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

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September 19, 2014 — Kīlauea


June 27th lava flow continues moving northeast, reaches open ground

The June 27th flow remains active and heading northeast, moving through Kaohe Homesteads. For several weeks the flow has been moving through thick forest, and today the flow front reached the forest boundary and more open ground. Nevertheless, active portions of the flow remain in the forest and fires continue. The flow front today was 2.4 km (1.5 miles) upslope of Apaʻa St.
Left: Another view of the narrow flow front. Kaohe Homesteads is in the lower left portion of the image. The vent for the June 27th lava flow is on Puʻu ʻŌʻō, which can be seen on the skyline. Right: View of the flow front, looking north. Pāhoa is located in the upper right portion of the photograph. The flow front today was 3.4 km (2.1 miles) from Pāhoa Village Road.
Views of the flow front from two different angles, with equivalent thermal images for comparison. The thermal images show that surface breakouts were focused on three areas near the flow front: 1) the flow front itself, 2) an area 300 meters (yards) behind the flow front and 3) a larger area about 1 km (0.6 miles) behind the flow front.
Left: A close-up view of the surface of the June 27th lava flow, near the flow front. The pāhoehoe flow is too thin and slow to topple trees as it passes, but instead the lava surrounds the trees and burns through the base. When the trees fall over, the flow surface may have cooled enough that the trunks remain intact. If the surface is hot enough to burn through the fallen trunks, all that remains is a line of ashen residue (see right side of image). Right: This Quicktime movie gives a quick aerial overview of the activity at the front of the June 27th lava flow. Kaohe Homesteads is in the lower left.

September 17, 2014 — Kīlauea


June 27th lava flow continues advancing northeast in Kaohe Homesteads

The June 27th lava flow remains active and continues advancing northeast in the forested, northwest portion of Kaohe Homesteads. The flow front today was 2.7 km (1.7 miles) from Apaʻa st. and 3.8 km (2.3 miles) from Pāhoa Village Road. Over past two days, the flow front has advanced at an average rate of 290 m/day (960 ft/day).
Left: Another view of the flow front in the northwest portion of Kaohe Homesteads. The leading portion of the flow front narrowed over the past two days and was roughly 150 m (500 ft) wide. Right: A view looking down the axis of the flow at the flow front. Pāhoa is in the upper right portion of the photograph.
Left: A close-up view of the flow surface near the flow front, which consisted of numerous, scattered small pāhoehoe lobes. Right: A view of the leading tip of the flow, which was moving through thick forest.
This Quicktime movie provides a brief aerial overview of activity at the flow front. Kaohe Homesteads is in the lower left.
Left: This thermal image shows the scattered pāhoehoe lobes that are active near the front of the June 27th flow. Right: A view of the flow front from tree level, with the lava hidden behind numerous tall trees.

Lava lake activity continues at Kīlauea's summit

Left: The summit eruption continues, with an active lava lake within Halemaʻumaʻu Crater. Halemaʻumaʻu fills up most of the image, and the lava lake can be seen near the bottom of the image contained within the smaller Overlook crater. Right: A closer look at the lava lake at Kīlauea's summit. The lake was roughly 53 m (170 ft) below the floor of Halemaʻumaʻu Crater this morning.

September 15, 2014 — Kīlauea


June 27th flow enters northwest portion of Kaohe Homesteads

The June 27th lava flow remains active and continues advancing towards the northeast. Recently, the flow front entered the Kaohe Homesteads subdivision, and is currently within the vacant, forested northwest portion of the subdivision. The flow front was 3.3 km (2.1 miles) upslope from Apaʻa Road and 4.3 km (2.7 miles) from Pāhoa Village Road.
Left: Another view of the flow front, in the northwest portion of Kaohe Homesteads subdivision. Right: A closer view of surface activity on the June 27th lava flow. This pāhoehoe flow consists of many small, scattered, slow-moving lobes burning vegetation.
Left: HVO geologists conduct a VLF (very-low frequency) survey to measure the rate of lava flowing through the lava tube on the June 27th lava flow. Right: An HVO geologist conducts a very-low frequency (VLF) survey of the lava tube to measure the rate of lava flowing through the tube. The measurement consists of two steps. First, a transect of VLF measurements across the roof of the tube is used to measure the cross-sectional area of lava flowing through the tube. Second, a radar gun is used to measure the speed that lava is flowing at that location. An open skylight is required for this speed measurement. By multiplying the cross-sectional area with the velocity, the volume rate of lava flowing through the tube can be estimated. Today's measurement showed a flow rate of 5.8 cubic meters per second (roughly 1500 gallons per second). Tracking the lava supply rate like this can be helpful for anticipating fluctuations in activity at the flow front.
This Quicktime movie provides an aerial view of activity near the front of the June 27th flow, where numerous pāhoehoe lobes are slowly burning vegetation.
This Quicktime movie shows the view through a skylight on the lava tube, which provided a clear view of the flowing lava stream.

September 12, 2014 — Kīlauea


June 27 flow moving to the northeast

As of Friday afternoon, September 12, 2014, the most distal front of the June 27th lava flow had reached a straight-line distance of 14.9 km (9.3 miles) from the source vent on the northeast flank of the Puʻu ʻŌʻō cone. The flow has continued in the northeast direction that it assumed in the middle of the week and is now only 171 meters (0.1 miles) from the boundary of the Kaohe Homesteads community. The flow is still within thick forest, so that dense plumes of smoke are created as vegetation is consumed. Small breakouts (visible as plumes in the middle distance) are also active closer to Puʻu ʻŌʻō, roughly midway along the length of the June 27th flow.
Left: View looking northeast along the terminus of the July 27th flow. Kaohe Homesteads is to the right, and Pāhoa town is in the middle center. The active flow is in the middle left. Right: View from above the middle part of the June 27th flow looking south at a small breakout that is burning forest along the previously existing flow margin. Heiheiahulu cone is in the upper left.
This Quicktime movie provides an aerial view of the flow front and its position relative to Kaohe Homesteads.
The photo on the left is compared here to a thermal image on the right, which provides a clear view of the flow front of the June 27th flow through the thick smoke. The vent for the June 27th flow is on Puʻu ʻŌʻō, which can be seen at the top of the normal photograph. After pouring in and out of ground cracks in late August, the flow finally emerged from the cracks around September 3 and began spilling out towards the north. The northwest portion of Kaohe Homesteads subdivision can be seen in the lower left of the images.

September 10, 2014 — Kīlauea


June 27th flow moves closer to Kaohe Homesteads

The June 27th lava flow remained active Wednesday afternoon, September 10, 2014, with the most distal flow front 14.5 km (9.0 mi; straight-line distance) from the vent on the northeast flank of the Puʻu ʻŌʻō cone, which is visible in the far background. Over the past day, the flow front direction shifted from a north trend to a more northeast trend, bringing the flow closer to the Forest Reserve boundary. The flow continued to advance through thick forest, creating smoke plumes as it engulfed trees and other vegetation. The smell of smoke has been detected far downwind of the flow, but fires are not spreading beyond the margin of the flow. Small, sluggish breakouts of lava (smoke plumes in far distance) also remain active closer to Puʻu ʻŌʻō, roughly midway along the length of the June 27th flow.
Left: View from above the end of the June 27th lava flow, looking along its northeast trend through the Wao Kele o Puna Forest Reserve. On the afternoon of September 10, 2014, the flow front was 0.6 km (0.4 mi) from the boundary between the Forest Reserve and Kaohe Homesteads, visible at far right. Right: Smoke plumes indicate the location of the June 27th lava flow, which was 0.6 km (0.4 mi) from the edge of Kaohe Homesteads, visible in foreground, on September 10. The flow was advancing toward the northeast.
This Quicktime movie provides an overview of activity near the front of the June 27th lava flow, and shows the position of the flow front relative to Kaohe Homesteads and Pahoa.

September 8, 2014 — Kīlauea


June 27th flow continues to advance north

Left: The June 27th flow continues its advance toward the north, creating a dense smoke plume as it spreads through the forest. The tip of the active flow today was 13.7 km (8.5 miles) straight-line distance from the vent, and 1.2 km (0.7 miles) from the eastern boundary of the Wao Kele o Puna Forest Reserve. This boundary is the western edge of Kaohe Homesteads subdivision, seen in the foreground. Puʻu ʻŌʻō is visible on the horizon, partly obscured by the smoke plume. The actual length of the flow, measured along its axis, is 15.7 km (9.8 miles). Right: This view shows the active flow front from behind. The lava feeding the flow emerges from a crack parallel to the road at lower right, which goes to the True/Mid-Pacific geothermal well site. Kaohe Homesteads is to the right, Pāhoa is at the upper right, and Ainaloa and Hawaiian Paradise Park are at upper left.
This Quicktime video provides an aerial view of the activity at the front of the June 27th lava flow.

Breakouts remain active closer to Puʻu ʻŌʻō

Several small breakouts persist along the middle part of the June 27th flow, closer to Puʻu ʻŌʻō. Most of these breakouts are burning trees as well, as seen in this photo. The flow front is in the distance, at upper left, and the closer smoke plumes are from these other breakouts.

September 6, 2014 — Kīlauea


June 27th flow remains active, with flow front moving north from ground crack

Following a reduction in surface activity yesterday, we observed an increase in surface flows today issuing from the ground crack. The reduction yesterday was likely due to lava filling the deep ground cracks. The flow front today was moving towards the north from the ground crack, through thick forest, creating a dense plume of smoke. The farthest active flows today were 13.2 km (8.2 miles) from the vent on Puʻu ʻŌʻō, and 1.4 km (0.9 miles) from the eastern boundary of the Wao Kele o Puna forest reserve. This boundary is the western edge of Kaohe Homesteads subdivision, seen at the bottom of this photograph. Puʻu ʻŌʻō is visible on the horizon in the upper right portion of the photograph.
Another view of the flow front, looking west. Lava issued from several spots along a deep ground crack earlier this week, as shown by the distinct fingers of lava making up the flow front. The thick smoke plumes show the flow front this morning was moving downslope towards the north (right in image), but it is too soon to know if this northerly flow direction will be sustained. Puʻu ʻŌʻō is in the upper left portion of the photograph.
This Quicktime movie gives a quick aerial overview of activity at the flow front.
This thermal image looks west at the June 27th flow front. The active tip of the flow is at the right side of the image, moving north. Lava issued from several spots along a deep ground crack, which has been traced with the dotted line in the left portion of the image. In addition, lava was filling another crack, also marked, closer to the active tip of the flow.
Left: Lava was filling another ground crack near the flow front, as indicated by a line of steam that extended a short distance west of the flow tip. At two spots along this ground crack we observed small pads of lava near the surface. Right: A wide view of Kīlauea and Mauna Loa volcanoes, looking northwest. Puʻu ʻŌʻō Crater, on Kīlauea's East Rift Zone, is the large fuming crater just to the left of the image center. Just to the right of the center point, on the northeast flank of Puʻu ʻŌʻō cone, smaller fume sources trace the lava tube supplying lava to the June 27th lava flow (the front of this flow is out of view to the right). In the distance, a faint plume of volcanic gas from the summit of Kīlauea can be seen below the clouds. The broad slopes of Mauna Loa form the skyline.
Breakouts remain scattered along the June 27th lava flow, and are not just limited to the flow front. Here surface flows have recently cut a swath through thick forest.

September 3, 2014 — Kīlauea


June 27th lava flow front emerges again from ground crack, continues advancing eastward

The June 27th lava flow remains active, with lava at the flow front issuing from a ground crack and advancing through thick forest, creating dense plumes of smoke. The farthest lava this afternoon was 13.2 km (8.2 miles) from the vent on Puʻu ʻŌʻō, and 1.3 km (0.8 miles) from the eastern boundary of the Wao Kele o Puna forest reserve. This forest reserve boundary is at the western boundary of Kaohe Homesteads subdivision, a portion of which is visible at the bottom of the photograph.
Left: This view looks east at the far end of the June 27th lava flow. In the center of the photograph is an isolated pad of lava which came out of ground crack last week. Further movement of lava within ground cracks has enabled the flow front to advance farther east, with lava issuing from a ground crack in the upper left portion of the photograph, where plumes of smoke mark the location of lava burning forest. Right: A closer view of the flow front, looking west. It is difficult to see the active lava surface through the thick smoke. Puʻu ʻŌʻō can be seen in the upper left portion of the photograph, partly obscured by smoke.
One small portion of the flow front was quite vigorous, with an open stream of lava moving through the forest.
This Quicktime movie shows activity at the front of the June 27th lava flow. The flow front continues to advance eastward, with lava issuing out of a ground crack and spreading through dense forest, creating thick plumes of smoke. The farthest lava this afternoon was 1.3 km (0.8 miles) from the eastern boundary of the Wao Kele o Puna forest reserve.
The surface flows at the front of the June 27th lava flow are fed by lava that is supplied through a lava tube that originates at the vent on Puʻu ʻŌʻō. This thermal image shows the lava tube close to Puʻu ʻŌʻō. Although the lava is several meters (yards) beneath the surface, it heats the surface sufficiently to be easily detected with thermal cameras.

September 1, 2014 — Kīlauea


June 27th lava flow continues advancing eastward, with lava plunging into another ground crack

This wide view, looking west, shows the position of the June 27th flow front relative to the nearby Kaohe Homesteads subdivision. The front of the flow is moving through thick forest, and its position can be seen by the plumes of smoke above the center of the photograph. Near these active surface flows, there was also steaming from a ground crack, resulting from lava deep in the crack. The farthest point of this steaming was 1.7 km (1.1 miles) west of the boundary of the Kaohe Homesteads subdivision.
The June 27th lava flow remains active at its leading edge, where lava is spreading out slowly into thick forest and also plunging into one of the many deep ground cracks that form Kīlauea's East Rift Zone. This Quicktime video shows the activity near the eastern edge of the flow. This swiftly moving stream of lava was about 2 meters (yards) wide, and was visible down to about 30 meters (100 feet) depth in the crack, where it disappeared from view.
The Quicktime video begins with a view of the steaming ground crack, where lava is moving deep within the crack. As the view rotates west, lava can be seen on the surface burning thick forest. Finally, the camera focuses on the eastern edge of the flow, where lava is plunging into the deep ground crack. This swiftly moving stream of lava was about 2 meters (yards) wide, and was visible down to about 30 meters (100 feet) depth in the crack, where it disappeared from view.
Left: Surface flows at the front of the June 27th flow continue slowly moving through thick forest, creating scattered brush fires. This view looks south, and the cone of Heiheiahulu is in the upper left. Right: Extending slightly beyond the lava flows on the surface, a steaming ground crack indicates that lava is continuing to move beneath the surface. The front of the surface flows is just above and to the right of the center point of the photograph, and the steaming ground crack runs along the vertical center line of the photograph. Puʻu ʻŌʻō can be seen on the horizon in the upper left.
Left: Near the leading edge of the lava on the surface, there was a swiftly moving stream of lava pouring into a deep ground crack (see Quicktime videos above). Puʻu ʻŌʻō is at the top of the photograph. Right: A closer look at the stream of lava pouring into the deep ground crack. See Quicktime videos above.

August 29, 2014 — Kīlauea


Far end of June 27th lava flow reactivates, lava spills out of steaming crack

The steaming ground crack observed yesterday suggested that lava was close to the surface within the crack, and today lava in the crack reached the surface and began spilling out into the thick forest. The leading edge of the lava today was near the abandoned well site (cleared area at left). This farthest lava was about 11.9 km (7.4 miles) from the vent on Puʻu ʻŌʻō (visible on horizon) and 2.6 km (1.6 miles) from the eastern boundary of the Wao Kele o Puna forest reserve.
A closer view of the pad of lava that emerged from the ground crack earlier this week, which had renewed surface flows today. At the east end (upper left in photograph) of the lava pad new breakouts spilled into adjacent ground cracks, and lava was visible within the ground crack extending farther to the east (visible by line of smoke extending towards upper left portion of photo). Heiheiahulu is visible in the upper right.
Left: A wide view of the leading edge of the June 27th lava flow, looking east down Kīlauea's East Rift Zone. The main body of the June 27th flow ends near the center of the photograph, where lava poured into a deep ground crack. After traveling along the ground crack, lava emerged at the surface earlier this week, creating an isolated pad of lava (where the thick smoke is just above the center of the photograph). This pad of lava had renewed surface activity today, with lava filling and spilling out of a ground crack extending farther to the east of the lava pad. Right: Another wide view of the leading edge of the June 27th lava flow, again looking east. This shows the east end of the isolated lava pad. The thick smoke originates from lava filling a deep ground crack up to the surface. The smoke partly obscures the abandoned well site.
At the site of the isolated pad of lava near the leading edge of the June 27th flow, renewed surface flows today resurfaced the existing lava flow and also spilled into nearby ground cracks. In this photograph, two large streams of lava plunge into a crack that is a couple meters (yards) wide.
At the far end of the lava-filled crack, lava spilled out towards the north a very short distance. In this view from a thermal camera, the small lobe of lava moving north is easily visible. The trees surrounding the crack show brighter colors as they are heated by the lava flow, but not to the point of combustion.
The vent for the June 27th lava flow is on the upper northeast flank of Puʻu ʻŌʻō. The vent area is now covered by lava, but the lava tube that carries lava to the flow front is easily visible by the line of blue-colored fume. In the lower right, two skylights can be seen.

August 28, 2014 — Kīlauea


Steaming extends northeast along ground crack, suggesting lava is advancing again along the crack

Steaming (center of photograph) was reported this morning east of the small pad of lava (just above center) that emerged from a ground crack this past week. This renewed progression of steaming suggests that lava is again continuing to advance beneath the surface, along these ground cracks. On our afternoon overflight, the farthest point of steaming was near an abandoned well site, which serves as a convenient landmark in this broad expanse of forest. The farthest steaming was 11.9 km (7.4 miles) northeast of the vent on Puʻu ʻŌʻō, and 2.6 km (1.6 miles) from the eastern boundary of the Wao Kele o Puna forest reserve. In the top portion of the photograph, numerous plumes of smoke originate from scattered surface flows burning vegetation. Puʻu ʻŌʻō can be seen on the horizon.
This figure compares the photo above with an equivalent view from a thermal camera. The plumes of smoke mark the farthest active lava on the surface (small, scattered lobes of pāhoehoe), which are also shown as small hotspots in the thermal image. The pad of lava that emerged from the ground crack earlier this week was inactive at the surface but still quite warm (high temperature patch in center of image). East of this pad of lava, steaming (just below the center of the photograph) has appeared over the past day, suggesting that lava is continuing to advance below the surface along a ground crack. Direct views into the crack were not possible due to thick vegetation, but close views of the steaming areas with the thermal camera reveal temperatures up to 190 C (370 F). These high temperature are further evidence of lava moving through the crack.
A closer of the new steaming. The thick vegetation obscures direct views of the ground crack, and only a line of steaming and browned vegetation is evident at the surface.
Slow-moving pāhoehoe advances through thick forest northeast of Puʻu ʻŌʻō. The pāhoehoe lobes surround, and burn through, the base of the trees. By the time the trees topple over, the lava surface temperature has cooled sufficiently that the downed trees do not completely burn through, leaving a field of tree trunks on the recent lava surface. One tree in the center of the photograph is completely surrounded by active lava, and likely on the brink of toppling over.
Left: Another view of the lava expanding into the forest. Right: Closer to the vent on Puʻu ʻŌʻō, one of several skylights provides a view of the flowing lava stream within the lava tube. This lava tube supplies lava from the vent to the active surface flows near the flow front.

August 27, 2014 — Kīlauea


Activity at flow front appears to stall but surface flows remain active behind flow front

The June 27th flow remains active, but surface flows at the very farthest reaches of the flow appear to have stalled today. The lava flow front consisted of an isolated pad of lava that emerged from a deep ground crack several days ago. Today, this pad of lava appeared inactive at the surface, with no sign obvious activity in the adjacent crack. On today's overflight, the farthest active surface flows were on the main body of the June 27th flow, and were 8.5 km (5.3 miles) from the vent on Puʻu ʻŌʻō, or about 6 km (3.7 miles) from the eastern boundary of the Wao Kele o Puna forest reserve.
A closer view of the southern lobe of the June 27th lava flow. Smoke plumes originate from active surface breakouts, the farthest today reached 8.5 km (5.3 miles) from the vent on Puʻu ʻŌʻō. The spot at which this lobe plunged into a deep ground crack last week can be seen near the bottom of the photograph. In the upper right portion of the photograph, smoke originating from active breakouts on the northern lobe can be seen.
A comparison of the normal photograph (see above) of the south lobe of the June 27th flow with an equivalent view from the thermal camera. The thermal camera clearly shows the extent of the farthest active breakout, which was relatively small.
Left: Another view of the south lobe of the June 27th flow, which plunged into a deep ground crack last week (this spot is visible at the right side of the photograph). This wide view, looking west, also shows another deep crack nearby, a short distance to the south of the active flows (which are producing the smoke plumes). This immediate area contains many ground cracks, which are part of Kīlauea's East Rift Zone. Puʻu ʻŌʻō can be seen in the distance. Right: The isolated pad of lava that emerged from the deep ground crack several days ago did not have any active breakouts at the surface today, but incandescent lava could be seen in numerous cracks on the surface. This likely represents lava that had ponded within the flow and remains hot, but immobile.

August 25, 2014 — Kīlauea


Lava resurfaces along crack, continues advancing through thick forest

The leading edge of the June 27th lava flow plunged into a deep crack on Kīlauea's East Rift Zone last week, and lava within the crack remained hidden for several days. Over the past day, lava returned to the surface at a point slightly farther along the crack, creating a small island of lava surrounded by thick forest. The farthest tip of the flow today was 11.4 km (7.1 miles) northeast of the vent on Puʻu ʻŌʻō, and 3.1 km (1.9 miles) from the eastern boundary of the Wao Kele o Puna forest reserve.
Left: A view of the small pad of lava that has emerged from the crack over the past day. The lava pad was about 800 m (0.5 miles) long, and was about 1.3 km (0.8 miles) east of the point where lava plunged into the crack. Right: Another view of the isolated pad of lava that has emerged from the crack. This view is towards the east, along the East Rift Zone. The spot at which lava flowed into the crack is to the west, out of view beyond the bottom of the photograph.
View of the pad of lava with the equivalent view from a thermal camera.
Puʻu ʻŌʻō crater remains partly obscured by thick fume. In particular, the northeastern portion of the crater (bottom left part of image) has recently been entirely obscured to the naked eye, but the thermal camera provides a clear view through the fume, revealing a small lava pond.

August 22, 2014 — Kīlauea


June 27th lava flow continues advancing northeast, with a portion entering a deep crack

This image shows a broad overview of activity at the front of the June 27th lava flow. Steaming in the lower-center portion of the photograph issues from a crack on the East Rift Zone. A portion of the lava flow has entered this crack, and the steaming extends out 1.4 km (0.9 miles) from the visible flow margin at the surface. Presumably, this steaming results from groundwater heated by lava deep within the crack. In the upper-right part of the image, a smoke plume originates from a more northerly lobe that is advancing through thick forest, triggering small brush fires. The vent for the June 27th lava flow is on Puʻu ʻŌʻō, the cone in the upper left part of the photo.
This Quicktime movie shows the southern front of the June 27th lava flow from Puʻu ʻŌʻō. Lava here has flowed into a deep crack on Kīlauea's East Rift Zone. The line of steam extending out from the visible flow margin at the surface is inferred to be caused by lava deep within the crack. This video also shows the lava stream beneath the flow surface, supplied by a lava tube, plunging into the crack.
Left: Looking west, this photo shows the far end of the steaming that extends out beyond the visible flow margin at the surface. Right: A closer look at one of the steam sources. The crack from which steam is issuing is not visible through the thick vegetation.
Left: A view looking east, near the front of the southern lobe that has entered the crack. Lava is inferred to be present in the deep crack beyond the visible margin of the flow, based on the line of steam sources as well as a vigorous cascade of lava seen in a skylight in the bottom portion of the photo. Right: A closer look at the lava stream plunging into the crack. The lava is fed from the vent on Puʻu ʻŌʻō via a lava tube.
North of where lava is entering the crack, another lobe is pushing through thick forest, triggering small brush fires. The source of the smoke marks the front of this lobe, and Puʻu ʻŌʻō can be seen just above this spot.
Puʻu ʻŌʻō crater remains partly obscured by thick fume. The thermal camera today revealed that several lava ponds persist in their usual locations in the northeast and southeast portions of the crater floor.

August 14, 2014 — Kīlauea


June 27 lava flow remains active in forest northeast of Puʻu ʻŌʻō

The June 27 lava flow remains active as a narrow lobe pushing through thick forest northeast of Puʻu ʻŌʻō, triggering small brush fires. This view is to the east, with the forested cone of Heiheiahulu partly obscured by the smoke plume from this angle. The flow front today was 8.7 km (5.4 miles) northeast of the vent on Puʻu ʻŌʻō.
Left: The surface flows active at the front of the June 27 lava flow are fed from lava flowing through a lava tube. This collapse of a portion of the roof has produced a skylight, and a direct view of the fluid lava stream several meters (yards) beneath the surface. Right: A remarkable perched lava pond was active on the June 27 lava flow more than a month ago. On August 12 a small lava flow erupted from the rim of the inactive pond, with the flow presumably originating from fluid lava that remained in the perched pond interior. This type of flow is commonly erupted from perched lava ponds and small lava shields, and we informally refer to these as "seeps". The seeps have a characteristic spiny, toothpaste-like, flow texture. Today, this seep was inactive, but the flow interior remained incandescent. The front of this small flow can be seen at the top of the photograph.
Another skylight and view into the tube supplying lava to the front of the June 27 lava flow.

August 12, 2014 — Kīlauea


June 27 flow continues advancing through forest northeast of Puʻu ʻŌʻō

The June 27 flow remains active, and has advanced further into the forest over the past week. The flow front today was 8.5 km (5.3 miles) northeast of the vent on Puʻu ʻŌʻō (see "map" link above for current flow field map). The flow's continued brisk advance rate is likely related, in part, to its continued confinement by local topography. Today, the narrow flow front was within one of the many linear depressions (grabens) on the East Rift Zone. Puʻu ʻŌʻō can be seen in the distance.
Left: Another view of the flow front, looking east. The small bump on the horizon, near the center of the photograph, is the forested cone of Heiheiahulu. Right: Portions of the June 27 lava flow continue to expand and cover older flows from Puʻu ʻŌʻō.
Left: Thick fume continues to obscure views into Puʻu ʻŌʻō Crater with the naked eye. The thermal camera has proven useful recently to see the hidden activity, which includes several small lava ponds (see thermal image from the July 29 overflight, below). Right: A skylight reveals the fluid lava stream within the main tube on the June 27 lava flow. The recently active perched lava pond is in the upper left portion of the photograph.
A closer look into the skylight on the June 27 lava flow, revealing complex structure within the lava tube. The bright incandescent area is the fluid lava stream, which was slowly but steadily flowing through the tube.

August 10, 2014 — Kīlauea


Lava lake activity continues in Halemaʻumaʻu Crater

The usual lava lake activity continues in Halemaʻumaʻu Crater with no major changes related to the recent hurricane. This afternoon the lake surface was about 40 meters (130 ft) below the floor of Halemaʻumaʻu Crater, which has been typical over the past several weeks. Lake surface migration was from north to south (top of photo to bottom), and occasional gas bubbles were bursting through the crust.

August 6, 2014 — Kīlauea


June 27 lava flow reaches forest boundary

The June 27 flow continues to advance at a brisk rate, and has reached the forest boundary over the past week. On today's overflight, thick plumes of smoke from burning vegetation partially obscured the flow front. See the "maps" link above for today's flow field map.
A wider view of the flow front, looking east. The June 27 flow is the lighter-colored lava passing through the center of the photograph.

July 29, 2014 — Kīlauea


June 27 lava flow advance rate increases

The June 27 flow front has advanced more rapidly over the past four days, and is now 4.2 km (2.6 miles) from the vent. This recent increased advance rate is due to the confinement of the flow against the slopes of an older perched lava channel, from 2007. The advance rate will likely drop in the coming days as the flow passes the confines of the perched channel and spreads out on flatter topography.
Left: Another view of the front of the June 27 flow, looking northeast. The flow front has narrowed as it has been confined against the slopes of the 2007 perched lava channel, and this is associated with a higher advance rate of the flow front over the past four days. Right: View, looking southwest, of Puʻu ʻŌʻō and the new perched lava pond. Puʻu ʻŌʻō is the fume-filled crater in the top half of the image. The circular feature in the lower portion of the photograph is the perched lava pond active earlier this month, which was fed by the June 27 lava flow. This perched lava pond is now inactive, but the June 27 flows continue to advance towards the northeast (see other photos from today).
Visual-thermal comparison of Puʻu ʻŌʻō crater, looking west. In the normal photograph on the left, large portions of the crater floor are obscured by thick volcanic fume. The thermal image on the right can "see" through this fume, revealing features in the crater. Over the past month, a large portion of the crater floor has subsided. Within this triangular subsidence area, three small lava ponds were active today. Two are visible in this thermal image, while a third (near the South lava pond) is blocked by a steep wall from this angle.

July 28, 2014 — Kīlauea


Puʻu ʻŌʻō crater at dawn

A time-lapse camera on the rim of Puʻu ʻŌʻō crater captured this image at dawn. The view is towards the southeast, and shows two glowing pits in the southern portion of the crater floor. Our overflight the next day showed that these pits are filled with small lava ponds.
 


 October 2013 and before -  Lava  Updates:

October 21, 2013 — Kīlauea


Lava flows at forest boundary northeast of Puʻu ʻŌʻō

Left: Pāhoehoe lava on the Kahaualeʻa 2 flow invades the forest northeast of Puʻu ʻŌʻō, burning and toppling trees and creating plumes of smoke. Right: A wider view of the Kahaualeʻa 2 flow margin at the forest boundary.
This thermal image looks southwest towards the vent on Puʻu ʻŌʻō, and shows much of the Kahaualeʻa 2 flow. Hotter colors (yellow and white) represent active breakouts, while warm colors (red and purple) show recently active portions of the flow. The Kahaualeʻa 2 flow consists of numerous scattered breakouts of pāhoehoe lava, with a narrow finger of lava forming the flow front. The flow front today was 5.8 km (3.6 miles) northeast of the vent on Puʻu ʻŌʻō.
Left: A close-up view of one of the many breakouts of pāhoehoe on the Kahaualeʻa 2 flow. Right: An HVO geologist shields his face from the intense heat as he takes a sample of active lava on the Kahaualeʻa 2 flow. The chemistry of the lava is analyzed through time and used to study changes in the magmatic system.

September 19, 2013 — Kīlauea


Kahaualeʻa 2 source vent and Puʻu ʻŌʻō

Left: The Kahaualeʻa 2 flow is fed from a spatter cone, shown here, on the northeast edge of Puʻu ʻŌʻō's crater floor. The spatter cone is about 8 m (26 ft) high. Right: The Kahaualeʻa 2 flow extends to the north and northeast of Puʻu ʻŌʻō. From the edge of the flow, where it first reaches the forest, Puʻu ʻŌʻō still appears to tower above the surrounding plain.

Views of Kahaualeʻa 2 flow

Left: Active breakouts on the Kahaualeʻa 2 are scattered over a broad area. Here, a breakout near the edge of the forest engulfs trees and burns dead foliage. Right: This beautiful bubble of glass, about the size of an small orange, adorns the surface of a breakout on the Kahaualeʻa 2 flow. Note the delicate bubble walls stretched so thin that they grade from the color of honey to transparent.

Halemaʻumaʻu lava lake

The lava lake in Halemaʻumaʻu has fallen slightly over the past few weeks. It is now about 55 m (180 ft) below the surrounding crater floor.

August 27, 2013 — Kīlauea


Halemaʻumaʻu and HVO

The Hawaiian Volcano Observatory and Jaggar Museum are located near the summit of Kīlauea and are visible atop the cliff to the right. They are about 2 km (1.25 miles) north-northwest of the lava lake in Halemaʻumaʻu, fuming (but not directly visible) at the left edge of the photo.

Puʻu ʻŌʻō and northeast spatter cone

Left: Early morning view of Puʻu ʻŌʻō, looking toward the southwest. The fume rising from the bottom of the photo marks the trace of the lava tube carrying lava to the Kahaualeʻa 2 flow front. Right: The Kahaualeʻa 2 flow is fed from a spatter cone on the northeast edge of Puʻu ʻŌʻō’s crater. Today, this spatter cone, which is about 6 m (20 ft) tall, was weakly spattering from it top.

August 23, 2013 — Kīlauea


Small explosion at Halemaʻumaʻu

Left: At 9:48 PM on Friday, August 23, a collapse of a piece of the wall above the lava lake in Halemaʻumaʻu triggered a small explosion. The explosion bombarded the rim of Halemaʻumaʻu around the old visitor overlook with molten gobs of spatter as big as dinner plates. Dense lithic fragments from the collapsed wall, and at least as large as a baseball, were also thrown back out of the vent and onto the rim. These images were recorded by a webcam positioned on the rim of Halemaʻumaʻu, about 120 m (395 ft) above the lake surface. The smaller time-stamp at the upper left corner is the correct acquisition time (the larger time-stamp is based on the camera clock, which drifts over time). Right:

August 16, 2013 — Kīlauea


Ocean entry near Kupapaʻu Point hangs on

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

Rain, steam, smoke, and lava

The Kahaualeʻa 2 flow continues to invade the forest line north of Puʻu ʻŌʻō. Poor weather prevented good views but made for an eerie scene.

Lava lake in Halemaʻumaʻu at a relatively high level

The lava lake in Halemaʻumaʻu was 35 m (115 ft) below the floor of the crater this morning. The lake is about 220 m (720 ft) long and 160 m (525 ft) wide.
Left: A thin gas plume permitted a decent view of the south wall of the pit holding the lava lake in Halemaʻumaʻu. This wall is overhung by up to 15 m. Today the lava lake was not spattering at its usual point near the left side of the lake in this view. Right: Instead, the lava lake was spattering at points on the west and northwest side of the lake. 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). If the lake continues to rise, pieces of this overhang may collapse (note the cracks at lower right marking planes of weakness).

August 9, 2013 — Kīlauea


Satellite view of activity at summit and east rift zone

This image was captured on Friday, August 9, by the Advanced Land Imager sensor aboard NASA's Earth Observing 1 satellite, and shows Kīlauea volcano from the summit down the east rift zone. Although this is a false-color image, the color map has been chosen to mimic what the human eye would expect to see. Bright red pixels depict areas of very high temperatures, and show active lava. Two areas are active on Kīlauea. At the summit, a circulating lava lake in Halemaʻumaʻu crater produces the bright pixels at the left edge of the image. Along the east rift zone, the ongoing Puʻu ʻŌʻō eruption is now feeding two lava flows. The Peace Day flow has active surface flows on the coastal plain and an active ocean entry, just west of Kalapana village, while the Kahaualeʻa 2 flow is active at the forest boundary north of Puʻu ʻŌʻō. Satellite images such as this help fill in observational gaps between field visits.

August 8, 2013 — Kīlauea


Kupapaʻu Point ocean entry weak, but still active

Using a telephoto camera lens, an HVO scientist captured this view of the Kupapaʻu Point ocean entry on the morning of August 7. Although no lava flow activity was observed on the coastal plain near the ocean entry, small streams of lava still poured into the sea.
Zooming his camera in even more.... An up-close view of the easternmost lava streams entering the ocean. Reminder to all lava observers: Peering through a telephoto lens is the safest way to view Kīlauea Volcano's ocean entry.

July 19, 2013 — Kīlauea


Ocean entry at Kupapaʻu Point is still active

The ocean entry at Kupapaʻu Point remains active, with several lava steams entering the water creating a moderate plume.
Several birds take a closer view of the ocean entry. Narrow streams of lava were battered by the surf as they poured into the water.

June 27, 2013 — Kīlauea


Kahaualeʻa 2 flow still expanding north of Puʻu ʻŌʻō, ocean entries remain active

The Kahaualeʻa 2 flow remains active north of Puʻu ʻŌʻō, and has expanded a very minor amount into the forest, burning trees. The flow, which consists of slowly moving pāhoehoe, has widened but advanced little over the past two weeks.
Left: A wider view of a portion of the Kahaualeʻa 2 flow margin at the forest boundary. Right: The Kahaualeʻa 2 flow, which is active north of Puʻu ʻŌʻō, is fed from a vent at this cone on the northeast rim of Puʻu ʻŌʻō crater. Small openings at the top of the cone contain sloshing lava, and two skylights at the very start of the Kahaualeʻa 2 lava tube provided views of a swiftly moving lava stream rushing downslope.
This thermal image shows the eastern ocean entry at Kupapaʻu Point. Just inland from the entry point a patch of slightly warmer temperatures indicates an area of recent small breakouts. Inland from this warm patch you can see a narrow line of elevated temperatures that traces the path of the lava tube beneath the surface that is supplying lava to this ocean entry. Two plumes of high temperature water spread out from the entry point.

June 11, 2013 — Kīlauea


Lava flows near Puʻu ʻŌʻō and on coastal plain; ocean entry continues

Two ocean entry points remain active near Kupapaʻu Point, near the boundary of Hawaiʻi Volcanoes National Park. The eastern entry has produced a larger plume than that at the western entry, which tends to be weak and wispy. Today several small breakouts were active just inland of the eastern entry point, creating a narrow cascade of lava pouring down the sea cliff.
Left: This photo looks south towards Puʻu ʻŌʻō, where a vent is supplying lava to the Kahaualeʻa II flow, north of the cone. This slow-moving flow has reached the forest line, producing small scattered brush fires. Right: A close-up of the Kahaualeʻa II flow burning vegetation at the forest line, just north of Puʻu ʻŌʻō. The flow consists of numerous slow-moving pāhoehoe lobes.
The summit eruption in Halemaʻumaʻu crater remains active. The lava lake is within the Overlook crater (the source of the gas plume), which is in the southeast portion of Halemaʻumaʻu Crater.

 

Eruption-viewing opportunities change constantly, so refer to this page often. Those readers planning a visit to Kilauea or Mauna Loa volcanoes can get much useful information from Hawai`i Volcanoes National Park.

 

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
November 21, 2009


PActivity Summary for past 24 hours: A DI event is nearly complete. At the summit, a circulating, bubbling, and spattering lava pond surface was visible in a hole in the vent cavity floor deep beneath Halema`uma`u Crater floor; its level rose several meters covering the entire vent floor before dropping but remaining visible in the Overlook vent Webcam. Sulfur dioxide emission rates from the Halema`uma`u and east rift zone vents remain elevated. Lava flows are active on the coastal plain; lava flows through tubes to the coast and is entering the ocean at two locations west of Kalapana.

Past 24 hours at Kilauea summit: The lava pond continued bubbling and circulating at its low level within a hole in the vent cavity floor deep beneath the vent rim (in the Halema`uma`u Crater floor) until 7:23 pm when it abruptly rose several meters, peaking and covering the entire vent floor at about 7:30 pm, then draining back into the hole nearly an hour later; the lava level in the hole remained higher than it was when the night started but lower than the 7:30 pm peak. Glow is visible from the Jaggar Museum Overlook. This morning, the dense white plume moves to the southwest through beautiful clear skies. The most recent sulfur dioxide emission rate measurement was 800 tonnes/day on November 20, still elevated above the 2003-2007 average of 140 tonnes/day. Very small amounts of mostly ash-sized tephra continued to drop out of the plume near the vent.

The summit tiltmeter network recorded weak inflation completing the most recent DI event. The GPS network, which is less sensitive than the tiltmeter network, recorded contraction starting at the beginning of November switching to extension after November 12th.

Seismic tremor levels remained at low values with a drop. The number of RB2S2BL earthquakes remained below background levels. Two earthquakes were strong enough to be located on south flank faults.

Past 24 hours at the middle east rift zone vents and flow field: Magma continued to degas 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 1,300 tonnes/day on November 21, below the 2003-2007 average of 1,700 tonnes/day. Very weak glow was again recorded from the crater last night.

The tiltmeter on the north flank of Pu`u `O`o recorded the switch to DI inflation around 9:30 an yesterday and continued slow inflation. The GPS network, which is less sensitive than the tiltmeter network, recorded continued slow contraction of the cone, amounting to almost 3 cm of contraction over the past 3 months. Seismic tremor levels at Pu`u `O`o and the TEB vent were at low values.

Lava flows through two tube branches to the coast, across State- and privately-owned land, and was entering the ocean at two general locations - Waikupanaha and west Waikupanaha 700 m (2,300 ft) to the west. Yesterday, HVO geologists found scattered surface flows over the coastal plain and at least one possible surface flow on the pali; a single entry at Waikupanaha and several at the west Waikupanaha location were active. GOES-WEST imagery showed thermal anomalies on the coastal plain suggesting continuing surface flow activity through dawn.

HAZARD ALERT: The lava delta and adjacent areas both inland and out to sea are 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 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://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:

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.

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.

 

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

Previous Archived 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 |

 

 

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