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Images related to natural hazards.
This photograph looks towards the ocean, from a spot along the west margin of the flow, showing the ocean entry plume just minutes after lava first reached the water.
This photograph looks towards the ocean, from a spot along the west margin of the flow, showing the ocean entry plume just minutes after lava first reached the water.
This map shows recent changes to Kīlauea's East Rift Zone lava flow field. The area of the active flow field as of July 19 is shown in pink, while widening and advancement of the active flow as mapped on July 26 is shown in red. Lava reached the ocean on the morning of July 26. Older Pu‘u ‘Ō‘ō lava flows (1983-2016) are shown in gray.
This map shows recent changes to Kīlauea's East Rift Zone lava flow field. The area of the active flow field as of July 19 is shown in pink, while widening and advancement of the active flow as mapped on July 26 is shown in red. Lava reached the ocean on the morning of July 26. Older Pu‘u ‘Ō‘ō lava flows (1983-2016) are shown in gray.
Video of the ocean entry, showing lava spilling over the sea cliff.
Video of the ocean entry, showing lava spilling over the sea cliff.
This image shows a thermal map of the flow on the pali and coastal plain, created from airborne thermal images. White pixels are hot, and show areas of active surface breakouts. The background image is a satellite image collected before the current lava flow was active.
This image shows a thermal map of the flow on the pali and coastal plain, created from airborne thermal images. White pixels are hot, and show areas of active surface breakouts. The background image is a satellite image collected before the current lava flow was active.
USGS HVO geochemist measuring gases released from Kīlauea with a Fourier transform infrared (FTIR) spectrometer, an instrument that detects gas compositions on the basis of absorbed infrared light.
USGS HVO geochemist measuring gases released from Kīlauea with a Fourier transform infrared (FTIR) spectrometer, an instrument that detects gas compositions on the basis of absorbed infrared light.
The active lava flow on Kīlauea Volcano's south flank providing wonderful lava-viewing experiences for Park visitors. A section of the road can be seen here, with fume from the active lava tube in the far distance behind it, and the active flow front in the foreground. The flow front was less than 100 meters (yards) from the ocean when this photo was taken.
The active lava flow on Kīlauea Volcano's south flank providing wonderful lava-viewing experiences for Park visitors. A section of the road can be seen here, with fume from the active lava tube in the far distance behind it, and the active flow front in the foreground. The flow front was less than 100 meters (yards) from the ocean when this photo was taken.
Just over two months since the start of the 61g flow, it reached the ocean on July 26 at 1:15 am HST. The narrow ocean entry was creating a small plume of gas and steam during today's overflight as the lava came into contact with the ocean.
Just over two months since the start of the 61g flow, it reached the ocean on July 26 at 1:15 am HST. The narrow ocean entry was creating a small plume of gas and steam during today's overflight as the lava came into contact with the ocean.
HVO geologists in the field overnight observed lava crossing the stretch of land between the "emergency" gravel road and the sea cliff. This photograph shows the flow front a short time before lava reached the ocean.
HVO geologists in the field overnight observed lava crossing the stretch of land between the "emergency" gravel road and the sea cliff. This photograph shows the flow front a short time before lava reached the ocean.
View of the slabby pāhoehoe flow front as it crosses to the ocean side of the emergency access road inside Hawai'i Volcanoes National Park.
View of the slabby pāhoehoe flow front as it crosses to the ocean side of the emergency access road inside Hawai'i Volcanoes National Park.
Summit of Cleveland Volcano in Alaska's central Aleutian Islands. A lava dome is visible in the crater.
Summit of Cleveland Volcano in Alaska's central Aleutian Islands. A lava dome is visible in the crater.
Flow 61G reached the emergency access road inside Hawai'i Volcanoes National Park on July 25 at 3:20 pm and crossed the road in about 30 minutes. At 4:00 pm, the flow front was approximately 110 m (0.07 miles) from the ocean.
Flow 61G reached the emergency access road inside Hawai'i Volcanoes National Park on July 25 at 3:20 pm and crossed the road in about 30 minutes. At 4:00 pm, the flow front was approximately 110 m (0.07 miles) from the ocean.
Southeast flanks of Mount Cleveland, a volcano in the Alaskan Aleutian Islands. Gas and steam plume seen emanating from the summit.
Southeast flanks of Mount Cleveland, a volcano in the Alaskan Aleutian Islands. Gas and steam plume seen emanating from the summit.
This image shows a thermal map of the flow on the pali and coastal plain, created from airborne thermal images. White pixels are hot, and show areas of active surface breakouts. The background image is a satellite image collected before the current lava flow was active.
This image shows a thermal map of the flow on the pali and coastal plain, created from airborne thermal images. White pixels are hot, and show areas of active surface breakouts. The background image is a satellite image collected before the current lava flow was active.
A faint double rainbow provided a beautiful backdrop for sluggish pāhoehoe lava oozing out from near the flow front this morning.
A faint double rainbow provided a beautiful backdrop for sluggish pāhoehoe lava oozing out from near the flow front this morning.
The flow front remains active and consists of slowly advancing pāhoehoe. There are scattered breakouts along the margins of the flow on the coastal plain and base of the pali. During the overflight today, the flow front was 730 m (0.45 miles) from the ocean.
The flow front remains active and consists of slowly advancing pāhoehoe. There are scattered breakouts along the margins of the flow on the coastal plain and base of the pali. During the overflight today, the flow front was 730 m (0.45 miles) from the ocean.
A breakout at the base of the pali viewed by a field crew this morning has formed a channelized ‘A‘ā flow on the steeper portion of the coastal plain.
A breakout at the base of the pali viewed by a field crew this morning has formed a channelized ‘A‘ā flow on the steeper portion of the coastal plain.
During early morning field observations, a large breakout of lava near the base of Pūlama Pali (steep fault scarp in background) was visible through fumes from the lava tube and heat shimmer from lava on the coastal plain. The approximate location of the lava tube feeding Kīlauea's active lava flow is visible as degassing sources (white fume) on the pali.
During early morning field observations, a large breakout of lava near the base of Pūlama Pali (steep fault scarp in background) was visible through fumes from the lava tube and heat shimmer from lava on the coastal plain. The approximate location of the lava tube feeding Kīlauea's active lava flow is visible as degassing sources (white fume) on the pali.
A close up view of the ‘A‘ā channel.
The active lava flow continues to creep across the coastal plain on Kīlauea's south flank. Breakouts of pāhoehoe (foreground) are fed by lava traveling through lava tubes from the Pu‘u ‘Ō‘ō vent and down Pūlama pali (top background). USGS photo.
The active lava flow continues to creep across the coastal plain on Kīlauea's south flank. Breakouts of pāhoehoe (foreground) are fed by lava traveling through lava tubes from the Pu‘u ‘Ō‘ō vent and down Pūlama pali (top background). USGS photo.
Map of Kīlauea's active lava flow as of July 19, 2016. Red shows the extent of new breakouts since July 8; pink shows the flow prior as of July 8, and gray shows areas covered by earlier Pu‘u ‘Ō‘ō lava flows (1983-2016).
Map of Kīlauea's active lava flow as of July 19, 2016. Red shows the extent of new breakouts since July 8; pink shows the flow prior as of July 8, and gray shows areas covered by earlier Pu‘u ‘Ō‘ō lava flows (1983-2016).
The HVO field crew mapped new breakouts on the lava flow by recording GPS points along the active flow margin.
The HVO field crew mapped new breakouts on the lava flow by recording GPS points along the active flow margin.