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Section of sediment core from Rush Lake, Lower Geyser Basin, Yellowstone National Park, showing different layers that accumulated over time
Section of sediment core from Rush Lake, Lower Geyser Basin, Yellowstone National Park, showing different layers that accumulated over time
Section of sediment core from Rush Lake, Lower Geyser Basin, Yellowstone National Park, showing different layers that accumulated over time
Section of sediment core from Rush Lake, Lower Geyser Basin, Yellowstone National Park, showing different layers that accumulated over time

Section of a sediment core from Rush Lake, Lower Geyser Basin, Yellowstone National Park.

A portion of organic-rich lake mud recovered from Rush Lake, Lower Geyser Basin, Yellowstone National Park
A portion of organic-rich lake mud recovered from Rush Lake, Lower Geyser Basin, Yellowstone National Park
A portion of organic-rich lake mud recovered from Rush Lake, Lower Geyser Basin, Yellowstone National Park
A portion of organic-rich lake mud recovered from Rush Lake, Lower Geyser Basin, Yellowstone National Park

A portion of organic-rich lake mud recovered from Rush Lake, in the Lower Geyser Basin of Yellowstone National Park. Younger sediments are to the left and older sediments are to the right. The researcher is pointing to a thin, white layer—the Mazama ash, produced during the eruption 7600 years ago that formed Crater Lake in Oregon.

A portion of organic-rich lake mud recovered from Rush Lake, in the Lower Geyser Basin of Yellowstone National Park. Younger sediments are to the left and older sediments are to the right. The researcher is pointing to a thin, white layer—the Mazama ash, produced during the eruption 7600 years ago that formed Crater Lake in Oregon.

Streamgage site and profiling tool on the Yellowstone River at Corwin Springs, Montana
Streamgage site and profiling tool on the Yellowstone River at Corwin Springs, Montana
Streamgage site and profiling tool on the Yellowstone River at Corwin Springs, Montana
Streamgage site and profiling tool on the Yellowstone River at Corwin Springs, Montana

Streamgage site and profiling tool on the Yellowstone River at Corwin Springs, Montana.  The gage house narrowly avoided damage during the June 2022 flood, which eroded the downstream bank.  The river profiling instrument helps to map the river bottom to assess streamflow rates and conditions.  USGS photo by Mike Poland, July 31, 2023.

Streamgage site and profiling tool on the Yellowstone River at Corwin Springs, Montana.  The gage house narrowly avoided damage during the June 2022 flood, which eroded the downstream bank.  The river profiling instrument helps to map the river bottom to assess streamflow rates and conditions.  USGS photo by Mike Poland, July 31, 2023.

Photograph showing orange fountains of lava inside a crater with orange and black lava flows filling the crater.
Screen Shot 2023-07-14 at 9.52.56 AM.png
Screen Shot 2023-07-14 at 9.52.56 AM.png
Screen Shot 2023-07-14 at 9.52.56 AM.png

Web camera view of the onset of the June 7 eruption of Kīlauea volcano from the summit caldera.

Web camera view of the onset of the June 7 eruption of Kīlauea volcano from the summit caldera.

Animated GIF of the Porcelain Basin and Nuphar Lake areas of Norris Geyser Basin
Animated GIF of the Porcelain Basin and Nuphar Lake areas of Norris Geyser Basin
Animated GIF of the Porcelain Basin and Nuphar Lake areas of Norris Geyser Basin
Animated GIF of the Porcelain Basin and Nuphar Lake areas of Norris Geyser Basin

High-resolution satellite images of the Porcelain Basin and Nuphar Lake areas of Norris Geyser Basin acquired by Quickbird-2 on September 11, 2006 and WorldView-3 on March 30, 2022.  Note the change in color of Nuphar lake, from deep green to light blue, over time, as well as the increased evidence of flow from thermal features on the east side of Porcelain Bas

High-resolution satellite images of the Porcelain Basin and Nuphar Lake areas of Norris Geyser Basin acquired by Quickbird-2 on September 11, 2006 and WorldView-3 on March 30, 2022.  Note the change in color of Nuphar lake, from deep green to light blue, over time, as well as the increased evidence of flow from thermal features on the east side of Porcelain Bas

Map of Norris Geyser Basin
Map of Norris Geyser Basin
Map of Norris Geyser Basin
Map of Norris Geyser Basin

Map of Norris Geyser Basin showing the locations of major subbasins, roads and trails, and Nuphar Lake.

Map of Norris Geyser Basin showing the locations of major subbasins, roads and trails, and Nuphar Lake.

High-resolution satellite images of the Porcelain Basin and Nuphar Lake areas of Norris Geyser Basin
High-resolution satellite images of the Porcelain Basin and Nuphar Lake areas of Norris Geyser Basin
High-resolution satellite images of the Porcelain Basin and Nuphar Lake areas of Norris Geyser Basin
High-resolution satellite images of the Porcelain Basin and Nuphar Lake areas of Norris Geyser Basin

High-resolution satellite images of the Porcelain Basin and Nuphar Lake areas of Norris Geyser Basin acquired by Quickbird-2 on September 11, 2006 (left), WorldView-3 on July 7, 2016 (middle), and WorldView-3 on March 30, 2022 (right).  Note the change in color of Nuphar lake, from deep green to light blue, over time, as well as the increased evidence of flow f

High-resolution satellite images of the Porcelain Basin and Nuphar Lake areas of Norris Geyser Basin acquired by Quickbird-2 on September 11, 2006 (left), WorldView-3 on July 7, 2016 (middle), and WorldView-3 on March 30, 2022 (right).  Note the change in color of Nuphar lake, from deep green to light blue, over time, as well as the increased evidence of flow f

Visible (top) and thermal (bottom) images of Porcelain Basin
Visible (top) and thermal (bottom) images of Porcelain Basin
Visible (top) and thermal (bottom) images of Porcelain Basin
Visible (top) and thermal (bottom) images of Porcelain Basin

Visible (top) and thermal (bottom) images of Porcelain Basin looking to the north from the old roadbed.  Nuphar Lake is off the photograph to the right.  Cool-water seeps into Porcelain Basin are clearly evident in the thermal image and appear to flow underground from Nuphar Lake.  USGS photos by Mike Poland, July 1, 2023.

Visible (top) and thermal (bottom) images of Porcelain Basin looking to the north from the old roadbed.  Nuphar Lake is off the photograph to the right.  Cool-water seeps into Porcelain Basin are clearly evident in the thermal image and appear to flow underground from Nuphar Lake.  USGS photos by Mike Poland, July 1, 2023.

Color graphics of earthquakes
Map of American Samoa volcano-monitoring network.
Map of American Samoa volcano-monitoring network.
Map of American Samoa volcano-monitoring network.

Map of the American Samoa volcano-monitoring network (top). Data from Wake Island hydrograph (located about 4,500 km, or 2,900 miles, northwest of Taʻū Island) shows the general trend in the number of events during the 2022 earthquake swarm (bottom left). Locations for larger earthquakes (M2.5 and greater) are available starting August 20, 2022 (bottom right).

Map of the American Samoa volcano-monitoring network (top). Data from Wake Island hydrograph (located about 4,500 km, or 2,900 miles, northwest of Taʻū Island) shows the general trend in the number of events during the 2022 earthquake swarm (bottom left). Locations for larger earthquakes (M2.5 and greater) are available starting August 20, 2022 (bottom right).

Map of Yellowstone region showing the backbone and dense 2020 seismic networks
Map of Yellowstone region showing the backbone and dense 2020 seismic networks
Map of Yellowstone region showing the backbone and dense 2020 seismic networks
Map of Yellowstone region showing the backbone and dense 2020 seismic networks

Map of Yellowstone region showing the backbone (triangles) and dense 2020 (yellow squares) seismic networks, and based on Wu et al. (2023).

Comparison between the velocity structures outlining the Yellowstone’s upper-crustal magma reservoir at 5 km (3 mi) depth based on sparse (left) and dense (right) seismic networks
Velocity structures outlining the Yellowstone’s upper-crustal magma reservoir based on sparse (left) and dense (right) seismic networks
Velocity structures outlining the Yellowstone’s upper-crustal magma reservoir based on sparse (left) and dense (right) seismic networks
Velocity structures outlining the Yellowstone’s upper-crustal magma reservoir based on sparse (left) and dense (right) seismic networks

Comparison between the velocity structures outlining the Yellowstone’s upper-crustal magma reservoir at 5 km (3 mi) depth based on sparse (left) and dense (right) seismic networks. The open squares denote the locations of seismic sensors. Warmer color indicates lower velocity, representing higher melt fraction within the medium.

Comparison between the velocity structures outlining the Yellowstone’s upper-crustal magma reservoir at 5 km (3 mi) depth based on sparse (left) and dense (right) seismic networks. The open squares denote the locations of seismic sensors. Warmer color indicates lower velocity, representing higher melt fraction within the medium.

Schematic model of Yellowstone’s subsurface magmatic sill complex based on seismic data collected in 2020
Schematic model of Yellowstone’s subsurface magmatic sill complex based on seismic data collected in 2020
Schematic model of Yellowstone’s subsurface magmatic sill complex based on seismic data collected in 2020
Schematic model of Yellowstone’s subsurface magmatic sill complex based on seismic data collected in 2020

Schematic model of Yellowstone’s subsurface magmatic sill complex based on seismic data collected in 2020.

Four examples of vertical ground shaking during Steamboat Geyser eruptions as recorded by seismic station YNM
Four examples of vertical ground shaking during Steamboat Geyser eruptions as recorded by seismic station YNM
Four examples of vertical ground shaking during Steamboat Geyser eruptions as recorded by seismic station YNM
Four examples of vertical ground shaking during Steamboat Geyser eruptions as recorded by seismic station YNM

Four examples of vertical ground shaking during Steamboat Geyser eruptions as recorded by seismic station YNM. The vertical scale is the same for each seismogram.

Woman receiving lei from a man.
Interior Secretary, Deb Haaland, presented with lei.
Interior Secretary, Deb Haaland, presented with lei.
Interior Secretary, Deb Haaland, presented with lei.

Interior Secretary, Deb Haaland, presented with lei by David Phillips, Deputy Scientist-in-Charge of the USGS Hawaiian Volcano Observatory, during a ceremony to celebrate the creation of a new facility that will monitor volcanoes and support conservation science.

Interior Secretary, Deb Haaland, presented with lei by David Phillips, Deputy Scientist-in-Charge of the USGS Hawaiian Volcano Observatory, during a ceremony to celebrate the creation of a new facility that will monitor volcanoes and support conservation science.

People sitting on a lawn during a ceremony
Celebration for the creation of a new USGS facility
Celebration for the creation of a new USGS facility
Celebration for the creation of a new USGS facility

Federal, state, local and University of Hawai´i leaders and students celebrate the creation of a new facility that will monitor volcanoes and support conservation science.

Federal, state, local and University of Hawai´i leaders and students celebrate the creation of a new facility that will monitor volcanoes and support conservation science.

Earthquake Lake and the Madison slide
Earthquake Lake and the Madison slide
Earthquake Lake and the Madison slide
Earthquake Lake and the Madison slide

Earthquake Lake, which formed when the Madison River was blocked by a landslide that occurred as a consequence of the Hebgen Lake earthquake in 1959.  The lake inundated existing forest, now marked by standing dead trees in the lake water. The landslide scar is visible on the side of the mountain at the far end of the lake.

Earthquake Lake, which formed when the Madison River was blocked by a landslide that occurred as a consequence of the Hebgen Lake earthquake in 1959.  The lake inundated existing forest, now marked by standing dead trees in the lake water. The landslide scar is visible on the side of the mountain at the far end of the lake.

Map of Geyser Hill, Upper Geyser Basin, Yellowstone National Park, with selected thermal features
Map of Geyser Hill, Upper Geyser Basin, Yellowstone National Park, with selected thermal features
Map of Geyser Hill, Upper Geyser Basin, Yellowstone National Park, with selected thermal features
Map of Geyser Hill, Upper Geyser Basin, Yellowstone National Park, with selected thermal features

Map of Geyser Hill, Upper Geyser Basin, Yellowstone National Park, showing selected thermal features, including new and reactivated features that were active during the May-June 2023 thermal unrest.  Map prepared by by Kiernan Folz-Donahue, Yellowstone National Park.

Map of Geyser Hill, Upper Geyser Basin, Yellowstone National Park, showing selected thermal features, including new and reactivated features that were active during the May-June 2023 thermal unrest.  Map prepared by by Kiernan Folz-Donahue, Yellowstone National Park.

Map of ground deformation monitoring network in the Yellowstone region
Map of ground deformation monitoring network in the Yellowstone region
Map of ground deformation monitoring network in the Yellowstone region
Map of ground deformation monitoring network in the Yellowstone region

Map of continuous Global Positioning System (GPS), semipermanent GPS, borehole strainmeters, and borehole tiltmeters that provide surface deformation monitoring capability in and around Yellowstone National Park. Red line denotes boundary of Yellowstone Caldera.

Map of continuous Global Positioning System (GPS), semipermanent GPS, borehole strainmeters, and borehole tiltmeters that provide surface deformation monitoring capability in and around Yellowstone National Park. Red line denotes boundary of Yellowstone Caldera.

Thermal feature UNNG-GHG-17a, Upper Geyser Basin, Yellowstone National Park, on May 31, 2023
Thermal feature UNNG-GHG-17a, Upper Geyser Basin, Yellowstone National Park, on May 31, 2023
Thermal feature UNNG-GHG-17a, Upper Geyser Basin, Yellowstone National Park, on May 31, 2023
Thermal feature UNNG-GHG-17a, Upper Geyser Basin, Yellowstone National Park, on May 31, 2023

Thermal feature UNNG-GHG-17a, not far from Sponge Geyser on Geyser Hill in Upper Geyser Basin, Yellowstone National Park.  The feature formed during a period of thermal unrest that began in May 2023 and threw debris and hot water onto the adjacent boardwalk, which was closed for safety.  National Park Service photo by Kiernan Folz-Donahue, May 31, 2023.

Thermal feature UNNG-GHG-17a, not far from Sponge Geyser on Geyser Hill in Upper Geyser Basin, Yellowstone National Park.  The feature formed during a period of thermal unrest that began in May 2023 and threw debris and hot water onto the adjacent boardwalk, which was closed for safety.  National Park Service photo by Kiernan Folz-Donahue, May 31, 2023.

Color map of crater floor temperature
May 23, 2023 — Kīlauea summit thermal map
May 23, 2023 — Kīlauea summit thermal map
May 23, 2023 — Kīlauea summit thermal map

A helicopter overflight on May 23, 2023, allowed for aerial visual and thermal imagery to be collected of Halema‘uma‘u crater at the summit of Kīlauea. No active lava was present in the crater, with only scattered warm spots on the crater floor.

A helicopter overflight on May 23, 2023, allowed for aerial visual and thermal imagery to be collected of Halema‘uma‘u crater at the summit of Kīlauea. No active lava was present in the crater, with only scattered warm spots on the crater floor.

Color map of crater floor temperature
May 23, 2023 — Kīlauea summit thermal map
May 23, 2023 — Kīlauea summit thermal map
May 23, 2023 — Kīlauea summit thermal map

A helicopter overflight on May 23, 2023, allowed for aerial visual and thermal imagery to be collected of Halema‘uma‘u crater at the summit of Kīlauea. No active lava was present in the crater, with only scattered warm spots on the crater floor.

A helicopter overflight on May 23, 2023, allowed for aerial visual and thermal imagery to be collected of Halema‘uma‘u crater at the summit of Kīlauea. No active lava was present in the crater, with only scattered warm spots on the crater floor.