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Volcano Hazard Program images.

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Spatter cone and small lava pond on Pu‘u ‘Ō‘ō's crater floor...
Spatter cone and small lava pond on Pu‘u ‘Ō‘ō's crater floor
Spatter cone and small lava pond on Pu‘u ‘Ō‘ō's crater floor
Spatter cone and small lava pond on Pu‘u ‘Ō‘ō's crater floor

A small lava lake, which has been present on the northeast side of Pu‘u ‘Ō‘ō's crater floor for nearly a year, has evolved into a tiny pond perched several meters (yards) above the surrounding crater floor, as pictured here. The pond sits near the top of a mound of lava composed of spatter cones and lava pond overflows.

A small lava lake, which has been present on the northeast side of Pu‘u ‘Ō‘ō's crater floor for nearly a year, has evolved into a tiny pond perched several meters (yards) above the surrounding crater floor, as pictured here. The pond sits near the top of a mound of lava composed of spatter cones and lava pond overflows.

Pu‘u ‘Ō‘ō crater and the northern lava flow...
Pu‘u ‘Ō‘ō and the northern lava flow
Pu‘u ‘Ō‘ō and the northern lava flow
Pu‘u ‘Ō‘ō and the northern lava flow

The eastern rim of Pu‘u ‘Ō‘ō is no longer visible, having been buried by flows mostly from the small lava lake on the northeast side of the crater floor. A mound of lava with a complex of spatter cones, visible in the background, now surrounds the lava lake, which is only visible from the air.

The eastern rim of Pu‘u ‘Ō‘ō is no longer visible, having been buried by flows mostly from the small lava lake on the northeast side of the crater floor. A mound of lava with a complex of spatter cones, visible in the background, now surrounds the lava lake, which is only visible from the air.

This photo, identical to the previous one, just includes labels for...
This photo, identical to previous one, just includes labels for the...
This photo, identical to previous one, just includes labels for the...
This photo, identical to previous one, just includes labels for the...

This photo, identical to the previous one, just includes labels for the flows that spilled from the northern and southern sides of the crater.

This photo, identical to the previous one, just includes labels for...
This photo, identical to previous one, just includes labels for the...
This photo, identical to previous one, just includes labels for the...
This photo, identical to previous one, just includes labels for the...

This photo, identical to the previous one, just includes labels for the flows that spilled from the northern and southern sides of the crater.

The lava flow fed the northeastern lava lake in Pu‘u ‘Ō‘ō remains w...
Pu‘u ‘Ō‘ō — Active Lava Flow
Pu‘u ‘Ō‘ō — Active Lava Flow
Pu‘u ‘Ō‘ō — Active Lava Flow

The lava flow fed the northeastern lava lake in Pu‘u ‘Ō‘ō remains weakly active at the northern base of the Pu‘u ‘Ō‘ō cone. The front of the flow is burning lichen on old ‘A‘ā flows erupted from Pu‘u ‘Ō‘ō during 1983-1986. The eastern edge of Pu‘u ‘Ō‘ō is at the upper right side of the photo.

The lava flow fed the northeastern lava lake in Pu‘u ‘Ō‘ō remains weakly active at the northern base of the Pu‘u ‘Ō‘ō cone. The front of the flow is burning lichen on old ‘A‘ā flows erupted from Pu‘u ‘Ō‘ō during 1983-1986. The eastern edge of Pu‘u ‘Ō‘ō is at the upper right side of the photo.

High view of Pu‘u ‘Ō‘ō crater...
High view of Pu‘u ‘Ō‘ō
High view of Pu‘u ‘Ō‘ō
High view of Pu‘u ‘Ō‘ō

Lava flows have spilled from Pu‘u ‘Ō‘ō crater over the past few weeks. One flow went out the southern end of the crater and traveled a short distance downslope to the southeast before stopping.

Lava flows have spilled from Pu‘u ‘Ō‘ō crater over the past few weeks. One flow went out the southern end of the crater and traveled a short distance downslope to the southeast before stopping.

Pu‘u ‘Ō‘ō crater and the northern lava flow...
Pu‘u ‘Ō‘ō and the northern lava flow
Pu‘u ‘Ō‘ō and the northern lava flow
Pu‘u ‘Ō‘ō and the northern lava flow

The eastern rim of Pu‘u ‘Ō‘ō is no longer visible, having been buried by flows mostly from the small lava lake on the northeast side of the crater floor. A mound of lava with a complex of spatter cones, visible in the background, now surrounds the lava lake, which is only visible from the air.

The eastern rim of Pu‘u ‘Ō‘ō is no longer visible, having been buried by flows mostly from the small lava lake on the northeast side of the crater floor. A mound of lava with a complex of spatter cones, visible in the background, now surrounds the lava lake, which is only visible from the air.

The lava flow fed the northeastern lava lake in Pu‘u ‘Ō‘ō remains w...
Pu‘u ‘Ō‘ō — Active Lava Flow
Pu‘u ‘Ō‘ō — Active Lava Flow
Pu‘u ‘Ō‘ō — Active Lava Flow

The lava flow fed the northeastern lava lake in Pu‘u ‘Ō‘ō remains weakly active at the northern base of the Pu‘u ‘Ō‘ō cone. The front of the flow is burning lichen on old ‘A‘ā flows erupted from Pu‘u ‘Ō‘ō during 1983-1986. The eastern edge of Pu‘u ‘Ō‘ō is at the upper right side of the photo.

The lava flow fed the northeastern lava lake in Pu‘u ‘Ō‘ō remains weakly active at the northern base of the Pu‘u ‘Ō‘ō cone. The front of the flow is burning lichen on old ‘A‘ā flows erupted from Pu‘u ‘Ō‘ō during 1983-1986. The eastern edge of Pu‘u ‘Ō‘ō is at the upper right side of the photo.

This photo, identical to the previous one, just includes labels for...
This photo, identical to previous one, just includes labels for the...
This photo, identical to previous one, just includes labels for the...
This photo, identical to previous one, just includes labels for the...

This photo, identical to the previous one, just includes labels for the flows that spilled from the northern and southern sides of the crater.

The lava flow fed the northeastern lava lake in Pu‘u ‘Ō‘ō remains w...
Pu‘u ‘Ō‘ō — Active Lava Flow
Pu‘u ‘Ō‘ō — Active Lava Flow
Pu‘u ‘Ō‘ō — Active Lava Flow

The lava flow fed the northeastern lava lake in Pu‘u ‘Ō‘ō remains weakly active at the northern base of the Pu‘u ‘Ō‘ō cone. The front of the flow is burning lichen on old ‘A‘ā flows erupted from Pu‘u ‘Ō‘ō during 1983-1986. The eastern edge of Pu‘u ‘Ō‘ō is at the upper right side of the photo.

The lava flow fed the northeastern lava lake in Pu‘u ‘Ō‘ō remains weakly active at the northern base of the Pu‘u ‘Ō‘ō cone. The front of the flow is burning lichen on old ‘A‘ā flows erupted from Pu‘u ‘Ō‘ō during 1983-1986. The eastern edge of Pu‘u ‘Ō‘ō is at the upper right side of the photo.

Multiple lava streams entering the ocean, and breakouts near the ba...
Multiple lava streams entering ocean, and breakouts near base of pali
Multiple lava streams entering ocean, and breakouts near base of pali
Multiple lava streams entering ocean, and breakouts near base of pali

Several streams of lava were entering the water near Kupapa`u Point. Here at the eastern end of the ocean entry a narrow stream is battered by the surf.

Mauna Ulu—an opportunity to study a long-lived rift zone eruption...
Mauna Ulu—an opportunity to study a long-lived rift zone eruption
Mauna Ulu—an opportunity to study a long-lived rift zone eruption
Mauna Ulu—an opportunity to study a long-lived rift zone eruption

A lava fountain during the opening episode of the Mauna Ulu eruption feeds lava flows that cover Chain of Craters Road. Both ‘Ālo‘i Crater (lower left) and ‘Alae Crater (upper right) were filled with lava later in the eruption. Photo taken on May 28, 1969.

A lava fountain during the opening episode of the Mauna Ulu eruption feeds lava flows that cover Chain of Craters Road. Both ‘Ālo‘i Crater (lower left) and ‘Alae Crater (upper right) were filled with lava later in the eruption. Photo taken on May 28, 1969.

Multiple lava streams entering the ocean, and breakouts near the ba...
Multiple lava streams entering ocean, and breakouts near base of pali
Multiple lava streams entering ocean, and breakouts near base of pali
Multiple lava streams entering ocean, and breakouts near base of pali

Several streams of lava were entering the water near Kupapa`u Point. Here at the eastern end of the ocean entry a narrow stream is battered by the surf.

Breakouts near the shoreline have diminished over the past week, bu...
Breakouts near shoreline have diminished over the past week, but su...
Breakouts near shoreline have diminished over the past week, but su...
Breakouts near shoreline have diminished over the past week, but su...

Breakouts near the shoreline have diminished over the past week, but surface flows remain active closer to the base of the pali on the coastal plain.

As this pāhoehoe lobe flows into the crack, the surface layer rolls...
As this pāhoehoe lobe flows into crack, the surface layer rolls up ...
As this pāhoehoe lobe flows into crack, the surface layer rolls up ...
As this pāhoehoe lobe flows into crack, the surface layer rolls up ...

As this pāhoehoe lobe flows into the crack, the surface layer rolls up creating a ropy texture that is common on pāhoehoe flows.

Ocean entry and coastal plain surface flows remain active...
Ocean entry and coastal plain surface flows remain active
Ocean entry and coastal plain surface flows remain active
Ocean entry and coastal plain surface flows remain active

The ocean entry near Kupapa`u Point remains active, with numerous streams of lava entering the water over a wide section of coastline.

Only a few scattered breakouts were active near the shoreline, with...
Only a few scattered breakouts were active near shoreline, with mos...
Only a few scattered breakouts were active near shoreline, with mos...
Only a few scattered breakouts were active near shoreline, with mos...

Only a few scattered breakouts were active near the shoreline, with most of the activity on the coastal plain closer to the base of the pali. This pāhoehoe lobe was active near the east margin of the Peace Day flow field just a few hundred meters (yards) from the coastline.

Only a few scattered breakouts were active near the shoreline, with most of the activity on the coastal plain closer to the base of the pali. This pāhoehoe lobe was active near the east margin of the Peace Day flow field just a few hundred meters (yards) from the coastline.

A surge of "blue glassy" pāhoehoe flows out of an inflated flow mar...
A surge of "blue glassy" pāhoehoe flows out of an inflated flow mar...
A surge of "blue glassy" pāhoehoe flows out of an inflated flow mar...
A surge of "blue glassy" pāhoehoe flows out of an inflated flow mar...

A surge of "blue glassy" pāhoehoe flows out of an inflated flow margin near the shoreline. This type of lava is thought to be stored within an inflating flow for up to a few days, changing its color and texture.

A surge of "blue glassy" pāhoehoe flows out of an inflated flow margin near the shoreline. This type of lava is thought to be stored within an inflating flow for up to a few days, changing its color and texture.

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