Images

At 2:30 p.m. HST, the flow front of Fissure 17 continues down slope. The barren, brown area to the right in the photograph is a lobe of the Kii Flow from the eruption of 1955. The Fissure 17 flow front is located approximately .7 miles makai of Highway 132 and is 1.4 miles mauka of Hwy 137.

7:00 a.m., HST. An early morning view of fissure 17, still erupting and supplying lava to a flow that was still advancing (out of view). View is looking toward the east.

Around 2:30 p.m. HST, a steam jet appears on fissure 17, above the area with active fountaining. Steam jets at this location were repeating about once a minute.

A U.S.

Examples of glide avalanches on Heaven's Peak, Glacier National Park.

Threatened giant gartersnake (Thamnophis gigas). This semi-aquatic snake lives in rice fields and the remaining wetlands of California's Central Valley.

USGS staff member positioned in a cable car, ready to collect streamflow data on Pine Creek near Pinedale, Wyoming.

At 10:31 a.m. HST. Cracks on Hwy 132 marked with orange spray paint to track changes through time.

At 8:00 a.m. HST. A slow sticky a'a flow emerges from a new fissure just over a half mile northeast of the end of Hinalo Street. The new fissure - fissure 17 - is about one half mile south of Hwy 132. Some reports have referred to this fissure as number 18 but that is not correct. Fissure 18 had not erupted by this time.

At 2:00 p.m. HST. This photo reveals a small pad of lava between Fissures 16 and 17 which did not appear in photos of the same scene taken this morning. (Red arrow points to the lava pad.) From the photo it appears that this fissure had stagnated. We have designated this small outbreak as Fissure 18.

Map as of 9:00 a.m. HST, May 13, shows the location of fissure 17, which opened this morning at approximately 4:30 a.m. HST. NOTE: This new fissure was initially referred to as fissure 18 in early reports, but that is incorrect (what was called fissure 17 yesterday did not erupt lava, so this morning's erupting fissure is actually 17).

The new Hammond Bay Biological Station laboratory building completed in 2019.

5/12/18, 12:57 p.m. HST - Lava was slowly advancing from fissure 16.

5/12/18, 08:27 a.m. HST - An aerial view of fissure 16, located about 1.3 km (0.8 miles) northeast of fissure 15 (top left). The fissure is located 500 m northeast of the Puna Geothermal Venture site (top right). Photograph courtesy of Hawai`i County Fire Department.

Main map shows the location of fissure 16, as well as earlier fissures, lava flows, and steaming areas, as of 12:00 p.m. HST, May 12. Inset map shows fissures in Leilani Estates in the order they occurred since May 3. Shaded purple areas indicate lava flows erupted in 1840, 1955, 1960, and 2014-2015.

High water mark sign at Yellowstone River at Carters Bridge

On the morning of May 9, 2018, a large rockfall in "Overlook crater" within Halema‘uma‘u at the summit of Kīlauea triggered a gas-driven explosion that sent an ash plume several thousand feet skyward. Phreatic (steam-driven) explosions can create larger ash plumes; the 1924 explosions sent ash plumes up to 20,000 feet high. USGS photo.

To help us understand what could happen at Kīlauea Volcano's summit, we look to past similar events, but this does not mean that future events will be exactly the same. This map shows the distribution of ballistics and tephra from the 1924 phreatic (steam-driven) explosions.

On May 10, 2018, Highway 130 (shown here) was newly cracked with steam coming up from the east side of the road due to the dike (tabular body of magma) that intruded Kīlauea's lower East Rift Zone. The two orange and white road markers are on slightly uplifted areas of the highway, which are about 100 m (330 ft) apart.

A team of USGS scientists work off the R/V Sallenger in Rockaway Beach, New York. One team member stands on a floating sled that enables sub‐bottom surveying in shallow water, nearshore, and shore‐face environments. The sled is equipped with an EdgeTech SB‐512i CHIRP system and single‐beam sonar.

USGS scientists measure beach elevation and other profile characteristics as part of a project that models how barrier islands will likely change with sea-level rise - and how those changes will ultimately affect piping plover and other shorebird nesting habitat availability.