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The farthest active breakout on the June 27th flow reached about 8 ...
Pu‘u ‘Ō‘ō — Breakout
Pu‘u ‘Ō‘ō — Breakout
Pu‘u ‘Ō‘ō — Breakout

The farthest active breakout on the June 27th flow reached about 8 km (5 miles) northeast of the vent on Pu‘u ‘Ō‘ō. The tip of this breakout was narrow and burning forest. Pu‘u ‘Ō‘ō is at the top of the photograph.

The farthest active breakout on the June 27th flow reached about 8 km (5 miles) northeast of the vent on Pu‘u ‘Ō‘ō. The tip of this breakout was narrow and burning forest. Pu‘u ‘Ō‘ō is at the top of the photograph.

Over the past week small flows have filled the bottom of Pu‘u ‘Ō‘ō ...
Over the past week small flows have filled the bottom of Pu‘u ‘Ō‘ō....
Over the past week small flows have filled the bottom of Pu‘u ‘Ō‘ō....
Over the past week small flows have filled the bottom of Pu‘u ‘Ō‘ō....

Over the past week small flows have filled the bottom of Pu‘u ‘Ō‘ō Crater. These flows originated from vents in the south portion of the crater, and one of the flows can be seen near the center of the photograph.

Over the past week small flows have filled the bottom of Pu‘u ‘Ō‘ō Crater. These flows originated from vents in the south portion of the crater, and one of the flows can be seen near the center of the photograph.

Lava lake in Halema‘uma‘u Crater reaches new high level...
Lava lake in Halema‘uma‘u reaches new high level
Lava lake in Halema‘uma‘u reaches new high level
Lava lake in Halema‘uma‘u reaches new high level

The Overlook crater lava lake, within Halema‘uma‘u Crater at Kīlauea's summit, has been rising over the past few days, and today reached the highest point yet measured for the current summit eruption. The lava lake this afternoon was 20 meters (66 feet) below the Overlook crater rim.

The Overlook crater lava lake, within Halema‘uma‘u Crater at Kīlauea's summit, has been rising over the past few days, and today reached the highest point yet measured for the current summit eruption. The lava lake this afternoon was 20 meters (66 feet) below the Overlook crater rim.

The lava level was high enough at the lava lake this evening that b...
The lava level was high enough at the lava lake this evening that b...
The lava level was high enough at the lava lake this evening that b...
The lava level was high enough at the lava lake this evening that b...

The lava level was high enough at the lava lake this evening that bits of spatter were reaching the rim of the Overlook crater.

Landsat satellite image shows June 27th flow...
Landsat satellite image shows June 27th flow
Landsat satellite image shows June 27th flow
Landsat satellite image shows June 27th flow

This satellite image was captured on Monday, April 20, 2015 by the Landsat 8 satellite. 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. White areas are clouds.

This satellite image was captured on Monday, April 20, 2015 by the Landsat 8 satellite. 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. White areas are clouds.

Brick signs for Fredericksburg Magnetic Observatory and National Ocean Service.
Geomagnetism Fredericksburg
Geomagnetism Fredericksburg
Geomagnetism Fredericksburg

Brick signs for Fredericksburg Magnetic Observatory and National Ocean Service.

Lava from Pu'u 'Ō'ō is still active, but not an immediate threat...
Lava from Pu'u 'Ō'ō is still active, but not an immediate threat
Lava from Pu'u 'Ō'ō is still active, but not an immediate threat
Lava from Pu'u 'Ō'ō is still active, but not an immediate threat

Active surface flows on the northeast flank of Pu‘u ‘Ō‘ō on March 12, 2015. The activity is a continuation of a breakout that began on February 21, which diverted lava from the tube system and helped to starve the supply of lava to the June 27th flow front near Pāhoa.

Active surface flows on the northeast flank of Pu‘u ‘Ō‘ō on March 12, 2015. The activity is a continuation of a breakout that began on February 21, which diverted lava from the tube system and helped to starve the supply of lava to the June 27th flow front near Pāhoa.

Barnegat Bay residence times in days
Barnegat Bay residence times in days
Barnegat Bay residence times in days
Barnegat Bay residence times in days

Barnegat Bay residence times in days for (a) scenario T, only tidal forcing; (b) scenario TB, combined offshore hydrodynamic forcing; (c) scenario TBR, streamflow with combined hydrodynamic forcing; and (d) scenario TBRM, full suite with meteorological forcing

Barnegat Bay residence times in days for (a) scenario T, only tidal forcing; (b) scenario TB, combined offshore hydrodynamic forcing; (c) scenario TBR, streamflow with combined hydrodynamic forcing; and (d) scenario TBRM, full suite with meteorological forcing

This photograph looks upslope and shows another narrow lobe on the ...
This photograph looks upslope and shows another narrow lobe on the ...
This photograph looks upslope and shows another narrow lobe on the ...
This photograph looks upslope and shows another narrow lobe on the ...

This photograph looks upslope and shows another narrow lobe on the breakout that is roughly 6 km (4 miles) northeast of Pu‘u ‘Ō‘ō. This lobe was moving along the south margin of the June 27th flow.

This photograph looks upslope and shows another narrow lobe on the breakout that is roughly 6 km (4 miles) northeast of Pu‘u ‘Ō‘ō. This lobe was moving along the south margin of the June 27th flow.

Map showing flow field changes...
Map showing flow field changes
Map showing flow field changes
Map showing flow field changes

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area of the flow on April 3 is shown in pink, while widening and advancement of the flow as of April 9 is shown in red. We were not able to map some parts of the flow field with breakouts today due to poor weather, and these areas are denoted in boxes.

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area of the flow on April 3 is shown in pink, while widening and advancement of the flow as of April 9 is shown in red. We were not able to map some parts of the flow field with breakouts today due to poor weather, and these areas are denoted in boxes.

Scattered breakouts northeast of Pu‘u ‘Ō‘ō continue...
Scattered breakouts NE of Pu‘u ‘Ō‘ō continue
Scattered breakouts NE of Pu‘u ‘Ō‘ō continue
Scattered breakouts NE of Pu‘u ‘Ō‘ō continue

Breakouts continue northeast of Pu‘u ‘Ō‘ō in three main areas: 1) at the northern base of Pu‘u ‘Ō‘ō cone, 2) north of Pu‘u Kahauale‘a and 3) about 6 km (4 miles) northeast of Pu‘u ‘Ō‘ō. This photograph looks east and shows the breakout about 6 km from Pu‘u ‘Ō‘ō.

Breakouts continue northeast of Pu‘u ‘Ō‘ō in three main areas: 1) at the northern base of Pu‘u ‘Ō‘ō cone, 2) north of Pu‘u Kahauale‘a and 3) about 6 km (4 miles) northeast of Pu‘u ‘Ō‘ō. This photograph looks east and shows the breakout about 6 km from Pu‘u ‘Ō‘ō.

A closer look at the leading tip of the farthest downslope breakout...
leading tip of the farthest downslope breakout. The tip of the bre...
leading tip of the farthest downslope breakout. The tip of the bre...
leading tip of the farthest downslope breakout. The tip of the bre...

A closer look at the leading tip of the farthest downslope breakout. The tip of the breakout was burning forest, and was 6.9 km (4.3 miles) northeast of the June 27th vent on Pu‘u ‘Ō‘ō.

Breakouts persist northeast of Pu‘u ‘Ō‘ō...
Breakouts persist NE of Pu‘u ‘Ō‘ō
Breakouts persist NE of Pu‘u ‘Ō‘ō
Breakouts persist NE of Pu‘u ‘Ō‘ō

Breakouts remain active in three general areas near Pu‘u ‘Ō‘ō: 1) at the northern base of Pu‘u ‘Ō‘ō, 2) just north of Kahauale‘a, and 3) the most distal breakout, about 6 km (4 miles) northeast of Pu‘u ‘Ō‘ō. This photograph shows much of the most distal breakout, a portion of which was burning forest. Pu‘u ‘Ō‘ō can be seen near the top of the photograph.

Breakouts remain active in three general areas near Pu‘u ‘Ō‘ō: 1) at the northern base of Pu‘u ‘Ō‘ō, 2) just north of Kahauale‘a, and 3) the most distal breakout, about 6 km (4 miles) northeast of Pu‘u ‘Ō‘ō. This photograph shows much of the most distal breakout, a portion of which was burning forest. Pu‘u ‘Ō‘ō can be seen near the top of the photograph.

The breakout north of Kahauale‘a has one lobe that has traveled alo...
The breakout north of Kahauale‘a has one lobe that has traveled alo...
The breakout north of Kahauale‘a has one lobe that has traveled alo...
The breakout north of Kahauale‘a has one lobe that has traveled alo...

The breakout north of Kahauale‘a has one lobe that has traveled along the west side of the perched lava channel that was active in late 2007. This breakout consists of blue glassy pāhoehoe, which is easily visible in the photograph on the left. The white box shows the rough extent of the thermal image on the right.

The breakout north of Kahauale‘a has one lobe that has traveled along the west side of the perched lava channel that was active in late 2007. This breakout consists of blue glassy pāhoehoe, which is easily visible in the photograph on the left. The white box shows the rough extent of the thermal image on the right.

In the time since our last overflight (March 24), a new collapse pi...
New collapse pit has formed in the western portion of Pu‘u ‘Ō‘ō
New collapse pit has formed in the western portion of Pu‘u ‘Ō‘ō
New collapse pit has formed in the western portion of Pu‘u ‘Ō‘ō

In the time since our last overflight (March 24), a new collapse pit has formed in the western portion of Pu‘u ‘Ō‘ō Crater. This circular pit can be seen in the lower left portion of the photograph, and measures about 27 m (roughly 90 ft) in diameter. Numerous hot cracks were observed in this general area during previous visits on foot.

In the time since our last overflight (March 24), a new collapse pit has formed in the western portion of Pu‘u ‘Ō‘ō Crater. This circular pit can be seen in the lower left portion of the photograph, and measures about 27 m (roughly 90 ft) in diameter. Numerous hot cracks were observed in this general area during previous visits on foot.

Map showing flow field changes...
Map showing flow field changes
Map showing flow field changes
Map showing flow field changes

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area of the flow on March 24 is shown in pink, while widening and advancement of the flow as of April 3 is shown in red.

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area of the flow on March 24 is shown in pink, while widening and advancement of the flow as of April 3 is shown in red.

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