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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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Aerial view of Kapoho Crater
Kīlauea Volcano — Aerial View of Kapoho Crater
Kīlauea Volcano — Aerial View of Kapoho Crater
Kīlauea Volcano — Aerial View of Kapoho Crater

Aerial view of Kapoho Crater looking toward the south-southeast. Part of the lava channelbecame blocked just upstream of Kapoho Crater yesterday, diverting flows to the west and then south around the crater (center right). Lava exiting a crusted section of the channel continued flowing in the channel pathway (lower center to left).

Aerial view of Kapoho Crater looking toward the south-southeast. Part of the lava channelbecame blocked just upstream of Kapoho Crater yesterday, diverting flows to the west and then south around the crater (center right). Lava exiting a crusted section of the channel continued flowing in the channel pathway (lower center to left).

View of fissure 8
Kīlauea Volcano — Fissure 8 and Lava Channel
Kīlauea Volcano — Fissure 8 and Lava Channel
Kīlauea Volcano — Fissure 8 and Lava Channel

Fissure 8 and a full lava channel as seen during HVO's early morning overflight. The visible road is Nohea Street in the Leilani Estates subdivision.

Fissure 8 and a full lava channel as seen during HVO's early morning overflight. The visible road is Nohea Street in the Leilani Estates subdivision.

Aerial of lava channel
Kīlauea Volcano — Landscape Differences
Kīlauea Volcano — Landscape Differences
Kīlauea Volcano — Landscape Differences

During HVO's morning overflight today, the dramatic difference in landscapes on the northern and southern sides of the fissure 8 lava channel was readily apparent.

During HVO's morning overflight today, the dramatic difference in landscapes on the northern and southern sides of the fissure 8 lava channel was readily apparent.

Night time view of Halekamahina
Kīlauea Volcano — Looking Uprift Past Halekamahina
Kīlauea Volcano — Looking Uprift Past Halekamahina
Kīlauea Volcano — Looking Uprift Past Halekamahina

View from Bryson's quarry around 11:45 p.m. HST last night looking uprift past Halekamahina (an older ash cone) to fissure 8, which is creating the glow behind the cone.

View from Bryson's quarry around 11:45 p.m. HST last night looking uprift past Halekamahina (an older ash cone) to fissure 8, which is creating the glow behind the cone.

 Deadly Mudslides in Japan
Deadly Mudslides in Japan
Deadly Mudslides in Japan
Deadly Mudslides in Japan

Torrential rainfall swamped western Japan in July of 2018. The rain caused mudslides that flooded cities, damaged buildings and rattled the nation’s infrastructure.

Torrential rainfall swamped western Japan in July of 2018. The rain caused mudslides that flooded cities, damaged buildings and rattled the nation’s infrastructure.

Dr. Meagan Gonneea (Cape Cod, MA) retrieves a core from an infilling salt marsh pond in the Great Barnstable Marsh
Core retrieval
Core retrieval
Core retrieval

Dr. Meagan Gonneea (Cape Cod, MA) retrieves a core from an infilling salt marsh pond in the Great Barnstable Marsh.

Dr. Meagan Gonneea (Cape Cod, MA) retrieves a core from an infilling salt marsh pond in the Great Barnstable Marsh.

Lava running past a residential area
Kīlauea Volcano — Fissure 8 and Leilani Estates
Kīlauea Volcano — Fissure 8 and Leilani Estates
Kīlauea Volcano — Fissure 8 and Leilani Estates

Fissure 8 and Leilani Estates viewed from the south. Houses in the foreground are located in the southern portion of Leilani Estates.

Fissure 8 and Leilani Estates viewed from the south. Houses in the foreground are located in the southern portion of Leilani Estates.

Lava entering the ocean through steam
Kīlauea Volcano — Lava Entering Ocean
Kīlauea Volcano — Lava Entering Ocean
Kīlauea Volcano — Lava Entering Ocean

Lava entering the ocean as seen through steam and rain early this morning.

Crusted over lava flow
Kīlauea Volcano — Lower Section of Fissure 8 Flow
Kīlauea Volcano — Lower Section of Fissure 8 Flow
Kīlauea Volcano — Lower Section of Fissure 8 Flow

The lower section of the fissure 8 lava channel appears to be almost completely crusted over, and the lava level in the channel was lower during this morning's overflight.

The lower section of the fissure 8 lava channel appears to be almost completely crusted over, and the lava level in the channel was lower during this morning's overflight.

Rain over a lava flow area
Kīlauea Volcano — Rain at Leilani Estates
Kīlauea Volcano — Rain at Leilani Estates
Kīlauea Volcano — Rain at Leilani Estates

This photograph taken during this morning's overflight shows heavy, localized rain at fissure 8 in Leilani Estates.

This photograph taken during this morning's overflight shows heavy, localized rain at fissure 8 in Leilani Estates.

small ash cloud rising from a recent crater collapse
Kīlauea Volcano — Small Ash Plume at Halema`uma`u Crater
Kīlauea Volcano — Small Ash Plume at Halema`uma`u Crater
Kīlauea Volcano — Small Ash Plume at Halema`uma`u Crater

Small, ash-poor plume associated with the summit collapse explosion event at 9:20 a.m. HST. The pinkish gray plume can be seen on left side of image near the ground.

Small, ash-poor plume associated with the summit collapse explosion event at 9:20 a.m. HST. The pinkish gray plume can be seen on left side of image near the ground.

Laze plume from ocean entry
Kīlauea Volcano — Warm Ponds Ocean Entry
Kīlauea Volcano — Warm Ponds Ocean Entry
Kīlauea Volcano — Warm Ponds Ocean Entry

Southern end of the active fissure 8 flow margin north of the Analannui Park, known as the warm ponds. The flow margin is estimated to be about 500 m (0.3 mi) from the park.

Southern end of the active fissure 8 flow margin north of the Analannui Park, known as the warm ponds. The flow margin is estimated to be about 500 m (0.3 mi) from the park.

View from the sky looking at mouth of river with lots of sediment deposited at a beach.
Estero de San Antonio
Estero de San Antonio
Estero de San Antonio

Aerial view of Estero de San Antonio on Bodega Bay, near Dillon Beach, California.

Aerial view of Estero de San Antonio on Bodega Bay, near Dillon Beach, California.

animated GIF showing subsidence at a crater
Kīlauea Volcano — Animated GIF of Crater Subsidence
Kīlauea Volcano — Animated GIF of Crater Subsidence
Kīlauea Volcano — Animated GIF of Crater 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 8 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 8 at about 6:00 a.m. HST.

Aerial of braided lava channel
Kīlauea Volcano — Braided Lava Channel
Kīlauea Volcano — Braided Lava Channel
Kīlauea Volcano — Braided Lava Channel

Braided section of the lava channel located "downstream" between about 3.5 to 6 km (2.2 to 3.7 mi) from fissure 8 (upper right). The width of the two channels in the middle center is about 325 m (1,065 ft). View is toward the southwest.

Braided section of the lava channel located "downstream" between about 3.5 to 6 km (2.2 to 3.7 mi) from fissure 8 (upper right). The width of the two channels in the middle center is about 325 m (1,065 ft). View is toward the southwest.

Aerial of lava flow
Kīlauea Volcano — Kapoho Crater
Kīlauea Volcano — Kapoho Crater
Kīlauea Volcano — Kapoho Crater

View of the partially filled Kapoho Crater (center) and the open lava channel where it makes a 90-degree turn around the crater. The open channel no longer directly enters the ocean. Lava flows freely through the channel only to the southern edge of Kapoho Crater (left side of image).

View of the partially filled Kapoho Crater (center) and the open lava channel where it makes a 90-degree turn around the crater. The open channel no longer directly enters the ocean. Lava flows freely through the channel only to the southern edge of Kapoho Crater (left side of image).

Aerial view over residential area
Kīlauea Volcano — Lava Near Cape Kumukahi
Kīlauea Volcano — Lava Near Cape Kumukahi
Kīlauea Volcano — Lava Near Cape Kumukahi

Lava still oozes from the northern edge of the ‘a‘ā flow near the lighthouse at Cape Kumukahi (upper right). Smoke from burning vegetation marks location of lava oozeouts. View is toward the northeast. 

Lava still oozes from the northern edge of the ‘a‘ā flow near the lighthouse at Cape Kumukahi (upper right). Smoke from burning vegetation marks location of lava oozeouts. View is toward the northeast. 

Laze plumes
Kīlauea Volcano — Multiple Laze Plumes
Kīlauea Volcano — Multiple Laze Plumes
Kīlauea Volcano — Multiple Laze Plumes

Multiple ocean entries were active this early morning, each contributing to the prominent "laze" plume above the area. Lava moves from the open channel through the molten core of the broad ‘a‘ā flow field to the ocean. Kapoho Crater is at middle right of photo.

Multiple ocean entries were active this early morning, each contributing to the prominent "laze" plume above the area. Lava moves from the open channel through the molten core of the broad ‘a‘ā flow field to the ocean. Kapoho Crater is at middle right of photo.

Lava channel
Kīlauea Volcano — Open-Ended Lava Channel
Kīlauea Volcano — Open-Ended Lava Channel
Kīlauea Volcano — Open-Ended Lava Channel

Close view of the "end" of the open lava channel where lava moves beneath the crusted ‘a‘ā flow.

Close view of the "end" of the open lava channel where lava moves beneath the crusted ‘a‘ā flow.

Satellite differences in imagery.
The Progress of Landsat Sensor Technology
The Progress of Landsat Sensor Technology
The Progress of Landsat Sensor Technology

Landsat sensor technology has come a long way since the days of the Return Beam Vidicon cameras on the first three Landsat satellites. Known as the RBV, it was originally intended to be the satellites’ primary sensor.

Landsat sensor technology has come a long way since the days of the Return Beam Vidicon cameras on the first three Landsat satellites. Known as the RBV, it was originally intended to be the satellites’ primary sensor.