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Images related to natural hazards.
Just before noon today, HVO's summit webcam (KIcam) captured this striking image of Kīlauea Volcano's ongoing summit eruption. A small rockfall on the north side of the Overlook crater triggered a small explosion in the lava lake, sending a dark-colored ash plume skyward.
Just before noon today, HVO's summit webcam (KIcam) captured this striking image of Kīlauea Volcano's ongoing summit eruption. A small rockfall on the north side of the Overlook crater triggered a small explosion in the lava lake, sending a dark-colored ash plume skyward.
HVO's HMcam also captured an image of today's rockfall and subsequent explosion (upper right) as it occurred.
HVO's HMcam also captured an image of today's rockfall and subsequent explosion (upper right) as it occurred.
On November 5, 1967, a line of vigorous lava fountains erupted on the floor of Halema‘uma‘u at the summit of Kīlauea. Lava soon covered the entire crater floor as volcanic gases billowed skyward (aerial view). Near the center, a pool of molten lava repeatedly overflowed a levee of crusted lava, spilling flows onto the lava-covered crater floor (inset).
On November 5, 1967, a line of vigorous lava fountains erupted on the floor of Halema‘uma‘u at the summit of Kīlauea. Lava soon covered the entire crater floor as volcanic gases billowed skyward (aerial view). Near the center, a pool of molten lava repeatedly overflowed a levee of crusted lava, spilling flows onto the lava-covered crater floor (inset).
A photo of the ledge that is building on Halema‘uma‘u lava lake's southern ledge. Small collapses of the unstable ledge are also common.
A photo of the ledge that is building on Halema‘uma‘u lava lake's southern ledge. Small collapses of the unstable ledge are also common.
Within Kīlauea Volcano's summit lava lake, vigorous spattering was occurring on the southern margin where a ledge of solidified lava has built out from the vent wall. The vigorous spattering site was active in an indentation in the ledge.
Within Kīlauea Volcano's summit lava lake, vigorous spattering was occurring on the southern margin where a ledge of solidified lava has built out from the vent wall. The vigorous spattering site was active in an indentation in the ledge.
Another ledge along the eastern margin has been building out from the vent wall, showing the recent high lava lake level mark (new black lava).
Another ledge along the eastern margin has been building out from the vent wall, showing the recent high lava lake level mark (new black lava).
BeachCam's perspective on the storm! This is the last image taken before the camera stopped working on Friday, March 2 at 11:23 a.m.
BeachCam's perspective on the storm! This is the last image taken before the camera stopped working on Friday, March 2 at 11:23 a.m.
Waves break between houses on White Cap Path in Sandwich, MA near high tide on Friday, March 2, 2018
Waves break between houses on White Cap Path in Sandwich, MA near high tide on Friday, March 2, 2018
photo taken at noon on Friday, March 2, 2018, shows floodwaters more than two feet deep on Water Street, Sandwich, MA, approaching the beach cam house (visible above the mailbox) and Town Neck Beach parking lot.
photo taken at noon on Friday, March 2, 2018, shows floodwaters more than two feet deep on Water Street, Sandwich, MA, approaching the beach cam house (visible above the mailbox) and Town Neck Beach parking lot.
The choice when issuing earthquake warnings is to: 1) issue alerts for weak shaking and potentially provide long warning times, but risk sending alerts for the many events that do not go on to produce damaging ground shaking, or 2) issue alerts only when ground shaking is expected to be damaging, with the tradeoff that the alert will be sent much later, reducing
The choice when issuing earthquake warnings is to: 1) issue alerts for weak shaking and potentially provide long warning times, but risk sending alerts for the many events that do not go on to produce damaging ground shaking, or 2) issue alerts only when ground shaking is expected to be damaging, with the tradeoff that the alert will be sent much later, reducing
Photo caption: USGS Hawaiian Volcano Observatory field engineers upgrade a tiltmeter on Kīlauea Volcano's East Rift Zone. The upgrade consisted of switching the old analog instrument to a newer digital model. This tiltmeter is used to track magma movement within the volcano. USGS photo by K. Kamibayashi.
Photo caption: USGS Hawaiian Volcano Observatory field engineers upgrade a tiltmeter on Kīlauea Volcano's East Rift Zone. The upgrade consisted of switching the old analog instrument to a newer digital model. This tiltmeter is used to track magma movement within the volcano. USGS photo by K. Kamibayashi.
Black arrows indicate the amount and direction of motion measured by GPS stations in HVO's monitoring network during the October 2015 slow slip event. Arrow lengths correspond to the amount of motion at each station (see scale at bottom of map); arrow points show the direction the stations moved.
Black arrows indicate the amount and direction of motion measured by GPS stations in HVO's monitoring network during the October 2015 slow slip event. Arrow lengths correspond to the amount of motion at each station (see scale at bottom of map); arrow points show the direction the stations moved.
The view from one of two video cameras atop the Dream Inn hotel in Santa Cruz, California, that overlook the coast in northern Monterey Bay. This view, from camera 1, looks eastward over Santa Cruz Main Beach and boardwalk.
The view from one of two video cameras atop the Dream Inn hotel in Santa Cruz, California, that overlook the coast in northern Monterey Bay. This view, from camera 1, looks eastward over Santa Cruz Main Beach and boardwalk.
(Left to right) Danny Brothers (USGS Pacific Coastal and Marine Science Center [PCMSC]), Peter Haeussler (USGS Alaska Science Center), Maureen Walton (PCMSC), and Jamie Conrad (PCMSC) select seafloor sediment samples from cores collected along the Queen Charlotte-Fairweather fault.
(Left to right) Danny Brothers (USGS Pacific Coastal and Marine Science Center [PCMSC]), Peter Haeussler (USGS Alaska Science Center), Maureen Walton (PCMSC), and Jamie Conrad (PCMSC) select seafloor sediment samples from cores collected along the Queen Charlotte-Fairweather fault.
Mauna Loa, Earth's largest active volcano, has erupted 33 times since 1843, producing the lava flows shown in black. All of these historic eruptions started at the summit of the volcano. From there, the eruptions either stayed in the summit area or migrated down the volcano's Northeast or Southwest Rift Zones.
Mauna Loa, Earth's largest active volcano, has erupted 33 times since 1843, producing the lava flows shown in black. All of these historic eruptions started at the summit of the volcano. From there, the eruptions either stayed in the summit area or migrated down the volcano's Northeast or Southwest Rift Zones.
Mauna Loa tends to erupt large, fast-moving lava flows. About 36 hours after the 1984 eruption began on March 25, lava flowed downstream (toward bottom-right of photo) through this ‘A‘ā channel down rift from the main vent. For scale, note the USGS scientists at work on the left side of the 70-m- (77-yard-) wide lava channel.
Mauna Loa tends to erupt large, fast-moving lava flows. About 36 hours after the 1984 eruption began on March 25, lava flowed downstream (toward bottom-right of photo) through this ‘A‘ā channel down rift from the main vent. For scale, note the USGS scientists at work on the left side of the 70-m- (77-yard-) wide lava channel.
A bursting bubble on the surface of a lava lake produces an impulsive signal on an infrasound recording. This photo shows a group of bubbles about 5 m (16 ft) across bursting on the Halema‘uma‘u lava lake at the summit of Kīlauea Volcano. The blue line is an infrasound recording of 50 seconds of similar activity.
A bursting bubble on the surface of a lava lake produces an impulsive signal on an infrasound recording. This photo shows a group of bubbles about 5 m (16 ft) across bursting on the Halema‘uma‘u lava lake at the summit of Kīlauea Volcano. The blue line is an infrasound recording of 50 seconds of similar activity.
Tim Collett, USGS research geologist, presenting at the Korean Institute of Geoscience and Mineral Resources' (KIGAM) international program for geoscience resources.
Tim Collett, USGS research geologist, presenting at the Korean Institute of Geoscience and Mineral Resources' (KIGAM) international program for geoscience resources.
USGS scientists, Bill Waite, Tim Collett, and Seth Haines in front of a archway in Daejeon, South Korea
USGS scientists, Bill Waite, Tim Collett, and Seth Haines in front of a archway in Daejeon, South Korea
Tim Collett, research geologist in gas hydrates, is chief for the U.S. Geological Survey (USGS) Energy Resources Program gas hydrate research efforts offering a presentation on unconventional oil and gas resources at KIGAM, the Korean Institute of Geoscience and Mineral Resources in Daejeon, South Korea
Tim Collett, research geologist in gas hydrates, is chief for the U.S. Geological Survey (USGS) Energy Resources Program gas hydrate research efforts offering a presentation on unconventional oil and gas resources at KIGAM, the Korean Institute of Geoscience and Mineral Resources in Daejeon, South Korea
International participants from Australia, New Zealand, Fiji, the Republic of the Marshall Islands, Hawaii, Spain, France, Belgium, the Netherlands, Germany, Israel, and the U.S. attended a workshop on “Understanding Flooding on Reef-lined Island Coastlines”, February 5-7, 2018.
International participants from Australia, New Zealand, Fiji, the Republic of the Marshall Islands, Hawaii, Spain, France, Belgium, the Netherlands, Germany, Israel, and the U.S. attended a workshop on “Understanding Flooding on Reef-lined Island Coastlines”, February 5-7, 2018.