Sluggish pāhoehoe briefly spills over a section the levee along the well-established lava channel. Such overflows generally travel short distances measured in meters (yards).
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Sluggish pāhoehoe briefly spills over a section the levee along the well-established lava channel. Such overflows generally travel short distances measured in meters (yards).
HVO geologist measures 260 degrees C (500 degrees F) along ground cracks near fissure 10 in Leilani Estates. Geologists routinely make temperature measurements to track changes throughout the fissure complex in the lower East Rift Zone.
HVO geologist measures 260 degrees C (500 degrees F) along ground cracks near fissure 10 in Leilani Estates. Geologists routinely make temperature measurements to track changes throughout the fissure complex in the lower East Rift Zone.
Map of the U.S. by state, showing total water withdrawals, 2015
Map of the U.S. by state, showing total water withdrawals, 2015Map of the U.S. by state, showing total water withdrawals, 2015
Map of the U.S. by state, showing total water withdrawals, 2015
Map of the U.S. by state, showing total water withdrawals, 2015Map of the U.S. by state, showing total water withdrawals, 2015
Source and Use of Freshwater in the United States, 2015
This diagram uses a "cylinder and pipe" layout to show the source (surface water or groundwater) of the Nation's freshwater and for what purposes the water was used in 2015. The data are broken out for each category of use by surface water and groundwater as the source.
Source and Use of Freshwater in the United States, 2015
This diagram uses a "cylinder and pipe" layout to show the source (surface water or groundwater) of the Nation's freshwater and for what purposes the water was used in 2015. The data are broken out for each category of use by surface water and groundwater as the source.
A spawning Yukon River Chinook salmon (Oncorhynchus tshawytscha) captured near Pilot Station, Alaska, in June 2018 as part of an experimental temperature manipulation study to validate heat stress biomarkers.
A spawning Yukon River Chinook salmon (Oncorhynchus tshawytscha) captured near Pilot Station, Alaska, in June 2018 as part of an experimental temperature manipulation study to validate heat stress biomarkers.
Verification of High Water Mark on Whitewood Creek above Whitewood, SD
Verification of High Water Mark on Whitewood Creek above Whitewood, SDOn June 20, 2018, hydrologic technician Kammy Durham verified the high water mark on Whitewood Creek above Whitewood, SD (streamgage 06436180) after the watershed received about 2 inches of rain the previous evening. Streams in the Black Hills of western South Dakota can rise and fall quickly in response to rain.
Verification of High Water Mark on Whitewood Creek above Whitewood, SD
Verification of High Water Mark on Whitewood Creek above Whitewood, SDOn June 20, 2018, hydrologic technician Kammy Durham verified the high water mark on Whitewood Creek above Whitewood, SD (streamgage 06436180) after the watershed received about 2 inches of rain the previous evening. Streams in the Black Hills of western South Dakota can rise and fall quickly in response to rain.
USGS employees measuring WInd River streamflows at Kinnear bridge soon after minor flooding had occurred on the highway.
USGS employees measuring WInd River streamflows at Kinnear bridge soon after minor flooding had occurred on the highway.
Der Wasserkreislauf für Kinder - The Water Cycle for Schools, German
Der Wasserkreislauf für Kinder - The Water Cycle for Schools, GermanDer Wasserkreislauf für Kinder
Du denkst vielleicht, jeder Regentropfen, der vom Himmel fällt, oder jedes Glas Wasser, das du trinkst, ist nagelneu, aber das asser ist schon immer da, und es ist Teil des Wasserkreislaufs.
Der Wasserkreislauf für Kinder - The Water Cycle for Schools, German
Der Wasserkreislauf für Kinder - The Water Cycle for Schools, GermanDer Wasserkreislauf für Kinder
Du denkst vielleicht, jeder Regentropfen, der vom Himmel fällt, oder jedes Glas Wasser, das du trinkst, ist nagelneu, aber das asser ist schon immer da, und es ist Teil des Wasserkreislaufs.
A thick, dense plume of SO2 and other volcanic gases billows from the lava fountains at fissure 8 on June 19, 2018. SO2 emission rates during the 2018 eruption of Kīlauea were so high that they required a new data analysis technique.
A thick, dense plume of SO2 and other volcanic gases billows from the lava fountains at fissure 8 on June 19, 2018. SO2 emission rates during the 2018 eruption of Kīlauea were so high that they required a new data analysis technique.
Kīlauea LERZ lava flows and fissures, June 19, 1:00 p.m.
Kīlauea LERZ lava flows and fissures, June 19, 1:00 p.m.Map as of 1:00 p.m. HST, June 19, 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 lava flows and fissures, June 19, 1:00 p.m.
Kīlauea LERZ lava flows and fissures, June 19, 1:00 p.m.Map as of 1:00 p.m. HST, June 19, 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 Volcano — Fissure 8 Eruption (June 18-19, 2018)
Kīlauea Volcano — Fissure 8 Eruption (June 18-19, 2018)Fissure 8 vigor increased overnight June 18-19 with lava fountains reaching up to 60 m (200 ft). Spatter built up the cone to the east and into the channel.
Kīlauea Volcano — Fissure 8 Eruption (June 18-19, 2018)
Kīlauea Volcano — Fissure 8 Eruption (June 18-19, 2018)Fissure 8 vigor increased overnight June 18-19 with lava fountains reaching up to 60 m (200 ft). Spatter built up the cone to the east and into the channel.
Fissure 8 cone, lava fountain, and channelized lava flow on the morning overflight - June 19 at about 6:10am HST. The lava channel is very full with many small overflows visible on the channel margins. Overflows are sluggish and move slowly downslope as they build up the levees.
Fissure 8 cone, lava fountain, and channelized lava flow on the morning overflight - June 19 at about 6:10am HST. The lava channel is very full with many small overflows visible on the channel margins. Overflows are sluggish and move slowly downslope as they build up the levees.
The northern channel margin of the fissure 8 lava flow. Small hill in the distance is the site of our PGcam. Overflows from the channel can be seen producing shiny black to silver pahoehoeflows (incandescent red breakout visible in center of photo).
The northern channel margin of the fissure 8 lava flow. Small hill in the distance is the site of our PGcam. Overflows from the channel can be seen producing shiny black to silver pahoehoeflows (incandescent red breakout visible in center of photo).
Kīlauea Volcano — Morning Overflight (June 19, 2018)
Kīlauea Volcano — Morning Overflight (June 19, 2018)Relict Acropora palmata coral-reef framework in the Dry Tortugas
Relict Acropora palmata coral-reef framework in the Dry TortugasAcropora palmata coral-reef framework in the Dry Tortugas National Park, Florida Keys built more than 3000 years ago. That framework, which serves as the foundation for all of the critical ecosystem services reefs provide to society, is now rapidly eroding away.
Relict Acropora palmata coral-reef framework in the Dry Tortugas
Relict Acropora palmata coral-reef framework in the Dry TortugasAcropora palmata coral-reef framework in the Dry Tortugas National Park, Florida Keys built more than 3000 years ago. That framework, which serves as the foundation for all of the critical ecosystem services reefs provide to society, is now rapidly eroding away.
Relict Holocene coral-reef framework in the Dry Tortugas National Park
Relict Holocene coral-reef framework in the Dry Tortugas National ParkRelict Holocene coral-reef framework in the Florida Keys. Like many reefs in the western Atlantic, reefs here were just a few coral species: primary Acropora palmata and Orbicella spp. Recent disturbances have led to declines in the populations of those corals and relative increases in the abundance of more weedy taxa.
Relict Holocene coral-reef framework in the Dry Tortugas National Park
Relict Holocene coral-reef framework in the Dry Tortugas National ParkRelict Holocene coral-reef framework in the Florida Keys. Like many reefs in the western Atlantic, reefs here were just a few coral species: primary Acropora palmata and Orbicella spp. Recent disturbances have led to declines in the populations of those corals and relative increases in the abundance of more weedy taxa.
Source and Use of Water in the United States, 2015
This diagram uses a "cylinder and pipe" layout to show the source (surface water or groundwater) of the Nation's water and for what purposes the water was used in 2015. The data are broken out for each category of use by surface water and groundwater as the source.
Source and Use of Water in the United States, 2015
This diagram uses a "cylinder and pipe" layout to show the source (surface water or groundwater) of the Nation's water and for what purposes the water was used in 2015. The data are broken out for each category of use by surface water and groundwater as the source.
Kīlauea LERZ lava flows and fissures, June 18, 9:00 a.m.
Kīlauea LERZ lava flows and fissures, June 18, 9:00 a.m.Map as of 9:00 a.m. HST, June 18, 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 lava flows and fissures, June 18, 9:00 a.m.
Kīlauea LERZ lava flows and fissures, June 18, 9:00 a.m.Map as of 9:00 a.m. HST, June 18, 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.
Fissure 8 lava fountains obscured by a longer exposure photograph taken early morning on June 18. The incandescent spots along a horizontal line mark the edge of the lava channel.
Fissure 8 lava fountains obscured by a longer exposure photograph taken early morning on June 18. The incandescent spots along a horizontal line mark the edge of the lava channel.
Fissure 6 (photo center) showed signs of activity overnight, producing small amounts of spatter and feeding short lava flows. Fissure 6 is located about 2.2 km (1.4 mi) downrift from Fissure 8.
Fissure 6 (photo center) showed signs of activity overnight, producing small amounts of spatter and feeding short lava flows. Fissure 6 is located about 2.2 km (1.4 mi) downrift from Fissure 8.