Monazite grains with rare earth elements lanthenum, cerium and neodinium are associated with zirconium, pyrite and potassium feldspar. Mineral identification performed by a combination of scanning of electron microscopy (SEM) and electron microprobe.
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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.
Monazite grains with rare earth elements lanthenum, cerium and neodinium are associated with zirconium, pyrite and potassium feldspar. Mineral identification performed by a combination of scanning of electron microscopy (SEM) and electron microprobe.
The iconic Sonoran Desert is home to many species of cactus, vascular plants, and wildlife, including the giant saguaro, cholla, and prickley pear cacti seen here. Plants and animals have adapted to living in such a harsh dry environment.
The iconic Sonoran Desert is home to many species of cactus, vascular plants, and wildlife, including the giant saguaro, cholla, and prickley pear cacti seen here. Plants and animals have adapted to living in such a harsh dry environment.
Sunset at Big Meadows in Shenandoah National Park, Virginia with tree silhouettes.
Sunset at Big Meadows in Shenandoah National Park, Virginia with tree silhouettes.
Drilling and core sampling on the Shinnecock Tribal Lands, Long Island, NY
Drilling and core sampling on the Shinnecock Tribal Lands, Long Island, NY
Examining bucket of seafloor sediment collected off southeast Alaska
Examining bucket of seafloor sediment collected off southeast AlaskaUSGS research geophysicist Danny Brothers (right) and colleagues examine the surface of a sediment grab sample just pulled onto the deck of the Canadian Coast Guard Ship John P. Tully. The sample was collected from the top of a mud volcano north of the border between southeast Alaska and British Columbia.
Examining bucket of seafloor sediment collected off southeast Alaska
Examining bucket of seafloor sediment collected off southeast AlaskaUSGS research geophysicist Danny Brothers (right) and colleagues examine the surface of a sediment grab sample just pulled onto the deck of the Canadian Coast Guard Ship John P. Tully. The sample was collected from the top of a mud volcano north of the border between southeast Alaska and British Columbia.
Legacy of Mount St. Helens 1980 eruption still defies perfect solution
Legacy of Mount St. Helens 1980 eruption still defies perfect solutionAerial view of Spirit Lake (center) looking north from above the crater of Mount St. Helens. The lake's outlet to the west (left) was blocked by the 1980 landslide, which required a new engineered outlet to maintain the lake at a safe level. A tunnel was drilled through a bedrock ridge on west side of lake in 1984-1985. Glacier covered Mount Rainier in distance.
Legacy of Mount St. Helens 1980 eruption still defies perfect solution
Legacy of Mount St. Helens 1980 eruption still defies perfect solutionAerial view of Spirit Lake (center) looking north from above the crater of Mount St. Helens. The lake's outlet to the west (left) was blocked by the 1980 landslide, which required a new engineered outlet to maintain the lake at a safe level. A tunnel was drilled through a bedrock ridge on west side of lake in 1984-1985. Glacier covered Mount Rainier in distance.
Pine Island Glacier in Antarctica has snapped off its share of icebergs in recent years. The frequency of noteworthy breaks is evidence that the ice shelf is becoming increasingly fragile. The latest iceberg cracked off the end of the Pine Island Glacier ice shelf around September 23, 2017.
Pine Island Glacier in Antarctica has snapped off its share of icebergs in recent years. The frequency of noteworthy breaks is evidence that the ice shelf is becoming increasingly fragile. The latest iceberg cracked off the end of the Pine Island Glacier ice shelf around September 23, 2017.
USGS scientists collect a sediment sample from Brownlee Reservoir
USGS scientists collect a sediment sample from Brownlee ReservoirScientists from the U.S. Geological Survey and Idaho Power Company collected water, sediment, and biological samples from Brownlee Reservoir as part of an ongoing, cooperative study of mercury cycling in the Hells Canyon complex of reservoirs along the Snake River bordering Idaho and Oregon.
USGS scientists collect a sediment sample from Brownlee Reservoir
USGS scientists collect a sediment sample from Brownlee ReservoirScientists from the U.S. Geological Survey and Idaho Power Company collected water, sediment, and biological samples from Brownlee Reservoir as part of an ongoing, cooperative study of mercury cycling in the Hells Canyon complex of reservoirs along the Snake River bordering Idaho and Oregon.
USGS WERC scientist Emily (Emma) Kelsey at False Klamath Rock
USGS WERC scientist Emily (Emma) Kelsey at False Klamath RockUSGS WERC scientist Emily (Emma) Kelsey at False Klamath Rock doing seabird monitoring research.
USGS WERC scientist Emily (Emma) Kelsey at False Klamath Rock
USGS WERC scientist Emily (Emma) Kelsey at False Klamath RockUSGS WERC scientist Emily (Emma) Kelsey at False Klamath Rock doing seabird monitoring research.
USGS WERC scientist Jonathan Felis at False Klamath Rock
USGS WERC scientist Jonathan Felis at False Klamath RockUSGS WERC scientist Jonathan Felis on False Klamath Rock doing seabird monitoring research.
USGS WERC scientist Jonathan Felis at False Klamath Rock
USGS WERC scientist Jonathan Felis at False Klamath RockUSGS WERC scientist Jonathan Felis on False Klamath Rock doing seabird monitoring research.
A boat moves off the banks of the Kootenai River in northern Idaho. Researchers from USGS EROS conducted topobathymetry surveys of the river in 2017 using LiDAR and sonar equipment.
A boat moves off the banks of the Kootenai River in northern Idaho. Researchers from USGS EROS conducted topobathymetry surveys of the river in 2017 using LiDAR and sonar equipment.
A GPS device on the banks of the Kootenai River of northern Idaho, where USGS EROS researchers conducted topobathymetry surveys in 2017 using LiDAR and sonar equipment.A GPS device on the banks of the Kootenai River of northern Idaho, where USGS EROS researchers conducted topobathymetry surveys in 2017 using LiDAR and sonar equipment.
A GPS device on the banks of the Kootenai River of northern Idaho, where USGS EROS researchers conducted topobathymetry surveys in 2017 using LiDAR and sonar equipment.A GPS device on the banks of the Kootenai River of northern Idaho, where USGS EROS researchers conducted topobathymetry surveys in 2017 using LiDAR and sonar equipment.
NYWSC scientist collecting groundwater samples
NYWSC scientist collecting groundwater samples
A view of the Kootenai River in northern Idaho from a boat. USGS EROS researchers conducted topobathymetry surveys of the river in 2017 using LiDAR and sonar equipment.
A view of the Kootenai River in northern Idaho from a boat. USGS EROS researchers conducted topobathymetry surveys of the river in 2017 using LiDAR and sonar equipment.
Pelicans on a rock, observed by the USGS Western Ecological Center Seabird Studies team.
Pelicans on a rock, observed by the USGS Western Ecological Center Seabird Studies team.
Sockeye salmon preparing to spawn upstream of Cle Elum Dam, Washington.
Sockeye salmon preparing to spawn upstream of Cle Elum Dam, Washington.
Colonies of the Bacteria Bacillus Globigii on a Petri Dish
Colonies of the Bacteria Bacillus Globigii on a Petri DishScientists optimized existing methods to collect and identify microorganisms including Bacillus anthracis, a pathogenic microorganism, in 4,800 soil samples across the United States, and developed a
Colonies of the Bacteria Bacillus Globigii on a Petri Dish
Colonies of the Bacteria Bacillus Globigii on a Petri DishScientists optimized existing methods to collect and identify microorganisms including Bacillus anthracis, a pathogenic microorganism, in 4,800 soil samples across the United States, and developed a
Fog surrounds the USGS Research Vessel Arcticus as it comes into port at Sturgeon Bay, Wisconsin.
Fog surrounds the USGS Research Vessel Arcticus as it comes into port at Sturgeon Bay, Wisconsin.
Collecting a piston core of seafloor sediment off British Columbia
Collecting a piston core of seafloor sediment off British ColumbiaScientists prepare to lower a piston corer off Haida Gwaii, British Columbia, to sample seafloor sediment near the Queen Charlotte-Fairweather fault. Expedition scientists are studying layers of sediment in the cores they collected to identify and determine ages of past earthquakes along the fault.
Collecting a piston core of seafloor sediment off British Columbia
Collecting a piston core of seafloor sediment off British ColumbiaScientists prepare to lower a piston corer off Haida Gwaii, British Columbia, to sample seafloor sediment near the Queen Charlotte-Fairweather fault. Expedition scientists are studying layers of sediment in the cores they collected to identify and determine ages of past earthquakes along the fault.
Microscopic video imaging is used for computerized analysis of sperm m
Microscopic video imaging is used for computerized analysis of sperm mPhotomicroscopy and Flow Cytometry Laboratory — Lafayette, Louisiana. Microscopic video imaging is used for computerized analysis of sperm motility parameters
Microscopic video imaging is used for computerized analysis of sperm m
Microscopic video imaging is used for computerized analysis of sperm mPhotomicroscopy and Flow Cytometry Laboratory — Lafayette, Louisiana. Microscopic video imaging is used for computerized analysis of sperm motility parameters
Top: Map view of well recorded historical seismicity at Mount Rainier since 2007 (gray circles) with seismicity since September 11 plotted as filled red circles. Location of seismic stations indicated by arrows. Bottom: Cross-sectional view looking north shows earthquake depths. Black outline is a west-east elevation profile of Mount Rainier.
Top: Map view of well recorded historical seismicity at Mount Rainier since 2007 (gray circles) with seismicity since September 11 plotted as filled red circles. Location of seismic stations indicated by arrows. Bottom: Cross-sectional view looking north shows earthquake depths. Black outline is a west-east elevation profile of Mount Rainier.