1977 shows explosive eruptions from East Maar, one of two new craters that formed in glacial sediments, in an area without previous volcanic activity. The hummocky, snow-covered surface in the foreground is a debris avalanche deposit from Peulik.

Photo by Jim Faro (Alaska Department of Fish and Game).
An aerial view into East Maar on 3 April 1977 shows incandescent lava on the floor of the crater and a small vent above it that is producing an ash plume. The 1977 eruptions of Ukinrek Maars began on 30 March at West Maar, which formed during the first three days of the eruption. East Maar formed during the next seven days at a location 600 m E. A lava dome, now covered by a crater lake, formed on the floor of East Maar.

Photo by Ken Parker, 1977 (Alaska Department of Fish and Game).
Ukinrek Maars are two phreatomagmatic explosion craters that were created in an area without previous volcanic activity during a 10-day-long eruption that began on 30 March 1977. A greenish lake fills East Maar, the largest of the two in this 1994 view from the south. The smaller West Maar is surrounded by dark tephra near the left margin. Gas Rocks, an older volcanic center, forms the peninsula extending into Becharof Lake in the background.

Photo by Chris Nye, 1994 (Alaska Division of Geological and Geophysical Surveys, Alaska Volcano Observatory).
An ash plume erupts from eastern crater of the newly formed Ukinrek Maars on 6 April 1977. West Maar formed during the initial days of the eruption that began on 30 March. Three days later explosions began at East Maar, 600 m away. At the peak of the eruption ash plumes reached up to 6 km above the vent. On the 4th day of the eruption a lava dome appeared within East Maar.

Photo by R. Russell, 1977 (Alaska Department of Fish and Game).
The interaction of magma with groundwater produced this dark, ash-rich eruption column in 1977 from the Ukinrek Maars on the Alaska Peninsula. The eruption occurred in an area without previous volcanic activity, through surficial glacial deposits. The phreatomagmatic explosions created two new craters, which were named after the Yupik words for "two holes in the ground." This photo was taken from the WSW on 6 April 1977.

Photo by R. Russell, 1977 (Alaska Department of Fish and Game).
This lake-filled maar and another small crater (left) are the Ukinrek Maars, which formed during an eruption in 1977 in a lowland area of the Alaska Peninsula west of the main volcanic chain. The contact between lighter and darker material in the walls of the lake-filled eastern maar marks the original pre-eruption surface, which is now buried by a dark apron of ejecta produced during the eruption.

Photo by Christina Neal, 1993 (Alaska Volcano Observatory, U.S. Geological Survey).
GVP Map Holdings

The maps shown below have been scanned from the GVP map archives and include the volcano on this page. Clicking on the small images will load the full 300 dpi map. Very small-scale maps (such as world maps) are not included. The maps database originated over 30 years ago, but was only recently updated and connected to our main database. We welcome users to tell us if they see incorrect information or other problems with the maps; please use the Contact GVP link at the bottom of the page to send us email.

Smithsonian Sample Collections Database

There are no samples for Ukinrek Maars in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection.

External Sites