Images

 The beach-dependent shorebirds project at the Woods Hole Coastal and Marine Science Center relies heavily on collaborations with other DOI agencies, such as the U.S. Fish and Wildlife Service and National Park Service.

This map shows the locations of fissures and an ‘A‘ā flow erupted since May 3 in the order that they occurred in Leilani Estates as of 7:00 p.m. HST, May 8. The purple areas are lava flows erupted in 1840, 1955, 1960, and 2014-2015.

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.

Severe ground cracks associated with fissure 14 in Leilani Estates. 

Ash column rises from the Overlook crater at the summit of Kīlauea Volcano. HVO's interpretation is that the explosion was triggered by a rockfall from the steep walls of Overlook crater. The photograph was taken at 8:29 a.m. HST from the Jaggar Museum overlook. The explosion was short-lived.

Preliminary map showing location of fissures 13 and 14, prepared by geologists on site in Leilani Estates at 16:06 p.m. today. Both fissures were briefly active this afternoon. Geologists reported fissure 13 activity had diminished by about 5 p.m. HST.

Aerial view of fissure 13 that became active mid-afternoon today.

Cracks in Highway 130; orange paint was used to outline the cracks. The road remained closed for much of the day on 5/7/18.

Aerial view of fissure 12 at 1:15 p.m. HST.

Steam rises from fissure 9 on Moku Street in the Leilani Estates Subdivision.

An in-progress piping plover nest on Parramore Island, Virginia -- females typically lay 3 to 4 eggs in a nest over the course of a week. Both the male and female will take turns incubating eggs when the final egg is laid. This nest was established in new overwash habitat created by storms during the winter of 2017-2018. 

The summit lava lake has dropped significantly over the past few days, and, as of the evening of 5/6/18, was roughly 220m below the crater rim. This very wide angle camera view captures the entire north portion of the Overlook crater.

This map shows the locations, mapped by USGS-HVO scientists, of eruptive fissures in the order that they occurred in the Leilani Estates Subdivision as of 6:00 a.m. HST today (May 6).

This map shows the locations of eruptive fissures on Kīlauea Volcano's East Rift Zone in the order that they occurred in the Leilani Estates Subdivision as of 6:00 a.m. HST today (May 6). The blue lines are paths of steepest descent that identify likely paths of a lava flow, if and when lava moves downhill from an erupting vent.

Lava moving down Makamae Street in Leilani Estates at 9:32 a.m. on May 6, 2018.

 A lava flow moves on Makamae Street in Leilani Estates at 09:32 am local time, on May 6, 2018.

A new fissure erupted this evening near fissures 2 and 7, beginning with small lava spattering at about 8:44 p.m. HST. By 9:00 p.m., lava fountains as high as about 70 m (230 ft) were erupting from the fissure.

With each large earthquake, ground shaking causes additional collapse within the Pu‘u ‘Ō‘ō crater, sending a plume of reddish-brown ash skyward. The size and vigor of a plume depends on the size of the earthquake and subsequent collapse. This roiling ash plume followed the magnitude-6.9 earthquake on May 4.

An intrusion of magma into Kīlauea Volcano's lower East Rift Zone resulted in an eruption in Leilani Estates in the lower Puna District on the Island of Hawai‘i. The first four fissures to erupt in the subdivision are shown here on May 4, emitting copious amounts of hazardous sulfur dioxide gas.

This map shows the locations, mapped by USGS-HVO scientists, of eruptive fissures in the order that they occurred in the Leilani Estates Subdivision as of 10:00 a.m. HST today (May 5).

This map shows the locations of eruptive fissures in the order that they occurred in the Leilani Estates Subdivision as of 10:00 a.m. HST today (May 5). The blue lines are paths of steepest descent that identify likely paths of a lava flow, if and when lava moves downhill from an erupting vent.