Multimedia Gallery

Photos from a Scanning Electron Microscope (SEM) showing reacted rhyolite fragments at the end of the laboratory experiments. (a) Image magnified by 500 times showing the rhyolite after it reacted with water at 250 degrees Celsius (482 F). The reacted rhyolite fragments show very little change compared with the unreacted fragments. (b) Image magnified by 300 times showing

Steam vents along the Yellowstone River near Mud Volcano thermal area, Yellowstone National Park.

Mudpot located in the Mud Volcano thermal area of Yellowstone National Park.  This type of thermal feature indicates an acid-sulfate system.

Drilling through ice on the Green River.

The arrival of nightfall at Halema‘uma‘u on January 9, 2021, provided a clearer view of ongoing eruptive activity for USGS scientists monitoring the eruption this Saturday evening. This photo is focused on areas of active crustal motion in the western half of the lava lake; the eastern half (off to the right) is mostly stagnated and displays significantly less

Around sunset on Saturday (January 9, 2021), a break in the rain allowed HVO scientists to visit and monitor the ongoing eruption in Halema‘uma‘u. The west vent is still actively effusing lava, but outflow into the lava lake is increasingly sluggish, as evidenced by slow-moving crustal plates near the once-vigorous vent outlet. Also, much of the crust in the eastern half

Kīlauea’s summit lava lake, in Halema‘uma‘u, just after sunset on January 8, 2021. This view is to the north, from the south rim of the crater.  HVO scientists continue to monitor the eruption within an area of Hawai‘i Volcanoes National Park that remains closed to the public for safety reasons. USGS image by N. Deligne. 

This thermal image, looking northwest, shows the distribution of activity on the lava lake at Kīlauea's summit. The lake is slightly perched and surrounded along its perimeter by a lower ledge of cooler lava. The western fissure, in the wall of Halema‘uma‘u crater, is visible in the upper left portion of the image, just above the lake. Today, the eastern end of the lake (

Islands have been observed in Kīlauea lava lakes for more than 100 years—some move and some are moored. These two photographs of Halemaʻumaʻu crater from 1917 (top) and 2021 (bottom) show islands floating in lava lakes. The 1917 photographic panorama was taken from the edge of the lava lake, which was only about 30 m (100 ft) below crater rim and Kīlauea caldera floor. At

This photo, taken during an overflight of Kīlauea's summit this morning (January 7, 2021), shows the southeast margin of Halemaʻumaʻu's growing lava lake. The photo shows the boundary between the active portion of the lava lake (left) and the subtle levee around the lake perimeter that allows the lake to be slightly perched. The photo shows that a margin around the lake (

Aerial image of the active west vent area and the largest island in Halemaʻumaʻu's growing lava lake. During the overflight of Kīlauea's summit today (January 7, 2021) at approximately 10:30 a.m. HST, HVO geologists noted that the dome fountain, which had been persistent near the base of the west vent area, had subsided and was no longer present. USGS photo by K. Mulliken

During an overflight of Kīlauea summit today (January 7, 2021) at approximately 10:30 a.m. HST, HVO geologists captured this image of the growing lava lake within Halemaʻumaʻu. Sunny weather allowed for clear views of Mauna Loa, to the west. USGS photo by M. Patrick. 

View to the north-northwest from the south rim of Halemaʻumaʻu crater and showing the activity at the western fissure, partly obscured by a rainbow. Today, the western fissure was erupting periodic small spatter bursts from the southwest vent of the fissure that is incandescent in this image and nearly as tall as the previously active cone to the right (northeast). Today,

An HVO geologist takes Kīlauea summit eruption lake-level, spatter-cone, and dome-fountain measurements with a laser rangefinder. The top of the dome fountain in Halemaʻumaʻu was up to 5 meters (16 ft) above the lake surface. The lake elevation suggests a maximum lava lake depth of approximately 193 m (211 yd). HVO scientists monitor the ongoing Kīlauea summit eruption

View to the northwest from the south rim of Halemaʻumaʻu crater showing the lava lake in Halemaʻumaʻu at Kīlauea Volcano's summit. The active western fissure is visible above the lake, producing minor spatter and a gas plume from vents at the top. This vent is also sending lava into the lake from a lava tube opening at the lake surface, and producing a small dome fountain

Geologist hikes across folded Cretaceous rocks in the central North Slope. These rocks were assessed by the USGS in 2017 and lie above the rocks assessed in the USGS 2021 Western North Slope assessment.

The Kukpowruk River cuts through folded Cretaceous rocks in the central North Slope. These rocks were assessed by the USGS in 2017 and lie above the rocks assessed in the USGS 2021 Western North Slope assessment.

Jurassic rocks exposed in thurst-faulted structures near the southern limit of Western North Slope. In the subsurface farther north, these rocks may be reservoir rocks for natural gas.

Kīlauea summit KW webam image taken on January 6, 2021, just after 6:30 a.m. HST. The eruption in Halemaʻumaʻu continues and this photo shows that activity remains focused at the west vent as of Jan. 6 morning. You can view live KW webcam images here. USGS

Telephoto view of the lava flow and “dome fountain” activity at the west vent of the ongoing eruption in Halema‘uma‘u, Kīlauea Volcano summit, at 5:45 p.m. HST on 5 January, 2021. USGS photo by K. Lynn. 

View looking north across Kīlauea caldera from the south rim of Halema‘uma‘u, showing the ongoing eruption around 5:30 p.m. HST on January 5, 2021. The west vent activity included the “dome fountain,” effusive lava flows from a mid-elevation vent, and weak strombolian spattering activity from the high-elevation vent. USGS photo by K. Lynn. 

View through the laser rangefinder from the south rim of Halema‘uma‘u, Kīlauea Volcano summit, and showing the “dome fountain” and west vent effusive lava flow around 3:30 p.m. HST on January 5, 2021. A glowing vent is also visible at the top of the spatter structure. USGS photo by K. Lynn.

The west vent in Halema‘uma‘u crater continues to erupt at Kīlauea’s summit. These telephoto images from December 29 (left) and December 30 (right) compare the lava lake surface below the west vent. The west vent is supplying lava to the lake through a crusted over channel, which was starting to form by December 30. USGS photos by H. Dietterich.

At Halema‘uma‘u, the west vents (visible in the foreground of this photo as two glowing holes on a cone-shaped feature) erupt occaisional spatter. Lava is also emerging in a small dome fountain above the lake crust in front of the west vents, probably from a submerged portion of the vent (visible in the background of this photo as a bright spot with lava crust boundaries

Early this morning, the west vents in Halema‘uma‘u spattered from two places at the top of a small cone plastered on the northwest wall. This process can be seen in Kīlauea Volcano's summit F1 thermal webcam view of the lava lake. USGS photo by H.

Telephoto photograph of the west vent area and lava lake in Halema‘uma‘u, at Kīlauea Volcano's summit. USGS photo by K. Lynn.

View of the west vent area and lava lake in Halema‘uma‘u, at Kīlauea Volcano's summit. USGS photo by K. Lynn.

HVO field crews deployed a dense network of temporary seismic instruments at Kīlauea’s summit on January 1, 2021, and with permission from Hawai‘i Volcanoes National Park. The temporary instruments supplement data already being collected by HVO's permanent seismic network and will help to track the migration and storage of magma in the shallow volcanic plumbing system

With the onset of the eruption at Kīlauea summit on December 20, 2020, the HVO monitoring network has been recording volcanic tremor, a signal that travels through the subsurface as magma degasses and erupts from vents to fill a lava lake at the summit. Since the signal is continuous, it can be used to track the migration and storage of magma in Kīlauea's shallow volcanic

Within an hour of the Kīlauea summit eruption starting on December 20, 2020, HVO's permanent seismic network detected a signal called volcanic tremor. This tremor signal has been continuous since that time, creating an uninterrupted signal that travels through the subsurface as magma degasses and erupts from vents to fill a lava lake at the summit.  This photo shows a an

On January 1, 2021, with permission from Hawai‘i Volcanoes National Park, HVO researchers set up temporary seismic instruments around Halema‘uma‘u crater to collect data that will help them learn more about how magma travels in the shallow magmatic plumbing system beneath Kīlauea Volcano. In this photo, the field crew hikes along a portion of Crater Rim Drive road that was

The western portion of the lava lake in Halema‘uma‘u, Kīlauea Volcano summit. The island has migrated closer to the west vent area, which remains active. USGS photo by M. Patrick. 

Another telephoto view of the west vent area in Halema‘uma‘u, Kīlauea Volcano. The west vents are in the northwestern wall of Halema‘uma‘u crater; intermittent spattering at the vents has constructed a perched pointed cone on the crater wall. USGS photo by M. Patrick. 

Telephoto view of the west vent area in Halema‘uma‘u, Kīlauea Volcano. The west vents are in the northwestern wall of Halema‘uma‘u crater; intermittent spattering at the vents has constructed a perched pointed cone on the crater wall. USGS photo by M. Patrick. 

The margins of the lava lake in Halema‘uma‘u are showing a subtle levee around the perimeter. The levees grow from repeated small overflows, and the rafting and piling of pieces of surface crust that fuse together into a barrier that impounds the lake. This results in a "perched" lava lake, and this geometry has been common for lava lakes at Kīlauea's summit and rift zones

Kīlauea's summit lava lake in Halemaʻumaʻu continues to re-surface. This process is called crustal foundering, in which pieces of solidified lava crust on the surface of the lava lake break and sink back into the liquid portion. USGS photo by M. Patrick. 

Kīlauea's summit lava lake in Halemaʻumaʻu is continually re-surfacing. Like the 2008-2018 lava lake, the current lava lake is exhibiting crustal foundering, when fragments of solidified lava crust on the surface break and sink back into the liquid portion.  USGS photo by M. Patrick. 

Kīlauea eruption in Halema‘uma‘u on Jan. 1, 2021. The channel-like feature remains visible on the lava lake surface within Halemaʻumaʻu crater at Kīlauea Volcano's summit. This feature originates from the influx of lava from the western fissure. USGS photo by M. Patrick. 

Over the past week, the lava lake in Halema‘uma‘u has developed a subtle levee around its perimeter that allows the lake to be slightly perched above its base, like a mesa. The levees grow from repeated small overflows, and the rafting and piling of pieces of surface crust that fuse together into a barrier that impounds the fluid lake. This is called a "perched" lava lake

The KW webcam captured this image of Kīlauea's ongoing summit eruption, which continued overnight. The KW webcam looks in an east direction; north is to the left in the photo, south to the right, west to the bottom, and east to the top. This photo, taken at 6:30 a.m. HST on January 1, 2021, shows that the west vent (bottom of photo) remains active. You can view live KW

Hydrologic Technician Matt Bach measures discharge in Ashwaubenon Creek near Little Rapids, WI (NWIS site: 04085068) on May 21, 2020, as part of a cooperative project with NEWWater (Green Bay Metropolitan Sewage District) utilizing an adaptive management approach to meet phosphorus

Hydrologic Technician Matt Bach measures discharge in Ashwaubenon Creek near Little Rapids, WI (NWIS site: 04085068) on May 21, 2020, as part of a cooperative project with NEWWater (Green Bay Metropolitan Sewage District) utilizing an adaptive management approach to meet phosphorus

Experimental apparatus for reacting hot water and rhyolite. The photo on the left shows the inert gold bags into which the rhyolite fragments and water were inserted. After being sealed, the gold bag is then placed into a steel pressure vessel, which itself is loaded into a furnace (photo on the right). The furnace is connected through several wires to a controller that

Dave Brower (left) and Taylor Nagleri (right) working on logging data that was being collected by Rob Lorens in the stream (not pictured).

USGS employee taking surface water measurement at gage 11453500 Putah Creek near Guenoc, CA

Devin McGinty collecting measurements in the field including surveying and installing a new staff gage. 

Dr. Graham Sextone downloading weather station data in Rocky Mountain National Park. Station ID 401719105394311