This movie (at x2 speed) shows a small explosive event in the Halema'uma'u vent at 9:20am. The explosion was immediately preceded by a portion of the vent rim collapsing into the vent cavity. The brown plume rises rapidly from the vent, and in the full resolution video large particles can be seen ejected in front of the plume.
Videos
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This movie (at x2 speed) shows a small explosive event in the Halema'uma'u vent at 9:20am. The explosion was immediately preceded by a portion of the vent rim collapsing into the vent cavity. The brown plume rises rapidly from the vent, and in the full resolution video large particles can be seen ejected in front of the plume.
movie shows lava within the Halema`uma`u vent cavity, at a depth of about 200 m below the vent rim. The lava surface, which is about 20 m wide, is extremely vigorous, with constant roiling and semi-continuous spattering.
movie shows lava within the Halema`uma`u vent cavity, at a depth of about 200 m below the vent rim. The lava surface, which is about 20 m wide, is extremely vigorous, with constant roiling and semi-continuous spattering.
PubTalk 11/2009 — Geohazards in the Aleutian Islands
PubTalk 11/2009 — Geohazards in the Aleutian IslandsGreat Earthquakes, Great Waves, and Great Volcanic Explosions!
by Steve Kirby, Geophsicist, and Dave Scholl, Scientist Emeritus
PubTalk 11/2009 — Geohazards in the Aleutian Islands
PubTalk 11/2009 — Geohazards in the Aleutian IslandsGreat Earthquakes, Great Waves, and Great Volcanic Explosions!
by Steve Kirby, Geophsicist, and Dave Scholl, Scientist Emeritus
This movie shows lava within the Halema'uma'u vent cavity, at a depth of about 200 m below the vent rim. The lava surface, which is about 20 m wide, is extremely vigorous, with constant roiling and semi-continuous spattering.
This movie shows lava within the Halema'uma'u vent cavity, at a depth of about 200 m below the vent rim. The lava surface, which is about 20 m wide, is extremely vigorous, with constant roiling and semi-continuous spattering.
PubTalk 10/2009 — Paddling for a Purpose in a Troubled Sea
PubTalk 10/2009 — Paddling for a Purpose in a Troubled SeaSampling the Salish Sea During Tribal Canoe Journeys
by Eric Grossman, USGS Tribal Journey Science Advisor
PubTalk 10/2009 — Paddling for a Purpose in a Troubled Sea
PubTalk 10/2009 — Paddling for a Purpose in a Troubled SeaSampling the Salish Sea During Tribal Canoe Journeys
by Eric Grossman, USGS Tribal Journey Science Advisor
Whether you drink water from your tap, use electricity or canoe down your local river, chances are you benefit from USGS streamgage information. So what is a streamgage and what does it do for you? This CoreCast episode gives you the inside scoop on your silent superhero.
Transcript and captions available soon.
Whether you drink water from your tap, use electricity or canoe down your local river, chances are you benefit from USGS streamgage information. So what is a streamgage and what does it do for you? This CoreCast episode gives you the inside scoop on your silent superhero.
Transcript and captions available soon.
Disappearance of the lava pond within Halema`uma`u
Disappearance of the lava pond within Halema`uma`umovie shows the disappearance of the lava pond deep within the Halema`uma`u vent cavity during the early morning hours of October 3. The lava surface undergoes two filling and draining cycles, and then retreats to deeper levels in the conduit, completely out of view, around 2 am.
Disappearance of the lava pond within Halema`uma`u
Disappearance of the lava pond within Halema`uma`umovie shows the disappearance of the lava pond deep within the Halema`uma`u vent cavity during the early morning hours of October 3. The lava surface undergoes two filling and draining cycles, and then retreats to deeper levels in the conduit, completely out of view, around 2 am.
Cycles of filling and draining within Halema`uma`u
Cycles of filling and draining within Halema`uma`umovie shows lava pond activity within the Halema`uma`u vent cavity captured with the low-light camera situated at the Halema`uma`u Overlook. The entire night of Oct 1-2, 2009, is shown here in 26 seconds, so the speed of the video is increased considerably. You can see many cycles of filling and draining, with each cycle lasting about two hours.
Cycles of filling and draining within Halema`uma`u
Cycles of filling and draining within Halema`uma`umovie shows lava pond activity within the Halema`uma`u vent cavity captured with the low-light camera situated at the Halema`uma`u Overlook. The entire night of Oct 1-2, 2009, is shown here in 26 seconds, so the speed of the video is increased considerably. You can see many cycles of filling and draining, with each cycle lasting about two hours.
Fluid motion of pāhoehoe flow at Royal Gardens subdivision
Fluid motion of pāhoehoe flow at Royal Gardens subdivisionThis video shows the remarkable fluid motion of a finger of pāhoehoe flowing into an old skylight at the top of Royal Gardens subdivision. The movement of the viscous lava resembles that of soft-serve ice cream.
Fluid motion of pāhoehoe flow at Royal Gardens subdivision
Fluid motion of pāhoehoe flow at Royal Gardens subdivisionThis video shows the remarkable fluid motion of a finger of pāhoehoe flowing into an old skylight at the top of Royal Gardens subdivision. The movement of the viscous lava resembles that of soft-serve ice cream.
Collapse of the unstable walls within Halema`uma`u vent
Collapse of the unstable walls within Halema`uma`u ventmovie shows two separate rockfalls impacting and disrupting the active lava pond in Halema`uma`u. Rockfalls here result from collapse of the unstable walls of the vent cavity, and are a common occurrence.
Collapse of the unstable walls within Halema`uma`u vent
Collapse of the unstable walls within Halema`uma`u ventmovie shows two separate rockfalls impacting and disrupting the active lava pond in Halema`uma`u. Rockfalls here result from collapse of the unstable walls of the vent cavity, and are a common occurrence.
video thumbnail: Raven RQ-11A sUAS: USGS Training Exercise
U.S. Geological Survey (USGS) biologist Leanne Hanson narrates this video showing how the Raven-A small unmanned aircraft system, also called an sUAS or simply a drone, works in the field and what it “sees” from the air. In the first application of the Raven A system to a natural resource management need, the USGS and U.S.
U.S. Geological Survey (USGS) biologist Leanne Hanson narrates this video showing how the Raven-A small unmanned aircraft system, also called an sUAS or simply a drone, works in the field and what it “sees” from the air. In the first application of the Raven A system to a natural resource management need, the USGS and U.S.
movie shows vigorous spattering at the northeast margin of the lava pond that is deep within the Halema`uma`u vent cavity. The lava surface, cut by incandescent cracks, is slowly migrating towards the southeast (down in this image). The lava pond has been visible the last several nights in the Halema`uma`u Overlook webcam (see 'webcams' link above).
movie shows vigorous spattering at the northeast margin of the lava pond that is deep within the Halema`uma`u vent cavity. The lava surface, cut by incandescent cracks, is slowly migrating towards the southeast (down in this image). The lava pond has been visible the last several nights in the Halema`uma`u Overlook webcam (see 'webcams' link above).
movie shows spattering on the northeast margin of a small lava pond deep within the Halema`uma`u vent cavity. The video was shot in "nightshot" mode, which provides improved views through the thick fume at night. Each spatter burst represents a gas bubble, or bubbles, breaking at the surface.
movie shows spattering on the northeast margin of a small lava pond deep within the Halema`uma`u vent cavity. The video was shot in "nightshot" mode, which provides improved views through the thick fume at night. Each spatter burst represents a gas bubble, or bubbles, breaking at the surface.
Brown plume event within the Halema`uma`u vent cavity
Brown plume event within the Halema`uma`u vent cavitymovie shows a brown plume event resulting from a collapse within the Halema`uma`u vent cavity. Later views into the vent cavity with a thermal camera revealed that the floor of the vent cavity—at about 200 yards below the vent rim—had fallen away, deepening the vent cavity even further.
Brown plume event within the Halema`uma`u vent cavity
Brown plume event within the Halema`uma`u vent cavitymovie shows a brown plume event resulting from a collapse within the Halema`uma`u vent cavity. Later views into the vent cavity with a thermal camera revealed that the floor of the vent cavity—at about 200 yards below the vent rim—had fallen away, deepening the vent cavity even further.
PubTalk 9/2009 — Meeting the Challenge of the Loma Prieta Earthquake
PubTalk 9/2009 — Meeting the Challenge of the Loma Prieta Earthquakeby Jack Boatwright, USGS Seismologist
An explosion at 3:13am from the vent in Halema`uma`u ejected hot particles about a hundred yards above the vent rim, and several tens of yards above the Halema`uma`u Overlook. This Quicktime movie (shown at x2 speed) shows the event captured by a low-light camera in the HVO observation tower.
An explosion at 3:13am from the vent in Halema`uma`u ejected hot particles about a hundred yards above the vent rim, and several tens of yards above the Halema`uma`u Overlook. This Quicktime movie (shown at x2 speed) shows the event captured by a low-light camera in the HVO observation tower.
Thermal movie showing a view inside the Halema`uma`u vent cavity
Thermal movie showing a view inside the Halema`uma`u vent cavitymovie shows a view into the Halema`uma`u vent cavity with a thermal camera. To the naked eye, the vent is entirely obscured by thick fume, but the thermal camera can 'see' through much of this and provide views of the cavity interior. These views show four puffing holes on the floor of the cavity. North is to the right.
Thermal movie showing a view inside the Halema`uma`u vent cavity
Thermal movie showing a view inside the Halema`uma`u vent cavitymovie shows a view into the Halema`uma`u vent cavity with a thermal camera. To the naked eye, the vent is entirely obscured by thick fume, but the thermal camera can 'see' through much of this and provide views of the cavity interior. These views show four puffing holes on the floor of the cavity. North is to the right.
movie shows two degassing holes on the floor of the Halema`uma`u cavity. Lava is just below the rim of the two holes, creating frequent spattering which falls around their rims. Within the larger of the two (on the right), lava can be seen vigorously sloshing. For scale, these openings are about 10 yards wide.
movie shows two degassing holes on the floor of the Halema`uma`u cavity. Lava is just below the rim of the two holes, creating frequent spattering which falls around their rims. Within the larger of the two (on the right), lava can be seen vigorously sloshing. For scale, these openings are about 10 yards wide.
Upper Midwest Environmental Sciences Center Open House 2009/50th Ann.
Upper Midwest Environmental Sciences Center Open House 2009/50th Ann.
Upper Midwest Environmental Sciences Center Open House 2009/50th Ann.Highlights of UMESC's open house September 2009. Commentary from the Center Director, Outreach Coordinator and Center Scientists.
Upper Midwest Environmental Sciences Center Open House 2009/50th Ann.
Upper Midwest Environmental Sciences Center Open House 2009/50th Ann.Highlights of UMESC's open house September 2009. Commentary from the Center Director, Outreach Coordinator and Center Scientists.
video thumbnail: Indonesian Capacity Building in Seismology and Tsunami Detection
Indonesian Capacity Building in Seismology and Tsunami Detection
Indonesian Capacity Building in Seismology and Tsunami DetectionThe December 2004 Indian Ocean Tsunami was one of the deadliest natural disasters of modern history, killing over 225,000 people. As a result of this catastrophe, the U.S. Geological Survey has partnered with the international community to create an Indian Ocean Tsunami Warning System (IOTWS).
Indonesian Capacity Building in Seismology and Tsunami Detection
Indonesian Capacity Building in Seismology and Tsunami DetectionThe December 2004 Indian Ocean Tsunami was one of the deadliest natural disasters of modern history, killing over 225,000 people. As a result of this catastrophe, the U.S. Geological Survey has partnered with the international community to create an Indian Ocean Tsunami Warning System (IOTWS).
This film presents a summary of the natural hazards of Hong Kong. Such natural hazards include earthquakes, typhoons, tsunamis, and landslides.
This film presents a summary of the natural hazards of Hong Kong. Such natural hazards include earthquakes, typhoons, tsunamis, and landslides.