Images

Looking south toward the MLK pit (straight) and Puka Nui pit (right). Lava is only a few meters (yards) away from overtopping the pits and flowing onto the southwest flank of Pu‘u ‘Ō‘ō.

At 2:02 p.m., HST, on August 3, the floor of Pu‘u ‘Ō‘ō crater, which had risen significantly over the past month, forming a dome beneath the perched lava lake, started to subside. By 3:15 p.m., the crater floor and perched lava lake began to collapse. Within a couple of hours, the lava lake was no longer visible, and the crater floor was covered in rubble.

This thermal image, looking south, shows the individual vents feeding distinct channels.

One of the more vigorous vents, in the lower left, is topped by a tall (6 m, or 20 ft, high) spatter cone. The flow from this vent cascades down several steps, joining the flow from two other nearby vents, before flowing under a small bridge and into the broad area of ponded lava to the west.

View looking east into Pu‘u ‘Ō‘ō, its crater partly filled by lava flows accumulating on the crater floor. The active lava lake in the crater is 205 m (673 ft) long and varies in width from 80-115 m (262-377 ft). The West Gap pit is in the central foreground, and the Puka Nui and MLK pits are to the right (the MLK pit is in back).

A breach in the south wall of the perched pond allowed lava to gush out onto the floor of Pu‘u ‘Ō‘ō Crater.

This thermal image, looking southwest, shows the very small flow, at the bottom of the image, active in the bottom of Pu‘u ‘Ō‘ō crater. In the upper right, the active flows on the lower west flank of Pu‘u ‘Ō‘ō can be seen.

The new lava lake has become slightly perched above the surrounding crater floor, as shown by the distinct levees visible in this photo.

This photo, similar to the previous, was taken from the same location as photos posted on July 21 and June 9 (and several other dates scattered over the past several months) to provide a comparison to past activity in Pu‘u ‘Ō‘ō.

Over the past week, the lava pond in Pu‘u ‘Ō‘ō Crater has rebuilt its retaining walls and is once again perched 3-5 m (10-16 ft) above the surrounding crater floor.

Along with overflows, low-level spattering from points wandering around the perimeter of the lava lake continually builds up the levee that impounds the lake.

The lava lake's levee stands up to 8 m (26 ft) above the surrounding crater floor. This steep-sided levee impounds the lava and forms what is called a "perched" lava lake. Pieces of the rim occasionally collapse into the lake, leading to sudden and fast-moving overflows of lava onto the crater floor.

Starting in late June, the crater floor around the lava lake began to uplift. The photo here shows the flank of the east side of the lava lake. Prior to uplift, this steeply dipping surface was nearly flat-lying.

Pu‘u ‘Ō‘ō crater, following the collapse of the crater floor on August 3, has been filled with thick fume. A very tiny flow, visible only with a thermal camera, was active on the crater floor.

The new lava lake in Pu‘u ‘Ō‘ō has buried much of the floor of the August 3, 2011, collapse crater beneath a maximum of about 45 m (~148 ft) of lava. Most of the lava upwells at the east end of the lake (lower right) and flows toward the west, much like the lava lake prior to the August 3 flank breakout and crater collapse.

The lava accumulating on the southeast side of the crater has begun to form a low shield that extends out from the crater and has buried the Puka Nui and MLK pits. Compare this photo to one taken last week (July 21) from the same spot.

Around 2:20 p.m., HST, on August 3, lava broke out from a vent (center) low on the west flank of the Pu‘u ‘Ō‘ō cone. Lava erupting from the flank vent is entirely within Hawai‘i Volcanoes National Park, and pose no hazard to residents.

Lava flowing from vents on the west flank of Pu‘u ‘Ō‘ō formed two branches. A weak north arm advanced northward into forested kipuka (upper right). A higher-volume south arm quickly advanced down Kīlauea's south flank along the edge of flows erupted in 2002-2004 (upper left).

HVO geologist and helicopter pilot repair a mobile Webcam on Kupaianaha to continue monitoring the east flank of Pu‘u ‘Ō‘ō.

Looking west into Pu‘u ‘Ō‘ō Crater. Recent flows that have spilled out of the perched pond stand out by their silver color. These overflows have built up the crater floor another 5 m (16 ft) since last week. Kane Nui o Hamo, Mauna Ulu, and Pu‘u Huluhulu are in the background.

A different perspective of the perched pond, from the west side of Pu‘u ‘Ō‘ō Crater.