Images

A slightly closer view of the lava flow from the eastern breakout on Pu‘u ‘Ō‘ō. This flow has not advanced significantly since yesterday, but it is slowly widening.

Despite heavy rain, which resulted in blurry spots on this photo due to water droplets on the camera lens, HVO scientists were able to do some of the work they hoped to accomplish during this morning's overflight. Here, an HVO geologist maps the location of active lava from the eastern breakout on Pu‘u ‘Ō‘ō.

Amidst steam created by rain falling on the hot lava, another HVO geologist uses a rock hammer to collect a sample of the active flow. Analyses of this sample will yield data on the temperature and chemical makeup of the lava, information that is needed to help determine what's happening within the volcano.

This small-scale map shows Kīlauea's active East Rift Zone lava flow field in relation to the eastern part of the Island of Hawai‘i. The new breakouts from Pu‘u ‘Ō‘ō that began on May 24 are shown in red, as mapped on May 25. The area of the original June 27th lava flow field is shown in pink, as last mapped in detail on May 9.

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The new breakouts from Pu‘u ‘Ō‘ō that began on May 24 are shown in red, as mapped on May 25. The area of the original June 27th lava flow field is shown in pink, as last mapped in detail on May 9. Pu‘u ‘Ō‘ō lava flows erupted prior to June 27, 2014, are shown in gray.

The second flow from the eastern breakout on Pu‘u ‘Ō‘ō—in the area of the "Peace Day" flow that broke out in September 2011—remained active as of this morning, and its total length was about 1.2 km (0.75 mi) long. This lava flow was slowly spreading laterally, but the flow front had stalled.

Two new breakouts at Pu‘u ‘Ō‘ō began this morning just before 7:00 a.m., HST. The larger of the two breakouts, shown here, originated on the northeast flank of the cone, at the site of the vent for the ongoing June 27th lava flow. This breakout point fed a vigorous channelized flow that extended about 1 km (0.6 miles).

A wider view of the larger breakout traveling down the north flank of Pu‘u ‘Ō‘ō, towards the northwest. This photo was taken at about 8:30am.

Another breakout occurred just east of Pu‘u ‘Ō‘ō, about 500 m (0.3 miles) from the crater, in the area of the "Peace Day" flow that broke out in September 2011. This second breakout was smaller than the one on the northeast flank, but was still feeding an impressive lava channel.

A video of the larger breakout, flowing northwest.

This map of two new breakouts at Pu‘u ‘Ō‘ō, which began just before 7:00 a.m., HST, this morning, shows the extent of the lava flows based on aerial photos that were taken at 8:30 a.m.

The crater floor at Pu‘u ‘Ō‘ō has recently experienced minor uplift due to inflation within Pu‘u ‘Ō‘ō cone. The crater floor uplift is subtle, and probably no more than about 1 meter (3 feet) since May 15. Small, hot cracks have appeared on the crater floor during the uplift.

A USGS Hawaiian Volcano Observatory chemist conducts thermal imaging measurements as part of a geochemical survey on Mauna Loa's upper Southwest Rift Zone in March 2016. Areas like the one shown here can indicate where gases are escaping from magma at depth. USGS photo.

The red line shows the total number of earthquakes that have occurred at Mount Hood between the year 2000 and May 16, 2016. During this period, there have been 829 earthquakes greater than magnitude 1. Note the number of earthquakes during the 2002 swarm.

This image of Kīlauea Volcano's summit, probably taken in the 1860s from a site near where Jaggar Museum in Hawai‘i Volcanoes National Park is located today, was once thought to be the first photograph of Kīlauea. It shows part of the caldera rim and floor with a fuming Halema‘uma‘u Crater near the center of the image. USGS/HVO photo archives.

This daguerreotype image, captured in 1855 by Hugo Stangenwald, is the earliest known photograph of Kīlauea Volcano. Although scratched and faded, the 161-year-old photo shows a line of steaming vents across the floor of Kīlauea's summit caldera as viewed from a location near today's Volcano House Hotel. The caldera rim is visible in the lower third of the image.

Kure atoll, the northernmost coral atoll in the world, is a former volcano, and the oldest part of the Hawaiian Island Chain still above water. Diameter of the atoll is 9.3 km (5.8 mi).

A closer look at the spattering and agitation in the small lava pond in Pu‘u ‘Ō‘ō.

An HVO geologist approaches one of the small vents in Pu‘u ‘Ō‘ō Crater to obtain a spatter sample.

This small-scale map shows Kīlauea's active East Rift Zone lava flow field in relation to the eastern part of the Island of Hawai‘i. The area of the flow field on March 25 is shown in pink, while widening and advancement of the flow field as mapped on May 9 is shown in red. Pu‘u ‘Ō‘ō lava flows erupted prior to June 27, 2014, are shown in gray.

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area of the flow field on March 25 is shown in pink, while widening and advancement of the flow field as mapped on May 9 is shown in red. The yellow lines show the mapped portion of the active lava tube system.