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Kīlauea images of eruptive activity, field work, and more.
Scientists on the early morning overflight of Kīlauea Volcano's lower East Rift Zone documented a very weak ocean entry. For the easternmost lobe, only a few small finger channels of lava were entering the ocean.
Scientists on the early morning overflight of Kīlauea Volcano's lower East Rift Zone documented a very weak ocean entry. For the easternmost lobe, only a few small finger channels of lava were entering the ocean.
Map as of 6:00 p.m. HST, May 29, 2018. Given the dynamic nature of Kīlauea's lower East Rift Zone eruption, with changing vent locations, fissures starting and stopping, and varying rates of lava effusion, map details shown here are accurate as of the date/time noted—and could have changed rapidly since that time.
Map as of 6:00 p.m. HST, May 29, 2018. Given the dynamic nature of Kīlauea's lower East Rift Zone eruption, with changing vent locations, fissures starting and stopping, and varying rates of lava effusion, map details shown here are accurate as of the date/time noted—and could have changed rapidly since that time.
Fissure 8 reactivated on the afternoon of May 28, when, at times, lava fountains were reaching heights of 200 feet and feeding a lava flow&
Fissure 8 reactivated on the afternoon of May 28, when, at times, lava fountains were reaching heights of 200 feet and feeding a lava flow&
Scientists on the early morning overflight of Kīlauea Volcano's lower East Rift Zone documented a very weak ocean entry. For the easternmost lobe, only a few small finger channels of lava were entering the ocean.
Scientists on the early morning overflight of Kīlauea Volcano's lower East Rift Zone documented a very weak ocean entry. For the easternmost lobe, only a few small finger channels of lava were entering the ocean.
Close view of lava channel in middle of the lava flow erupting from fissure 8 during this morning's overflight at about 7 a.m. HST. The tallest lava fountain is fissure 8, active since yesterday evening. The eruption rate at fissure 8 diminished significantly later in the morning.
Close view of lava channel in middle of the lava flow erupting from fissure 8 during this morning's overflight at about 7 a.m. HST. The tallest lava fountain is fissure 8, active since yesterday evening. The eruption rate at fissure 8 diminished significantly later in the morning.
Close view of weak ocean entry at about 1:05 p.m. HST. Only small and intermittent "laze" plumes have been observed today.
Close view of weak ocean entry at about 1:05 p.m. HST. Only small and intermittent "laze" plumes have been observed today.
View of the now-sluggish lava flow that crossed Pohoiki Road earlier today; the flow originated from fissure 8. This fissure was very active overnight, slowed this morning, and stopped by about noon.
View of the now-sluggish lava flow that crossed Pohoiki Road earlier today; the flow originated from fissure 8. This fissure was very active overnight, slowed this morning, and stopped by about noon.
Map as of 3:00 p.m. HST, May 28, 2018. Shaded purple areas indicate lava flows erupted in 1840, 1955, 1960, and 2014-2015.
Map as of 3:00 p.m. HST, May 28, 2018. Shaded purple areas indicate lava flows erupted in 1840, 1955, 1960, and 2014-2015.
Aerial view of active lava flow crossing Pohoiki Road during an overflight this morning about 7 a.m. HST. Pohoiki Road cuts through middle of photograph.
Aerial view of active lava flow crossing Pohoiki Road during an overflight this morning about 7 a.m. HST. Pohoiki Road cuts through middle of photograph.
View of the fissurecomplex is toward the southeast during this afternoon's overflight of the lower East Rift Zone at about 1:15 p.m. HST. The lava channel in middle of photograph is filling with lava erupted from fissure 22.
View of the fissurecomplex is toward the southeast during this afternoon's overflight of the lower East Rift Zone at about 1:15 p.m. HST. The lava channel in middle of photograph is filling with lava erupted from fissure 22.
View of the fissure complex looking toward the southwest (uprift) during this afternoon's overflight at about 1:15 p.m. HST. The small lava flows spreading to the southeast from the fissure complex (lower middle) originate in the area of between fissures 16 and 18.
View of the fissure complex looking toward the southwest (uprift) during this afternoon's overflight at about 1:15 p.m. HST. The small lava flows spreading to the southeast from the fissure complex (lower middle) originate in the area of between fissures 16 and 18.
U.S. Geological Survey Volcanologist Matthew Patrick photographs and observes a lava fountain in the Leilani Estates near Hilo, Hawai`i on Sunday, May 27, 2018.
U.S. Geological Survey Volcanologist Matthew Patrick photographs and observes a lava fountain in the Leilani Estates near Hilo, Hawai`i on Sunday, May 27, 2018.
Pāhoehoe lava advancing west from fissure 7 (lava fountain in background) on Leilani Avenue. Fissure 7 activity increased overnig
Pāhoehoe lava advancing west from fissure 7 (lava fountain in background) on Leilani Avenue. Fissure 7 activity increased overnig
USGS scientist in the Lower East Rift Zone documenting the spectacular ~50 m tall fissure 7 lava fountain to the east which had lit up the sky in a red hue.
USGS scientist in the Lower East Rift Zone documenting the spectacular ~50 m tall fissure 7 lava fountain to the east which had lit up the sky in a red hue.
Aerial view of the ocean-entry areas at about 12:30 p.m. HST. Lava flowing into the ocean diminished overnight and this morning (note lack of obvious plume at the entry areas). View is toward the northwest.
Aerial view of the ocean-entry areas at about 12:30 p.m. HST. Lava flowing into the ocean diminished overnight and this morning (note lack of obvious plume at the entry areas). View is toward the northwest.
This image shows radar data acquired by the European Space Agency's Sentinel-1 satellite over Kīlauea Volcano on May 19 at 6:30 PM HST (left) compared to May 25 at 6:30 PM HST (right). The satellite transmits a radar signal toward the surface and measures the strength of the return, with bright areas indicating a strong return and dark areas a weak return.
This image shows radar data acquired by the European Space Agency's Sentinel-1 satellite over Kīlauea Volcano on May 19 at 6:30 PM HST (left) compared to May 25 at 6:30 PM HST (right). The satellite transmits a radar signal toward the surface and measures the strength of the return, with bright areas indicating a strong return and dark areas a weak return.
Aerial view of the eastern-most end of the fissure complex (top right) and active lava channels and inactive flows south of the fissures (toward left side of photo) at about 12:30 p.m. HST; the ocean is out of view left side of photo. In this view, fissure 22 in top right is supplying most of the lava to the active channel.
Aerial view of the eastern-most end of the fissure complex (top right) and active lava channels and inactive flows south of the fissures (toward left side of photo) at about 12:30 p.m. HST; the ocean is out of view left side of photo. In this view, fissure 22 in top right is supplying most of the lava to the active channel.
Ash rises above Halema‘uma‘u within Kīlauea's summit caldera in this May 27, 2018, telephoto image from near Volcano House Hotel in Hawai‘i Volcanoes National Park.
Ash rises above Halema‘uma‘u within Kīlauea's summit caldera in this May 27, 2018, telephoto image from near Volcano House Hotel in Hawai‘i Volcanoes National Park.
An aerial view, looking west, of the two active ocean entries on Kīlauea Volcano's lower East Rift Zone. The large white plume (foreground) is the eastern ocean entry; the weaker, western plume can be seen in the distance.
An aerial view, looking west, of the two active ocean entries on Kīlauea Volcano's lower East Rift Zone. The large white plume (foreground) is the eastern ocean entry; the weaker, western plume can be seen in the distance.
This ‘a‘ā flow, erupted from fissures 7 and 21, was approximately 3–4 meters (yards) high at the flow front and slowly advancing to the northeast in the Leilani Estates subdivision around 10:30 a.m. HST today.
This ‘a‘ā flow, erupted from fissures 7 and 21, was approximately 3–4 meters (yards) high at the flow front and slowly advancing to the northeast in the Leilani Estates subdivision around 10:30 a.m. HST today.
