This map overlays a georegistered mosaic of thermal images collected during a helicopter overflight of the distal part of Kīlauea's active East Rift Zone lava flow on March 10 at about 10:35 AM. The base image is a satellite image acquired in March 2014 (provided by Digital Globe).
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Images related to natural hazards.
This map overlays a georegistered mosaic of thermal images collected during a helicopter overflight of the distal part of Kīlauea's active East Rift Zone lava flow on March 10 at about 10:35 AM. The base image is a satellite image acquired in March 2014 (provided by Digital Globe).
Map of flow field west of Kaohe Homesteads with thermal overlay
Map of flow field west of Kaohe Homesteads with thermal overlayThis map overlays a georegistered mosaic of thermal images collected during a helicopter overflight of Kīlauea's active East Rift Zone lava flow west of Kaohe Homesteads on March 10 at about 10:30 AM. The perimeter of the flow at the time the imagery was acquired is outlined in yellow.
Map of flow field west of Kaohe Homesteads with thermal overlay
Map of flow field west of Kaohe Homesteads with thermal overlayThis map overlays a georegistered mosaic of thermal images collected during a helicopter overflight of Kīlauea's active East Rift Zone lava flow west of Kaohe Homesteads on March 10 at about 10:30 AM. The perimeter of the flow at the time the imagery was acquired is outlined in yellow.
This map overlays georegistered mosaics of thermal images collected during a helicopter overflight of Kīlauea's active East Rift Zone lava flow near Pu‘u ‘Ō‘ō on March 10 at about 10:25 AM. The perimeter of the flow at the time the imagery was acquired is outlined in yellow.
This map overlays georegistered mosaics of thermal images collected during a helicopter overflight of Kīlauea's active East Rift Zone lava flow near Pu‘u ‘Ō‘ō on March 10 at about 10:25 AM. The perimeter of the flow at the time the imagery was acquired is outlined in yellow.
This small-scale map shows Kīlauea's active East Rift Zone lava flow in relation to lower Puna. The area of the flow on February 27 is shown in pink, while widening and advancement of the flow as of March 10 is shown in red.
This small-scale map shows Kīlauea's active East Rift Zone lava flow in relation to lower Puna. The area of the flow on February 27 is shown in pink, while widening and advancement of the flow as of March 10 is shown in red.
Closeup of the new breakout near Pu‘u Kahauale‘a.
Closeup of the new breakout near Pu‘u Kahauale‘a.
The leading edge of the lobe nearest Pahoa Marketplace is still stalled but, for the past few days, a new breakout has been advancing along its southern margin and is approaching the AP‘A‘ā St. firebreak.
The leading edge of the lobe nearest Pahoa Marketplace is still stalled but, for the past few days, a new breakout has been advancing along its southern margin and is approaching the AP‘A‘ā St. firebreak.
The thin crust over the lava lake within the Halema‘uma‘u Overlook crater was moving slowly to the southeast. During our overflight, there was no spattering and wispy gas emissions allowed clear views.
The thin crust over the lava lake within the Halema‘uma‘u Overlook crater was moving slowly to the southeast. During our overflight, there was no spattering and wispy gas emissions allowed clear views.
This large-scale map uses a satellite image acquired in March 2014 (provided by Digital Globe) as a base to show the area around the front of Kīlauea's active East Rift Zone lava flow. The area of the flow on February 27 is shown in pink, while widening and advancement of the flow as of March 10 is shown in red.
This large-scale map uses a satellite image acquired in March 2014 (provided by Digital Globe) as a base to show the area around the front of Kīlauea's active East Rift Zone lava flow. The area of the flow on February 27 is shown in pink, while widening and advancement of the flow as of March 10 is shown in red.
HVO welcomes its new Scientist-in-Charge: Christina Neal
HVO welcomes its new Scientist-in-Charge: Christina NealLeft: Christina (Tina) Neal leaves the snowy stratovolcanoes of Alaska, where she spent almost 25 years as a USGS geologist with the Alaska Volcano Observatory, to become the new Scientist-in-Charge of the USGS Hawaiian Volcano Observatory on March 8, 2015. Photo courtesy of Tina Neal.
HVO welcomes its new Scientist-in-Charge: Christina Neal
HVO welcomes its new Scientist-in-Charge: Christina NealLeft: Christina (Tina) Neal leaves the snowy stratovolcanoes of Alaska, where she spent almost 25 years as a USGS geologist with the Alaska Volcano Observatory, to become the new Scientist-in-Charge of the USGS Hawaiian Volcano Observatory on March 8, 2015. Photo courtesy of Tina Neal.
Satellite image around front of Kīlauea's ERZ lava flow
Satellite image around front of Kīlauea's ERZ lava flowThis satellite image was captured on Tuesday, March 3, 2015 by the Landsat 8 satellite. Although this is a false-color image, the color map has been chosen to mimic what the human eye would expect to see. Bright red pixels depict areas of very high temperatures and show active lava. White areas are clouds.
Satellite image around front of Kīlauea's ERZ lava flow
Satellite image around front of Kīlauea's ERZ lava flowThis satellite image was captured on Tuesday, March 3, 2015 by the Landsat 8 satellite. Although this is a false-color image, the color map has been chosen to mimic what the human eye would expect to see. Bright red pixels depict areas of very high temperatures and show active lava. White areas are clouds.
The leading tip of the June 27th flow remains stalled, but breakouts persist upslope of the stalled tip. Over the past few days, summit deflation has led to a reduction in overall surface activity on the June 27th flow, particularly in the upslope portion of the flow field near Pu‘u ‘Ō‘ō.
The leading tip of the June 27th flow remains stalled, but breakouts persist upslope of the stalled tip. Over the past few days, summit deflation has led to a reduction in overall surface activity on the June 27th flow, particularly in the upslope portion of the flow field near Pu‘u ‘Ō‘ō.
Another small breakout upslope of the stalled flow front, triggerin...
Another small breakout upslope of the stalled flow front, triggerin...Another small breakout upslope of the stalled flow front, triggering a small brush fire. Low clouds and rain prevented wider views of the flow activity today.
Another small breakout upslope of the stalled flow front, triggerin...
Another small breakout upslope of the stalled flow front, triggerin...Another small breakout upslope of the stalled flow front, triggering a small brush fire. Low clouds and rain prevented wider views of the flow activity today.
Summit lava lake level has dropped with recent deflation
Summit lava lake level has dropped with recent deflationSummit deflation over the past few days has been associated with a steadily dropping lava lake level. This morning, the lake was 72 m (240 ft) below the rim of the Overlook crater.
Summit lava lake level has dropped with recent deflation
Summit lava lake level has dropped with recent deflationSummit deflation over the past few days has been associated with a steadily dropping lava lake level. This morning, the lake was 72 m (240 ft) below the rim of the Overlook crater.
The breakout on the north flank of Pu‘u ‘Ō‘ō that began last weekend remains active, but has advanced only a minor distance over the past four days. The new breakout is visible as the light-colored area just to the right of the center of the photograph. Pu‘u ‘Ō‘ō Crater is in the upper left portion of the photograph.
The breakout on the north flank of Pu‘u ‘Ō‘ō that began last weekend remains active, but has advanced only a minor distance over the past four days. The new breakout is visible as the light-colored area just to the right of the center of the photograph. Pu‘u ‘Ō‘ō Crater is in the upper left portion of the photograph.
Geologist sets up a time-lapse camera to monitor breakout on Pu‘u ‘Ō‘ō
Geologist sets up a time-lapse camera to monitor breakout on Pu‘u ‘Ō‘ōAn HVO geologist sets up a time-lapse camera to monitor the breakout on Pu‘u ‘Ō‘ō.
Geologist sets up a time-lapse camera to monitor breakout on Pu‘u ‘Ō‘ō
Geologist sets up a time-lapse camera to monitor breakout on Pu‘u ‘Ō‘ōAn HVO geologist sets up a time-lapse camera to monitor the breakout on Pu‘u ‘Ō‘ō.
This view looks north and shows Pu‘u ‘Ō‘ō. Much of the original cone has been covered by subsequent lava flows, many of which poured out of the crater. Within the crater, a depression holds a number of smaller pits, some of which contain active lava ponds.
This view looks north and shows Pu‘u ‘Ō‘ō. Much of the original cone has been covered by subsequent lava flows, many of which poured out of the crater. Within the crater, a depression holds a number of smaller pits, some of which contain active lava ponds.
This view looks west and shows the depression within Pu‘u ‘Ō‘ō. Th...
This view looks west and shows the depression within Pu‘u ‘Ō‘ō. Th...This view looks west and shows the depression within Pu‘u ‘Ō‘ō Crater. This depression formed following the start of the June 27th lava flow.
This view looks west and shows the depression within Pu‘u ‘Ō‘ō. Th...
This view looks west and shows the depression within Pu‘u ‘Ō‘ō. Th...This view looks west and shows the depression within Pu‘u ‘Ō‘ō Crater. This depression formed following the start of the June 27th lava flow.
A closer look at a glowing hole in the NE pit in Pu‘u ‘Ō‘ō. Recent...
A closer look at a glowing hole in the NE pit in Pu‘u ‘Ō‘ō. Recent...A closer look at a glowing hole in the northeast pit in Pu‘u ‘Ō‘ō Crater. Recent overflows from the opening created the dark flows filling the bottom of the pit.
A closer look at a glowing hole in the NE pit in Pu‘u ‘Ō‘ō. Recent...
A closer look at a glowing hole in the NE pit in Pu‘u ‘Ō‘ō. Recent...A closer look at a glowing hole in the northeast pit in Pu‘u ‘Ō‘ō Crater. Recent overflows from the opening created the dark flows filling the bottom of the pit.
This lava pond was active in the southern pit in Pu‘u ‘Ō‘ō. The di...
This lava pond was active in the southern pit in Pu‘u ‘Ō‘ō. The di...This lava pond was active in the southern pit in Pu‘u ‘Ō‘ō crater. The diameter of the lava pond was roughly 18 m (60 ft). Weak spattering was active on the pond margin.
This lava pond was active in the southern pit in Pu‘u ‘Ō‘ō. The di...
This lava pond was active in the southern pit in Pu‘u ‘Ō‘ō. The di...This lava pond was active in the southern pit in Pu‘u ‘Ō‘ō crater. The diameter of the lava pond was roughly 18 m (60 ft). Weak spattering was active on the pond margin.
hole in the NE pit. An active, bubbling lava surface could be seen...
hole in the NE pit. An active, bubbling lava surface could be seen...A closer look at the hole in the northeast pit. An active, bubbling lava surface could be seen a couple meters (yards) below the rim.
hole in the NE pit. An active, bubbling lava surface could be seen...
hole in the NE pit. An active, bubbling lava surface could be seen...A closer look at the hole in the northeast pit. An active, bubbling lava surface could be seen a couple meters (yards) below the rim.
This large-scale map uses a satellite image acquired in March 2014 (provided by Digital Globe) as a base to show the area around the front of Kīlauea's active East Rift Zone lava flow. The area of the flow on February 23 is shown in pink, while widening and advancement of the flow as of February 27 is shown in red.
This large-scale map uses a satellite image acquired in March 2014 (provided by Digital Globe) as a base to show the area around the front of Kīlauea's active East Rift Zone lava flow. The area of the flow on February 23 is shown in pink, while widening and advancement of the flow as of February 27 is shown in red.