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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 man stands smiling on a high coastal bluff near solar panels and a pole supported by guy wires, with a camera mounted on top.
Video camera installation, Barter Island
Video camera installation, Barter Island
Video camera installation, Barter Island

USGS oceanographer Shawn Harrison poses in front of the USGS video camera installation atop the coastal bluff of Barter Island in northern Alaska.

USGS oceanographer Shawn Harrison poses in front of the USGS video camera installation atop the coastal bluff of Barter Island in northern Alaska.

A coastal cliff is covered in grasses and some snow, and chunks of the cliff are beginning to crack and fall into the ocean.
Camera set-up on Barter Island coastal bluffs
Camera set-up on Barter Island coastal bluffs
Camera set-up on Barter Island coastal bluffs

For a short study period, two video cameras overlooked the coast from atop the coastal bluff of Barter Island in northern Alaska. The purpose was to observe and quantify coastal processes such as wave run-up, development of rip channels, bluff erosion, and movement of sandbars and ice floes.

For a short study period, two video cameras overlooked the coast from atop the coastal bluff of Barter Island in northern Alaska. The purpose was to observe and quantify coastal processes such as wave run-up, development of rip channels, bluff erosion, and movement of sandbars and ice floes.

Fissure eruption
Kīlauea Volcano — Fissure 8
Kīlauea Volcano — Fissure 8
Kīlauea Volcano — Fissure 8

View of Fissure 8 and channel during the morning overflight on July 7.

Camera looking over a summit
Kīlauea Volcano — SO2 Camera
Kīlauea Volcano — SO2 Camera
Kīlauea Volcano — SO2 Camera

For several years, a special ultraviolet camera has been located near Keanakākoʻi Crater at Kīlauea's summit. The camera was capable of detecting SO2 gas coming from Halema‘uma‘u crater. This morning, the camera was removed because there is very little SO2 to measure these days at the summit.

For several years, a special ultraviolet camera has been located near Keanakākoʻi Crater at Kīlauea's summit. The camera was capable of detecting SO2 gas coming from Halema‘uma‘u crater. This morning, the camera was removed because there is very little SO2 to measure these days at the summit.

USGS ecologists map and monitor vegetation and landscape characteristics at long-term ecological monitoring sites on the YKD
USGS ecologists map monitor vegetation and landscape characteristics
USGS ecologists map monitor vegetation and landscape characteristics
USGS ecologists map monitor vegetation and landscape characteristics

USGS ecologists map and monitor vegetation and landscape characteristics at long-term ecological monitoring sites on the Yukon-Kuskokwim Delta, AK

USGS ecologists map and monitor vegetation and landscape characteristics at long-term ecological monitoring sites on the Yukon-Kuskokwim Delta, AK

Men and women sitting in a room with tables and chairs listening to a woman talk, she's pointing at a screen on the wall.
USGS hosts community outreach event on Barter Island
USGS hosts community outreach event on Barter Island
USGS hosts community outreach event on Barter Island

USGS oceanographer Li Erikson speaks at a community outreach event on Barter Island, Alaska, to present results from earlier USGS studies and to discuss ongoing USGS research.

USGS oceanographer Li Erikson speaks at a community outreach event on Barter Island, Alaska, to present results from earlier USGS studies and to discuss ongoing USGS research.

 Female Pribilof rock sandpiper on breeding grounds, St. Matthew Island in the Bering Sea, Alaska
Female Pribilof rock sandpiper, St. Matthew Island, Bering Sea
Female Pribilof rock sandpiper, St. Matthew Island, Bering Sea
Female Pribilof rock sandpiper, St. Matthew Island, Bering Sea

In 2018, biologists conducted a second population survey to reassess the population status and habitat associations of Pribilof rock sandpipers breeding on St. Matthew and Hall Islands in the Bering Sea, Alaska. Previous work estimated the population size at approximately 19,800 birds (Ruthrauff et al. 2012).

In 2018, biologists conducted a second population survey to reassess the population status and habitat associations of Pribilof rock sandpipers breeding on St. Matthew and Hall Islands in the Bering Sea, Alaska. Previous work estimated the population size at approximately 19,800 birds (Ruthrauff et al. 2012).

Lava entering the ocean
Kīlauea Volcano — Kapoho Bay
Kīlauea Volcano — Kapoho Bay
Kīlauea Volcano — Kapoho Bay

Ocean entry in Kapoho as viewed from morning helicopter overflight.

Satellite image over crater
Kīlauea Volcano — Satellite View of Kīlauea Summit
Kīlauea Volcano — Satellite View of Kīlauea Summit
Kīlauea Volcano — Satellite View of Kīlauea Summit

The WorldView-3 satellite acquired this view of Kīlauea's summit on July 3. Despite a few clouds, the area of heaviest fractures in the caldera is clear. Views into the expanding Halema‘uma‘u crater reveal a pit floored by rubble. HVO, on the northwest caldera rim, is labeled.

The WorldView-3 satellite acquired this view of Kīlauea's summit on July 3. Despite a few clouds, the area of heaviest fractures in the caldera is clear. Views into the expanding Halema‘uma‘u crater reveal a pit floored by rubble. HVO, on the northwest caldera rim, is labeled.

A man wearing cold-weather gear and standing on a high coastal bluff points to an instrument that is mounted on short a pole.
Installing ground-shaking detection instrument
Installing ground-shaking detection instrument
Installing ground-shaking detection instrument

USGS scientist Cordell Johnson points to the Raspberry Shake, a sensitive instrument used to detect ground shaking. Johnson mounted the Raspberry Shake to an aluminum pole which he will then drive into the ground to bury the instrument beneath the tundra. This process will help isolate it from the wind.

USGS scientist Cordell Johnson points to the Raspberry Shake, a sensitive instrument used to detect ground shaking. Johnson mounted the Raspberry Shake to an aluminum pole which he will then drive into the ground to bury the instrument beneath the tundra. This process will help isolate it from the wind.

Aerial photo over Kapoho area showing lava entering ocean and passing residential areas
Kīlauea Volcano — Aerial of Kapoho Area
Kīlauea Volcano — Aerial of Kapoho Area
Kīlauea Volcano — Aerial of Kapoho Area

Aerial view of the lava channel and active margins between Kapoho Crater (upper right) and the coast (lower left). The northern margin of the flow field is advancing at several points in the area of Kapoho Ag and Beach Lots (vegetated areas in center of image). Image courtesy of Hawaii County Fire Department.

Aerial view of the lava channel and active margins between Kapoho Crater (upper right) and the coast (lower left). The northern margin of the flow field is advancing at several points in the area of Kapoho Ag and Beach Lots (vegetated areas in center of image). Image courtesy of Hawaii County Fire Department.

Dust rising from a crater after a rock collapse
Kīlauea Volcano — Collapse and Dust Rising at Halema`uma`u Crater
Kīlauea Volcano — Collapse and Dust Rising at Halema`uma`u Crater
Kīlauea Volcano — Collapse and Dust Rising at Halema`uma`u Crater

At 1:20 PM HST on July 5, a collapse explosion event occurred at Kīlauea's summit. The energy released by the event was equivalent to a M5.2 earthquake.

At 1:20 PM HST on July 5, a collapse explosion event occurred at Kīlauea's summit. The energy released by the event was equivalent to a M5.2 earthquake.

Dust rising from inside a crater after a rock collapse
Kīlauea Volcano — Dust from Summit Explosion
Kīlauea Volcano — Dust from Summit Explosion
Kīlauea Volcano — Dust from Summit Explosion

Rocks generate brown dust as they tumble down the western caldera wall during the collapse explosion event on July 5, 2018.

Rocks generate brown dust as they tumble down the western caldera wall during the collapse explosion event on July 5, 2018.

Lava entering the ocean with laze plumes rising
Kīlauea Volcano — Kapoho Coastline Delta
Kīlauea Volcano — Kapoho Coastline Delta
Kīlauea Volcano — Kapoho Coastline Delta

Lava enters the sea along the Kapoho coastline, building a delta that is now over 555 acres in size.

Lava enters the sea along the Kapoho coastline, building a delta that is now over 555 acres in size.

Levees created from cooled lava
Kīlauea Volcano — Lava Levees
Kīlauea Volcano — Lava Levees
Kīlauea Volcano — Lava Levees

Lava, from small overflows, cools and congeals along the banks of the lava channel to build lava levees. The levees also build up as moving lava pushes cooled crust over the edge.

Lava, from small overflows, cools and congeals along the banks of the lava channel to build lava levees. The levees also build up as moving lava pushes cooled crust over the edge.

A small lavafall in the middle of a lava flow.
Kīlauea Volcano — Lavafall Near Kapoho Crater
Kīlauea Volcano — Lavafall Near Kapoho Crater
Kīlauea Volcano — Lavafall Near Kapoho Crater

Near the Kapoho Crater, in the area called Four Corners, the lava channel makes a 90-degree bend. After lava exits the bend, it makes a short drop to form a lavafall. A side channel makes a short surface diversion before rejoining the existing channel.

Near the Kapoho Crater, in the area called Four Corners, the lava channel makes a 90-degree bend. After lava exits the bend, it makes a short drop to form a lavafall. A side channel makes a short surface diversion before rejoining the existing channel.

Lave entering the ocean with laze plumes rising
Kīlauea Volcano — Ocean Entry at Kapoho
Kīlauea Volcano — Ocean Entry at Kapoho
Kīlauea Volcano — Ocean Entry at Kapoho

Having crusted over about 0.8 km (0.5 mi) upchannel from the ocean entry, lava oozes from the flow's molten interior to enter the sea along a broad flow front on the northern (Kapoho) side of the flow.

Having crusted over about 0.8 km (0.5 mi) upchannel from the ocean entry, lava oozes from the flow's molten interior to enter the sea along a broad flow front on the northern (Kapoho) side of the flow.

A small instrument with a USGS logo sticker with wires coming out of it is in a hole in the ground.
Sensitive instrument used to detect ground shaking
Sensitive instrument used to detect ground shaking
Sensitive instrument used to detect ground shaking

This device, called a Raspberry Shake, is a sensitive instrument used to detect ground shaking. It is being carefully buried in this shallow hole in the tundra, to isolate it from wind.

This device, called a Raspberry Shake, is a sensitive instrument used to detect ground shaking. It is being carefully buried in this shallow hole in the tundra, to isolate it from wind.

Color photograph of caldera wall
Black streak of water on Kīlauea caldera wall
Black streak of water on Kīlauea caldera wall
Black streak of water on Kīlauea caldera wall

Black streak on caldera wall (center) is about 50 m (yards) long, and white steam plume (lower right) rises from northwestern part of Halema‘uma‘u. Photo from Volcano House Hotel on July 4, 2018. The configuration of this area changed considerably after the photo was taken, as collapse continued into early August.

Black streak on caldera wall (center) is about 50 m (yards) long, and white steam plume (lower right) rises from northwestern part of Halema‘uma‘u. Photo from Volcano House Hotel on July 4, 2018. The configuration of this area changed considerably after the photo was taken, as collapse continued into early August.

Animated GIF showing changes in size of the crater over a two month period
Kīlauea Volcano — Animation of Summit Subsidence
Kīlauea Volcano — Animation of Summit Subsidence
Kīlauea Volcano — Animation of Summit Subsidence

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 July 4 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 July 4 at about 6:00 a.m. HST.

Lava flowing at night time seen as bright red and orange
Kīlauea Volcano — Fissure 8 at Night
Kīlauea Volcano — Fissure 8 at Night
Kīlauea Volcano — Fissure 8 at Night

USGS Unmanned Aircraft Systems image of fissure 8 looking east.