Images

Why did the lava tube cross the road? This image shows the Peace Day lava tube coming down the pali in Royal Gardens subdivision. The lava tube parallels Ali`i avenue, shown by the straight line of warm temperatures that represent asphalt heated in the sun.

HVO geologists use a laser rangefinder to measure the height of the shield and cone built up around the northeast lava lake, on the east rim of Pu‘u ‘Ō‘ō crater. The peak of the cone is now about 18 m (60 ft) above the former crater rim.

The spatter cone near the north rim of Pu‘u ‘Ō‘ō crater continues to produce pulsating gas jetting sounds. Compare this photo to one taken of the same cone on May 2 to see how much taller the cone has grown.

The small lava lake on the northeast rim of Pu‘u ‘Ō‘ō crater has been built into a small cone, with only a few small openings at the top. One of these small openings had sloshing lava near the surface.

Why did the lava tube cross the road? This image shows the Peace Day lava tube coming down the pali in Royal Gardens subdivision. The lava tube parallels Ali`i avenue, shown by the straight line of warm temperatures that represent asphalt heated in the sun.

The Kahauale`a II flow began as a breakout on the east rim of Pu‘u ‘Ō‘ō crater on May 6, and has advanced northward towards the forest. Today, slowly moving pāhoehoe lobes (light colored flows in this image) were burning moss and lichen on older Pu‘u ‘Ō‘ō ‘A‘ā flows and approaching the forest boundary. Pu‘u ‘Ō‘ō cone is obscured by thick clouds in this photo.

A sensor is deployed to measure flow in a channel of the marsh in Rachel Carlson National Wildlife Refuge in 2013.

Do not be misguided by the risky actions of this person (upper right), who is standing on an active lava delta that could collapse without warning, amidst a plume of superheated steam, hydrochloric acid, and tiny particles of volcanic glass. To avoid these ocean entry hazards, HVO advises staying at least 400 m (one-quarter mile) from where lava enters the sea.

This false-color image obtained from NASA's Terra satellite on January 19, 2009, shows an ash plume (white plume spreading north, top) erupting from Chaitén Volcano. Red color indicates green vegetation.

Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).

Methane gas bubbles rise from the seafloor—this type of activity, originally noticed by NOAA Ship Okeanos Explorer in 2012 on a multibeam sonar survey, is what led scientists to the area. Image courtesy of Deepwater Canyons 2013 – Pathways to the Abyss expedition, NOAA-OER/BOEM/USGS.

A lithodid crab seen on a bed of deep sea mussels living near a gas seep 1,600 meters below the surface of the Atlantic Ocean. Images courtesy Deepwater Canyons 2013 - Pathways to the Abyss expedition, NOAA-OER/BOEM/USGS.

Images of the remotely operated vehicle Jason2 sampling a sea urchin in a deep sea mussel community found near a gas seep on the U.S. outer continental shelf. Images courtesy Deepwater Canyons 2013 - Pathways to the Abyss expedition, NOAA-OER/BOEM/USGS.

This image was captured on Monday, May 6, by the Advanced Land Imager sensor aboard NASA's Earth Observing 1 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 or very recently active lava flows.

Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).

Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).

Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).

Another entry point has two larger lava streams entering the water. The lava fragments due to cooling and disruption by the battering surf, and some of these pieces float on the water's surface in front of the entry point (see lower left portion of photo).

Over the past week this spatter cone on the floor of Pu‘u ‘Ō‘ō crater has been the source of several large, but brief, lava flows on the crater floor. Today, the cone was producing pulsating gas jetting sounds.

Children from a village near Kathmandu greet visitors on May 2, 2013

After a 12 km (7.5 mile) journey from the vent on Pu‘u ‘Ō‘ō cone through a lava tube, lava pours into the ocean in narrow streams at one of the eastern entry points.