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.
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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 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.
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 deflationKīlauea'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.
lava lake level began to drop in concert with summit deflation
lava lake level began to drop in concert with summit deflationKīlauea'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 eruptionThe 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.
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 eruptionThe 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.
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.
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.
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 FahrenheitWhen 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).
lava temperatures were about 2000 degrees Fahrenheit
lava temperatures were about 2000 degrees FahrenheitWhen 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).
School Branch at Maloney Road near Brownsburg IN - downstream view
School Branch at Maloney Road near Brownsburg IN - downstream viewSchool Branch at Maloney Road near Brownsburg IN - downstream view
School Branch at Maloney Road near Brownsburg IN - downstream view
School Branch at Maloney Road near Brownsburg IN - downstream viewSchool Branch at Maloney Road near Brownsburg IN - downstream view
School Branch at Maloney Road near Brownsburg IN - equipment in stream
School Branch at Maloney Road near Brownsburg IN - equipment in streamSchool Branch at Maloney Road near Brownsburg IN - equipment in stream
School Branch at Maloney Road near Brownsburg IN - equipment in stream
School Branch at Maloney Road near Brownsburg IN - equipment in streamSchool Branch at Maloney Road near Brownsburg IN - equipment in stream
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.
Joshua Tree, Edwards Air Force Base, Antelope Valley, CA
Joshua Tree, Edwards Air Force Base, Antelope Valley, CAJoshua trees dot the desert landscape on Edwards Air Force Base in Antelope Valley, CA.
Joshua Tree, Edwards Air Force Base, Antelope Valley, CA
Joshua Tree, Edwards Air Force Base, Antelope Valley, CAJoshua trees dot the desert landscape on Edwards Air Force Base in Antelope Valley, CA.
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.
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.
Stratigraphic contact marking 1964 uplift of Montague Island, Alaska
Stratigraphic contact marking 1964 uplift of Montague Island, AlaskaStratigraphic contact marking uplift of Montague Island, caused by slip on the Patton Bay fault system during the 1964 M9.2 Great ALaska Earthquake.
Stratigraphic contact marking 1964 uplift of Montague Island, Alaska
Stratigraphic contact marking 1964 uplift of Montague Island, AlaskaStratigraphic contact marking uplift of Montague Island, caused by slip on the Patton Bay fault system during the 1964 M9.2 Great ALaska Earthquake.
Alkalinity Sample Analysis to Ensure Accuracy of Field Results
Alkalinity Sample Analysis to Ensure Accuracy of Field Results
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.
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
NASA image of Bear Lake with beautiful swirls in blue water showing mixing
Bird's eye view of Woods Hole's Quissett Campus, MA
Bird's eye view of Woods Hole's Quissett Campus, MAView from a drone! Aerial view of Woods Hole Coastal and Marine Science Center's Quissett Campus.
Bird's eye view of Woods Hole's Quissett Campus, MA
Bird's eye view of Woods Hole's Quissett Campus, MAView from a drone! Aerial view of Woods Hole Coastal and Marine Science Center's Quissett Campus.
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.