Scientists from the USGS Woods Hole Coastal and Marine Science Center using a helium powered kite-balloon at Head of the Meadow Beach and Marconi Beach, Cape Cod National Seashore in Massachusetts.
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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.
Scientists from the USGS Woods Hole Coastal and Marine Science Center using a helium powered kite-balloon at Head of the Meadow Beach and Marconi Beach, Cape Cod National Seashore in Massachusetts.
In February of 2021, scientists from the USGS Woods Hole Coastal and Marine Science Center and Woods Hole Oceanographic Institution (WHOI) conducted near-shore bathymetric surveys on Cape Cod National Seashore. Bathymetry is the study of underwater depth of ocean floors or lake floors.
In February of 2021, scientists from the USGS Woods Hole Coastal and Marine Science Center and Woods Hole Oceanographic Institution (WHOI) conducted near-shore bathymetric surveys on Cape Cod National Seashore. Bathymetry is the study of underwater depth of ocean floors or lake floors.
Scientists from the USGS Woods Hole Coastal and Marine Science Center using a helium powered kite-balloon at Head of the Meadow Beach and Marconi Beach, Cape Cod National Seashore in Massachusetts.
Scientists from the USGS Woods Hole Coastal and Marine Science Center using a helium powered kite-balloon at Head of the Meadow Beach and Marconi Beach, Cape Cod National Seashore in Massachusetts.
Scientists from the USGS Woods Hole Coastal and Marine Science Center using a helium powered kite-balloon at Head of the Meadow Beach and Marconi Beach, Cape Cod National Seashore in Massachusetts.
Scientists from the USGS Woods Hole Coastal and Marine Science Center using a helium powered kite-balloon at Head of the Meadow Beach and Marconi Beach, Cape Cod National Seashore in Massachusetts.
Scientists from the USGS Woods Hole Coastal and Marine Science Center using a helium powered kite-balloon at Head of the Meadow Beach and Marconi Beach, Cape Cod National Seashore in Massachusetts.
Scientists from the USGS Woods Hole Coastal and Marine Science Center using a helium powered kite-balloon at Head of the Meadow Beach and Marconi Beach, Cape Cod National Seashore in Massachusetts.
Scientists from the USGS Woods Hole Coastal and Marine Science Center using a helium powered kite-balloon at Head of the Meadow Beach and Marconi Beach, Cape Cod National Seashore in Massachusetts.
Scientists from the USGS Woods Hole Coastal and Marine Science Center using a helium powered kite-balloon at Head of the Meadow Beach and Marconi Beach, Cape Cod National Seashore in Massachusetts.
Property damage caused by a large NorEaster Storm, Sandwich, MA February 2021
Property damage caused by a large NorEaster Storm, Sandwich, MA February 2021
A large NorEaster Storm caused extensive property damage along the beach ,Sandwich, MA February 2021
A large NorEaster Storm caused extensive property damage along the beach ,Sandwich, MA February 2021
Photo Contest Winner | February 2021 | Where We Work
North Fork Patapsco River
Photo Contest Winner | February 2021 | Where We Work
North Fork Patapsco River
Overflight of Halema‘uma‘u crater—Kīlauea summit Feb. 1
Overflight of Halema‘uma‘u crater—Kīlauea summit Feb. 1An aerial view of Halema‘uma‘u crater from the northeast during a helicopter overflight of the Kīlauea summit eruption on February 1. The dull black color on the eastern (lower left) portion of the lava lake is the inactive surface.
Overflight of Halema‘uma‘u crater—Kīlauea summit Feb. 1
Overflight of Halema‘uma‘u crater—Kīlauea summit Feb. 1An aerial view of Halema‘uma‘u crater from the northeast during a helicopter overflight of the Kīlauea summit eruption on February 1. The dull black color on the eastern (lower left) portion of the lava lake is the inactive surface.
Rockfall debris on lava lake surface crust—Kīlauea summit eruption
Rockfall debris on lava lake surface crust—Kīlauea summit eruptionRockfalls have been a frequent occurrence in Halema‘uma‘u crater, both before and during the current eruption. Debris from a recent rockfall can be seen sitting on the solidified lava lake crust (center). The crust on the southern edge of the lava lake is thick enough to support the weight of the boulders that have fallen. USGS photo taken by B.
Rockfall debris on lava lake surface crust—Kīlauea summit eruption
Rockfall debris on lava lake surface crust—Kīlauea summit eruptionRockfalls have been a frequent occurrence in Halema‘uma‘u crater, both before and during the current eruption. Debris from a recent rockfall can be seen sitting on the solidified lava lake crust (center). The crust on the southern edge of the lava lake is thick enough to support the weight of the boulders that have fallen. USGS photo taken by B.
Photo Contest Winner | February 2021 | People
Scouting Marconi Beach
Photo Contest Winner | February 2021 | People
Scouting Marconi Beach
Woods Hole Coastal and Marine Center scientists prepare to deploy a seafloor tripod loaded with oceanographic equipment offshore of Sandwich, MA , March 2021
Woods Hole Coastal and Marine Center scientists prepare to deploy a seafloor tripod loaded with oceanographic equipment offshore of Sandwich, MA , March 2021
In February of 2021, scientists from the USGS Woods Hole Coastal and Marine Science Center and Woods Hole Oceanographic Institution (WHOI) conducted near-shore bathymetric surveys on Cape Cod National Seashore. Bathymetry is the study of underwater depth of ocean floors or lake floors.
In February of 2021, scientists from the USGS Woods Hole Coastal and Marine Science Center and Woods Hole Oceanographic Institution (WHOI) conducted near-shore bathymetric surveys on Cape Cod National Seashore. Bathymetry is the study of underwater depth of ocean floors or lake floors.
The United States continues to rely on foreign sources for some raw and processed mineral materials, including some critical minerals. This map shows the countries that supply mineral commodities for which the United States was more than 50% net import reliant in 2020.
The United States continues to rely on foreign sources for some raw and processed mineral materials, including some critical minerals. This map shows the countries that supply mineral commodities for which the United States was more than 50% net import reliant in 2020.
A close-up view of the main island in Halema‘uma‘u
A close-up view of the main island in Halema‘uma‘uA close-up view of the main island near the center of the lava lake in Halema‘uma‘u. All the islands have been stationary since approximately January 10. USGS photo by M. Patrick.
A close-up view of the main island in Halema‘uma‘u
A close-up view of the main island in Halema‘uma‘uA close-up view of the main island near the center of the lava lake in Halema‘uma‘u. All the islands have been stationary since approximately January 10. USGS photo by M. Patrick.
A close-up view of the western fissure in Halema‘uma‘u crater
A close-up view of the western fissure in Halema‘uma‘u craterA close-up view of the western fissure, which is supplying lava to the lava lake in Halema‘uma‘u crater. A slow-moving lava stream marked the inlet where lava entered the lake. Several incandescent openings remain over the vent region. USGS photo by M. Patrick.
A close-up view of the western fissure in Halema‘uma‘u crater
A close-up view of the western fissure in Halema‘uma‘u craterA close-up view of the western fissure, which is supplying lava to the lava lake in Halema‘uma‘u crater. A slow-moving lava stream marked the inlet where lava entered the lake. Several incandescent openings remain over the vent region. USGS photo by M. Patrick.
A view of the central region of the lava lake in Halema‘uma‘u. On the left is the main island. In the center, a lobe of surface lava is moving south (towards the bottom of the photo) as surface crust founders along its leading edge.
A view of the central region of the lava lake in Halema‘uma‘u. On the left is the main island. In the center, a lobe of surface lava is moving south (towards the bottom of the photo) as surface crust founders along its leading edge.
Close-up view of surface lava—Halema‘uma‘u lava lake, Kīlauea summit
Close-up view of surface lava—Halema‘uma‘u lava lake, Kīlauea summitA close-up view of the leading edge of the active lobe of surface lava slowly moving south in the central part of the Halema‘uma‘u lava lake. USGS photo by M. Patrick.
Close-up view of surface lava—Halema‘uma‘u lava lake, Kīlauea summit
Close-up view of surface lava—Halema‘uma‘u lava lake, Kīlauea summitA close-up view of the leading edge of the active lobe of surface lava slowly moving south in the central part of the Halema‘uma‘u lava lake. USGS photo by M. Patrick.
Rilling and a shallow landslide in CZU Fire near Eagle Rock, California. Soil ~3 cm below surface was almost completely dry after the rain storm, highlighting soil water repellancy.
Rilling and a shallow landslide in CZU Fire near Eagle Rock, California. Soil ~3 cm below surface was almost completely dry after the rain storm, highlighting soil water repellancy.
Eruptive activity continues in Halema‘uma‘u crater, at Kīlauea summit
Eruptive activity continues in Halema‘uma‘u crater, at Kīlauea summitEruptive activity continues in Halema‘uma‘u crater, at the summit of Kīlauea. The active surface lava remains largely confined to the western (left) portion of the lava lake. As of the afternoon of January 31 lava had filled about 212 m (695 ft) of Halemaʻumaʻu in the active western portion of the lava lake. USGS photo by M. Patrick.
Eruptive activity continues in Halema‘uma‘u crater, at Kīlauea summit
Eruptive activity continues in Halema‘uma‘u crater, at Kīlauea summitEruptive activity continues in Halema‘uma‘u crater, at the summit of Kīlauea. The active surface lava remains largely confined to the western (left) portion of the lava lake. As of the afternoon of January 31 lava had filled about 212 m (695 ft) of Halemaʻumaʻu in the active western portion of the lava lake. USGS photo by M. Patrick.