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Kīlauea East Rift Zone Eruption (May 4, 2018)
Kīlauea East Rift Zone Eruption (May 4, 2018)
Kīlauea East Rift Zone Eruption (May 4, 2018)

Fissure 3 opened around 6:00 a.m. HST on Friday, May 4, with weak fuming from a crack on Kaupili Street. This fuming increased, as did rumbling sounds. Eventually spatter was ejected and accumulated around the fissure. Large, loud bubble bursts were common at this fissure.

Fissure 3 opened around 6:00 a.m. HST on Friday, May 4, with weak fuming from a crack on Kaupili Street. This fuming increased, as did rumbling sounds. Eventually spatter was ejected and accumulated around the fissure. Large, loud bubble bursts were common at this fissure.

Kīlauea East Rift Zone Eruption (May 4, 2018)
Kīlauea East Rift Zone Eruption (May 4, 2018)
Kīlauea East Rift Zone Eruption (May 4, 2018)

Fissure 2 opened around 1:00 a.m. HST on Friday, May 4, with a small area of spattering in a residential driveway. Within an hour the spattering was more vigorous, with spatter reaching about 30 meters (100 feet). This spatter was thrown over the power lines and landed on Makamae Street.

Fissure 2 opened around 1:00 a.m. HST on Friday, May 4, with a small area of spattering in a residential driveway. Within an hour the spattering was more vigorous, with spatter reaching about 30 meters (100 feet). This spatter was thrown over the power lines and landed on Makamae Street.

Kīlauea East Rift Zone Map as of 8:00 a.m., May 4...
Kīlauea ERZ Map as of 8:00 a.m., May 5
Kīlauea ERZ Map as of 8:00 a.m., May 5
Kīlauea ERZ Map as of 8:00 a.m., May 5

This map shows the locations, mapped by USGS-HVO scientists, of the three eruptive fissures in the order that they occurred in the Leilani Estates Subdivision as of 8:00 a.m. HST today (May 4). The fissures are jetting copious amounts of sulfur dioxide gas, which should be avoided.

This map shows the locations, mapped by USGS-HVO scientists, of the three eruptive fissures in the order that they occurred in the Leilani Estates Subdivision as of 8:00 a.m. HST today (May 4). The fissures are jetting copious amounts of sulfur dioxide gas, which should be avoided.

lava lake level began to drop in concert with summit deflation
lava lake level began to drop in concert with summit deflation
lava lake level began to drop in concert with summit deflation
lava lake level began to drop in concert with summit deflation

Kīlauea's summit eruption within Halema‘uma‘u did not initially respond to the volcano's East Rift Zone activity (collapse of the Pu‘u ‘Ō‘ō crater floor and magmatic intrusion into the rift zone) on April 30. But on May 2, the lava lake level began to drop in concert with summit deflation, suggesting that magma was moving from the summit into the East Rift Zone.

Kīlauea's summit eruption within Halema‘uma‘u did not initially respond to the volcano's East Rift Zone activity (collapse of the Pu‘u ‘Ō‘ō crater floor and magmatic intrusion into the rift zone) on April 30. But on May 2, the lava lake level began to drop in concert with summit deflation, suggesting that magma was moving from the summit into the East Rift Zone.

The start of fissure 3 during Kīlauea's lower East Rift Zone eruption
The start of fissure 3 during Kīlauea's lower East Rift Zone eruption
The start of fissure 3 during Kīlauea's lower East Rift Zone eruption
The start of fissure 3 during Kīlauea's lower East Rift Zone eruption

The start of fissure 3 during Kīlauea's lower East Rift Zone eruption. Lava erupting to the surface cut across Kaupili Street around 7:00 a.m. on May 4, 2018.

 A Zone-tailed Hawk in flight.
Zone-tailed hawk in flight
Zone-tailed hawk in flight
Zone-tailed hawk in flight

Raptors in the Trans Pecos, Texas Cooperative Fish and Wildlife Research Unit: State-Threatened, Riparian-Obligate Raptors in the Trans Pecos:  Desert riparian systems are distinct narrow drainages that provide environmental conditions for vegetation dependent on permanent or ephemeral surface and subsurface water.

Raptors in the Trans Pecos, Texas Cooperative Fish and Wildlife Research Unit: State-Threatened, Riparian-Obligate Raptors in the Trans Pecos:  Desert riparian systems are distinct narrow drainages that provide environmental conditions for vegetation dependent on permanent or ephemeral surface and subsurface water.

helicopter overflight
helicopter overflight
helicopter overflight
helicopter overflight

Pu‘u ‘Ō‘ō on May 3, 2018, as viewed from the helicopter overflight. The crater floor is collapsed, and a thin plume escapes from the gaping crater. The west flank cracked on April 30th around 2:30 pm HST, and minor amounts of lava oozed out of the crack (line of steaming features) just before the plumbing system catastrophically failed.

Pu‘u ‘Ō‘ō on May 3, 2018, as viewed from the helicopter overflight. The crater floor is collapsed, and a thin plume escapes from the gaping crater. The west flank cracked on April 30th around 2:30 pm HST, and minor amounts of lava oozed out of the crack (line of steaming features) just before the plumbing system catastrophically failed.

Kīlauea East Rift Zone Eruption (May 3, 2018)
Kīlauea East Rift Zone Eruption (May 3, 2018)
Kīlauea East Rift Zone Eruption (May 3, 2018)

This small fissure = opened in the Leilani Estates subdivision on the lower East Rift Zone of Kilauea Volcano around 5:00 p.m. Lava erupted from the fissure until about 6:30pm, when it became inactive.

This small fissure = opened in the Leilani Estates subdivision on the lower East Rift Zone of Kilauea Volcano around 5:00 p.m. Lava erupted from the fissure until about 6:30pm, when it became inactive.

lava temperatures were about 2000 degrees Fahrenheit
lava temperatures were about 2000 degrees Fahrenheit
lava temperatures were about 2000 degrees Fahrenheit
lava temperatures were about 2000 degrees Fahrenheit

When Kīlauea Volcano's lower East Rift Zone first erupted on May 3, 2018, lava temperatures were about 2000 degrees Fahrenheit. As the eruption progressed, with fresher magma feeding the fissures, the erupted lava became progressively hotter, resulting in more fluid and far-reaching lava flows (May 21 shown here).

When Kīlauea Volcano's lower East Rift Zone first erupted on May 3, 2018, lava temperatures were about 2000 degrees Fahrenheit. As the eruption progressed, with fresher magma feeding the fissures, the erupted lava became progressively hotter, resulting in more fluid and far-reaching lava flows (May 21 shown here).

Flooding in Soldier Pond, Maine
Flooding in Soldier Pond, Maine
Flooding in Soldier Pond, Maine
Flooding in Soldier Pond, Maine

Flooding in Soldier Pond, Maine, following rainfall and snowmelt that led to high water levels in the Fish and St. John Rivers in April and May of 2018. 

Flooding in Soldier Pond, Maine, following rainfall and snowmelt that led to high water levels in the Fish and St. John Rivers in April and May of 2018. 

a lone Joshua tree stands out amongs desert scrub and fluffy clouds in a blue sky
Joshua Tree, Edwards Air Force Base, Antelope Valley, CA
Joshua Tree, Edwards Air Force Base, Antelope Valley, CA
Joshua Tree, Edwards Air Force Base, Antelope Valley, CA

Joshua trees dot the desert landscape on Edwards Air Force Base in Antelope Valley, CA.  

Rapid Deployment Gage in Soldier Pond, Maine
Rapid Deployment Gage in Soldier Pond, Maine
Rapid Deployment Gage in Soldier Pond, Maine
Rapid Deployment Gage in Soldier Pond, Maine

USGS field crews installed a temporary rapid deployment gage on May 2, 2018, at Soldier Pond in the Fish River to monitor flooding near Fort Kent in Maine.  

USGS field crews installed a temporary rapid deployment gage on May 2, 2018, at Soldier Pond in the Fish River to monitor flooding near Fort Kent in Maine.  

Rapid Deployment Gage in Soldier Pond, Maine
Rapid Deployment Gage in Soldier Pond, Maine
Rapid Deployment Gage in Soldier Pond, Maine
Rapid Deployment Gage in Soldier Pond, Maine

USGS field crews installed a temporary rapid deployment gage on May 2, 2018, at Soldier Pond in the Fish River to monitor flooding near Fort Kent in Maine. 

USGS field crews installed a temporary rapid deployment gage on May 2, 2018, at Soldier Pond in the Fish River to monitor flooding near Fort Kent in Maine. 

Man pointing to ground
Stratigraphic contact marking 1964 uplift of Montague Island, Alaska
Stratigraphic contact marking 1964 uplift of Montague Island, Alaska
Stratigraphic contact marking 1964 uplift of Montague Island, Alaska

Stratigraphic contact marking uplift of Montague Island, caused by slip on the Patton Bay fault system during the 1964 M9.2 Great ALaska Earthquake. 

As of this afternoon (May 1), the eruption at the summit of Kīlauea...
As of this afternoon (May 1), the eruption at the summit of Kīlauea...
As of this afternoon (May 1), the eruption at the summit of Kīlauea...
As of this afternoon (May 1), the eruption at the summit of Kīlauea...

As of this afternoon (May 1), the eruption at the summit of Kīlauea has apparently not been affected by the collapse of Pu‘u ‘Ō‘ō or intrusion of magma along the volcano's Lower East Rift Zone.

NASA image of Bear Lake with beautiful swirls in blue water showing mixing
Bear Lake Mixing
Bear Lake Mixing
Bear Lake Mixing

NASA image of Bear Lake with beautiful swirls in blue water showing mixing

NASA image of Bear Lake with beautiful swirls in blue water showing mixing

Students stand in front of a scientific poster at a poster fair
Collaborating with university students
Collaborating with university students
Collaborating with university students

The Southwest Biological Science Center loves working with students. Here, a group of undergraduates from Northern Arizona University help RAMPS define the reasons why ecosystem restoration is important for human health and the economy. Follow the link to learn more about RAMPS.

The Southwest Biological Science Center loves working with students. Here, a group of undergraduates from Northern Arizona University help RAMPS define the reasons why ecosystem restoration is important for human health and the economy. Follow the link to learn more about RAMPS.

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