Images

Lava fountains, occasionally surging to heights of 45-55 m (150-180 ft), erupted south and north of Keanakāko‘i Crater (top and middle fissures, respectively) and on the floor of Kīlauea Caldera (foreground fissure) in a spectacular summit eruption on July 19, 1974.

USGS geologist uses a UV spectrometer to detect gases from fumarole at Crater Rock, Mount Hood.

Exploring Mount Rainier: living near a volcano provides an opportunity for field-based learning.

Several openings on the floor of the Pu‘u ‘Ō‘ō crater and along the Peace Day flow tube system continue to degas profusely. The only visible lava, however, is the small lava lake confined to a pit on the northeastern side of the crater floor. The lava lake has been present for the last several months.

Surface flows remain active on the coastal plain, but have retreated inland compared to their position last week. The active front is now about 1.3 km (0.8 miles) from the ocean.

The lava lake on the northeastern edge of the Pu‘u ‘Ō‘ō crater floor is about 30 m (100 ft) across. It's level rises and falls with changes in pressure in the magma storage body beneath Pu‘u ‘Ō‘ō. Today, the lava lake was at a relatively low level, compared to its condition over the last few months.

In addition to the active flows on the coastal plain, lava flows were also active on the pali and at the base of the pali. Pu‘u ‘Ō‘ō and the Halema‘uma‘u plume are visible near the top of the image.

Back at the USGS Cascades Volcano Observatory office, these data are merged with airborne LiDAR data to calculate lake volume.

A view of the lava lake within the Halema‘uma‘u Overlook vent on an unusually clear day (May 16, 2012) with the Jaggar Museum and the HVO building in the distance.

Lava flows remain active on the pali and coastal plain, but the flow front has made no significant progress towards the ocean over the past week. This image is a composite of a thermal image and a normal photograph, with active breakouts shown by yellow and white areas, and recent, but inactive, flows shown in red and purple.

A narrow channelized flow cascades down the steep lower portion of the pali in Royal Gardens subdivision. This flow was close to the former location of Paradise St.

View from near the top of Mount Tarawera looking northeast along part of the string of explosion craters that split the volcano on June 10, 1886. Mount Edgecumbe stands in the distance.

View of Pu‘u ‘Ō‘ō crater, looking southwest. In the foreground, an active, spattering lava pond is contained within a collapse pit near the east rim of the crater. Two additional vents, both emitting fume, can be seen behind the fume from the lava pond.

Lava flows remain active on the pali and coastal plain, and continue to slowly migrate towards the ocean. This thermal-visual composite shows the distribution of active flows, which are extensive and consist of several lobes. The active flow front today was 1.1 km (0.7 miles) from the water.

A close-up of the lava pond in the eastern portion of Pu‘u ‘Ō‘ō crater. The lava pond is about 30 meters (100 ft) in diameter. The dark lava flows at the bottom of the photo are crater overflows that swept down the east flank of Pu‘u ‘Ō‘ō in September 2011.

This false-color satellite image shows the ongoing lava flow activity on the east rift zone of Kīlauea volcano along with nearby cities and towns on the east side of the Big Island. The image was acquired at 10:28 am on June 12 by the Advanced Land Imager sensor aboard the NASA Earth Observing 1 satellite.

This composite image combines a thermal image with a normal photograph, and shows the recent breakouts on the pali and coastal plain in Royal Gardens subdivision. The two large vegetated areas in this view are some of the only remaining portions of Royal Gardens not covered by lava.

Map showing the extent of lava flows erupted during Kīlauea's ongoing east rift zone eruption and labeled with the years in which they were active.

A major eruption of Mount Hood would pose a great hazard to the regional economy.

A circular lava pond has recently been active near the eastern rim of Pu‘u ‘Ō‘ō crater. Today, the lava pond had low-level but continuous spattering from its eastern margin, and a mostly crusted lava surface.

The lava flows on the coastal plain are still slowly advancing towards the water. On today's overflight, the active breakouts were about 750 m (0.5 miles) from the ocean. These flows have once again entered the National Park.