HVO geologist uses a laser rangefinder to measure the depth of the lava lake at the summit of Kīlauea in the Overlook crater. The lake level was about 58 m (190 ft) below the crater rim this afternoon. In recent days the lake level has dropped about 35 m (115 ft) as tiltmeters at the summit have recorded a larger than usual deflationary trend.
Images
Volcano Hazard Program images.
HVO geologist uses a laser rangefinder to measure the depth of the lava lake at the summit of Kīlauea in the Overlook crater. The lake level was about 58 m (190 ft) below the crater rim this afternoon. In recent days the lake level has dropped about 35 m (115 ft) as tiltmeters at the summit have recorded a larger than usual deflationary trend.
Mauna Loa 1950 eruption: A lot of lava with little warning
Mauna Loa 1950 eruption: A lot of lava with little warningDuring the Mauna Loa 1950 eruption, three large, fast-moving lava flows advanced down the west flank of the volcano, each crossing the main highway before reaching the ocean. The Ka‘apuna flow, shown here, traveled from the Southwest Rift Zone vent (7,800 ft elevation) to the coast in just 17 hours, creating a huge steam plume as lava flowed into the sea.
Mauna Loa 1950 eruption: A lot of lava with little warning
Mauna Loa 1950 eruption: A lot of lava with little warningDuring the Mauna Loa 1950 eruption, three large, fast-moving lava flows advanced down the west flank of the volcano, each crossing the main highway before reaching the ocean. The Ka‘apuna flow, shown here, traveled from the Southwest Rift Zone vent (7,800 ft elevation) to the coast in just 17 hours, creating a huge steam plume as lava flowed into the sea.
Photomicrograph of rock thin section: Gabbroic inclusion
Photomicrograph of rock thin section: Gabbroic inclusionPhotomicrograph of gabbroic inclusion in Ogres Brow basaltic andesite. A rock thin section is created by gluing a small piece of rock onto a glass slide, then grinding it down to a thickness of 30 microns (the average human hair is about 100 microns in diameter) so that light shines through it when examined under the microscope.
Photomicrograph of rock thin section: Gabbroic inclusion
Photomicrograph of rock thin section: Gabbroic inclusionPhotomicrograph of gabbroic inclusion in Ogres Brow basaltic andesite. A rock thin section is created by gluing a small piece of rock onto a glass slide, then grinding it down to a thickness of 30 microns (the average human hair is about 100 microns in diameter) so that light shines through it when examined under the microscope.
Brian Shiro in the Wind River Range, Wyoming during a National Outdoor Leadership School expedition. Photo courtesy B. Shiro.
Brian Shiro in the Wind River Range, Wyoming during a National Outdoor Leadership School expedition. Photo courtesy B. Shiro.
USGS-CVO crew digs out Mount St. Helens' Sep. Lobe monitoring station.
USGS-CVO crew digs out Mount St. Helens' Sep. Lobe monitoring station.During the first few days of Mount St. Helen's earthquake swarm in March 2016, the September Lobe monitoring station (located on the 1980-86 dome) was buried in deep snow and not transmitting data.
USGS-CVO crew digs out Mount St. Helens' Sep. Lobe monitoring station.
USGS-CVO crew digs out Mount St. Helens' Sep. Lobe monitoring station.During the first few days of Mount St. Helen's earthquake swarm in March 2016, the September Lobe monitoring station (located on the 1980-86 dome) was buried in deep snow and not transmitting data.
Large-scale map with thermal overlay showing active flows
Large-scale map with thermal overlay showing active flowsThis map overlays a georeferenced thermal image mosaic onto the current map of the flow field near Pu‘u ‘Ō‘ō to show the distribution of active and recently active breakouts. The thermal images were collected during a helicopter overflight on March 25. The June 27th flow field as of March 25 is outlined in green for comparison.
Large-scale map with thermal overlay showing active flows
Large-scale map with thermal overlay showing active flowsThis map overlays a georeferenced thermal image mosaic onto the current map of the flow field near Pu‘u ‘Ō‘ō to show the distribution of active and recently active breakouts. The thermal images were collected during a helicopter overflight on March 25. The June 27th flow field as of March 25 is outlined in green for comparison.
In Pu‘u ‘Ō‘ō, there has been a small pit for nearly a year.
In Pu‘u ‘Ō‘ō, there has been a small pit for nearly a year.In the western portion of Pu‘u ‘Ō‘ō Crater, there has been a small pit for nearly a year. The pit is about 60 m (200 feet) wide, and a small circular lava pond resides beneath the overhanging west rim of this pit.
In Pu‘u ‘Ō‘ō, there has been a small pit for nearly a year.
In Pu‘u ‘Ō‘ō, there has been a small pit for nearly a year.In the western portion of Pu‘u ‘Ō‘ō Crater, there has been a small pit for nearly a year. The pit is about 60 m (200 feet) wide, and a small circular lava pond resides beneath the overhanging west rim of this pit.
Geologists walk along the edge of the inner crater in Pu‘u ‘Ō‘ō, ma...
Geologists walk along the edge of the inner crater in Pu‘u ‘Ō‘ō, ma...HVO geologists walk along the edge of the inner crater in Pu‘u ‘Ō‘ō, making stops periodically to perform laser rangefinder measurements of crater dimensions.
Geologists walk along the edge of the inner crater in Pu‘u ‘Ō‘ō, ma...
Geologists walk along the edge of the inner crater in Pu‘u ‘Ō‘ō, ma...HVO geologists walk along the edge of the inner crater in Pu‘u ‘Ō‘ō, making stops periodically to perform laser rangefinder measurements of crater dimensions.
One of the more vigorous breakouts on the flow field today
One of the more vigorous breakouts on the flow field todayshows one of the more vigorous breakouts on the flow field today.
One of the more vigorous breakouts on the flow field today
One of the more vigorous breakouts on the flow field todayshows one of the more vigorous breakouts on the flow field today.
Breakouts NE of Pu‘u ‘Ō‘ō, small lobe advancing through forest
Breakouts NE of Pu‘u ‘Ō‘ō, small lobe advancing through forestBreakouts persist northeast of Pu‘u ‘Ō‘ō, with scattered activity along the north margin of the flow field at the forest boundary. One narrow lobe of lava has pushed through forest over the past few weeks, and is 7.6 km (4.7 miles) northeast of the vent on Pu‘u ‘Ō‘ō.
Breakouts NE of Pu‘u ‘Ō‘ō, small lobe advancing through forest
Breakouts NE of Pu‘u ‘Ō‘ō, small lobe advancing through forestBreakouts persist northeast of Pu‘u ‘Ō‘ō, with scattered activity along the north margin of the flow field at the forest boundary. One narrow lobe of lava has pushed through forest over the past few weeks, and is 7.6 km (4.7 miles) northeast of the vent on Pu‘u ‘Ō‘ō.
Another view, looking west, showing the activity along the forest b...
Another view, looking west, showing the activity along the forest b...Another view, looking west, showing the activity along the forest boundary and northern flow margin. Scattered breakouts were burning forest in this area. In the upper left portion of the image, Pu‘u ‘Ō‘ō can be seen.
Another view, looking west, showing the activity along the forest b...
Another view, looking west, showing the activity along the forest b...Another view, looking west, showing the activity along the forest boundary and northern flow margin. Scattered breakouts were burning forest in this area. In the upper left portion of the image, Pu‘u ‘Ō‘ō can be seen.
Last Saturday, March 19, marked the 8-year anniversary of the start of Kīlauea's ongoing summit eruption in Halema‘uma‘u Crater. Halema‘uma‘u spans much of the width of this photo, and the small inner crater in the foreground is the Overlook crater, which contains the active lava lake.
Last Saturday, March 19, marked the 8-year anniversary of the start of Kīlauea's ongoing summit eruption in Halema‘uma‘u Crater. Halema‘uma‘u spans much of the width of this photo, and the small inner crater in the foreground is the Overlook crater, which contains the active lava lake.
June 27th lava flow and steepest descent paths near Pāhoa, Kīlauea
June 27th lava flow and steepest descent paths near Pāhoa, KīlaueaThis small-scale map shows Kīlauea's June2th lava flow boundaries on March 25, 2016, in relation to the eastern part of the Island of Hawai‘i. The area of the flow field on February 20 is shown in pink, while widening and advancement of the flow field as mapped on March 25 is shown in red. Pu‘u ‘Ō‘ō lava flows erupted prior to June 27, 2014, are shown in gray.
June 27th lava flow and steepest descent paths near Pāhoa, Kīlauea
June 27th lava flow and steepest descent paths near Pāhoa, KīlaueaThis small-scale map shows Kīlauea's June2th lava flow boundaries on March 25, 2016, in relation to the eastern part of the Island of Hawai‘i. The area of the flow field on February 20 is shown in pink, while widening and advancement of the flow field as mapped on March 25 is shown in red. Pu‘u ‘Ō‘ō lava flows erupted prior to June 27, 2014, are shown in gray.
The altered and fractured rim of Pu‘u ‘Ō‘ō Crater is prone to small collapses. Portions of the eastern crater rim, shown here, have collapsed onto the crater floor, covering the recent lava flows with rubble.
The altered and fractured rim of Pu‘u ‘Ō‘ō Crater is prone to small collapses. Portions of the eastern crater rim, shown here, have collapsed onto the crater floor, covering the recent lava flows with rubble.
This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area of the flow field on February 20 is shown in pink, while widening and advancement of the flow field as mapped on March 25 is shown in red. The yellow lines show the active lava tube system. Pu‘u ‘Ō‘ō lava flows erupted prior to June 27, 2014, are shown in gray.
This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area of the flow field on February 20 is shown in pink, while widening and advancement of the flow field as mapped on March 25 is shown in red. The yellow lines show the active lava tube system. Pu‘u ‘Ō‘ō lava flows erupted prior to June 27, 2014, are shown in gray.
USGS geologist Deborah Bergfeld measures the temperature of a thermal feature near Big Boiler at Bumpass Hell in Lassen Volcanic National Park.
USGS geologist Deborah Bergfeld measures the temperature of a thermal feature near Big Boiler at Bumpass Hell in Lassen Volcanic National Park.
USGS geologist Laura Clor (right) and Rachel Teasdale (California State University – Chico, left) collect gas samples from a thermal feature at Sulphur Works in Lassen Volcanic National Park.
USGS geologist Laura Clor (right) and Rachel Teasdale (California State University – Chico, left) collect gas samples from a thermal feature at Sulphur Works in Lassen Volcanic National Park.
USGS geologist Deborah Bergfeld collects a gas sample from a superheated (hotter than the boiling point) fumarole in Little Hot Springs Valley at Lassen Volcanic National Park.
USGS geologist Deborah Bergfeld collects a gas sample from a superheated (hotter than the boiling point) fumarole in Little Hot Springs Valley at Lassen Volcanic National Park.
Annotated photo of air-quality particulate monitoring instruments, showing temperature and humidity sensors, air-sample inlet tube, wind sensor, power supply, and communication connections.
Annotated photo of air-quality particulate monitoring instruments, showing temperature and humidity sensors, air-sample inlet tube, wind sensor, power supply, and communication connections.
Kīlauea's eruption in Halema‘uma‘u reaches 8th anniv
Kīlauea's eruption in Halema‘uma‘u reaches 8th annivKīlauea Volcano's summit eruption began on March 19, 2008, and continues today. The lava lake is contained within the Overlook crater, which is set within the larger Halema‘uma‘u Crater. In this February 28, 2016, photo, the lava lake surface was just 30 m (100 ft) below the rim of the Overlook crater. Spattering is visible in the southeast portion of the lake.
Kīlauea's eruption in Halema‘uma‘u reaches 8th anniv
Kīlauea's eruption in Halema‘uma‘u reaches 8th annivKīlauea Volcano's summit eruption began on March 19, 2008, and continues today. The lava lake is contained within the Overlook crater, which is set within the larger Halema‘uma‘u Crater. In this February 28, 2016, photo, the lava lake surface was just 30 m (100 ft) below the rim of the Overlook crater. Spattering is visible in the southeast portion of the lake.
Footprints in Ash from 1790 Kilauea Volcano Eruption
Footprints in Ash from 1790 Kilauea Volcano EruptionFootprints made in muddy ash during Kilauea's 1790 eruption are reminders that people experienced the largest explosive eruption in Hawai‘i in 1,000 years. More than 80, and possibly several hundred, people were killed by the eruption soon after the footprints were made.
Footprints in Ash from 1790 Kilauea Volcano Eruption
Footprints in Ash from 1790 Kilauea Volcano EruptionFootprints made in muddy ash during Kilauea's 1790 eruption are reminders that people experienced the largest explosive eruption in Hawai‘i in 1,000 years. More than 80, and possibly several hundred, people were killed by the eruption soon after the footprints were made.