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Recent Kilauea Status Reports, Updates, and Information Releases
HAWAIIAN VOLCANO OBSERVATORY DAILY UPDATEThursday, January 15, 2009 8:23 AM HST (Thursday, January 15, 2009 18:23 UTC)
This report on the status of Kilauea volcanic activity, in addition to maps, photos, and webcam images (available using the menu bar above), was prepared by the USGS Hawaiian Volcano Observatory (HVO). Hawai`i Volcanoes National Park status can be found at http://www.nps.gov/havo/ or 985-6000. Hawai`i County Viewing Area status can be found at 961-8093.
KILAUEA VOLCANO (CAVW #1302-01-)
19°25'16" N 155°17'13" W, Summit Elevation 4091 ft (1247 m)
Current Aviation Color Code: ORANGE
Current Volcano Alert Level: WATCH
Activity Summary for past 24 hours: There were no significant changes. Sulfur dioxide emission rates from Halema`uma`u vent remain elevated above pre-2008 values; tephra production has stopped. At the east rift eruption site, sulfur dioxide emission rates from the Pu`u `O`o vents remain elevated. Lava from nearby east rift zone vents flows through tubes to the ocean; surface flows remain active on the coastal plain.
Past 24 hours at Kilauea summit: Due to southwesterly winds, high SO2 concentrations plagued the Kilauea Visitors Center persistently over the last day. Forecast wind conditions will result in continued poor air quality there today. The vent remained dark overnight, and vent temperatures measured yesterday were at background levels. This morning, heavy fog obscures views of the vent. GOES-WEST imagery indicates that the plume is blowing to the northeast over the Kilauea Visitors Center.
Sulfur dioxide emission rates remain elevated and variable. The most recent average measurement was 1,000 tonnes/day on January 13, still elevated above the 2003-2007 average rate of 140 tonnes/day.
The network of tiltmeters within the caldera has recorded no significant ground tilt over the past 2 days, since the end of a DI event on Tuesday. The GPS network (less sensitive than the tiltmeter network) has recorded about 2 cm of contraction across the caldera over the previous 3 months.
Only three earthquakes were located in the summit area during the past day, mostly in the central part of the caldera. Three earthquakes were also located beneath the east rift zone. Seismic tremor levels have been steady across the volcano over the past 24 hours. The number of RB2S2BL earthquakes remains at background values.
Past 24 hours at the middle east rift zone vents and flow field: Magma continues to degas through Pu`u `O`o Crater. The most recent sulfur dioxide emission rate measurement was 1,800 tonnes/day measured on January 7 compared to the 2003-2007 average of about 1,700 tonnes/day for this vent. No incandescence was observed within the crater overnight.
The tiltmeter on the north side of Pu`u `O`o recorded no changes in ground tilt. GPS stations spanning the crater (less sensitive than tiltmeters) have recorded about 2 cm of contraction over the past month. Seismic tremor levels near Pu`u `O`o and the TEB vent remain at low and steady values.
Lava from the TEB vent and the rootless shield complex flows through tubes to the ocean. Variable winds again shut down the County Viewing Area yesterday. An overflight on Wednesday morning confirmed the presence of active lava on the coastal plain, and a thermal anomaly in overnight GOES-WEST imagery indicates continuing surface flow activity. West of the currently active Waikupanaha entry, surface lava flows have stalled within 150 meters of the ocean.
HAZARD ALERT: The lava delta and adjacent areas both inland and out to sea are still some of the most hazardous areas on the flow field. Frequent delta/bench collapses give little warning, can produce hot rock falls inland and in the adjacent ocean and can produce large but local waves. The steam plume produced by lava entering the ocean contains fine lava fragments and an assortment of acid droplets that can be harmful to your health. The rapidly changing conditions near the ocean entry have been responsible for many injuries and a few deaths.
Maps, photos, webcam views, and other information about Kilauea Volcano are available at http://volcano.wr.usgs.gov/kilaueastatus.php. A daily update summary is available by phone at (808) 967-8862.
A map with details of earthquakes located within the past two weeks can be found at http://tux.wr.usgs.gov/
A definition of alert levels can be found at http://volcanoes.usgs.gov/2006/warnschemes.html
The Hawaiian Volcano Observatory is one of five volcano observatories within the U.S. Geological Survey and is responsible for monitoring volcanoes and earthquakes in Hawai`i.
HAWAIIAN VOLCANO OBSERVATORY DAILY UPDATEWednesday, January 14, 2009 7:08 AM HST (Wednesday, January 14, 2009 17:08 UTC)
This report on the status of Kilauea volcanic activity, in addition to maps, photos, and webcam images (available using the menu bar above), was prepared by the USGS Hawaiian Volcano Observatory (HVO). Hawai`i Volcanoes National Park status can be found at http://www.nps.gov/havo/ or 985-6000. Hawai`i County Viewing Area status can be found at 961-8093.
KILAUEA VOLCANO (CAVW #1302-01-)
19°25'16" N 155°17'13" W, Summit Elevation 4091 ft (1247 m)
Current Aviation Color Code: ORANGE
Current Volcano Alert Level: WATCH
Activity Summary for past 24 hours: There were no significant changes. Sulfur dioxide emission rates from Halema`uma`u vent remain elevated above pre-2008 values; tephra production has stopped. At the east rift eruption site, sulfur dioxide emission rates from the Pu`u `O`o vents remain elevated. Lava from nearby east rift zone vents flows through tubes to the ocean; surface flows remain active on the coastal plain.
Past 24 hours at Kilauea summit: Yesterday, southwesterly winds produced high SO2 concentrations intermittently at the Kilauea Visitors Center; since then, air quality has been better but still moderately bad. The vent remained dark overnight. This morning, the white plume is still blowing to the northeast over the Kilauea Visitors Center.
Sulfur dioxide emission rates remain elevated and variable. The most recent average measurement was 1,000 tonnes/day on January 13, still elevated above the 2003-2007 average rate of 140 tonnes/day.
The network of tiltmeters within the caldera recorded no coherent tilting after completion of the DI event yesterday. The GPS receiver networks (less sensitive than tiltmeters) recorded more than 2 cm of contraction across the caldera over the previous 3 months.
Seismic activity continues to be focused on the south caldera; tremor levels decreased abruptly at 1:35 am this morning but remain elevated. The number of RB2S2BL earthquakes remain at background values. A total of 10 earthquakes were strong enough to be located beneath Kilauea or nearby, with 4 beneath the summit caldera and 2 on south flank faults.
Past 24 hours at the middle east rift zone vents and flow field: Magma continues to degas through Pu`u `O`o Crater. The most recent sulfur dioxide emission rate measurement was 1,800 tonnes/day measured on January 7 compared to the 2003-2007 average of about 1,700 tonnes/day for this vent. No incandescence was observed within the crater overnight.
The tiltmeter on the north side of Pu`u `O`o recorded weak tilting inward toward the crater. GPS stations spanning the crater (less sensitive than tiltmeters) recorded more than 4 cm of contraction over the past 3 months and about 1.5 cm of contraction in the past two weeks. Seismic tremor levels near Pu`u `O`o and the TEB vent remain at low values.
Lava from the TEB vent and the rootless shield complex flows through tubes to the ocean. Variable winds again shut down the County Viewing Area yesterday. GOES-WEST imagery showed a strong thermal anomaly overnight suggesting continuing surface flow activity on the coastal plain.
HAZARD ALERT: The lava delta and adjacent areas both inland and out to sea are still some of the most hazardous areas on the flow field. Frequent delta/bench collapses give little warning, can produce hot rock falls inland and in the adjacent ocean and can produce large but local waves. The steam plume produced by lava entering the ocean contains fine lava fragments and an assortment of acid droplets that can be harmful to your health. The rapidly changing conditions near the ocean entry have been responsible for many injuries and a few deaths.
Maps, photos, webcam views, and other information about Kilauea Volcano are available at http://volcano.wr.usgs.gov/kilaueastatus.php. A daily update summary is available by phone at (808) 967-8862.
A map with details of earthquakes located within the past two weeks can be found at http://tux.wr.usgs.gov/
A definition of alert levels can be found at http://volcanoes.usgs.gov/2006/warnschemes.html
The Hawaiian Volcano Observatory is one of five volcano observatories within the U.S. Geological Survey and is responsible for monitoring volcanoes and earthquakes in Hawai`i.
HAWAIIAN VOLCANO OBSERVATORY DAILY UPDATETuesday, January 13, 2009 8:10 AM HST (Tuesday, January 13, 2009 18:10 UTC)
This report on the status of Kilauea volcanic activity, in addition to maps, photos, and webcam images (available using the menu bar above), was prepared by the USGS Hawaiian Volcano Observatory (HVO). Hawai`i Volcanoes National Park status can be found at http://www.nps.gov/havo/ or 985-6000. Hawai`i County Viewing Area status can be found at 961-8093.
KILAUEA VOLCANO (CAVW #1302-01-)
19°25'16" N 155°17'13" W, Summit Elevation 4091 ft (1247 m)
Current Aviation Color Code: ORANGE
Current Volcano Alert Level: WATCH
Activity Summary for past 24 hours: There were no significant changes. Sulfur dioxide emission rates from Halema`uma`u vent remain elevated above pre-2008 values; tephra production has stopped. At the east rift eruption site, sulfur dioxide emission rates from the Pu`u `O`o vents remain elevated. Lava from nearby east rift zone vents flows through tubes to the ocean; surface flows remain active on the coastal plain.
Past 24 hours at Kilauea summit: Variable winds produced SO2 concentrations high enough to close the Jaggar Museum yesterday around noon; since then, air quality has been better but still moderately bad. The vent remained dark overnight. This morning, the white plume is blowing to the northeast over the Kilauea Visitors Center.
Sulfur dioxide emission rates remain elevated and variable. The most recent average measurement was 800 tonnes/day on January 7, still elevated above the 2003-2007 average rate of 140 tonnes/day. The next emission rate measurement will await the return of moderate trade winds.
The network of tiltmeters within the caldera recorded sharp DI inflation beginning at about 3:15 pm yesterday. The GPS receiver networks (less sensitive than tiltmeters) recorded more than 2 cm of contraction across the caldera over the previous 3 months along with a slight contraction and extension mimicking the DI tilt deflation and inflation.
Seismic activity continues to be focused on the south caldera; tremor levels remain elevated. The number of RB2S2BL earthquakes decreased to background values by this morning. A total of 8 earthquakes were strong enough to be located beneath Kilauea or nearby, with 5 beneath the summit caldera and 3 beneath the upper east rift zone.
Past 24 hours at the middle east rift zone vents and flow field: Magma continues to degas through Pu`u `O`o Crater. The most recent sulfur dioxide emission rate measurement was 1,800 tonnes/day measured on January 7 compared to the 2003-2007 average of about 1,700 tonnes/day for this vent. No incandescence was observed within the crater overnight.
The tiltmeter on the north side of Pu`u `O`o mimicked the DI tilt signal recorded at the summit but delayed by a little more than an hour. GPS stations spanning the crater (less sensitive than tiltmeters) recorded more than 4 cm of contraction over the past 3 months and about 1.5 cm of contraction in the past two weeks. Seismic tremor levels near Pu`u `O`o and the TEB vent remain at low values.
Lava from the TEB vent and the rootless shield complex flows through tubes to the ocean. Variable winds shut down the County Viewing Area at 4 pm yesterday. GOES-WEST imagery showed a persistent thermal anomaly overnight suggesting continuing surface flow activity on the coastal plain; the size of the anomaly seemed to decrease and its intensity appeared to weaken possibly suggesting that surface activity waned in response to the DI event. This morning, the Waikupanaha plume is going steady and there is no evidence of a second plume.
HAZARD ALERT: The lava delta and adjacent areas both inland and out to sea are still some of the most hazardous areas on the flow field. Frequent delta/bench collapses give little warning, can produce hot rock falls inland and in the adjacent ocean and can produce large but local waves. The steam plume produced by lava entering the ocean contains fine lava fragments and an assortment of acid droplets that can be harmful to your health. The rapidly changing conditions near the ocean entry have been responsible for many injuries and a few deaths.
Definitions of terms used in the update:
HAVO: Hawai`i Volcanoes National Park
UHH: University of Hawai`i at Hilo
glow: light from an unseen source; indirect light.
FLIR: Forward Looking InfraRed, a camera which directly images heat rather than visible light. If volcanic fume is not too rich in water vapor, a FLIR can see through it to image hot surfaces.
pali: Hawaiian word for cliff or steep incline. In the context of the TEB flow field, 'pali' usually refers to Pulama pali that bisects the abandoned Royal Gardens subdivision.
CD: Hawai`i County Civil Defense
DOH air quality monitoring: see Hawai`i State Department of Health Air Quality website http://hawaii.gov/doh/air-quality/index.html .
bomb: lava fragment ejected into the air while molten acquiring aerodynamic shapes in flight; the term is restricted to pieces larger than 6.4 cm (2.5 in.). See http://volcanoes.usgs.gov/Products/Pglossary/bomb.html
hybrid, or explosion, seismic signals: complex earthquakes that are a hybrid of different signals. They start as a high frequency earthquake, similar to typical rock-breaking or rock fall events, that transitions to very long, 20-30 second, period (VLP) oscillations that continue for several minutes. At HVO, we observed these signals with the four small Halema`uma`u explosive eruptions in March, April, and August 2008. Several more similar signals, some as strong as the explosion signals associated with the four explosive eruptions, have been recorded without obvious evidenceof surface eruption such as rock fragments or other debris.
MODIS satellite: a NASA satellite pair, Aqua and Terra, which passes over Hawai`i twice a day. During daylight hours, the images are taken at about 11 am and 2 pm H.s.t. This imagery can be viewed about 3-5 hours after acquisition at http://rapidfire.sci.gsfc.nasa.gov/subsets/?subset=AERONET_Mauna_Loa.
GOES-WEST satellite: a geostationary NOAA satellite used most often for weather tracking. Images are typically acquired every 15 minutes. The loop http://www.ssd.noaa.gov/VAAC/kilauea/sloop-vis.html is posted by the Washington DC Volcanic Ash Advisory Center for the purpose of tracking emissions from Hawai`i volcanoes. The imagery automatically switches from infrared at night to visual during the day. Recently, it has been useful for tracking volcanic gas emissions from Halema`uma`u, Pu`u `O`o, and the Waikupanaha ocean entry during the day and hot lava flows at night.
Volcano Watch: weekly newspaper-like article written by HVO scientists on a volcano topic of interest. These articles are usually printed in the Sunday editions of the Hawai`i Island newspapers Hawaii Tribune Herald and West Hawaii Today. More than 800 of these articles have been written and are archived on the HVO website (menu at the bottom of the homepage hvo.wr.usgs.gov).
VLP seismic tremor: seismic tremor is continuous ground vibrations simultaneously at many different frequencies. VLP is a very long period or very low frequency component which, at the Halema`uma`u vent, has a period of 20-30 seconds or a frequency of 0.03-0.05 cycles per second (Hertz or Hz).
RB2S2BL earthquakes: earthquakes that were recorded but were too small to be located. These quakes have magnitudes less than 1.7 and may only be recorded by one or two seismometers. Recording at a minimum of 4 seismometer sites is required to locate an earthquake.
wink: an abrupt shutting off of incandescence at a vent lasting for several minutes. At the Halema`uma`u vent, winks usually start with or immediately follow a small, local earthquake. The diminishment of incandescence is due to the plume changing from translucent to opaque with rock dust.
tonne: metric unit equal to 1,000 kilograms, 2,204.6 lbs, or 1.1 English tons.
microradian: a measure of angle equivalent to 0.000057 degrees.
ppm: parts-per-million; 10,000 ppm = 1 %.
littoral cone: usually small cones built near active ocean entries; the cones are constructed of tephra from steam explosions that are sometimes produced when 1,150 degree C lava enters the 25 degree C ocean.
incandescence: the production of visible light from a hot surface. The term also refers to the light emitted from a hot surface. The color of the light is related to surface temperature. Some surfaces can display dull red incandescence at temperatures as low as 430 degrees Centigrade (806 degrees Fahrenheit). By contrast, molten lava displays bright orange to orange-yellow light from surfaces that are hotter than 900 degrees C (1,650 degrees F).
tephra: all material deposited by fallout from an eruption-related plume, regardless of size.
ash: tephra less than 2 mm (5/64 inches) in size.
TEB: Thanksgiving Eve Breakout, the designation used for lava flows that started with a breakout on November 21, 2007.
DI tilt event: DI is an abbreviation for 'deflation-inflation' and describes a volcanic event of uncertain significance. DI events are recorded by tiltmeters at Kilauea summit as an abrupt deflation of up to a few microradians in magnitude lasting several hours to 2-3 days followed by an abrupt inflation of approximately equal magnitude. The tilt events are usually accompanied by an increase in summit tremor during the deflation phase. A careful analysis of these events suggests that they may be related to changes in magma supply to a storage reservoir at less than 1 km depth, just east of Halema`uma`u crater. Usually, though not always, these changes propagate through the magma conduit from the summit to the eruption site, as many of the DI events at Kilauea summit are also recorded at a tiltmeter at Pu`u `O`o, delayed by 1-2 hours. DI events often correlate with lava pulses and/or pauses in the eruption at the Pu`u `O`o/July 21/TEB vents.
Maps, photos, webcam views, and other information about Kilauea Volcano are available at http://volcano.wr.usgs.gov/kilaueastatus.php. A daily update summary is available by phone at (808) 967-8862.
A map with details of earthquakes located within the past two weeks can be found at http://tux.wr.usgs.gov/
A definition of alert levels can be found at http://volcanoes.usgs.gov/2006/warnschemes.html
The Hawaiian Volcano Observatory is one of five volcano observatories within the U.S. Geological Survey and is responsible for monitoring volcanoes and earthquakes in Hawai`i.
HAWAIIAN VOLCANO OBSERVATORY DAILY UPDATE
Monday, January 12, 2009 07:50 HST (Monday, January 12, 2009 17:50 UTC)
KILAUEA VOLCANO (CAVW#1302-01-)
19.42°N 155.29°W, Summit Elevation 4091 ft (1247 m)
Volcano Alert Level: WATCH
Aviation Color Code: ORANGE
This report on the status of Kilauea volcanic activity, in addition to maps, photos, and webcam images (available using the menu bar above), was prepared by the USGS Hawaiian Volcano Observatory (HVO). Hawai`i Volcanoes National Park status can be found at http://www.nps.gov/havo/ or 985-6000. Hawai`i County Viewing Area status can be found at 961-8093.
Activity Summary for past 24 hours: There were no significant changes. Sulfur dioxide emission rates from Halema`uma`u vent remain elevated above pre-2008 values; tephra production has stopped. At the east rift eruption site, sulfur dioxide emission rates from the Pu`u `O`o vents remain elevated. Lava from nearby east rift zone vents flows through tubes to the ocean; surface flows remain active on the coastal plain.
Past 24 hours at Kilauea summit: Variable winds continued through yesterday and overnight to produce several episodes of unhealthy air quality in summit communities. The vent remained dark overnight. This morning, the white plume is vertically into low haze.
Sulfur dioxide emission rates remain elevated and variable. The most recent average measurement was 800 tonnes/day on January 7, still elevated above the 2003-2007 average rate of 140 tonnes/day. The next emission rate measurement will await the return of moderate trade winds.
Production of tephra essentially stopped in mid December although rockfalls within the vent continue. Views into the vent at the end of December using an infrared camera show that the conduit is closed by rubble deep beneath the Halema`uma`u Crater floor.
The network of tiltmeters within the caldera recorded sharp deflation beginning at 5:30 am this morning; this may be the start of a DI tilt event. The GPS receiver networks (less sensitive than tiltmeters) recorded more than 2 cm of contraction across the caldera over the previous 3 months; contraction may have occurred at a slightly increased rate over the past few weeks.
Seismic activity continues to be focused on the south caldera; tremor levels remain elevated. The number of RB2S2BL earthquakes remain elevated. A total of 11 earthquakes were strong enough to be located beneath Kilauea or nearby, with 2 beneath the summit caldera and 4 on south flank faults.
Past 24 hours at the middle east rift zone vents and flow field: Magma continues to degas through Pu`u `O`o Crater. The most recent sulfur dioxide emission rate measurement was 1,800 tonnes/day measured on January 7 compared to the 2003-2007 average of about 1,700 tonnes/day for this vent. No incandescence was observed within the crater overnight.
The tiltmeter on the north side of Pu`u `O`o recorded tilting inward toward the crater. GPS stations spanning the crater (less sensitive than tiltmeters) recorded more than 4 cm of contraction over the past 3 months and about 1.5 cm of contraction in the past two weeks. Seismic tremor levels near Pu`u `O`o and the TEB vent remain at low values.
Lava from the TEB vent and the rootless shield complex flows through tubes to the ocean. esterday morning, HVO geologists found that the Prince (west) lobe had advanced to a point that is 160 m (525 ft) from the shoreline. GOES-WEST imagery showed a persistent thermal anomaly overnight suggesting continuing surface flow activity on the coastal plain. This morning, CD officials report that the Waikupanaha entry is active but don't see a second entry yet.
HAZARD ALERT: The lava delta and adjacent areas both inland and out to sea are still some of the most hazardous areas on the flow field. Frequent delta/bench collapses give little warning, can produce hot rock falls inland and in the adjacent ocean and can produce large but local waves. The steam plume produced by lava entering the ocean contains fine lava fragments and an assortment of acid droplets that can be harmful to your health. The rapidly changing conditions near the ocean entry have been responsible for many injuries and a few deaths.
Definitions of terms used in the update:
HAVO: Hawai`i Volcanoes National Park
UHH: University of Hawai`i at Hilo
glow: light from an unseen source; indirect light.
FLIR: Forward Looking InfraRed, a camera which directly images heat rather than visible light. If volcanic fume is not too rich in water vapor, a FLIR can see through it to image hot surfaces.
pali: Hawaiian word for cliff or steep incline. In the context of the TEB flow field, 'pali' usually refers to Pulama pali that bisects the abandoned Royal Gardens subdivision.
CD: Hawai`i County Civil Defense
DOH air quality monitoring: see Hawai`i State Department of Health Air Quality website http://hawaii.gov/doh/air-quality/index.html .
bomb: lava fragment ejected into the air while molten acquiring aerodynamic shapes in flight; the term is restricted to pieces larger than 6.4 cm (2.5 in.). See http://volcanoes.usgs.gov/Products/Pglossary/bomb.html
hybrid, or explosion, seismic signals: complex earthquakes that are a hybrid of different signals. They start as a high frequency earthquake, similar to typical rock-breaking or rock fall events, that transitions to very long, 20-30 second, period (VLP) oscillations that continue for several minutes. At HVO, we observed these signals with the four small Halema`uma`u explosive eruptions in March, April, and August 2008. Several more similar signals, some as strong as the explosion signals associated with the four explosive eruptions, have been recorded without obvious evidenceof surface eruption such as rock fragments or other debris.
MODIS satellite: a NASA satellite pair, Aqua and Terra, which passes over Hawai`i twice a day. During daylight hours, the images are taken at about 11 am and 2 pm H.s.t. This imagery can be viewed about 3-5 hours after acquisition at http://rapidfire.sci.gsfc.nasa.gov/subsets/?subset=AERONET_Mauna_Loa.
GOES-WEST satellite: a geostationary NOAA satellite used most often for weather tracking. Images are typically acquired every 15 minutes. The loop http://www.ssd.noaa.gov/VAAC/kilauea/sloop-vis.html is posted by the Washington DC Volcanic Ash Advisory Center for the purpose of tracking emissions from Hawai`i volcanoes. The imagery automatically switches from infrared at night to visual during the day. Recently, it has been useful for tracking volcanic gas emissions from Halema`uma`u, Pu`u `O`o, and the Waikupanaha ocean entry during the day and hot lava flows at night.
Volcano Watch: weekly newspaper-like article written by HVO scientists on a volcano topic of interest. These articles are usually printed in the Sunday editions of the Hawai`i Island newspapers Hawaii Tribune Herald and West Hawaii Today. More than 800 of these articles have been written and are archived on the HVO website (menu at the bottom of the homepage hvo.wr.usgs.gov).
VLP seismic tremor: seismic tremor is continuous ground vibrations simultaneously at many different frequencies. VLP is a very long period or very low frequency component which, at the Halema`uma`u vent, has a period of 20-30 seconds or a frequency of 0.03-0.05 cycles per second (Hertz or Hz).
RB2S2BL earthquakes: earthquakes that were recorded but were too small to be located. These quakes have magnitudes less than 1.7 and may only be recorded by one or two seismometers. Recording at a minimum of 4 seismometer sites is required to locate an earthquake.
wink: an abrupt shutting off of incandescence at a vent lasting for several minutes. At the Halema`uma`u vent, winks usually start with or immediately follow a small, local earthquake. The diminishment of incandescence is due to the plume changing from translucent to opaque with rock dust.
tonne: metric unit equal to 1,000 kilograms, 2,204.6 lbs, or 1.1 English tons.
microradian: a measure of angle equivalent to 0.000057 degrees.
ppm: parts-per-million; 10,000 ppm = 1 %.
littoral cone: usually small cones built near active ocean entries; the cones are constructed of tephra from steam explosions that are sometimes produced when 1,150 degree C lava enters the 25 degree C ocean.
incandescence: the production of visible light from a hot surface. The term also refers to the light emitted from a hot surface. The color of the light is related to surface temperature. Some surfaces can display dull red incandescence at temperatures as low as 430 degrees Centigrade (806 degrees Fahrenheit). By contrast, molten lava displays bright orange to orange-yellow light from surfaces that are hotter than 900 degrees C (1,650 degrees F).
tephra: all material deposited by fallout from an eruption-related plume, regardless of size.
ash: tephra less than 2 mm (5/64 inches) in size.
TEB: Thanksgiving Eve Breakout, the designation used for lava flows that started with a breakout on November 21, 2007.
DI tilt event: DI is an abbreviation for 'deflation-inflation' and describes a volcanic event of uncertain significance. DI events are recorded by tiltmeters at Kilauea summit as an abrupt deflation of up to a few microradians in magnitude lasting several hours to 2-3 days followed by an abrupt inflation of approximately equal magnitude. The tilt events are usually accompanied by an increase in summit tremor during the deflation phase. A careful analysis of these events suggests that they may be related to changes in magma supply to a storage reservoir at less than 1 km depth, just east of Halema`uma`u crater. Usually, though not always, these changes propagate through the magma conduit from the summit to the eruption site, as many of the DI events at Kilauea summit are also recorded at a tiltmeter at Pu`u `O`o, delayed by 1-2 hours. DI events often correlate with lava pulses and/or pauses in the eruption at the Pu`u `O`o/July 21/TEB vents.
Maps, photos, webcam views, and other information about Kilauea Volcano are available at http://volcano.wr.usgs.gov/kilaueastatus.php. A daily update summary is available by phone at (808) 967-8862.
A map with details of earthquakes located within the past two weeks can be found at http://tux.wr.usgs.gov/
A definition of alert levels can be found at http://volcanoes.usgs.gov/2006/warnschemes.html
HAWAIIAN VOLCANO OBSERVATORY DAILY UPDATE
Sunday, January 11, 2009 07:32 HST (Sunday, January 11, 2009 17:32 UTC)
KILAUEA VOLCANO (CAVW#1302-01-)
19.42°N 155.29°W, Summit Elevation 4091 ft (1247 m)
Volcano Alert Level: WATCH
Aviation Color Code: ORANGE
This report on the status of Kilauea volcanic activity, in addition to maps, photos, and webcam images (available using the menu bar above), was prepared by the USGS Hawaiian Volcano Observatory (HVO). Hawai`i Volcanoes National Park status can be found at http://www.nps.gov/havo/ or 985-6000. Hawai`i County Viewing Area status can be found at 961-8093.
Activity Summary for past 24 hours: There were no significant changes. Sulfur dioxide emission rates from Halema`uma`u vent remain elevated above pre-2008 values; tephra production has stopped. At the east rift eruption site, sulfur dioxide emission rates from the Pu`u `O`o vents remain elevated. Lava from nearby east rift zone vents flows through tubes to the ocean; surface flows remain active on the coastal plain.
Past 24 hours at Kilauea summit: Southerly and westerly winds yesterday produced some spectacularly bad air quality in summit communities and Kulani Prison. The vent remained dark overnight. This morning, the white plume is heading to the northeast toward Kilauea Iki.
Sulfur dioxide emission rates remain elevated and variable. The most recent average measurement was 800 tonnes/day on January 7, still elevated above the 2003-2007 average rate of 140 tonnes/day.
Production of tephra has essentially stopped although rockfalls within the vent continue. Recent views into the vent using an infrared camera show that the conduit is closed by rubble deep beneath the Halema`uma`u Crater floor.
The network of tiltmeters within the caldera recorded weak tilting inward toward the south caldera reflecting weak deflation. The GPS receiver networks (less sensitive than tiltmeters) recorded a total of 2 cm of contraction across the caldera over the previous 3 months.
Seismic activity continues to be focused on the south caldera; tremor levels remain elevated. The number of RB2S2BL earthquakes nearly doubled between 08:30 am and 10 pm yesterday. A total of 15 earthquakes were strong enough to be located beneath Kilauea or nearby, with 8 beneath the summit caldera and 3 on south flank faults.
Past 24 hours at the middle east rift zone vents and flow field: Magma continues to degas through Pu`u `O`o Crater. The most recent sulfur dioxide emission rate measurement was 1,800 tonnes/day measured on January 7 compared to the 2003-2007 average of about 1,700 tonnes/day for this vent. No incandescence was observed within the crater overnight.
The tiltmeter on the north side of Pu`u `O`o continued to record rain-induced tilting in a direction outward from the crater; 6 cm (2.4 in) of rain fell at Pu`u `O`o in the past 32 hours. GPS stations spanning the crater (less sensitive than tiltmeters) recorded more than 4 cm of contraction over the past 3 months and about 1.5 cm of contraction in the past two weeks. Seismic tremor levels near Pu`u `O`o and the TEB vent remain at low values.
Lava from the TEB vent and the rootless shield complex flows through tubes to the ocean. Last night, CD officials noted several sources of incandescence on the pali and the coastal plain and glow and occasional explosions from the Waikupanaha ocean entry. GOES-WEST imagery showed a persistent thermal anomaly overnight suggesting continuing surface flow activity on the coastal plain. This morning, CD officials report cloudy and rainy conditions preventing views of the ocean entry plume.
HAZARD ALERT: The lava delta and adjacent areas both inland and out to sea are still some of the most hazardous areas on the flow field. Frequent delta/bench collapses give little warning, can produce hot rock falls inland and in the adjacent ocean and can produce large but local waves. The steam plume produced by lava entering the ocean contains fine lava fragments and an assortment of acid droplets that can be harmful to your health. The rapidly changing conditions near the ocean entry have been responsible for many injuries and a few deaths.
Definitions of terms used in the update:
HAVO: Hawai`i Volcanoes National Park
UHH: University of Hawai`i at Hilo
glow: light from an unseen source; indirect light.
FLIR: Forward Looking InfraRed, a camera which directly images heat rather than visible light. If volcanic fume is not too rich in water vapor, a FLIR can see through it to image hot surfaces.
pali: Hawaiian word for cliff or steep incline. In the context of the TEB flow field, 'pali' usually refers to Pulama pali that bisects the abandoned Royal Gardens subdivision.
CD: Hawai`i County Civil Defense
DOH air quality monitoring: see Hawai`i State Department of Health Air Quality website http://hawaii.gov/doh/air-quality/index.html .
bomb: lava fragment ejected into the air while molten acquiring aerodynamic shapes in flight; the term is restricted to pieces larger than 6.4 cm (2.5 in.). See http://volcanoes.usgs.gov/Products/Pglossary/bomb.html
hybrid, or explosion, seismic signals: complex earthquakes that are a hybrid of different signals. They start as a high frequency earthquake, similar to typical rock-breaking or rock fall events, that transitions to very long, 20-30 second, period (VLP) oscillations that continue for several minutes. At HVO, we observed these signals with the four small Halema`uma`u explosive eruptions in March, April, and August 2008. Several more similar signals, some as strong as the explosion signals associated with the four explosive eruptions, have been recorded without obvious evidenceof surface eruption such as rock fragments or other debris.
MODIS satellite: a NASA satellite pair, Aqua and Terra, which passes over Hawai`i twice a day. During daylight hours, the images are taken at about 11 am and 2 pm H.s.t. This imagery can be viewed about 3-5 hours after acquisition at http://rapidfire.sci.gsfc.nasa.gov/subsets/?subset=AERONET_Mauna_Loa.
GOES-WEST satellite: a geostationary NOAA satellite used most often for weather tracking. Images are typically acquired every 15 minutes. The loop http://www.ssd.noaa.gov/VAAC/kilauea/sloop-vis.html is posted by the Washington DC Volcanic Ash Advisory Center for the purpose of tracking emissions from Hawai`i volcanoes. The imagery automatically switches from infrared at night to visual during the day. Recently, it has been useful for tracking volcanic gas emissions from Halema`uma`u, Pu`u `O`o, and the Waikupanaha ocean entry during the day and hot lava flows at night.
Volcano Watch: weekly newspaper-like article written by HVO scientists on a volcano topic of interest. These articles are usually printed in the Sunday editions of the Hawai`i Island newspapers Hawaii Tribune Herald and West Hawaii Today. More than 800 of these articles have been written and are archived on the HVO website (menu at the bottom of the homepage hvo.wr.usgs.gov).
VLP seismic tremor: seismic tremor is continuous ground vibrations simultaneously at many different frequencies. VLP is a very long period or very low frequency component which, at the Halema`uma`u vent, has a period of 20-30 seconds or a frequency of 0.03-0.05 cycles per second (Hertz or Hz).
RB2S2BL earthquakes: earthquakes that were recorded but were too small to be located. These quakes have magnitudes less than 1.7 and may only be recorded by one or two seismometers. Recording at a minimum of 4 seismometer sites is required to locate an earthquake.
wink: an abrupt shutting off of incandescence at a vent lasting for several minutes. At the Halema`uma`u vent, winks usually start with or immediately follow a small, local earthquake. The diminishment of incandescence is due to the plume changing from translucent to opaque with rock dust.
tonne: metric unit equal to 1,000 kilograms, 2,204.6 lbs, or 1.1 English tons.
microradian: a measure of angle equivalent to 0.000057 degrees.
ppm: parts-per-million; 10,000 ppm = 1 %.
littoral cone: usually small cones built near active ocean entries; the cones are constructed of tephra from steam explosions that are sometimes produced when 1,150 degree C lava enters the 25 degree C ocean.
incandescence: the production of visible light from a hot surface. The term also refers to the light emitted from a hot surface. The color of the light is related to surface temperature. Some surfaces can display dull red incandescence at temperatures as low as 430 degrees Centigrade (806 degrees Fahrenheit). By contrast, molten lava displays bright orange to orange-yellow light from surfaces that are hotter than 900 degrees C (1,650 degrees F).
tephra: all material deposited by fallout from an eruption-related plume, regardless of size.
ash: tephra less than 2 mm (5/64 inches) in size.
TEB: Thanksgiving Eve Breakout, the designation used for lava flows that started with a breakout on November 21, 2007.
DI tilt event: DI is an abbreviation for 'deflation-inflation' and describes a volcanic event of uncertain significance. DI events are recorded by tiltmeters at Kilauea summit as an abrupt deflation of up to a few microradians in magnitude lasting several hours to 2-3 days followed by an abrupt inflation of approximately equal magnitude. The tilt events are usually accompanied by an increase in summit tremor during the deflation phase. A careful analysis of these events suggests that they may be related to changes in magma supply to a storage reservoir at less than 1 km depth, just east of Halema`uma`u crater. Usually, though not always, these changes propagate through the magma conduit from the summit to the eruption site, as many of the DI events at Kilauea summit are also recorded at a tiltmeter at Pu`u `O`o, delayed by 1-2 hours. DI events often correlate with lava pulses and/or pauses in the eruption at the Pu`u `O`o/July 21/TEB vents.
Maps, photos, webcam views, and other information about Kilauea Volcano are available at http://volcano.wr.usgs.gov/kilaueastatus.php. A daily update summary is available by phone at (808) 967-8862.
A map with details of earthquakes located within the past two weeks can be found at http://tux.wr.usgs.gov/
A definition of alert levels can be found at http://volcanoes.usgs.gov/2006/warnschemes.html
HAWAIIAN VOLCANO OBSERVATORY DAILY UPDATE
Saturday, January 10, 2009 07:54 HST (Saturday, January 10, 2009 17:54 UTC)
KILAUEA VOLCANO (CAVW#1302-01-)
19.42°N 155.29°W, Summit Elevation 4091 ft (1247 m)
Volcano Alert Level: WATCH
Aviation Color Code: ORANGE
This report on the status of Kilauea volcanic activity, in addition to maps, photos, and webcam images (available using the menu bar above), was prepared by the USGS Hawaiian Volcano Observatory (HVO). Hawai`i Volcanoes National Park status can be found at http://www.nps.gov/havo/ or 985-6000. Hawai`i County Viewing Area status can be found at 961-8093.
Activity Summary for past 24 hours: There were no significant changes. Sulfur dioxide emission rates from Halema`uma`u vent remain elevated above pre-2008 values; tephra production has stopped. At the east rift eruption site, sulfur dioxide emission rates from the Pu`u `O`o vents remain elevated. Lava from nearby east rift zone vents flows through tubes to the ocean; surface flows remain active on the coastal plain.
Past 24 hours at Kilauea summit: The vent remained dark overnight. This morning, the white plume is heading east toward Kilauea Iki; the wind shift produced unhealthy air at HVO and Park facilities early this morning.
Sulfur dioxide emission rates remain elevated and variable. The most recent average measurement was 800 tonnes/day on January 7, still elevated above the 2003-2007 average rate of 140 tonnes/day.
Production of tephra has essentially stopped although rockfalls within the vent continue. Recent views into the vent using an infrared camera show that the conduit is closed by rubble deep beneath the Halema`uma`u Crater floor.
The network of tiltmeters within the caldera recorded tilting inward toward the south caldera reflecting general deflation. The GPS receiver networks (less sensitive than tiltmeters) recorded a total of 2 cm of contraction across the caldera over the previous 3 months.
Seismic activity continues to be focused on the south caldera; tremor levels remain elevated. The number of RB2S2BL earthquakes remain around background values. A total of 6 earthquakes were strong enough to be located beneath Kilauea or nearby, with 1 beneath the summit caldera and 2 on south flank faults.
Past 24 hours at the middle east rift zone vents and flow field: Magma continues to degas through Pu`u `O`o Crater. The most recent sulfur dioxide emission rate measurement was 1,800 tonnes/day measured on January 7 compared to the 2003-2007 average of about 1,700 tonnes/day for this vent. No incandescence was observed within the crater overnight.
The tiltmeter on the north side of Pu`u `O`o recorded rain-induced tilting in a direction outward from the crater. GPS stations spanning the crater (less sensitive than tiltmeters) recorded more than 4 cm of contraction over the past 3 months. Seismic tremor levels near Pu`u `O`o and the TEB vent remain at low values.
Lava from the TEB vent and the rootless shield complex flows through tubes to the ocean. GOES-WEST imagery showed a strong ocean entry plume yesterday and a persistent thermal anomaly overnight suggesting continuing ocean entry and surface flow activity on the coastal plain.
HAZARD ALERT: The lava delta and adjacent areas both inland and out to sea are still some of the most hazardous areas on the flow field. Frequent delta/bench collapses give little warning, can produce hot rock falls inland and in the adjacent ocean and can produce large but local waves. The steam plume produced by lava entering the ocean contains fine lava fragments and an assortment of acid droplets that can be harmful to your health. The rapidly changing conditions near the ocean entry have been responsible for many injuries and a few deaths.
Definitions of terms used in the update:
HAVO: Hawai`i Volcanoes National Park
UHH: University of Hawai`i at Hilo
glow: light from an unseen source; indirect light.
FLIR: Forward Looking InfraRed, a camera which directly images heat rather than visible light. If volcanic fume is not too rich in water vapor, a FLIR can see through it to image hot surfaces.
pali: Hawaiian word for cliff or steep incline. In the context of the TEB flow field, 'pali' usually refers to Pulama pali that bisects the abandoned Royal Gardens subdivision.
CD: Hawai`i County Civil Defense
DOH air quality monitoring: see Hawai`i State Department of Health Air Quality website http://hawaii.gov/doh/air-quality/index.html .
bomb: lava fragment ejected into the air while molten acquiring aerodynamic shapes in flight; the term is restricted to pieces larger than 6.4 cm (2.5 in.). See http://volcanoes.usgs.gov/Products/Pglossary/bomb.html
hybrid, or explosion, seismic signals: complex earthquakes that are a hybrid of different signals. They start as a high frequency earthquake, similar to typical rock-breaking or rock fall events, that transitions to very long, 20-30 second, period (VLP) oscillations that continue for several minutes. At HVO, we observed these signals with the four small Halema`uma`u explosive eruptions in March, April, and August 2008. Several more similar signals, some as strong as the explosion signals associated with the four explosive eruptions, have been recorded without obvious evidenceof surface eruption such as rock fragments or other debris.
MODIS satellite: a NASA satellite pair, Aqua and Terra, which passes over Hawai`i twice a day. During daylight hours, the images are taken at about 11 am and 2 pm H.s.t. This imagery can be viewed about 3-5 hours after acquisition at http://rapidfire.sci.gsfc.nasa.gov/subsets/?subset=AERONET_Mauna_Loa.
GOES-WEST satellite: a geostationary NOAA satellite used most often for weather tracking. Images are typically acquired every 15 minutes. The loop http://www.ssd.noaa.gov/VAAC/kilauea/sloop-vis.html is posted by the Washington DC Volcanic Ash Advisory Center for the purpose of tracking emissions from Hawai`i volcanoes. The imagery automatically switches from infrared at night to visual during the day. Recently, it has been useful for tracking volcanic gas emissions from Halema`uma`u, Pu`u `O`o, and the Waikupanaha ocean entry during the day and hot lava flows at night.
Volcano Watch: weekly newspaper-like article written by HVO scientists on a volcano topic of interest. These articles are usually printed in the Sunday editions of the Hawai`i Island newspapers Hawaii Tribune Herald and West Hawaii Today. More than 800 of these articles have been written and are archived on the HVO website (menu at the bottom of the homepage hvo.wr.usgs.gov).
VLP seismic tremor: seismic tremor is continuous ground vibrations simultaneously at many different frequencies. VLP is a very long period or very low frequency component which, at the Halema`uma`u vent, has a period of 20-30 seconds or a frequency of 0.03-0.05 cycles per second (Hertz or Hz).
RB2S2BL earthquakes: earthquakes that were recorded but were too small to be located. These quakes have magnitudes less than 1.7 and may only be recorded by one or two seismometers. Recording at a minimum of 4 seismometer sites is required to locate an earthquake.
wink: an abrupt shutting off of incandescence at a vent lasting for several minutes. At the Halema`uma`u vent, winks usually start with or immediately follow a small, local earthquake. The diminishment of incandescence is due to the plume changing from translucent to opaque with rock dust.
tonne: metric unit equal to 1,000 kilograms, 2,204.6 lbs, or 1.1 English tons.
microradian: a measure of angle equivalent to 0.000057 degrees.
ppm: parts-per-million; 10,000 ppm = 1 %.
littoral cone: usually small cones built near active ocean entries; the cones are constructed of tephra from steam explosions that are sometimes produced when 1,150 degree C lava enters the 25 degree C ocean.
incandescence: the production of visible light from a hot surface. The term also refers to the light emitted from a hot surface. The color of the light is related to surface temperature. Some surfaces can display dull red incandescence at temperatures as low as 430 degrees Centigrade (806 degrees Fahrenheit). By contrast, molten lava displays bright orange to orange-yellow light from surfaces that are hotter than 900 degrees C (1,650 degrees F).
tephra: all material deposited by fallout from an eruption-related plume, regardless of size.
ash: tephra less than 2 mm (5/64 inches) in size.
TEB: Thanksgiving Eve Breakout, the designation used for lava flows that started with a breakout on November 21, 2007.
DI tilt event: DI is an abbreviation for 'deflation-inflation' and describes a volcanic event of uncertain significance. DI events are recorded by tiltmeters at Kilauea summit as an abrupt deflation of up to a few microradians in magnitude lasting several hours to 2-3 days followed by an abrupt inflation of approximately equal magnitude. The tilt events are usually accompanied by an increase in summit tremor during the deflation phase. A careful analysis of these events suggests that they may be related to changes in magma supply to a storage reservoir at less than 1 km depth, just east of Halema`uma`u crater. Usually, though not always, these changes propagate through the magma conduit from the summit to the eruption site, as many of the DI events at Kilauea summit are also recorded at a tiltmeter at Pu`u `O`o, delayed by 1-2 hours. DI events often correlate with lava pulses and/or pauses in the eruption at the Pu`u `O`o/July 21/TEB vents.
Maps, photos, webcam views, and other information about Kilauea Volcano are available at http://volcano.wr.usgs.gov/kilaueastatus.php. A daily update summary is available by phone at (808) 967-8862.
A map with details of earthquakes located within the past two weeks can be found at http://tux.wr.usgs.gov/
A definition of alert levels can be found at http://volcanoes.usgs.gov/2006/warnschemes.html
HAWAIIAN VOLCANO OBSERVATORY DAILY UPDATE
Friday, January 9, 2009 08:00 HST (Friday, January 9, 2009 18:00 UTC)
KILAUEA VOLCANO (CAVW#1302-01-)
19.42°N 155.29°W, Summit Elevation 4091 ft (1247 m)
Volcano Alert Level: WATCH
Aviation Color Code: ORANGE
This report on the status of Kilauea volcanic activity, in addition to maps, photos, and webcam images (available using the menu bar above), was prepared by the USGS Hawaiian Volcano Observatory (HVO). Hawai`i Volcanoes National Park status can be found at http://www.nps.gov/havo/ or 985-6000. Hawai`i County Viewing Area status can be found at 961-8093.
Activity Summary for past 24 hours: There were no significant changes. Sulfur dioxide emission rates from Halema`uma`u vent remain elevated above pre-2008 values; tephra production has stopped. At the east rift eruption site, sulfur dioxide emission rates from the Pu`u `O`o vents remain elevated. Lava from nearby east rift zone vents flows through tubes to the ocean; surface flows remain active on the coastal plain.
Past 24 hours at Kilauea summit: The vent remained dark overnight. This morning, the white plume is heading southwest low over the Ka`u Desert. Recent rains are still making fume from hot gas vents more visible along the south and west rims of Halema`uma`u Crater.
Sulfur dioxide emission rates remain elevated and variable. The most recent average measurement was 800 tonnes/day on January 7, still elevated above the 2003-2007 average rate of 140 tonnes/day.
Production of tephra has essentially stopped although rockfalls within the vent continue. Recent views into the vent using an infrared camera show that the conduit is closed by rubble deep beneath the Halema`uma`u Crater floor.
The network of tiltmeters within the caldera recorded incoherent tilt directions dominated by minor diurnal oscillations. The GPS receiver networks (less sensitive than tiltmeters) recorded a total of 2 cm of contraction across the caldera over the previous 3 months.
Seismic activity continues to be focused on the south caldera; tremor levels remain elevated. The number of RB2S2BL earthquakes remain around background values. A total of 8 earthquakes were strong enough to be located beneath Kilauea or nearby, with 5 beneath the summit caldera and 3 on south flank faults.
Past 24 hours at the middle east rift zone vents and flow field: Magma continues to degas through Pu`u `O`o Crater. The most recent sulfur dioxide emission rate measurement was 1,800 tonnes/day measured on January 7 compared to the 2003-2007 average of about 1,700 tonnes/day for this vent. No incandescence was observed within the crater overnight.
The tiltmeter on the north side of Pu`u `O`o continued to record weak tilting inward toward the crater. GPS stations spanning the crater (less sensitive than tiltmeters) recorded more than 4 cm of contraction over the past 3 months. Seismic tremor levels near Pu`u `O`o and the TEB vent remain at low values.
Lava from the TEB vent and the rootless shield complex flows through tubes to the ocean. Yesterday, HVO geologists mapped surface flow activity from both the TEB lobe (feeds the Waikupanaha ocean entry) and the Prince lobe to the west. The advancing front of the Prince lobe was about 300 m (1,000 ft) inside the Hawai`i Volcanoes National Park boundary still about 450 m (1,500 ft) from the coast (see map). Last night, CD officials reported a mellow ocean entry with few explosions and not much glow from surface flows. GOES-WEST imagery showed a persistent thermal anomaly overnight suggesting continuing surface flow activity on the coastal plain. This morning, CD officials report an active ocean entry and steam plume.
HAZARD ALERT: The lava delta and adjacent areas both inland and out to sea are still some of the most hazardous areas on the flow field. Frequent delta/bench collapses give little warning, can produce hot rock falls inland and in the adjacent ocean and can produce large but local waves. The steam plume produced by lava entering the ocean contains fine lava fragments and an assortment of acid droplets that can be harmful to your health. The rapidly changing conditions near the ocean entry have been responsible for many injuries and a few deaths.
Definitions of terms used in the update:
HAVO: Hawai`i Volcanoes National Park
UHH: University of Hawai`i at Hilo
glow: light from an unseen source; indirect light.
FLIR: Forward Looking InfraRed, a camera which directly images heat rather than visible light. If volcanic fume is not too rich in water vapor, a FLIR can see through it to image hot surfaces.
pali: Hawaiian word for cliff or steep incline. In the context of the TEB flow field, 'pali' usually refers to Pulama pali that bisects the abandoned Royal Gardens subdivision.
CD: Hawai`i County Civil Defense
DOH air quality monitoring: see Hawai`i State Department of Health Air Quality website http://hawaii.gov/doh/air-quality/index.html .
bomb: lava fragment ejected into the air while molten acquiring aerodynamic shapes in flight; the term is restricted to pieces larger than 6.4 cm (2.5 in.). See http://volcanoes.usgs.gov/Products/Pglossary/bomb.html
hybrid, or explosion, seismic signals: complex earthquakes that are a hybrid of different signals. They start as a high frequency earthquake, similar to typical rock-breaking or rock fall events, that transitions to very long, 20-30 second, period (VLP) oscillations that continue for several minutes. At HVO, we observed these signals with the four small Halema`uma`u explosive eruptions in March, April, and August 2008. Several more similar signals, some as strong as the explosion signals associated with the four explosive eruptions, have been recorded without obvious evidenceof surface eruption such as rock fragments or other debris.
MODIS satellite: a NASA satellite pair, Aqua and Terra, which passes over Hawai`i twice a day. During daylight hours, the images are taken at about 11 am and 2 pm H.s.t. This imagery can be viewed about 3-5 hours after acquisition at http://rapidfire.sci.gsfc.nasa.gov/subsets/?subset=AERONET_Mauna_Loa.
GOES-WEST satellite: a geostationary NOAA satellite used most often for weather tracking. Images are typically acquired every 15 minutes. The loop http://www.ssd.noaa.gov/VAAC/kilauea/sloop-vis.html is posted by the Washington DC Volcanic Ash Advisory Center for the purpose of tracking emissions from Hawai`i volcanoes. The imagery automatically switches from infrared at night to visual during the day. Recently, it has been useful for tracking volcanic gas emissions from Halema`uma`u, Pu`u `O`o, and the Waikupanaha ocean entry during the day and hot lava flows at night.
Volcano Watch: weekly newspaper-like article written by HVO scientists on a volcano topic of interest. These articles are usually printed in the Sunday editions of the Hawai`i Island newspapers Hawaii Tribune Herald and West Hawaii Today. More than 800 of these articles have been written and are archived on the HVO website (menu at the bottom of the homepage hvo.wr.usgs.gov).
VLP seismic tremor: seismic tremor is continuous ground vibrations simultaneously at many different frequencies. VLP is a very long period or very low frequency component which, at the Halema`uma`u vent, has a period of 20-30 seconds or a frequency of 0.03-0.05 cycles per second (Hertz or Hz).
RB2S2BL earthquakes: earthquakes that were recorded but were too small to be located. These quakes have magnitudes less than 1.7 and may only be recorded by one or two seismometers. Recording at a minimum of 4 seismometer sites is required to locate an earthquake.
wink: an abrupt shutting off of incandescence at a vent lasting for several minutes. At the Halema`uma`u vent, winks usually start with or immediately follow a small, local earthquake. The diminishment of incandescence is due to the plume changing from translucent to opaque with rock dust.
tonne: metric unit equal to 1,000 kilograms, 2,204.6 lbs, or 1.1 English tons.
microradian: a measure of angle equivalent to 0.000057 degrees.
ppm: parts-per-million; 10,000 ppm = 1 %.
littoral cone: usually small cones built near active ocean entries; the cones are constructed of tephra from steam explosions that are sometimes produced when 1,150 degree C lava enters the 25 degree C ocean.
incandescence: the production of visible light from a hot surface. The term also refers to the light emitted from a hot surface. The color of the light is related to surface temperature. Some surfaces can display dull red incandescence at temperatures as low as 430 degrees Centigrade (806 degrees Fahrenheit). By contrast, molten lava displays bright orange to orange-yellow light from surfaces that are hotter than 900 degrees C (1,650 degrees F).
tephra: all material deposited by fallout from an eruption-related plume, regardless of size.
ash: tephra less than 2 mm (5/64 inches) in size.
TEB: Thanksgiving Eve Breakout, the designation used for lava flows that started with a breakout on November 21, 2007.
DI tilt event: DI is an abbreviation for 'deflation-inflation' and describes a volcanic event of uncertain significance. DI events are recorded by tiltmeters at Kilauea summit as an abrupt deflation of up to a few microradians in magnitude lasting several hours to 2-3 days followed by an abrupt inflation of approximately equal magnitude. The tilt events are usually accompanied by an increase in summit tremor during the deflation phase. A careful analysis of these events suggests that they may be related to changes in magma supply to a storage reservoir at less than 1 km depth, just east of Halema`uma`u crater. Usually, though not always, these changes propagate through the magma conduit from the summit to the eruption site, as many of the DI events at Kilauea summit are also recorded at a tiltmeter at Pu`u `O`o, delayed by 1-2 hours. DI events often correlate with lava pulses and/or pauses in the eruption at the Pu`u `O`o/July 21/TEB vents.
Maps, photos, webcam views, and other information about Kilauea Volcano are available at http://volcano.wr.usgs.gov/kilaueastatus.php. A daily update summary is available by phone at (808) 967-8862.
A map with details of earthquakes located within the past two weeks can be found at http://tux.wr.usgs.gov/
A definition of alert levels can be found at http://volcanoes.usgs.gov/2006/warnschemes.html
HAWAIIAN VOLCANO OBSERVATORY DAILY UPDATE
Thursday, January 8, 2009 08:16 HST (Thursday, January 8, 2009 18:16 UTC)
KILAUEA VOLCANO (CAVW#1302-01-)
19.42°N 155.29°W, Summit Elevation 4091 ft (1247 m)
Volcano Alert Level: WATCH
Aviation Color Code: ORANGE
This report on the status of Kilauea volcanic activity, in addition to maps, photos, and webcam images (available using the menu bar above), was prepared by the USGS Hawaiian Volcano Observatory (HVO). Hawai`i Volcanoes National Park status can be found at http://www.nps.gov/havo/ or 985-6000. Hawai`i County Viewing Area status can be found at 961-8093.
Activity Summary for past 24 hours: There were no significant changes. Sulfur dioxide emission rates from Halema`uma`u vent remain elevated above pre-2008 values; tephra production has stopped. At the east rift eruption site, sulfur dioxide emission rates from the Pu`u `O`o vents remain elevated. Lava from nearby east rift zone vents flows through tubes to the ocean; surface flows remain active on the pali and the coastal plain.
Past 24 hours at Kilauea summit: The vent remained dark overnight. This morning, the white plume is barely visible through fog heading southwest low over the Ka`u Desert. Recent rains are making fume from hot gas vents more visible along the south and west rims of Halema`uma`u Crater.
Sulfur dioxide emission rates remain elevated and variable. The most recent average measurement was 800 tonnes/day on January 7, still elevated above the 2003-2007 average rate of 140 tonnes/day.
Production of tephra has essentially stopped although the rockfalls within the vent continue. Recent views into the vent using an infrared camera show that the conduit is closed by rubble deep beneath the Halema`uma`u Crater floor.
The network of tiltmeters within the caldera recorded weak deflation not consistent enough to indicate a unique source location. The GPS receiver networks (less sensitive than tiltmeters) recorded a total of 2 cm of contraction across the caldera over the previous 3 months.
Seismic activity continues to be focused on the south caldera; tremor levels remain elevated. The number of RB2S2BL earthquakes remain around background values. A total of 9 earthquakes were strong enough to be located beneath Kilauea or nearby, with 4 beneath the summit caldera and 2 on south flank faults.
Past 24 hours at the middle east rift zone vents and flow field: Magma continues to degas through Pu`u `O`o Crater. The most recent sulfur dioxide emission rate measurement was 1,800 tonnes/day measured on January 7 compared to the 2003-2007 average of about 1,700 tonnes/day for this vent. No incandescence was observed within the crater overnight.
The tiltmeter on the north side of Pu`u `O`o continued to record tilting inward toward the crater until midnight when it switch to outward tilting (inflation) without any corresponding change in seismicity. GPS stations spanning the crater (less sensitive than tiltmeters) recorded about 4 cm of contraction over the past 3 months. Seismic tremor levels near Pu`u `O`o and the TEB vent remain at low values.
Lava from the TEB vent and the rootless shield complex flows through tubes to the ocean. GOES-WEST imagery showed a persistent thermal anomaly overnight suggesting surface flow activity on the coastal plain.
HAZARD ALERT: The lava delta and adjacent areas both inland and out to sea are still some of the most hazardous areas on the flow field. Frequent delta/bench collapses give little warning, can produce hot rock falls inland and in the adjacent ocean and can produce large but local waves. The steam plume produced by lava entering the ocean contains fine lava fragments and an assortment of acid droplets that can be harmful to your health. The rapidly changing conditions near the ocean entry have been responsible for many injuries and a few deaths.
Definitions of terms used in the update:
HAVO: Hawai`i Volcanoes National Park
UHH: University of Hawai`i at Hilo
glow: light from an unseen source; indirect light.
FLIR: Forward Looking InfraRed, a camera which directly images heat rather than visible light. If volcanic fume is not too rich in water vapor, a FLIR can see through it to image hot surfaces.
pali: Hawaiian word for cliff or steep incline. In the context of the TEB flow field, 'pali' usually refers to Pulama pali that bisects the abandoned Royal Gardens subdivision.
CD: Hawai`i County Civil Defense
DOH air quality monitoring: see Hawai`i State Department of Health Air Quality website http://hawaii.gov/doh/air-quality/index.html .
bomb: lava fragment ejected into the air while molten acquiring aerodynamic shapes in flight; the term is restricted to pieces larger than 6.4 cm (2.5 in.). See http://volcanoes.usgs.gov/Products/Pglossary/bomb.html
hybrid, or explosion, seismic signals: complex earthquakes that are a hybrid of different signals. They start as a high frequency earthquake, similar to typical rock-breaking or rock fall events, that transitions to very long, 20-30 second, period (VLP) oscillations that continue for several minutes. At HVO, we observed these signals with the four small Halema`uma`u explosive eruptions in March, April, and August 2008. Several more similar signals, some as strong as the explosion signals associated with the four explosive eruptions, have been recorded without obvious evidenceof surface eruption such as rock fragments or other debris.
MODIS satellite: a NASA satellite pair, Aqua and Terra, which passes over Hawai`i twice a day. During daylight hours, the images are taken at about 11 am and 2 pm H.s.t. This imagery can be viewed about 3-5 hours after acquisition at http://rapidfire.sci.gsfc.nasa.gov/subsets/?subset=AERONET_Mauna_Loa.
GOES-WEST satellite: a geostationary NOAA satellite used most often for weather tracking. Images are typically acquired every 15 minutes. The loop http://www.ssd.noaa.gov/VAAC/kilauea/sloop-vis.html is posted by the Washington DC Volcanic Ash Advisory Center for the purpose of tracking emissions from Hawai`i volcanoes. The imagery automatically switches from infrared at night to visual during the day. Recently, it has been useful for tracking volcanic gas emissions from Halema`uma`u, Pu`u `O`o, and the Waikupanaha ocean entry during the day and hot lava flows at night.
Volcano Watch: weekly newspaper-like article written by HVO scientists on a volcano topic of interest. These articles are usually printed in the Sunday editions of the Hawai`i Island newspapers Hawaii Tribune Herald and West Hawaii Today. More than 800 of these articles have been written and are archived on the HVO website (menu at the bottom of the homepage hvo.wr.usgs.gov).
VLP seismic tremor: seismic tremor is continuous ground vibrations simultaneously at many different frequencies. VLP is a very long period or very low frequency component which, at the Halema`uma`u vent, has a period of 20-30 seconds or a frequency of 0.03-0.05 cycles per second (Hertz or Hz).
RB2S2BL earthquakes: earthquakes that were recorded but were too small to be located. These quakes have magnitudes less than 1.7 and may only be recorded by one or two seismometers. Recording at a minimum of 4 seismometer sites is required to locate an earthquake.
wink: an abrupt shutting off of incandescence at a vent lasting for several minutes. At the Halema`uma`u vent, winks usually start with or immediately follow a small, local earthquake. The diminishment of incandescence is due to the plume changing from translucent to opaque with rock dust.
tonne: metric unit equal to 1,000 kilograms, 2,204.6 lbs, or 1.1 English tons.
microradian: a measure of angle equivalent to 0.000057 degrees.
ppm: parts-per-million; 10,000 ppm = 1 %.
littoral cone: usually small cones built near active ocean entries; the cones are constructed of tephra from steam explosions that are sometimes produced when 1,150 degree C lava enters the 25 degree C ocean.
incandescence: the production of visible light from a hot surface. The term also refers to the light emitted from a hot surface. The color of the light is related to surface temperature. Some surfaces can display dull red incandescence at temperatures as low as 430 degrees Centigrade (806 degrees Fahrenheit). By contrast, molten lava displays bright orange to orange-yellow light from surfaces that are hotter than 900 degrees C (1,650 degrees F).
tephra: all material deposited by fallout from an eruption-related plume, regardless of size.
ash: tephra less than 2 mm (5/64 inches) in size.
TEB: Thanksgiving Eve Breakout, the designation used for lava flows that started with a breakout on November 21, 2007.
DI tilt event: DI is an abbreviation for 'deflation-inflation' and describes a volcanic event of uncertain significance. DI events are recorded by tiltmeters at Kilauea summit as an abrupt deflation of up to a few microradians in magnitude lasting several hours to 2-3 days followed by an abrupt inflation of approximately equal magnitude. The tilt events are usually accompanied by an increase in summit tremor during the deflation phase. A careful analysis of these events suggests that they may be related to changes in magma supply to a storage reservoir at less than 1 km depth, just east of Halema`uma`u crater. Usually, though not always, these changes propagate through the magma conduit from the summit to the eruption site, as many of the DI events at Kilauea summit are also recorded at a tiltmeter at Pu`u `O`o, delayed by 1-2 hours. DI events often correlate with lava pulses and/or pauses in the eruption at the Pu`u `O`o/July 21/TEB vents.
Maps, photos, webcam views, and other information about Kilauea Volcano are available at http://volcano.wr.usgs.gov/kilaueastatus.php. A daily update summary is available by phone at (808) 967-8862.
A map with details of earthquakes located within the past two weeks can be found at http://tux.wr.usgs.gov/
A definition of alert levels can be found at http://volcanoes.usgs.gov/2006/warnschemes.html