The June 27th flow remains active, but surface flows at the very farthest reaches of the flow appear to have stalled today. The lava flow front consisted of an isolated pad of lava that emerged from a deep ground crack several days ago. Today, this pad of lava appeared inactive at the surface, with no sign obvious activity in the adjacent crack.
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The June 27th flow remains active, but surface flows at the very farthest reaches of the flow appear to have stalled today. The lava flow front consisted of an isolated pad of lava that emerged from a deep ground crack several days ago. Today, this pad of lava appeared inactive at the surface, with no sign obvious activity in the adjacent crack.
south lobe of the June 27th flow, which plunged into a deep ground ...
south lobe of the June 27th flow, which plunged into a deep ground ...Another view of the south lobe of the June 27th flow, which plunged into a deep ground crack last week (this spot is visible at the right side of the photograph). This wide view, looking west, also shows another deep crack nearby, a short distance to the south of the active flows (which are producing the smoke plumes).
south lobe of the June 27th flow, which plunged into a deep ground ...
south lobe of the June 27th flow, which plunged into a deep ground ...Another view of the south lobe of the June 27th flow, which plunged into a deep ground crack last week (this spot is visible at the right side of the photograph). This wide view, looking west, also shows another deep crack nearby, a short distance to the south of the active flows (which are producing the smoke plumes).
USGS summer geology interns Alexandra Pickering and Nikita Avdievitch collecting topographic data with a three-dimensional laser scanner on August 26. Surface rupture from the 2014 South Napa Earthquake is visible in the foreground
USGS summer geology interns Alexandra Pickering and Nikita Avdievitch collecting topographic data with a three-dimensional laser scanner on August 26. Surface rupture from the 2014 South Napa Earthquake is visible in the foreground
MultiGAS monitoring station inside crater of Mount St. Helens
MultiGAS monitoring station inside crater of Mount St. HelensThe new volcanic-gas monitoring station installed at Mount St. Helens consists of weather monitoring equipment and sensors for measuring the concentrations of water vapor (H2O), carbon dioxide (CO2), sulfur dioxide (SO2), and hydrogen sulfide (H2S) in volcanic gas plumes.
MultiGAS monitoring station inside crater of Mount St. Helens
MultiGAS monitoring station inside crater of Mount St. HelensThe new volcanic-gas monitoring station installed at Mount St. Helens consists of weather monitoring equipment and sensors for measuring the concentrations of water vapor (H2O), carbon dioxide (CO2), sulfur dioxide (SO2), and hydrogen sulfide (H2S) in volcanic gas plumes.
Lava resurfaces along crack, continues advancing through thick forest
Lava resurfaces along crack, continues advancing through thick forestThe leading edge of the June 27th lava flow plunged into a deep crack on Kīlauea's East Rift Zone last week, and lava within the crack remained hidden for several days. Over the past day, lava returned to the surface at a point slightly farther along the crack, creating a small island of lava surrounded by thick forest.
Lava resurfaces along crack, continues advancing through thick forest
Lava resurfaces along crack, continues advancing through thick forestThe leading edge of the June 27th lava flow plunged into a deep crack on Kīlauea's East Rift Zone last week, and lava within the crack remained hidden for several days. Over the past day, lava returned to the surface at a point slightly farther along the crack, creating a small island of lava surrounded by thick forest.
Seismic Lab aboard R/V Marcus G. Langseth
Seismic Lab aboard R/V Marcus G. Langseth
View of the pad of lava with the equivalent view from a thermal camera
View of the pad of lava with the equivalent view from a thermal cameraView of the pad of lava with the equivalent view from a thermal camera.
View of the pad of lava with the equivalent view from a thermal camera
View of the pad of lava with the equivalent view from a thermal cameraView of the pad of lava with the equivalent view from a thermal camera.
Pu‘u ‘Ō‘ō remains partly obscured by thick fume. In particular, th...
Pu‘u ‘Ō‘ō remains partly obscured by thick fume. In particular, th...Pu‘u ‘Ō‘ō crater remains partly obscured by thick fume. In particular, the northeastern portion of the crater (bottom left part of image) has recently been entirely obscured to the naked eye, but the thermal camera provides a clear view through the fume, revealing a small lava pond.
Pu‘u ‘Ō‘ō remains partly obscured by thick fume. In particular, th...
Pu‘u ‘Ō‘ō remains partly obscured by thick fume. In particular, th...Pu‘u ‘Ō‘ō crater remains partly obscured by thick fume. In particular, the northeastern portion of the crater (bottom left part of image) has recently been entirely obscured to the naked eye, but the thermal camera provides a clear view through the fume, revealing a small lava pond.
Map showing the June 27th flow in Kīlauea's East Rift Zone as of August 25, 2014. The area of the flow as mapped on August 22 is shown in pink, while widening and advancement of the flow as of August 25 is shown in red. The brown line marks the ground crack that channeled lava to the east, where it emerged to form a new pad of lava over the past couple of days.
Map showing the June 27th flow in Kīlauea's East Rift Zone as of August 25, 2014. The area of the flow as mapped on August 22 is shown in pink, while widening and advancement of the flow as of August 25 is shown in red. The brown line marks the ground crack that channeled lava to the east, where it emerged to form a new pad of lava over the past couple of days.
small pad of lava that has emerged from the crack over the past day...
small pad of lava that has emerged from the crack over the past day...A view of the small pad of lava that has emerged from the crack over the past day. The lava pad was about 800 m (0.5 miles) long, and was about 1.3 km (0.8 miles) east of the point where lava plunged into the crack.
small pad of lava that has emerged from the crack over the past day...
small pad of lava that has emerged from the crack over the past day...A view of the small pad of lava that has emerged from the crack over the past day. The lava pad was about 800 m (0.5 miles) long, and was about 1.3 km (0.8 miles) east of the point where lava plunged into the crack.
isolated pad of lava that has emerged from the crack. This view is...
isolated pad of lava that has emerged from the crack. This view is...Another view of the isolated pad of lava that has emerged from the crack. This view is towards the east, along the East Rift Zone. The spot at which lava flowed into the crack is to the west, out of view beyond the bottom of the photograph.
isolated pad of lava that has emerged from the crack. This view is...
isolated pad of lava that has emerged from the crack. This view is...Another view of the isolated pad of lava that has emerged from the crack. This view is towards the east, along the East Rift Zone. The spot at which lava flowed into the crack is to the west, out of view beyond the bottom of the photograph.
Surface rupture in soil near the intersection of state Highway 12 and Cuttings Wharf Road in Napa, CA on August 24, 2104
Surface rupture in soil near the intersection of state Highway 12 and Cuttings Wharf Road in Napa, CA on August 24, 2104
Surface rupture across Los Carneros Ave just northwest of South Ave in Napa County, CA. Photo taken by USGS from California Highway Patrol helicopter on August 24, 2014
Surface rupture across Los Carneros Ave just northwest of South Ave in Napa County, CA. Photo taken by USGS from California Highway Patrol helicopter on August 24, 2014
Surface rupture across State Highway 12 at Cuttings Wharf Road - Photo taken by USGS from California Highway Patrol helicopter on August 24, 2014
Surface rupture across State Highway 12 at Cuttings Wharf Road - Photo taken by USGS from California Highway Patrol helicopter on August 24, 2014
Damage to a building in downtown Napa, CA caused by the South Napa earthquake. Photo taken by USGS from California Highway Patrol helicopter on August 24, 2014
Damage to a building in downtown Napa, CA caused by the South Napa earthquake. Photo taken by USGS from California Highway Patrol helicopter on August 24, 2014
Collecting topographic data with a three-dimensional laser scanner
Collecting topographic data with a three-dimensional laser scannerUSGS volunteer Whitney DeLong and geology intern Alexandra Pickering collecting topographic data with a three-dimensional laser scanner along Cuttings Wharf Road in Napa County, CA on August 26, 2014. In the background are engineers inspecting the earthquake surface rupture where is passes through a horse paddock.
Collecting topographic data with a three-dimensional laser scanner
Collecting topographic data with a three-dimensional laser scannerUSGS volunteer Whitney DeLong and geology intern Alexandra Pickering collecting topographic data with a three-dimensional laser scanner along Cuttings Wharf Road in Napa County, CA on August 26, 2014. In the background are engineers inspecting the earthquake surface rupture where is passes through a horse paddock.
Timeline of past drilling activities conducted by countries, private sector firms, government agencies, and academe that have helped to refine global gas hydrate estimates and possible future drilling and production testing
Timeline of past drilling activities conducted by countries, private sector firms, government agencies, and academe that have helped to refine global gas hydrate estimates and possible future drilling and production testing
Left-stepping en echelon fractures characteristic of right-lateral fault displacement at the ground surface. Total fault slip measured near this location was 40-46 cm. Photo taken on main rupture strand near Buhman Rd.
Left-stepping en echelon fractures characteristic of right-lateral fault displacement at the ground surface. Total fault slip measured near this location was 40-46 cm. Photo taken on main rupture strand near Buhman Rd.
Right-lateral offset of vineyard row of nearly 40 cm. Photo taken on the main fault rupture near Buhman Rd.
Right-lateral offset of vineyard row of nearly 40 cm. Photo taken on the main fault rupture near Buhman Rd.
Right lateral offset of Browns Valley Rd. centerline, on a secondary fault strand.
Right lateral offset of Browns Valley Rd. centerline, on a secondary fault strand.
Small displacement ground cracks along main rupture near Cuttings Wharf Rd., south of Hwy. 12, taken the day of the earthquake. Displacement in this area grew to ~20 cm right-lateral by Monday, 8/25, due to afterslip.
Small displacement ground cracks along main rupture near Cuttings Wharf Rd., south of Hwy. 12, taken the day of the earthquake. Displacement in this area grew to ~20 cm right-lateral by Monday, 8/25, due to afterslip.