This map shows the distribution of select Conservation Reserve Program (CRP) fields for on-site assessments.
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Select CRP fields for on-site assessments
This map shows the distribution of select Conservation Reserve Program (CRP) fields for on-site assessments.
Survey Requirements - Road Overflow/Broad-Crested Weir
Survey Requirements - Road Overflow/Broad-Crested WeirThis video describes how and where to flag high water marks for a road overflow or broad-crested weir indirect measurement of peak discharge.
Survey Requirements - Road Overflow/Broad-Crested Weir
Survey Requirements - Road Overflow/Broad-Crested WeirThis video describes how and where to flag high water marks for a road overflow or broad-crested weir indirect measurement of peak discharge.
USDA Conservation Reserve Program (CRP) field planted for pollinators
USDA Conservation Reserve Program (CRP) field planted for pollinatorsUSDA Conservation Reserve Program (CRP) field planted for pollinators
USDA Conservation Reserve Program (CRP) field planted for pollinators
USDA Conservation Reserve Program (CRP) field planted for pollinatorsUSDA Conservation Reserve Program (CRP) field planted for pollinators
USGS scientist conducting agricultural research
USGS scientist conducting agricultural research
USGS scientist conducting agricultural research
USGS Status Update of Kīlauea Volcano - June 1, 2018
USGS Status Update of Kīlauea Volcano - June 1, 2018USGS Hawaiian Volcano Observatory
Status of Kīlauea Volcano
June 1, 2018
Jessica Ball, USGS Volcanologist
USGS Status Update of Kīlauea Volcano - June 1, 2018
USGS Status Update of Kīlauea Volcano - June 1, 2018USGS Hawaiian Volcano Observatory
Status of Kīlauea Volcano
June 1, 2018
Jessica Ball, USGS Volcanologist
Using telemetry to track movement, habitat use and dispersal of frogs
Using telemetry to track movement, habitat use and dispersal of frogsUsing telemetry to track movement, habitat use and dispersal of frogs in an Iowa wetland.
Using telemetry to track movement, habitat use and dispersal of frogs
Using telemetry to track movement, habitat use and dispersal of frogsUsing telemetry to track movement, habitat use and dispersal of frogs in an Iowa wetland.
Evaluating the Effectiveness of Fish Rescue Programs
Evaluating the Effectiveness of Fish Rescue ProgramsA unique effort to seasonally translocate fish, termed “fish rescue”, has quietly emerged in the Pacific Northwest as a way to reduce drought related mortality in wild fish by manually moving individuals from fragmented areas to either free-flowing habitat or artificial rearing facilities, providing refuge during periods of low flow.
Evaluating the Effectiveness of Fish Rescue Programs
Evaluating the Effectiveness of Fish Rescue ProgramsA unique effort to seasonally translocate fish, termed “fish rescue”, has quietly emerged in the Pacific Northwest as a way to reduce drought related mortality in wild fish by manually moving individuals from fragmented areas to either free-flowing habitat or artificial rearing facilities, providing refuge during periods of low flow.
Halema‘uma‘u at the summit of Kīlauea Volcano captured from an Unmanne
Halema‘uma‘u at the summit of Kīlauea Volcano captured from an UnmanneAn aerial view of Halema‘uma‘u at the summit of Kīlauea Volcano captured from an Unmanned Aircraft Systems (UAS) overflight video on May 31, 2018. Limited UAS flights into this hazardous area are conducted with permission and coordination with Hawai‘i Volcanoes National Park to collect visual information on this changing eruption site.
Halema‘uma‘u at the summit of Kīlauea Volcano captured from an Unmanne
Halema‘uma‘u at the summit of Kīlauea Volcano captured from an UnmanneAn aerial view of Halema‘uma‘u at the summit of Kīlauea Volcano captured from an Unmanned Aircraft Systems (UAS) overflight video on May 31, 2018. Limited UAS flights into this hazardous area are conducted with permission and coordination with Hawai‘i Volcanoes National Park to collect visual information on this changing eruption site.
Jersey Shore Field Work
Deployment of an Edgetech 512i subbottom profiler from the deck of Stockton University's R/V Petrel near Little Egg Inlet, NJ. The USGS Coastal and Marine Geology Program is working to characterize the sea floor and shallow substrate in nearshore waters, using high-resolution geophysical techniques, sediment sampling, and sea-floor photography and videography.
Deployment of an Edgetech 512i subbottom profiler from the deck of Stockton University's R/V Petrel near Little Egg Inlet, NJ. The USGS Coastal and Marine Geology Program is working to characterize the sea floor and shallow substrate in nearshore waters, using high-resolution geophysical techniques, sediment sampling, and sea-floor photography and videography.
Kīlauea LERZ Fissures and Flows, May 31, 2:00 p.m.
Kīlauea LERZ Fissures and Flows, May 31, 2:00 p.m.Map as of 2:00 p.m. HST, May 31, 2018. Given the dynamic nature of Kīlauea's lower East Rift Zone eruption, with changing vent locations, fissures starting and stopping, and varying rates of lava effusion, map details shown here are accurate as of the date/time noted. Shaded purple areas indicate lava flows erupted in 1840, 1955, 1960, and 2014-2015.
Kīlauea LERZ Fissures and Flows, May 31, 2:00 p.m.
Kīlauea LERZ Fissures and Flows, May 31, 2:00 p.m.Map as of 2:00 p.m. HST, May 31, 2018. Given the dynamic nature of Kīlauea's lower East Rift Zone eruption, with changing vent locations, fissures starting and stopping, and varying rates of lava effusion, map details shown here are accurate as of the date/time noted. Shaded purple areas indicate lava flows erupted in 1840, 1955, 1960, and 2014-2015.
Kīlauea LERZ Fissures and Flows, May 31, 9:00 a.m.
Kīlauea LERZ Fissures and Flows, May 31, 9:00 a.m.Map as of 9:00 a.m. HST, May 31, 2018. Given the dynamic nature of Kīlauea lower East Rift Zone eruption, with changing vent locations, fissures starting and stopping, and varying rates of lava effusion, map details shown here are accurate as of the date/time noted. Shaded purple areas indicate lava flows erupted in 1840, 1955, 1960, and 2014-2015.
Kīlauea LERZ Fissures and Flows, May 31, 9:00 a.m.
Kīlauea LERZ Fissures and Flows, May 31, 9:00 a.m.Map as of 9:00 a.m. HST, May 31, 2018. Given the dynamic nature of Kīlauea lower East Rift Zone eruption, with changing vent locations, fissures starting and stopping, and varying rates of lava effusion, map details shown here are accurate as of the date/time noted. Shaded purple areas indicate lava flows erupted in 1840, 1955, 1960, and 2014-2015.
Kīlauea Volcano — Advancing Lobes from Fissure 8
Helicopter overflight shows advancing lobes from fissure 8 (fissure 8 is not pictured but located to the right, out of view). Advance rates were less than 100 yards per hour for the three lobes of the flow, as measured during the overnight hours.
Helicopter overflight shows advancing lobes from fissure 8 (fissure 8 is not pictured but located to the right, out of view). Advance rates were less than 100 yards per hour for the three lobes of the flow, as measured during the overnight hours.
Kīlauea Volcano — Early Morning Fissure 8 Activity
Kīlauea Volcano — Early Morning Fissure 8 ActivityCrews make visual observations of activity at fissure 8 around 5:30 a.m. HST. Fountain heights this morning continue to reach 70 to 80 m (230 to 260 ft) above ground level.
Kīlauea Volcano — Early Morning Fissure 8 Activity
Kīlauea Volcano — Early Morning Fissure 8 ActivityCrews make visual observations of activity at fissure 8 around 5:30 a.m. HST. Fountain heights this morning continue to reach 70 to 80 m (230 to 260 ft) above ground level.
Kīlauea Volcano — Fissure 18 Lava Flow
Lava from fissure 18 travels to the southeast (lower left of photo). The flow front that had approached the ocean yesterday has stalled. This view is looking uprift, with fissure 8 in the distance (upper right of photo).
Lava from fissure 18 travels to the southeast (lower left of photo). The flow front that had approached the ocean yesterday has stalled. This view is looking uprift, with fissure 8 in the distance (upper right of photo).
Kīlauea Volcano — Halema‘uma‘u Crater Changes
A UAS mission on May 31, 2018, filmed details of the dramatic changes occurring within Halema‘uma‘u crater at Kīlauea's summit since explosive eruptions of ash and gas and ongoing wall collapse bega
A UAS mission on May 31, 2018, filmed details of the dramatic changes occurring within Halema‘uma‘u crater at Kīlauea's summit since explosive eruptions of ash and gas and ongoing wall collapse bega
Kīlauea Volcano — Lava on Kahukai Street
Lava from fissure 8 advances on Kahukai Street. Lava in this area is as much as 3.5 yards in height.
Lava from fissure 8 advances on Kahukai Street. Lava in this area is as much as 3.5 yards in height.
Landsat in Action - Land Cover and Land Cover Change with Tom Loveland
Landsat in Action - Land Cover and Land Cover Change with Tom LovelandTom Loveland talks about using Landsat's data for land use and land cover change research.
Find this video and thousands more at https://usgs.gov/gallery.
Landsat in Action - Land Cover and Land Cover Change with Tom Loveland
Landsat in Action - Land Cover and Land Cover Change with Tom LovelandTom Loveland talks about using Landsat's data for land use and land cover change research.
Find this video and thousands more at https://usgs.gov/gallery.
Pele's Hair
This long thin, strand of volcanic glass is called Pele's hair. Named for Pele, the Hawaiian goddess of fire, Pele's hair is formed from lava fountains and rapidly moving lava flows. This strand of Pele’s hair was found on Kupono Street in Leilani Estates, Hawaii, during the Kīlauea volcano eruption.
This long thin, strand of volcanic glass is called Pele's hair. Named for Pele, the Hawaiian goddess of fire, Pele's hair is formed from lava fountains and rapidly moving lava flows. This strand of Pele’s hair was found on Kupono Street in Leilani Estates, Hawaii, during the Kīlauea volcano eruption.
PubTalk 5/2018 — Yes Humans really are causing induced earthquakes
PubTalk 5/2018 — Yes Humans really are causing induced earthquakesTitle: Yes, Humans Really Are Causing Earthquakes! How Energy Industry Practices are Causing Earthquakes in America's Heartland
PubTalk 5/2018 — Yes Humans really are causing induced earthquakes
PubTalk 5/2018 — Yes Humans really are causing induced earthquakesTitle: Yes, Humans Really Are Causing Earthquakes! How Energy Industry Practices are Causing Earthquakes in America's Heartland
USGS Status Update of Kīlauea Volcano - May 31, 2018
USGS Status Update of Kīlauea Volcano - May 31, 2018USGS Hawaiian Volcano Observatory status of Kilauea volcano in Hawaii on May 31, 2018.
USGS Status Update of Kīlauea Volcano - May 31, 2018
USGS Status Update of Kīlauea Volcano - May 31, 2018USGS Hawaiian Volcano Observatory status of Kilauea volcano in Hawaii on May 31, 2018.
Kīlauea LERZ Fissures and Flows, May 30, 3:00 p.m.
Kīlauea LERZ Fissures and Flows, May 30, 3:00 p.m.Map as of 3:00 p.m. HST, May 30, 2018. Given the dynamic nature of Kīlauea's lower East Rift Zone eruption, with changing vent locations, fissures starting and stopping, and varying rates of lava effusion, map details shown here are accurate as of the date/time noted. Shaded purple areas indicate lava flows erupted in 1840, 1955, 1960, and 2014-2015.
Kīlauea LERZ Fissures and Flows, May 30, 3:00 p.m.
Kīlauea LERZ Fissures and Flows, May 30, 3:00 p.m.Map as of 3:00 p.m. HST, May 30, 2018. Given the dynamic nature of Kīlauea's lower East Rift Zone eruption, with changing vent locations, fissures starting and stopping, and varying rates of lava effusion, map details shown here are accurate as of the date/time noted. Shaded purple areas indicate lava flows erupted in 1840, 1955, 1960, and 2014-2015.