Clear weather allowed HVO geologists to make observations and take measurements of the water pond at Kīlauea's summit. No major changes were observed, and the water level continues to slowly rise. Note the former HVO observation tower can be seen above the geologist's helmet.
Images
Volcano Hazard Program images.
Clear weather allowed HVO geologists to make observations and take measurements of the water pond at Kīlauea's summit. No major changes were observed, and the water level continues to slowly rise. Note the former HVO observation tower can be seen above the geologist's helmet.
Changes in color at Kīlauea's summit water pond are common
Changes in color at Kīlauea's summit water pond are commonThis compilation shows the appearance of the water pond at Kīlauea's summit over the past two weeks. Day to day changes in the color of the pond are common, with portions of the pond shifting from a green hue to brown. A sharp color boundary has been common for several months in the same general area of the pond.
Changes in color at Kīlauea's summit water pond are common
Changes in color at Kīlauea's summit water pond are commonThis compilation shows the appearance of the water pond at Kīlauea's summit over the past two weeks. Day to day changes in the color of the pond are common, with portions of the pond shifting from a green hue to brown. A sharp color boundary has been common for several months in the same general area of the pond.
Members of the Clear Lake Volcanic Field research team
Members of the Clear Lake Volcanic Field research teamMembers of the Clear Lake Volcanic Field research team
Members of the Clear Lake Volcanic Field research team
Members of the Clear Lake Volcanic Field research teamMembers of the Clear Lake Volcanic Field research team
Example 2-hours of seismic data from station near Mauna Kea
Example 2-hours of seismic data from station near Mauna KeaExample 2-hours of seismic data from station near Mauna Kea on April 14, 2020. The large spikes are earthquakes under Mauna Kea repeating every ~11 minutes. Bottom waveform zooms in on 15 seconds of an individual event.
Example 2-hours of seismic data from station near Mauna Kea
Example 2-hours of seismic data from station near Mauna KeaExample 2-hours of seismic data from station near Mauna Kea on April 14, 2020. The large spikes are earthquakes under Mauna Kea repeating every ~11 minutes. Bottom waveform zooms in on 15 seconds of an individual event.
This section of brown Icelandic soil (top) contains 800 years of ash deposits erupted from five different volcanoes. The black layers, 5-10 cm (2-4 in) thick, are from Katla Volcano. A white arrow points to a closeup of the 1755 Katla ash deposit (lower left).
This section of brown Icelandic soil (top) contains 800 years of ash deposits erupted from five different volcanoes. The black layers, 5-10 cm (2-4 in) thick, are from Katla Volcano. A white arrow points to a closeup of the 1755 Katla ash deposit (lower left).
Close monitoring of the summit water pond continues
Close monitoring of the summit water pond continuesClear weather allowed another water pond measurement to be made this morning. Results show continued slow rise of the water level. No major changes were observed. Note the former HVO observation tower can be seen above the geologist's helmet.
Close monitoring of the summit water pond continues
Close monitoring of the summit water pond continuesClear weather allowed another water pond measurement to be made this morning. Results show continued slow rise of the water level. No major changes were observed. Note the former HVO observation tower can be seen above the geologist's helmet.
Day to day changes in the color of the water pond are common. This morning the
Day to day changes in the color of the water pond are common. This morning theDay to day changes in the color of the water pond are common. This morning the pond had a browner hue compared to the previous observation on April 1, when the pond color was slightly more greenish yellow (see photo below).
Day to day changes in the color of the water pond are common. This morning the
Day to day changes in the color of the water pond are common. This morning theDay to day changes in the color of the water pond are common. This morning the pond had a browner hue compared to the previous observation on April 1, when the pond color was slightly more greenish yellow (see photo below).
Scanning electron microprobe images of Icelandic ash
Scanning electron microprobe images of Icelandic ashScanning electron microprobe images show the complexity of tiny Icelandic ash grains (150 micron, or 0.006 inch). Image (a) shows a dense and blocky grain, and (b) shows a foamy grain.
Scanning electron microprobe images of Icelandic ash
Scanning electron microprobe images of Icelandic ashScanning electron microprobe images show the complexity of tiny Icelandic ash grains (150 micron, or 0.006 inch). Image (a) shows a dense and blocky grain, and (b) shows a foamy grain.
Physical map of the western USA showing locations of strong earthquakes in March
Physical map of the western USA showing locations of strong earthquakes in MarchPhysical map of the western USA showing locations of strong earthquakes in March 2020 and Basin and Range extensional province. The Basin and Range stretches from the Sierra Nevada in the west to the Wasatch and Teton mountains in the east, and from central Idaho and southwest Montana in the north to Mexico in the south.
Physical map of the western USA showing locations of strong earthquakes in March
Physical map of the western USA showing locations of strong earthquakes in MarchPhysical map of the western USA showing locations of strong earthquakes in March 2020 and Basin and Range extensional province. The Basin and Range stretches from the Sierra Nevada in the west to the Wasatch and Teton mountains in the east, and from central Idaho and southwest Montana in the north to Mexico in the south.
HVO looks to the past to better understand future Mauna Loa eruptions
HVO looks to the past to better understand future Mauna Loa eruptionsDuring the 1926 Mauna Loa eruption, an ‘a‘ā flow about 457 m (1500 ft) wide and 9 m (30 ft) high headed straight for the village of Ho‘ōpūloa on April 18, as shown here. By the next day, the lava flow had destroyed a dozen houses, a church, and the wharf, and had nearly obliterated the bay. Photo by Army Air Corps, 11th Photo Section.
HVO looks to the past to better understand future Mauna Loa eruptions
HVO looks to the past to better understand future Mauna Loa eruptionsDuring the 1926 Mauna Loa eruption, an ‘a‘ā flow about 457 m (1500 ft) wide and 9 m (30 ft) high headed straight for the village of Ho‘ōpūloa on April 18, as shown here. By the next day, the lava flow had destroyed a dozen houses, a church, and the wharf, and had nearly obliterated the bay. Photo by Army Air Corps, 11th Photo Section.
The water pond from the webcam site. This view provides a better view of the gr
The water pond from the webcam site. This view provides a better view of the grThe water pond from the webcam site. This view provides a better view of the greenish zone in the west end of the pond (bottom right of photo).
The water pond from the webcam site. This view provides a better view of the gr
The water pond from the webcam site. This view provides a better view of the grThe water pond from the webcam site. This view provides a better view of the greenish zone in the west end of the pond (bottom right of photo).
A closeup of the northern shoreline shows how opaque the water is against the ro
A closeup of the northern shoreline shows how opaque the water is against the roA closeup of the northern shoreline shows how opaque the water is against the rocks. USGS photo by M. Patrick.
A closeup of the northern shoreline shows how opaque the water is against the ro
A closeup of the northern shoreline shows how opaque the water is against the roA closeup of the northern shoreline shows how opaque the water is against the rocks. USGS photo by M. Patrick.
Aerial view of a bomb detonating on Mauna Loa lava flows
Aerial view of a bomb detonating on Mauna Loa lava flowsAerial view of a bomb detonating on Mauna Loa near the source of the 1935 Humu‘ula lava flow on the morning of December 27, 1935. This was one of 20 demolition bombs dropped on the lava flow that morning by the Army Bombing Squadron from Luke Field, O‘ahu.
Aerial view of a bomb detonating on Mauna Loa lava flows
Aerial view of a bomb detonating on Mauna Loa lava flowsAerial view of a bomb detonating on Mauna Loa near the source of the 1935 Humu‘ula lava flow on the morning of December 27, 1935. This was one of 20 demolition bombs dropped on the lava flow that morning by the Army Bombing Squadron from Luke Field, O‘ahu.
U.S. Army Air Corps biplane prepares to drop bombs on 1935 lava flow
U.S. Army Air Corps biplane prepares to drop bombs on 1935 lava flowA U.S. Army Air Corps biplane is prepared for a mission to drop bombs on a lava flow advancing toward Hilo during the Mauna Loa 1935 eruption.
U.S. Army Air Corps biplane prepares to drop bombs on 1935 lava flow
U.S. Army Air Corps biplane prepares to drop bombs on 1935 lava flowA U.S. Army Air Corps biplane is prepared for a mission to drop bombs on a lava flow advancing toward Hilo during the Mauna Loa 1935 eruption.
Mushroom Pool, in the Lower Geyser Basin of Yellowstone National Park. The pool
Mushroom Pool, in the Lower Geyser Basin of Yellowstone National Park. The poolMushroom Pool, in the Lower Geyser Basin of Yellowstone National Park, as it looked in June 23, 1967. The sample that would be the source of Thermus aquaticus strain YT-1 came from this hot spring. Pictured is Thomas Brock standing near the edge of the pool. Image from the self-published "A Scientist in Yellowstone National Park" (Brock, 2017).
Mushroom Pool, in the Lower Geyser Basin of Yellowstone National Park. The pool
Mushroom Pool, in the Lower Geyser Basin of Yellowstone National Park. The poolMushroom Pool, in the Lower Geyser Basin of Yellowstone National Park, as it looked in June 23, 1967. The sample that would be the source of Thermus aquaticus strain YT-1 came from this hot spring. Pictured is Thomas Brock standing near the edge of the pool. Image from the self-published "A Scientist in Yellowstone National Park" (Brock, 2017).
This timelapse sequence shows the water pond in Halema‘uma‘u Crater, at Kīlauea's summit, between November 1, 2019, and March 26, 2020. Over this time the water level rose approximately 14 meters (46 feet), equivalent to 67 cm (about 2 feet) per week. The timelapse shows one image per day (with a few cloudy images removed), and is looped several times.
This timelapse sequence shows the water pond in Halema‘uma‘u Crater, at Kīlauea's summit, between November 1, 2019, and March 26, 2020. Over this time the water level rose approximately 14 meters (46 feet), equivalent to 67 cm (about 2 feet) per week. The timelapse shows one image per day (with a few cloudy images removed), and is looped several times.
Water, ash, and the great unknown of explosive volcanic eruptions
Water, ash, and the great unknown of explosive volcanic eruptionsScanning electron microprobe images show the complexity of tiny Icelandic ash grains (150 micron, or 0.006 inch). Image (a) shows a dense and blocky grain, and (b) shows a foamy grain. Photos by J. Schmith.
Water, ash, and the great unknown of explosive volcanic eruptions
Water, ash, and the great unknown of explosive volcanic eruptionsScanning electron microprobe images show the complexity of tiny Icelandic ash grains (150 micron, or 0.006 inch). Image (a) shows a dense and blocky grain, and (b) shows a foamy grain. Photos by J. Schmith.
Answer: a GPS capable of accurately measuring elevations to within 10 cm (~4 in)
Answer: a GPS capable of accurately measuring elevations to within 10 cm (~4 in)Answer: a GPS capable of accurately measuring elevations to within 10 cm (~4 in). In the summer of 2019, USGS organized a Light Detection and Ranging (LiDAR) survey of the Kīlauea summit and East Rift Zone, including both the Pu‘u ‘Ō‘ō and 2018 lower Puna lava flows.
Answer: a GPS capable of accurately measuring elevations to within 10 cm (~4 in)
Answer: a GPS capable of accurately measuring elevations to within 10 cm (~4 in)Answer: a GPS capable of accurately measuring elevations to within 10 cm (~4 in). In the summer of 2019, USGS organized a Light Detection and Ranging (LiDAR) survey of the Kīlauea summit and East Rift Zone, including both the Pu‘u ‘Ō‘ō and 2018 lower Puna lava flows.
HVO scientists conduct field checks of LiDAR survey
HVO scientists conduct field checks of LiDAR surveyQuestion: what's that in the shrubs?
HVO scientists conduct field checks of LiDAR survey
HVO scientists conduct field checks of LiDAR surveyQuestion: what's that in the shrubs?
Guide describes general protocols and provides templates for news media manageme
Guide describes general protocols and provides templates for news media managemeUSGS Cascades Volcano Observatory News Media Management Guide—General Protocols and Templates, USGS Circular 1462 (https://pubs.er.usgs.gov/publication/cir1462) provides protocols and templates for (1) normal conditions when CVO has an opportunity to be proactive with its messages and to raise general awaren
Guide describes general protocols and provides templates for news media manageme
Guide describes general protocols and provides templates for news media managemeUSGS Cascades Volcano Observatory News Media Management Guide—General Protocols and Templates, USGS Circular 1462 (https://pubs.er.usgs.gov/publication/cir1462) provides protocols and templates for (1) normal conditions when CVO has an opportunity to be proactive with its messages and to raise general awaren
USGS Hawaiian Volcano Observatory scientists examine an outcrop of reddish-brown Hilo ash during a recent study to investigate the origins of volcanic ash deposits on the Island of Hawai‘i. Age dates of lava flows above and below the Hilo ash deposit indicate that the ash was erupted between 3,000 and 14,000 years ago.
USGS Hawaiian Volcano Observatory scientists examine an outcrop of reddish-brown Hilo ash during a recent study to investigate the origins of volcanic ash deposits on the Island of Hawai‘i. Age dates of lava flows above and below the Hilo ash deposit indicate that the ash was erupted between 3,000 and 14,000 years ago.