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  • Current Volcano Activity

    The USGS Hawai'i Volcanoes Observatory, located in the Hawai'i Volcanoes National Park, provides a daily update of the eruption activity at Pu'u O'o and down on the coastal flats.

    The daily report is extracted from USGS by InstantHawaii and provided for you below, along with some of the most recent USGS pictures of the flow. Please visit the USGS website for more details and photographs.

    Volcano Report
    © USGS Hawaiian Volcano Observatory

    HAWAIIAN VOLCANO OBSERVATORY DAILY UPDATE
    Friday, March 12, 2010 7:57 AM HST (Friday, March 12, 2010 17:57 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. All times are Hawai`i Standard Time.

    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: Kilauea volcano continued with subdued activity at two locations. At the summit, an infrared cameras was the only way to see lava slowly rising from low levels in a deep pit inset within the floor of Halema`uma`u Crater but it still produced weak glow that was visible from the Jaggar Museum. At the east rift zone vents, lava trickled through tubes and fed few scattered surface flows on the pali and the coastal plain. Sulfur dioxide emission rates from both summit and east rift zone vents, however, remained elevated.

    Past 24 hours at Kilauea summit: The circulating and spattering lava surface was still not directly visible via webcam last night but it was visible to an infrared camera which showed lava slowly rising in the deep pit inset within the floor of Halema`uma`u Crater; when weather permitted, weak vent glow was visible from the Jaggar Museum Overlook last night.

    The summit tiltmeter network recorded continued DI inflation. Seismic tremor remained at elevated steady levels with a few long bursts early this morning. The number of RB2S2BL earthquakes was within background values. Seven earthquakes beneath Hawai`i Island were strong enough to be located - three beneath the area west of the summit and four on south flank faults.

    The summit vent gas plume is moving to the southwest this morning. The most recent sulfur dioxide emission rate measurement was 600 tonnes/day on March 11, 2010, still elevated above the 2003-2007 average of 140 tonnes/day. Small amounts of mostly ash-sized tephra were lifted out of the deep pit in ascending gases and deposited on nearby surfaces.

    Past 24 hours at the middle east rift zone vents and flow field: Magma degases through Pu`u `O`o crater before erupting from the TEB vent located 2 km to the east. The most recent sulfur dioxide emission rate measurement was 600 tonnes/day on March 10, 2010, lower than the 2003-2007 average of 1,700 tonnes/day. No incandescence has been recorded within Pu`u `O`o Crater since February 27.

    The tiltmeter on the north flank of Pu`u `O`o recorded the switch to DI inflation just before 2 pm yesterday. Seismic tremor levels in the Pu`u `O`o - TEB vent portion of the east rift zone have decreased in response to the inflation. The number of RB2STBL earthquakes remained at background levels.

    Lava from the TEB vent flowed through the upper portion of the tube system and probably fed scattered surface flows on the lower pali and the coastal plain. MODIS and GOES-WEST images contained few barely detectable thermal anomalies suggesting diminished surface flow activity. Surface activity is expected to increase 12-24 hours after the onset of DI inflation at Pu`u `O`o.

    Maps, photos, webcam views, and other information about Kilauea Volcano are available at http://volcanoes.usgs.gov/hvo/activity/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/activity/alertsystem/index.php

    Definitions of Terms Used:

    Halema`uma`u Overlook vent: has been difficult to describe concisely. The vent is actually a pit, or crater, in the floor of the larger Halema`uma`u Crater in the floor of the even larger Kilauea caldera or crater - a crater within a crater within a crater. It is easiest to describe as a pit inset within the floor of a crater within a caldera. The pit is about 140 m (460 ft) in diameter at the Halema`uma`u Crater floor, is about 50 m in diameter at the pit floor, and is about 200 m (660 ft) deep. As of November, 2009, a lava pond surface has been visible in a hole in the floor of this pit.

    glow: light from an unseen source; indirect light.

    CD: Hawai`i County Civil Defense

    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.

    tonne: metric unit equal to 1,000 kilograms, 2,204.6 lbs, or 1.1 English tons.

    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.

    microradian: a measure of angle equivalent to 0.000057 degrees.

    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.

    More definitions with photos can be found at http://volcano.wr.usgs.gov/about/pglossary/index.php .

    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.

    This Quicktime movie shows the active lava pond deep within the Halema`uma`u vent cavity.  The lava is upwelling at the northern margin of the pond (the upper margin in this view), and slowly migrating south towards the bottom of the image, where it sinks out of view.  The pond is about 50 yards wide.  Small spattering sources appear and disappear occasionally.  This video was taken with a thermal camera (white is hot, dark blue is cold), which is able to see through the thick fume.  No views were possible with the naked eye today due to the fume, and only loud gas roaring sounds could be heard.This image was collected from a thermal camera at the Halema`uma`u Overlook, and shows the current activity at the summit.  The active lava pond, about 40 yards across, is situated deep within the vent cavity, at a depth of about 200 yards.  The lava surface consists of slowly migrating crustal plates, with a spattering source on the east margin of the pond.  The lava surface is slightly deeper than its usual level, owing to deflation during the current deflation-inflation (DI) cycle.
    A lava flow burns what little vegetation is left in this small kipuka at the top of the pali.The FLIR image on the right is a close-up infrared image of the current flow field, shown on the left.

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