Current Kilauea Volcano Eruption Update 
  Current Eruption Status, Information, and Photos of
Kilauea Volcano, Hawaii

Come visit the most active Volcano in the World.  To see a REAL Volcano is a spectacular sight.   We advise you to always check in at the Visitor Center of the Hawaii Volcanoes National Park to get up to the minute current eruption updates.  The friendly rangers will gladly tell you where to go and how to view lava safely. 

17 July 2008

View into TEB and blankets of paper-thin limu o Pele at Waikupanaha

The top of the TEB collapsed in the past week, permitting a view into the vent for the first time in several weeks. Lava was rushing from left to right, in this view, then turning abruptly toward the top of the photo where it enters the tube system.
 

Flows in the past week expanded eastward and consumed more of the Royal Gardens subdivision. One house, at lower right, narrowly avoided destruction, while two more structures, near the burned trees in the center of the photo, were buried completely.
 

Left. The top of the TEB collapsed in the past week, permitting a view into the vent for the first time in several weeks. Lava was rushing from left to right, in this view, then turning abruptly toward the top of the photo where it enters the tube system. Right. Flows in the past week expanded eastward and consumed more of the Royal Gardens subdivision. One house, at lower right, narrowly avoided destruction, while two more structures, near the burned trees in the center of the photo, were buried completely.

The Waikupanaha plume was more modest today, illustrating the erratic behavior of the ocean entry. Shortly after this photo was taken, large explosions resumed and the plume grew again to enormous size. Notice the thick haze in the background. This the volcanic plume from Pu`u `O`o out of site at upper right.
 

The frequent littoral explosions at Waikupanaha have blanketed the down-wind lava surface with paper-thin limu o Pele fragments. Notice the abrupt boundary between the brown limu o Pele fallout and the shiny pahoehoe. Limu o Pele is composed, basically, of pieces of bubble walls.  It forms when lava bubbles burst and when wind blows laterally through sheets of molten lava thrown up during the explosions.
 

Left. The Waikupanaha plume was more modest today, illustrating the erratic behavior of the ocean entry. Shortly after this photo was taken, large explosions resumed and the plume grew again to enormous size. Notice the thick haze in the background. This the volcanic plume from Pu`u `O`o out of site at upper right.Right. The frequent littoral explosions at Waikupanaha have blanketed the down-wind lava surface with paper-thin limu o Pele fragments. Notice the abrupt boundary between the brown limu o Pele fallout and the shiny pahoehoe. Limu o Pele is composed, basically, of pieces of bubble walls. It forms when lava bubbles burst and when wind blows laterally through sheets of molten lava thrown up during the explosions.

Besides the blanket of limu of Pele described above, the large explosions at Waikupanaha have also built a littoral spatter cone in an arc around the ocean entry. The cone is not obvious in the photo on the left due to the oblique angle and shadowing from the plume. In the infrared (IR) image on the right, the portion of the littoral cone built on the beach shows up nicely just below image center.  A small littoral explosion, hidden by fume in the photo, is apparent just right of image center in the IR image. The bright dots scattered around on the littoral cone in the IR image are hot blobs of recently-ejected spatter.
 

Besides the blanket of limu of Pele described above, the large explosions at Waikupanaha have also built a littoral spatter cone in an arc around the ocean entry. The cone is not obvious in the photo on the left due to the oblique angle and shadowing from the plume. In the infrared (IR) image on the right, the portion of the littoral cone built on the beach shows up nicely just below image center. A small littoral explosion, hidden by fume in the photo, is apparent just right of image center in the IR image. The bright dots scattered around on the littoral cone in the IR image are hot blobs of recently-ejected spatter.

Volcano Live Camera :
 Pu`u `O`o  
Halema`uma`u

Eruption Maps

Eruption Updates:

  July 17, 2008
  July 16, 2008
  July 14, 2008
  July 10, 2008
  July 7, 2008
  July 5, 2008
  July 2, 2008
  June 30, 2008
 

Kilauea Volcano Time Lapse Movies:
| Pu`u `O`o Crater | Pu`u `O`o Flank Vents | Flow Field | Ocean Entry |


OCEAN ENTRY - LAVA VIEWING AREA:

Visitors are allowed entry to the viewing area every day from 2 p.m., with the last vehicles admitted at 8:00 p.m. This will allow officials to ensure that everybody is out of the area by 10 p.m. The viewing area is closed between 10 pm and 2 pm.  This schedule is subject to change; hazardous conditions may require changes to the schedule or closure.
County of Hawaii - Kilauea Eruption image
- click on map for larger view-

Hawai`i County Civil Defense has set up a new telephone hotline to provide daily updates on viewing at the Kalapana Safe Viewing site.  The lava hotline phone number is 961-8093, which lets you know the lava viewing hours for the day ahead.  The lava hotline automated message is updated every day at 10 a.m.

The Kalapana Safe Viewing program at the volcanic eruption site is a wonderful natural attraction, and the County Civil Defense Agency wants all visitors to enjoy the experience in safety and comfort.  With that in mind, we encourage visitors to prepare not only for sunny days at the lava viewing sight but also for rain.  Please note that there are no shelters at the site in case of rain.

For your comfort and convenience, please prepare for rain keeping in mind any trip hazard:

·        An umbrella and/or

·        Windbreaker or raincoat

Visitors are also strongly advised to take the following gear for both safety and comfort:

·        Bottled water (2-3 quarts or liters per person)

·        Sturdy closed boots or shoes and socks

·        Flashlight (1 per person) and fresh batteries

·        Long pants

·        Sun hat and sunscreen

·        Binoculars (optional)

 

Visitors are reminded to obey all the warning signs and stay within the allowed areas to ensure their safety. The newly formed lava and black sand beach are extremely unstable, and can collapse into the ocean at any time. Visitors must stay well away from the volcanic steam clouds which contain hydrochloric acid and glass particles.

Please note:  There is no cell phone coverage in the viewing area.

We ask that visitors show the greatest courtesy and respect to the local residents and property owners. Please remember never to go off the road or trail, and please dispose of all trash in the garbage cans provided. Guide/interpreters will be on hand in the viewing area to provide information and assistance.  For more information, please call Civil Defense at 935-0031.

For the Hawaiian Volcanoes Observatory’s eruption updates online, please click on http://lavainfo.us/ .

The Big Island Visitors Bureau has created a new section of its website with all of the information we've been trying to get out to the public. Click on  http://www.bigisland.org/parks/939/volcano-eruption-update .

Recent Kilauea Status Reports, Updates, and Information Releases

HAWAIIAN VOLCANO OBSERVATORY DAILY UPDATE
Saturday, July 19, 2008 07:36 HST (Saturday, July 19, 2008 17:36 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 http://www.lavainfo.us or 961-8093.

Activity Summary for last 24 hours: Kilauea summit is deflating. Small amounts of ash and elevated amounts of sulfur dioxide gas continued to issue from the Halema`uma`u vent. At the east rift eruption site, Pu`u `O`o cone is slowly contracting and incandescence was observed from the east wall vent; lava flows from the TEB vent through tubes to the ocean at Waikupanaha; ocean entry explosions continued.

Last 24 hours at Kilauea summit: Incandescence has been weak and continuous with no episodic pulsing. A few local earthquakes caused the vent to dim briefly. During one of the longer dimming events at 04:25 am, incandescent ejecta could be seen propelled out of the vent but not reaching Halema`uma`u rim.

A white plume rises from the Halema`uma`u vent and is blown to the southwest about 200-300 m (650-1,000 ft) above the Ka`u Desert at 6:30 am this morning. The SO2 emission rate remained high and variable; the most recent average measurement was 700 tonnes/day on July 17 compared to an average of 800 tonnes/day on July 15 and a pre-2008 background rate between 150-200 tonnes/day.

Kilauea caldera continued to deflate after the late June inflation. The summit tiltmeter network recorded 10 microradians of deflation in the south caldera since July 1; this is the most rapid rate of deflation since September 2007. GPS receivers on opposite sides of the summit caldera recorded almost 2 cm of contraction since July 1; this rate is almost double the rate prior to the late June summit inflation/extension.

Seismic tremor continued at elevated levels with occasional weak bursts. The number of RB2S2BL earthquakes beneath Halema`uma`u Crater remain at background values of about 20/d. One earthquake was located beneath Halema`uma`u Crater, two on south flank faults, and one beneath the lower portion of the southwest rift zone.

Last 24 hours at the middle east rift zone vents and flow field: Magma continued to degas through Pu`u `O`o Crater resulting in an unusually high emission of 6,300 tonnes/day of sulfur dioxide on July 17, up from 4,800 tonnes/day on July 6 and background values of about 2,000 tonnes/day. Overnight, the webcam recorded diffuse incandescence from only the east wall vent.

The tiltmeter on the north side of Pu`u `O`o cone recorded minor oscillations. GPS receivers recorded contraction across the crater. Seismic tremor levels at the TEB vent/Pu`u `O`o area remain at values elevated above those in late June.

Lava enters the tube system under the TEB vent and flows beneath the rootless shield complex through tubes to the ocean. Overnight, incandescence was observed from the TEB vent and the top of shield 3. The ocean entry continued to provide spectacular views.

Definitions of terms used in the update:

GOES-WEST satellite: a NOAA satellite used most often for weather tracking. 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 too small to be located. These quakes have magnitudes less than 1.7 and may only be recorded on 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 color of the light is related to the temperature of the surface. 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

 

 

 

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