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Explore our planet through photography and imagery, including climate change and water all the way back to the 1800s when the USGS was surveying the country by horse and buggy.

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A blocked lava channel
Kīlauea Volcano — Evolution of a Blocked Channel (Part 1)
Kīlauea Volcano — Evolution of a Blocked Channel (Part 1)
Kīlauea Volcano — Evolution of a Blocked Channel (Part 1)

Evolution of a blocked channel, photo 1. A blockage of rafted material within the lava channel causes lava to flow over its banks near the Kapoho cone. In this section of the lava channel a cold lava flow from the 1960 eruption forms a barrier on the north side, which initially directed the channel to the southeast.

Evolution of a blocked channel, photo 1. A blockage of rafted material within the lava channel causes lava to flow over its banks near the Kapoho cone. In this section of the lava channel a cold lava flow from the 1960 eruption forms a barrier on the north side, which initially directed the channel to the southeast.

Lava flowing
Kīlauea Volcano — Evolution of a Blocked Channel (Part 2)
Kīlauea Volcano — Evolution of a Blocked Channel (Part 2)
Kīlauea Volcano — Evolution of a Blocked Channel (Part 2)

Evolution of a blocked channel, image 2: While observing this area of the fissure 8 lava channel near Kapoho cone during the morning overflight, geologists witnesed an "apartment-building-sized" blockage within the channel give way and be pushed down stream by the pressurized lava behind.

Evolution of a blocked channel, image 2: While observing this area of the fissure 8 lava channel near Kapoho cone during the morning overflight, geologists witnesed an "apartment-building-sized" blockage within the channel give way and be pushed down stream by the pressurized lava behind.

Lava flowing out of a fissure at night
Kīlauea Volcano — Fissure 8 Flow at Night
Kīlauea Volcano — Fissure 8 Flow at Night
Kīlauea Volcano — Fissure 8 Flow at Night

During the overnight hours, the UAS (Unoccupied Aircraft Systems) team flew sections of the lower East Rift Zone, monitoring fissure 8 activity and reports of small overflows from the lava channel.

During the overnight hours, the UAS (Unoccupied Aircraft Systems) team flew sections of the lower East Rift Zone, monitoring fissure 8 activity and reports of small overflows from the lava channel.

Lava flowing from an active fissure
Kīlauea Volcano — Fissure 8 Lava Flow
Kīlauea Volcano — Fissure 8 Lava Flow
Kīlauea Volcano — Fissure 8 Lava Flow

Fissure 8 and the upper lava channel, viewed from the early morning helicopter overflight of the lower East Rift Zone. Recent heavy rains have soaked into the still-warm tephra and the moisture rises as steam (right side of lava channel).

Fissure 8 and the upper lava channel, viewed from the early morning helicopter overflight of the lower East Rift Zone. Recent heavy rains have soaked into the still-warm tephra and the moisture rises as steam (right side of lava channel).

Geologist making observations of an active fissure
Kīlauea Volcano — Geologist Making Observations of Fissure 8
Kīlauea Volcano — Geologist Making Observations of Fissure 8
Kīlauea Volcano — Geologist Making Observations of Fissure 8

Fisheye lens photograph of a USGS geologist making observations of the fissure 8 lava channel at sunset July 3, 2018. The field crew is at a high point overlooking the channel near where it makes a 90 degree turn around Kapoho Crater and flows south.

Fisheye lens photograph of a USGS geologist making observations of the fissure 8 lava channel at sunset July 3, 2018. The field crew is at a high point overlooking the channel near where it makes a 90 degree turn around Kapoho Crater and flows south.

View of a crater
Kīlauea Volcano — Sunrise at Halema`uma`u Crater
Kīlauea Volcano — Sunrise at Halema`uma`u Crater
Kīlauea Volcano — Sunrise at Halema`uma`u Crater

Inward slumping of Halema‘uma‘u continues in response to ongoing subsidence at Kīlauea Volcano's summit. This image, taken from a temporary observation post located at Volcano House, shows steep walls on the western side of the crater and sloping piles of rubble from rockfall events.

Inward slumping of Halema‘uma‘u continues in response to ongoing subsidence at Kīlauea Volcano's summit. This image, taken from a temporary observation post located at Volcano House, shows steep walls on the western side of the crater and sloping piles of rubble from rockfall events.

View of the ocean from above, through a window in the bottom of an airplane
Ocean through the belly of the plane
Ocean through the belly of the plane
Ocean through the belly of the plane

A view through the belly port of a plane while cameras collect images during an aerial photographic survey.

The Seabird Studies Team at the USGS Western Ecological Research Center is conducting aerial photographic surveys of the ocean off central and southern California to create comprehensive maps of seabird and marine mammal distributions.

A view through the belly port of a plane while cameras collect images during an aerial photographic survey.

The Seabird Studies Team at the USGS Western Ecological Research Center is conducting aerial photographic surveys of the ocean off central and southern California to create comprehensive maps of seabird and marine mammal distributions.

Drone shot looking at brightly colored red and orange lava flows
Kīlauea Volcano — Drone Over Lava Channel
Kīlauea Volcano — Drone Over Lava Channel
Kīlauea Volcano — Drone Over Lava Channel

USGS Mavic Pro drone image of the fissure 8 lava channel looking toward the vent. Overflows can be seen as incandescent spots beyond the channel margins. Drone flights and resultant imagery help scientists better identify areas of channel overflows and active flow advancement.

USGS Mavic Pro drone image of the fissure 8 lava channel looking toward the vent. Overflows can be seen as incandescent spots beyond the channel margins. Drone flights and resultant imagery help scientists better identify areas of channel overflows and active flow advancement.

Annotated photo looking at fissure 8 lava channels and identifying lava flows in residential areas and the ocean entry
Kīlauea Volcano — Fissure 8 Channel (Annotated)
Kīlauea Volcano — Fissure 8 Channel (Annotated)
Kīlauea Volcano — Fissure 8 Channel (Annotated)

Annotated drone image of Kīlauea Volcano's lower East Rift Zone fissure 8 lava channel. Image captured near Kapoho Crater looking east toward the ocean entry. Incandescent flow margin is more easily identified in the dark - specifically here in the area of Kapoho Beach Lots.

Annotated drone image of Kīlauea Volcano's lower East Rift Zone fissure 8 lava channel. Image captured near Kapoho Crater looking east toward the ocean entry. Incandescent flow margin is more easily identified in the dark - specifically here in the area of Kapoho Beach Lots.

Aerial shot showing lava flowing into residential area
Kīlauea Volcano — Lava at Kapoho Beach Lots
Kīlauea Volcano — Lava at Kapoho Beach Lots
Kīlauea Volcano — Lava at Kapoho Beach Lots

At the coast, the northern margin of the flow field is still oozing pasty lava at several points in the area of Kapoho Beach Lots.

Aerial view of an ocean entry with laze plumes
Kīlauea Volcano — Ocean Entry
Kīlauea Volcano — Ocean Entry
Kīlauea Volcano — Ocean Entry

The ocean entry being fed by a crusted over channel has fewer tiny ooze-out channels than yesterday spilling into the water. One larger ooze-out channel making dominant entry plume at the northern end of the broad ocean entry.

The ocean entry being fed by a crusted over channel has fewer tiny ooze-out channels than yesterday spilling into the water. One larger ooze-out channel making dominant entry plume at the northern end of the broad ocean entry.

Aerial of lava channels
Kīlauea Volcano — Open Lava Channels
Kīlauea Volcano — Open Lava Channels
Kīlauea Volcano — Open Lava Channels

Fountains from Fissure 8 spatter cone continue to supply lava to the open channel with intermittent small, short-lived overflows. Overflows appear as lighter gray to silver areas on the margins of the channel.

Fountains from Fissure 8 spatter cone continue to supply lava to the open channel with intermittent small, short-lived overflows. Overflows appear as lighter gray to silver areas on the margins of the channel.

Close up of a lava overflow
Kīlauea Volcano — Overfows
Kīlauea Volcano — Overfows
Kīlauea Volcano — Overfows

Close up image of overflows from the fissure 8 lava channel. Photograph taken during the morning overflight.

Close up image of overflows from the fissure 8 lava channel. Photograph taken during the morning overflight.

line graphs showing precipitation and temperature data for 3 future climate scenarios (hot/wet, hot/moderate precip, hot/dry)
Basin Characterization Model: Future Scenarios for Indian Wells Valley
Basin Characterization Model: Future Scenarios for Indian Wells Valley
Basin Characterization Model: Future Scenarios for Indian Wells Valley

Annual time series of precipitation and average air temperature for three future climate models for Indian Wells Valley, California as simulated by the Basin Characterization Model. Three future climate projections were selected from among 20 models used for California’s Fourth Climate Change Assessment for application to Indian Wells Valley.

Annual time series of precipitation and average air temperature for three future climate models for Indian Wells Valley, California as simulated by the Basin Characterization Model. Three future climate projections were selected from among 20 models used for California’s Fourth Climate Change Assessment for application to Indian Wells Valley.

View from the sky of a landscape with a river running through it, and the river is winding back and forth.
Mokelumne River Bathymetry
Mokelumne River Bathymetry
Mokelumne River Bathymetry

A winding strip of rainbow colors shows the bathymetry (depth) of the bed of the Mokelumne River just above its confluence with the San Joaquin in the Sacramento-San Joaquin River Delta east of San Francisco Bay.

A winding strip of rainbow colors shows the bathymetry (depth) of the bed of the Mokelumne River just above its confluence with the San Joaquin in the Sacramento-San Joaquin River Delta east of San Francisco Bay.

Animation showing changes in summit size on a map
Kīlauea Volcano — Animation of Summit Drop
Kīlauea Volcano — Animation of Summit Drop
Kīlauea Volcano — Animation of Summit Drop

This animated GIF shows a sequence of radar amplitude images that were acquired by the Agenzia Spaziale Italiana CosmoSkyMed satellite system. The images illustrate changes to the caldera area of Kīlauea Volcano that occurred between May 5 and June 30 at about 6:00 a.m. HST.

This animated GIF shows a sequence of radar amplitude images that were acquired by the Agenzia Spaziale Italiana CosmoSkyMed satellite system. The images illustrate changes to the caldera area of Kīlauea Volcano that occurred between May 5 and June 30 at about 6:00 a.m. HST.

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