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Lava Flow Crosses Highway, Enters Ocean

This is a Hawai‘i County Civil Defense Message for Saturday, May 19, 2018, at 11 p.m.

Hawaiian Volcano Observatory continues to monitor active flows. Flow front #1 has crossed Highway 137 at the 13-mile marker and has entered the ocean. Flow front #2 is approximately 400 Meters from Highway 137. Highway 137 is closed between Kamali‘i Road and Pohoiki Road.  Kamali‘i Road is closed between Highway 130 and Highway 137. Residents in the area have been evacuated. All persons are asked to stay out of the area.

The lava has entered the ocean. Be aware of the laze hazard and stay away from any ocean plume.

This thermal map shows the fissure system and lava flows as of 12:15 pm on Saturday, May 19. The two primary lava flows originate from the Fissure 20-22 area, and crossed Pohoiki Road over the past day. The flow front position based on a 6:40 p.m. update is shown by the red circle. The black and white area is the extent of the thermal map. Temperature in the thermal image is displayed as gray-scale values, with the brightest pixels indicating the hottest areas. The thermal map was constructed by stitching many overlapping oblique thermal images collected by a handheld thermal camera during a helicopter overflight of the flow field. The base is a copyrighted color satellite image (used with permission) provided by Digital Globe. (USGS Map)

  • Laze is formed when hot lava hits the ocean sending hydrochloric acid and steam with fine glass particles into the air.
  • Health hazards of laze include lung, eye and skin irritation.
  • Be aware that the laze plume travels with the wind and can change direction without warning.

USGS: Threat of Even Larger Steam-Driven Violent Explosion

The U.S. Geological Survey (USGS) announces that with ash eruptions occurring from Kīlauea’s summit this week, there is a threat of an even larger steam-driven violent explosion. Such an eruption could happen suddenly and send volcanic ash 20,000 feet into the air, threatening communities for miles. USGS and NOAA’s National Weather Service are working together to observe, model and warn the public of hazardous conditions. Here is where you can find the information you need to stay safe.

This photo was taken on Wednesday, May 15, 2018, At 11:05 a.m. Photograph from the Jaggar Museum, Hawai‘i Volcanoes National Park, captures an ash plume rising from the Overlook crater. Ash falling from the plume can be seen just to the right side (and below) the plume. (USGS Photo)

Observations and Status of Kīlauea

While the ​USGS Hawai‘i Volcanoes Observatory​ is positioning staff to observe the volcano and best communicate its status and evolution, they rely heavily on the weather forecasts from NOAA. Wind forecasts, ​along with dispersion models such as HYSPLIT,​ are critical in understanding where sulphur dioxide (SO2) and particulate matter (PM2.5) will disperse from fissures and vents to ensure safety of USGS observers, emergency managers and the public.

Ashfall Advisories, Warnings and Current Weather Forecast from Honolulu

On Tuesday, May 15, 2018 the National Weather Service issued the first ever ashfall advisory for Hawai‘i. Forecasters will issue ashfall advisories and warnings when ashfall is a hazard. NOAA predicts where an ash plume will go and how much ash will accumulate using USGS’s ​Ash3d Volcanic Ash Dispersion Model​.

Volcanic Ash Advisories​ and ​Aviation Warnings

Volcanic ash clouds can threaten air traffic by sandblasting windscreens, clogging pitot tubes, and in severe cases, causing jet engines to shut down. NOAA issues volcanic ash warnings to alert pilots to potential ash in the atmosphere and will include volcanic ash in forecasts for airports.

Tips to Stay Safe

During explosive eruptions, volcanic ash can disrupt downwind populations by causing breathing problems, impacting water quality, clogging air filters, shorting out power systems and making transportation difficult.​ If your community is threatened by ash, you are advised to do the following:

  • Seal windows and doors.
  • Protect electronics and cover air intakes and open water sources.
  • Avoid driving as visibility will be reduced and roads may become slippery.
  • Remain indoors to avoid inhaling ash particles unless it’s absolutely necessary to go outside. If you have a respiratory illness, do not go outside.
  • If you must go outside, cover your mouth and nose with a mask or cloth.

No-Entry Zone Established for Hawai‘i Electric Light Crews in Leilani Estates

Hawai‘i Electric Light announces that all of Lanipuna Gardens and a portion of Leilani Estates has been designated as a no-entry zone for its crews.

Hawaiian Electric Facebook Photo.

These areas are hazardous to enter due to continued ground swelling and cracking, sudden fissure activity, and unsafe levels of SO2. Crews were working in the subdivision in the last few days and have narrowly escaped situations that could have resulted in severe injury. Hawai‘i Electric Light’s priority continues to be safety and can no longer allow its employees to enter hazardous areas.

Poles and wires continue to fall due to changes in the ground formation and seismic activity. Hawai‘i Electric Light continues to warn residents to assume that all downed lines and equipment are energized and dangerous. Stay at least three cars lengths away from downed lines and use caution around all poles and overhead lines.

The following areas are in the no-entry zone. This area may be extended.

  • Leilani Avenue from Pomaikai Street to Pohoiki Road
  • Malama Street, east from Pomaikai Street
  • Kahukai Street from Nohea Street to Leilani Avenue
  • Pomaikai, Moku, and Kupono Streets south of Leilani Avenue
  • All streets east beginning with Nohea Street
  • All of Lanipuna Gardens including Hinalo, Lauone, and Honuaula Streets, and all connector roads into Lanipuna Gardens

Check Hawai‘i Electric Light’s website (www.hawaiielectriclight.com), Twitter (@HIElectricLight), and Facebook (HawaiianElectric) accounts for updates.

Volcano Activity Update 6: Civil Defense Message to Puna District

VIDEO UPDATE 6: May 1, 2018, 12:50 p.m.

HAWAI’I ISLAND: Hawai’i County Civil Defense talking to Big Island Now about the current lava activity. More information here: http://bigislandnow.com/2018/05/01/volcano-activity-update-puu-oo-crater-floor-collapses/#BigIslandNow

Posted by BigIslandNow.com on Tuesday, May 1, 2018

 

Hawai‘i County Civil Defense Administrator Talmadge Magno spoke to Big Island Now about the island’s recent seismic and lava activity.

Seismicity and ground deformation started increasing at about 3 a.m. on Tuesday, May, 1, 2018, between Pu‘u ‘Ō’ō and Highway 130, and has now migrated beyond 130, he said.

The East Rift runs underground from Kīlauea Summit at Halemaumau all the way down to the ocean at Cape Kumakahi.

Magno asks Puna District residents to stay informed and encourages residents to sign up for civil defense messages and alert via text, email and RSS feed.

He advises Puna residents to prepare themselves—not just for this event—but for any natural disaster, with at least 14 days worth of supplies.

Magno warns visitors to stay off the Kalapana flow field, as a rift could open up any time above that area.

UPDATE 5, May 1, 2018, 11:05 a.m.

Area residents felt the effects of the recent seismic and lava activity.

“I got a Red Cross message this morning informing me of the deflation and saying [the quake was] 3 miles from Highway 130 and EOC (Emergency Operations Center) was activated at 5 a.m.,” said Keoni Delacruz Veloria, a Hilo resident.

“I felt a couple [tremors] around this morning and figured that is what was happening,” said Pāhoa resident Holly Povlsen Johnson. Looks like the biggest one [earthquake] is by the road that we take down toward Kalapana. Will be interesting if it keeps going to the east toward the red road along the ocean.”

This map shows recent changes to Kīlauea’s East Rift Zone lava flow field. The area of the active flow field as of March 14, 2018, is shown in pink, while widening and advancement of the active flow as of April 13 is shown in red. Older Puʻu ʻŌʻō lava flows (1983–2016) are shown in gray. The yellow line is the trace of the active lava tubes. The Kamokuna ocean entry is inactive. The blue lines over the Puʻu ʻŌʻō flow field are steepest-descent paths calculated from a 2013 digital elevation model (DEM), while the blue lines on the rest of the map are steepest-descent paths calculated from a 1983 DEM (for calculation details, see http://pubs.usgs.gov/of/2007/1264/). Steepest-descent path analysis is based on the assumption that the DEM perfectly represents the Earth’s surface. DEMs, however, are not perfect, so the blue lines on this map can be used to infer only approximate flow paths. The base map is a partly transparent 1:24,000-scale USGS digital topographic map draped over the 1983 10-m DEM.

UPDATE 4, May 1, from a report published by USGS HVO at 8:49 a.m.

Just after 2 p.m. HST today, April 30, 2018, a marked increase in seismicity and ground deformation (change in ground surface shape) began at Pu‘u ‘Ō’ō on Kīlauea Volcano’s East Rift Zone. A few minutes later, a thermal webcam (PTcam) located on the rim of the Pu‘u ‘Ō’ō crater showed the first of two episodes of crater floor collapse; the second collapse began at 3:20 p.m. and lasted about an hour.

Webcam views into the crater and surrounding area were frequently obscured by poor weather conditions. However, shortly after 4 p.m., the PTcam recorded images that were likely the signature of small explosions from the western side of the crater as the floor collapsed.

Uplited Puʻu ʻŌʻō floor, April 23, 2018. PC: USGS

At the time of this update 6 p.m., April 30, there was no evidence of new lava within the crater, seismicity remained elevated in the vicinity of Pu’u ‘Ō’ō, and ground deformation at Pu’u ‘Ō’ō had significantly slowed.

Kīlauea’s summit eruption has thus far not been affected by the afternoon’s activity at Pu‘u ‘Ō’ō.

USGS Hawaiian Volcano Observatory scientists continue to closely monitor Kīlauea’s East Rift Zone and summit. A helicopter overflight of Pu’u ‘Ō’ō and the 61g flow field is scheduled for early Tuesday, weather permitting.

HVO webcam images are posted online.

Electronic Tilt at Kīlauea Summit and East Rift Zone, April 25 to May 1, 2018. The blue line shows the radial tilt at Uwēkahuna (UWE), on the northwest rim of Kīlauea’s caldera. The green line is radial tilt at Pu‘u ‘Ō‘ō (POC), on the north flank of Pu‘u ‘Ō‘ō cone. These are recorded by continuously operating electronic tiltmeters. Positive changes often indicate inflation of the magma storage areas beneath the caldera or Pu‘u ‘Ō‘ō, but may also result from heavy rainfall or, occasionally, instrumental malfunctions. USGS graphic

Activity Summary: An intrusion of magma occurred overnight in the lower East Rift Zone extending from the general area of Puʻu ʻŌʻō eastward at least as far as Highway 130. As of 8:30 this morning, the level of activity has decreased significantly, but it is too soon to know if this is merely a pause. The intrusion began yesterday afternoon (April 30) associated with collapse of the Puʻu ʻŌʻō crater floor. The summit lava lake is unchanged and has risen overnight to just below the rim of the Overlook crater vent. Early this morning (May 1), HVO issued a Volcano Activity Notice calling attention to this intrusion and raising the possibility of a new outbreak along the rift zone if activity intensifies.

Residents of lower Puna should remain on alert and monitor Hawai‘i County Civil Defense messages.

Number of earthquakes per day during the past week, April 25–May 1, 2018, indicated by (blue bars. The red line is the cumulative moment (energy) release. USGS graphic.

Summit Observations: The summit lava lake remains at a high level. Overall, the summit lava lake has shown no response to activity in the middle and lower East Rift Zone. Summit tiltmeters recorded very little change overnight. Tremor amplitude is fluctuating with lava lake spattering. Elevated summit sulfur dioxide emission rates persist.

Depth of earthquakes during the past week (April 25–May 1, 2018) in the area shown on the map above. USGS graphic.

Puʻu ʻŌʻō Observations: HVO tiltmeters recorded sudden and dramatic changes accompanying the onset of crater floor collapse at Puʻu ʻŌʻō yesterday (April 30) between about 2 and 4 pm. Weather obscured web camera views of the crater, however thermal camera images showed the collapse in progress followed by emission of high temperature gases continuing into this morning. HVO field crews attempting to reach Puʻu ʻŌʻō this morning (May 1) were turned back by ash in the air above Puʻu ʻŌʻō, likely due to continuing collapse within the crater and vigorous gas emissions. Reddish ash was also noted in abundance on the ground around Puʻu ʻŌʻō. Seismicity remains elevated at Puʻu ʻŌʻō but tiltmeters near the cone show no significant deformation at this time.

Lava Flow Observations: There is no lava flow activity from the 61g lava flow on the coastal plain or pali and no lava is flowing into the ocean. Lava flow activity continues on the upper flow field, above the pali and closer to Puʻu ʻŌʻō, and does not pose a threat to nearby communities at this time. Areas of the upper flow field with active lava flows are located within the Kahaualeʻa Natural Area Reserve, which has been closed to the public by DLNR since 2007 due to volcanic hazards.

Webcam views of the flow field are available here.

Maps of the lava flow field can be found here.

For more information about the Kahaualeʻa NAR closure, go online.

Lava Flow Field and Ocean Entry Hazards: Hazards of active or recent lava flows include, but are not limited to: hot lava surfaces that can cause serious burns upon contact with unprotected or exposed skin; rough, uneven, and sharp terrain that can lead to falls, abrasions, lacerations and other injuries; high air temperature and humidity that can lead to dehydration or heat exhaustion; and steamy ground-fog produced by heavy rain falling (sometimes with little warning) on active or recent lava flows; this steam can severely limit visibility, can be acidic and should be avoided.

UPDATE 3, May 1, 10:30 a.m.

The collapse of the Puʻu ʻŌʻō crater floor on Kīlauea Volcano’s East Rift Zone has
triggered increases in earthquake activity and deformation along a large section of the rift zone, according to Christina Neal, scientist-in- charge at Hawai’i Volcanoes Observatory (HVO).

Neal said that seismicity was occurring as far east as Highway 130, and warned residents of lower Puna to remain alert and watch for further information about the status of the volcano at www.hawaiicounty.gov/active-alert.

“An outbreak of lava in a new location is one possible outcome,” Neal said. “At this time it is not possible to say with certainty if or where such an outbreak may occur, but the area downrift (east) of Puʻu ʻŌʻō is the most likely location, as this is where seismicity and deformation have been concentrated overnight.”

Meanwhile, Hawai‘i County has closed the Kalapana lava viewing area amid the possibility of an eruption, and security has been posted to ensure than no unauthorized persons enter the area.

“We don’t want people hiking in that area, which is downslope from the rift,” Parks and Recreation Deputy Director Maurice Messina said.

Messina said that vendors at the viewing area were told to vacate the area. He noted that the lava viewing area can draw 500 to more than 2,000 visitors, depending on the level of volcanic activity.

A magnitude 4.0 earthquake just offshore of Puʻu ʻŌʻō occurred at 2:39 a.m. Tuesday, May 1, 2018—the largest of a sequence of tremors along the rift zone.

There is no risk of tsunami at that magnitude.

Deformation is the term used to describe change in the surface of a volcano, such as swelling, sinking or cracking, which can be caused by movements in the Earth’s crust due to motion along faults, according to the U.S. Geological Survey.

UPDATE 2: May 1, 2018, 9:30 a.m.

This is a Civil Defense message for Tuesday morning, May 1, 2018 at 9:30.

The Hawaiian Volcanoes Observatory reports increased shallow earthquake activity in the Puna District below Kīlauea Volcano in the area between Puʻu ʻŌʻō and Highway 130.

This means an outbreak of lava in a new location could occur. While it is not possible to predict where an outbreak could occur, the area east of Puʻu ʻŌʻō is a possible location.

Due to the increased seismic activity, the following are issued:

The Hawai‘i County Department of Parks and Recreation has shut down the lava viewing area in Kalapana due to the proximity to the increased hazardous activity.

Lower Puna area residents are advised to stay informed by listening to the radio and Civil Defense text alerts and social media sites; this webpage will also be updated.

ORIGINAL POST, May 1, 7:54 a.m.

The Hawaiian Volcanoes Observatory reports increased shallow earthquake activity in the Puna District below Kīlauea Volcano in the area between Puʻu ʻŌʻō and Highway 130.

This means an outbreak of lava in a new location could occur.

While it is not possible to predict where an outbreak could occur, the area east of Puʻu ʻŌʻō is a possible location.

Due to the increased seismic activity, lower Puna area residents are advised to stay informed. Monitor Hawai‘i County Civil Defense messages here.

Just before 10 a.m. on Monday, April 30, 2018, a break in the weather allowed HVO’s webcam to capture this image of the lava lake within Halema‘uma‘u at the summit of Kīlauea. Following multiple overflows of the lava lake last week, the lake level dropped over the weekend in concert with the switch to summit deflation. Early on Monday morning, the lava lake level was estimated to be about 49 feet below the vent rim, but shortly thereafter, the summit switched to inflation, with the possibility of the lake level rising in the hours/days. Instead, HVO reported the collapse of the Puʻu ʻŌʻō crater floor Monday afternoon, April 30, 2018. PC: USGS

On Tuesday, May 1, 2018, at 4:54 a.m. HVO reported that a collapse of the Puʻu ʻŌʻō crater floor Monday afternoon, April 30, on Kīlauea Volcano’s East Rift Zone has prompted increases in seismicity and deformation along a large section of the rift zone, with seismicity currently occurring as far east as Highway 130.

A outbreak of lava in a new location is one possible outcome. At this time it is not possible to say with certainty if or where such an outbreak may occur, but the area downrift (east) of Puʻu ʻŌʻō is the most likely location, as this is where seismicity and deformation have been concentrated overnight.

Recent Observations

Between about 2 and 4:30 p.m. on April 30, following weeks of uplift and increasing lava levels within the cone, the crater floor at Pu’u ‘Ō’ō on Kīlauea Volcano’s East Rift Zone collapsed.

Poor weather prevented HVO from flying over the activity or seeing details of the activity in our web cameras on site.

Following the collapse, HVO seismometers and tiltmeters recorded an increase in seismic activity and deformation from Kīlauea Volcano’s summit to an area about 6 to 10 miles downrift (east) of Puʻu ʻŌʻō.

Overnight, this activity localized downrift of Puʻu ʻŌʻō and continued to propagate eastward along the rift zone.

The largest earthquake of this sequence so far was a magnitude 4.0 earthquake just offshore south of Pu’u ‘Ō’ō at 2:39 a.m. this mornin.

Kīlauea’s summit eruption has thus far not been affected by the change at Pu’u ‘Ō’ō.

Hazard Analysis

The migration of seismicity and deformation downrift (east) of Puʻu ʻŌʻō cone following Monday’s collapse indicates that a large area along the East Rift Zone is potentially at risk for a new outbreak.

The location of any future outbreak will determine what areas are in the path of new lava flows.

The situation is rapidly evolving and USGS Hawaiian Volcano Observatory scientists continue to closely monitor Kīlauea’s East Rift Zone and summit.

Hawaiian Volcanoes Observatories and Hawai‘i County Civil Defense are continuing to monitor the situation. More updates will be posted at BigIslandNow.com as information becomes available.

For more information, email askHVO@usgs.gov.

Summit Deflation Leads to Slight Drop in Lava Lake Level

The U.S. Geological Survey reports summit deflation began the morning of Wednesday, April 18, 2018, and the lake level has dropped slightly.

In this photo, an HVO geologist checks on a time-lapse camera on the rim of Halema‘uma‘u Crater. A large spatter site is active along the east margin of the lake. Courtesy U.S. Geological Survey.

On Wednesday morning, April 18, the lake was about 14 meters (46 feet) below the overlook of the crater rim, having dropped roughly 4 meters (13 feet) since yesterday morning.

HVO Releases New Photo of Halemaumau Crater

One month ago the summit lava lake was at the rim of the Overlook crater (the small crater in the center of the photo), spilling lava onto the floor of Halemaʻumaʻu Crater (the larger crater that fills much of the photo), creating the dark flows surrounding the Overlook crater.

Click to enlarge

Click to enlarge

Since that time the lava lake has dropped, associated with summit deflation, and today the lake level was about 60 meters (200 feet) below the Overlook crater rim. The stack of recent overflows is visible on the wall of the Overlook crater as the layer of dark lava atop the older, light colored lava forming the majority of the Overlook crater wall.

The photo is taken from the southeast rim of Halemaʻumaʻu Crater. The closed Halemaʻumaʻu overlook is in the upper left corner of the photo. Jaggar Museum and HVO can be seen as a small bump on the horizon in the upper right portion of the photograph.

Lava Lake at Halemaumau Crater Continues to Drop

Kīlauea Volcano’s summit lava lake continued to drop today (May 15, 2015).

Click to enlarge

Click to enlarge

Measurements of the lake surface late this afternoon showed that it was 62 m (203 ft) below the top of the newly-created vent rim, a ridge (or levee) of solidified lava about 8 m (26 ft) thick that accumulated on top of the Halemaʻumaʻu Crater floor from multiple overflows of the vent during the past two weeks.

Click to enlarge

Click to enlarge

Webcam Captures “Bathtub Ring” Falling Into Lava Lake

This sequence of HVO webcam images of Kīlauea Volcano’s summit vent, recorded between 1:28 and 1:32 p.m., HST, on May 12, 2015, captures the moment a section of the dark-colored “bathtub ring” (a veneer of fresh lava that coats the vent wall as the lava lake level drops) fell into the lava lake (center).

Click to enlarge

Click to enlarge

The lava veneer collapse, which produced a visible cloud of rock and lava fragments, agitated the lava lake surface and exposed lighter-colored layers of older rock in the vent wall (right).

VIDEO – Lava Lake Remains High

The lava lake in the Overlook crater, within Halemaʻumaʻu Crater at Kīlauea’s summit, remains at a high level and close to the Overlook crater rim. Overflows onto the Halemaʻumaʻu Crater floor have built up the rim of the Overlook crater several meters, and recent overflows are visible in the right side of the photograph.

Spattering was vigorous today in the southern portion of the lake. From this view, the spattering was hidden behind a portion of the Halemaʻumaʻu Crater wall, but airborne spatter can be seen in the bottom left portion of the photo. The summit of Mauna Loa can be seen in the upper right.  (Click to enlarge)

Spattering was vigorous today in the southern portion of the lake. From this view, the spattering was hidden behind a portion of the Halemaʻumaʻu Crater wall, but airborne spatter can be seen in the bottom left portion of the photo. The summit of Mauna Loa can be seen in the upper right. (Click to enlarge)

The lake level this afternoon was about 7 meters (yards) above the original (pre-overflow) floor of Halemaʻumaʻu Crater.

VIDEO:

This Quicktime movie shows spattering at the margin of the summit lava lake in Halemaʻumaʻu Crater.

Click to view the Quick Time Movie

Click to view the Quick Time Movie

Spattering has been common at the lake, and when it occurs is easily visible from the public viewing area at Jaggar Museum. This video shows a closer view from the rim of Halemaʻumaʻu, which is closed to the public due to volcanic hazards.

Lava Breakouts Remain Active – Lava Lake Remains High

The June 27th lava flow remains active, with breakouts focused in several areas northeast of Puʻu ʻŌʻō.

Click to enlarge

Click to enlarge

The farthest downslope activity observed on today’s overflight was roughly 8 km (5 miles) northeast of Puʻu ʻŌʻō.

This photograph shows one of the active breakouts closer to Puʻu ʻŌʻō.  (Click to enlarge)

This photograph shows one of the active breakouts closer to Puʻu ʻŌʻō. (Click to enlarge)

One of several lobes on the June 27th flow that was at the forest boundary today, burning vegetation northeast of Puʻu ʻŌʻō.

Summit lava lake in Halemaʻumaʻu Crater remains at high level

Click to enlarge

Click to enlarge

Over the past week, the summit lava lake in the Overlook crater rose and spilled out onto the floor of Halemaʻumaʻu Crater, creating the dark flows in the south part of Halemaʻumaʻu (left side of crater from this direction). The extent of the lake itself, set within the Overlook crater, is slightly difficult to distinguish from this view but the spattering at the lake margin is visible. The overflows onto the Halemaʻumaʻu Crater floor, not counting the area of the lake itself, total about 11 hectares (28 acres).

A closer look at the lava lake and overflows on the floor of Halemaʻumaʻu Crater.

hvo147The outline of the Overlook crater, and the active lake, is easier to distinguish in this view.

From this angle, the extent of the lava lake within the Overlook crater is much easier to distinguish from the surrounding overflows.

hvo148

The closed Halemaʻumaʻu parking lot is in the right side of the photograph.

Video of Another Explosion at Lava Lake – Tourists Don’t Know What to Think!

A portion of the Halemaʻumaʻu Crater wall collapsed at 1:20 pm today, impacting the lava lake and triggering a small explosion of spatter and a robust particle-laden plume.

Click to enlarge

Click to enlarge

Fist-size clasts were deposited around the closed Halemaʻumaʻu visitor overlook.

A sequence of still images taken from the webcam positioned at the closed Halemaʻumaʻu overlook, spanning about six seconds.

explosion seriesThe collapse originated from a portion of the wall directly below the webcam, but just out of view. Large pieces of molten spatter can be seen flying through the air and being deposited on the crater walls below the camera.

This Quicktime movie shows a small explosive event that occurred at 1:20pm today at the summit lava lake. A collapse of a portion of the Halemaʻumaʻu Crater wall impacted the lake and triggered an explosion of spatter. Fist-size clasts were found scattered along the rim of Halemaʻumaʻu Crater near the  closed visitor overlook.  (Click to view Video)

This Quicktime movie shows a small explosive event that occurred at 1:20pm today at the summit lava lake. A collapse of a portion of the Halemaʻumaʻu Crater wall impacted the lake and triggered an explosion of spatter. Fist-size clasts were found scattered along the rim of Halemaʻumaʻu Crater near the closed visitor overlook. (Click to view Video)

Lava Lake Overflows Vent Rim

Photo from the rim of Halemaʻumaʻu showing the lava lake in the completely filled Overlook crater. Repeated overflows are beginning to construct levees around the lake, such that the level of the lake is now perched about 2 m (7 ft) above the original floor of Halemaʻumaʻu.

Kīlauea Volcano’s summit lava lake, which was about 12 m (40 ft) below the vent rim on April 25 (left), overflowed the vent rim for the first time at about 9:40 p.m., HST, on April 28. As of noon on April 29 (right), the lava lake had overflowed the vent rim several more times. These Webcam images capture the summit vent before and after the overflows. (Click to enlarge)

Kīlauea Volcano’s summit lava lake, which was about 12 m (40 ft) below the vent rim on April 25, overflowed the vent rim for the first time at about 9:40 p.m., HST, on April 28. As of noon on April 29, the lava lake had overflowed the vent rim several more times. (Click to enlarge)

Rise in Lava Lake Creates Surge in Visitation at Volcanoes National Park

Thousands of additional visitors are flocking to Hawai‘i Volcanoes National Park to witness the large lava lake steadily rise at the summit of Kīlauea volcano. lava Lake 427

Over the last several days, visitors waited up to 30 minutes or longer to park. To ease traffic once the Jaggar Museum and Kīlauea Overlook parking lots fill up, rangers are currently redirecting vehicles during peak visitation hours to park at the Kīlauea Military Camp ball field. From there, visitors can hike one mile to the Jaggar Museum observation deck, the closest and best vantage point to view the spectacular lava lake.

“Visitors should come prepared to ensure a safe and enjoyable park experience,” said Superintendent Cindy Orlando. “We encourage people to avoid peak hours, and arrive after 10 p.m. and before 4 a.m. if possible, or they will likely wait in line for parking. The park remains open 24 hours a day,” she said.

Tips for an optimal viewing experience:

  • Be prepared to hike one mile each way between Kīlauea Military Camp ball field and the Jaggar Museum observation deck on Crater Rim Trail. Wear sturdy closed-toe shoes, bring rain gear, water, binoculars, a flashlight, and extra batteries.  ​
  • Carpool if possible to reduce the number of vehicles in the parking areas.
  • As a courtesy to other visitors, no “tailgating” in the Jaggar Museum or Kīlauea Overlook parking lots. Choose another picnic location so others have a chance to view the eruption.
  • To observe viewing and weather conditions, monitor the USGS Hawaiian Volcano Observatory webcams. The KI camera provides a panoramic view of Halema‘uma‘u Crater from HVO.
  • High levels of dangerous sulfur dioxide (SO2) gas and volcanic ash can be blown over Jaggar Museum by southerly winds. These gases are a danger to everyone, particularly to people with heart or respiratory problems, young children and pregnant women. Kīlauea Visitor Center offers updates on air quality 24 hours a day, and visitors can monitor the Hawaii SO2 network website.

In addition, the public is reminded that park entrance fees apply and that the use of unmanned aircraft (drones) is prohibited in all national parks.

 

Lava Lake Within 10 Feet of Floor of Halema’uma’u Crater

This photo shows the lava lake in the Overlook crater this morning, when it reached to within 3 m (10 ft) of the floor of Halemaʻumaʻu. This is the highest the lava lake has reached during the current summit eruption.

Click to enlarge

Click to enlarge

This is a view of spattering at the east corner of the lava lake this morning.

Click to enlarge

Click to enlarge

Lava Lake Rises Close to Surface

This photo, taken yesterday mid-day, shows the lava lake as seen from the west side of Halemaʻumaʻu, which offers a different perspective.

Click to enlarge

Click to enlarge

The lava lake was about 10 m (33 ft) below the floor of Halemaʻumaʻu at this time.

This grainy evening photo shows the lake at 6:30 PM, when it was a mere 7 m (23 ft) below the Halemaʻumaʻu Crater floor.

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Click to enlarge

Lava Lake Now Visible From Jaggar Overlook

The level of the lava lake within the Overlook crater, set within Halemaʻumaʻu Crater at the summit of Kīlauea Volcano, continues to rise.

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Yesterday, the level was as high as 14 meters (46 feet) below the Overlook crater rim. This photograph was taken from the rim of Halemaʻumaʻu Crater, in an area closed to the public due to volcanic hazards, but the lava level was high enough today that the lava lake surface could be seen from Jaggar Overlook, which is open to the public.

Hawaiian Volcano Observatory Update – Kilauea Slowly Moving/Lava Lake in Halemaʻumaʻu Crater Remains Active

Kahaualeʻa 2 flow slowly moving through forest northeast of Puʻu ʻŌʻō

The Kahaualeʻa 2 flow continues to slowly move through the forest northeast of Puʻu ʻŌʻō. Yesterday, the active flow front was 6.3 km (3.9 miles) northeast of the vent on Puʻu ʻŌʻō.

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Puʻu ʻŌʻō is just left of the center of the photograph in the distance, partially obscured by the smoke.

A closer view of the active flows at the forest boundary, and the numerous plumes of smoke resulting from active lava igniting ʻōhiʻa trees and other vegetation.

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Click to Enlarge

This thermal image, taken from the helicopter on today’s overflight, shows the area of active pāhoehoe near the flow front of the Kahaualeʻa 2 flow, northeast of Puʻu ʻŌʻō. Blue and purple areas show warm but inactive areas of the flow, while the white and yellow areas are actively flowing lava. The flow surface consists of numerous scattered pāhoehoe lobes, and the advancement of the flow as a whole results from the combined, incremental movement of these individual lobes.

The black (cold) area at the top of the image is forest.  Click to Enlarge

The black (cold) area at the top of the image is forest. Click to Enlarge

Lava lake in Halemaʻumaʻu Crater remains active

The summit lava lake is contained within the Overlook crater, which is about 160 m (520 ft) by 210 m (690 ft) in size, and set within the larger Halemaʻumaʻu Crater.

 The lava lake this week has been about 50 m (160 ft) below the rim of the Overlook crater. Click to Enlarge

The lava lake this week has been about 50 m (160 ft) below the rim of the Overlook crater. Click to Enlarge

A closer look at the summit lava lake.

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Click to Enlarge

HVO Update – Kilauea Ocean Entry Near Kupapaʻu Point Hangs On – Lava Lake in Halemaʻumaʻu at Relatively High Level

The ocean entry east of the National Park boundary near Kupapaʻu Point remains weak, with a wispy plume, as seen in this photo looking southwest along the coast.

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Photos from Hawaii Volcanoes Observatory

The main entry point of the Kupapaʻu ocean entry comprises a few small streams of lava, seen here cascading into the water.

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The Kahaualeʻa 2 flow continues to invade the forest line north of Puʻu ʻŌʻō.

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Poor weather prevented good views but made for an eerie scene.

The lava lake in Halemaʻumaʻu was 35 m (115 ft) below the floor of the crater yesterday morning.

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The lake is about 220 m (720 ft) long and 160 m (525 ft) wide.

A thin gas plume permitted a decent view of the south wall of the pit holding the lava lake in Halemaʻumaʻu.  Yesterday the lava lake was not spattering at its usual point near the left side of the lake in this view.

This wall is overhung by up to 15 m.

This wall is overhung by up to 15 m.

Instead, the lava lake was spattering at points on the west and northwest side of the lake. If the lake continues to rise, pieces of this overhang may collapse (note the cracks at lower right marking planes of weakness).

This photo shows the spattering on the lake's northwest side. The pit wall to the right overhangs the lake by about 10 m (33 ft)

This photo shows the spattering on the lake’s northwest side. The pit wall to the right overhangs the lake by about 10 m (33 ft)

 

Hawaiian Volcano Observatory Update – Kahaualeʻa Flow Front Stalls, New Overflow in Puʻu ʻŌʻō

Breakouts have diminished over the past few days on the Kahaualeʻa flow (heading northeast of Puʻu ʻŌʻō), and the flow front has not advanced significantly since April 8.

Compare Saturday’s thermal image with that from the April 8 overflight. 

Thermal Image

During Saturday’s flight, there were no active breakouts at the flow front.

Breakouts have diminished over the past few days on the Kahaualeʻa flow (heading northeast of Puʻu ʻŌʻō), and the flow front has not advanced significantly since April 8. Compare today’s thermal image with that from the April 8 overflight. During Saturday’s flight, there were no active breakouts at the flow front.

A vigorous flow was erupted on the floor of Puʻu ʻŌʻō crater starting early this morning from a cone near the north rim, but a smaller flow was also erupted from a spatter cone near the south rim around noon. This photo captures a burst of spatter from the southern cone as the small flow was erupted.

Lava Flow 2

Lava erupted this morning from the cone near the north rim of Puʻu ʻŌʻō crater, with a small portion of the flow emptying out onto the east spillway. This new flow brings the floor of the crater slightly closer to the north crater rim.

Lava Flow 3

This short Quicktime movie shows spattering from a cone near the south rim of Puʻu ʻŌʻō crater as a short lava flow is erupted.

 

 

Lava Lake Continues Tantalizing Trend – Cool Youtube Clip of Lava Reaching the Ocean

The lava lake within Halema‘uma‘u Crater at Kīlauea is tantalizing visitors and park staff as it continues its current trend of repetitive rising and falling, attracting many to the best vantage point: the overlook at Jaggar Museum.

Photo taken Friday, October 19 courtesy of the U.S. Geological Survey Hawaiian Volcano Observatory

Scientists at the U.S. Geological Survey’s Hawaiian Volcano Observatory report that the lava lake rose to levels approximately 125 feet or less beneath the crater floor this morning, and HVO webcams today suggest the lake rose even higher, before sinking again this afternoon.

Dr. Jim Kauahikaua, HVO’s Scientist-in-Charge, says the lava lake will be visible from the overlook at Jaggar Museum if it comes within about 65 feet of the crater floor. The lava lake reached its highest level today since forming after an explosive eruption on March 19, 2008.

Meanwhile, rangers urge park visitors to obey traffic signs and to be safe. Visitors are gathering at park overlooks after dark to view the dramatic glow that lava beneath the surface casts upon clouds and the plume of volcanic gas, hoping molten lava will rise high enough to be seen. The parking lot at Jaggar Museum is busy with hopeful observers, who are reminded to park only in marked stalls and heed all signs.

All visitors who plan to come after dark are urged to bring flashlights, especially those who park at Kīlauea Overlook, which affords panoramic views of the crater and Kīlauea caldera. Earth cracks, rocks, and other hazards are not easily seen in the dark.

In addition, several pairs of nēnē, the federally endangered Hawaiian goose, are beginning to nest near the Jaggar Museum parking lot, and are sometimes spotted along roadsides and trails. Cars are the leading cause of nēnē fatalities, and drivers are cautioned to be alert, and to drive the speed limit.

“Safety is our number one priority,” said Park Superintendent Cindy Orlando. “We encourage everyone to visit during this fascinating episode, but to exercise caution. Staff will be assisting visitors with parking and interpretation of the current activities. If people come prepared and proceed as directed, they should have an unforgettable experience,” she said.

Hawai‘i Volcanoes National Park is open 24 hours a day.
For more information, visit www.nps.gov/havo. For webcams and daily Kīlauea status updates, visit the USGS HVO website, http://hvo.wr.usgs.gov/activity/kilaueastatus.php.

ALSO OF NOTE… check out this video that was uploaded to youtube today:

[youtube=http://youtu.be/MmXYwq6BV_Q]