Mark DeMulder, Director of the U.S. Geological Survey's National Geospatial Program (NGP) gives a briefing at the USGS All-Hands meeting during the ESRI UC on July 14, 2010.
Videos
The USGS is a science organization that provides impartial information on the health of our ecosystems and environment, the natural hazards that threaten us, the natural resources we rely on, the impacts of climate and land-use change, and the core science systems that help us provide timely, relevant, and useable information.
Mark DeMulder, Director of the U.S. Geological Survey's National Geospatial Program (NGP) gives a briefing at the USGS All-Hands meeting during the ESRI UC on July 14, 2010.
Former U.S.
Former U.S.
Former U.S.
USGS-MBARI Cooperative Oceanographic Research
By Charles K. Paull, Senior Scientist Monterey Bay Aquarium Research Institute, Moss Landing, CA
USGS-MBARI Cooperative Oceanographic Research
By Charles K. Paull, Senior Scientist Monterey Bay Aquarium Research Institute, Moss Landing, CA
An underwater video camera was mounted on a Helley-Smith bedload sampler and set on the bottom of the river during a flow of around 32,000 cubic feet per second (bankfull). The video was titled with the GPS coordinates, date, and time.
An underwater video camera was mounted on a Helley-Smith bedload sampler and set on the bottom of the river during a flow of around 32,000 cubic feet per second (bankfull). The video was titled with the GPS coordinates, date, and time.
An underwater video camera was mounted on a Helley-Smith bedload sampler and set on the bottom of the river during a flow of around 32,000 cubic feet per second (bankfull). The video was titled with the GPS coordinates, date, and time.
Part 2 is a clip from the first video, showing the mobilization of cobbles on the bottom of the river's braided reach.
An underwater video camera was mounted on a Helley-Smith bedload sampler and set on the bottom of the river during a flow of around 32,000 cubic feet per second (bankfull). The video was titled with the GPS coordinates, date, and time.
Part 2 is a clip from the first video, showing the mobilization of cobbles on the bottom of the river's braided reach.
An underwater video camera was mounted on a Helley-Smith bedload sampler and set on the bottom of the river during a flow of around 32,000 cubic feet per second (bankfull). The video was titled with the GPS coordinates, date, and time.
An underwater video camera was mounted on a Helley-Smith bedload sampler and set on the bottom of the river during a flow of around 32,000 cubic feet per second (bankfull). The video was titled with the GPS coordinates, date, and time.
An underwater video camera was mounted on a Helley-Smith bedload sampler and set on the bottom of the river during a flow of around 32,000 cubic feet per second (bankfull). The video was titled with the GPS coordinates, date, and time.
An underwater video camera was mounted on a Helley-Smith bedload sampler and set on the bottom of the river during a flow of around 32,000 cubic feet per second (bankfull). The video was titled with the GPS coordinates, date, and time.
movie shows video taken during today's field visit and overflight. The first portion of the video is taken at the rim of Pu`u `Ō `ō crater, and shows the north vent feeding the lava pond. The lava surface undulates due to rising gas bubbles, and a small overturn is triggered.
movie shows video taken during today's field visit and overflight. The first portion of the video is taken at the rim of Pu`u `Ō `ō crater, and shows the north vent feeding the lava pond. The lava surface undulates due to rising gas bubbles, and a small overturn is triggered.
This movie shows video taken during today's field visit and overflight. The first portion of the video is taken at the rim of PuuOo crater, and shows the north vent feeding the lava pond. The lava surface undulates due to rising gas bubbles, and a small overturn is triggered.
This movie shows video taken during today's field visit and overflight. The first portion of the video is taken at the rim of PuuOo crater, and shows the north vent feeding the lava pond. The lava surface undulates due to rising gas bubbles, and a small overturn is triggered.
Field measurements at about 4;00 p.m. on Wednesday, June 9, 2010 at gage 13246000, North Fork Payette River near Banks, Idaho. Measured discharge was at 7,500 cfs. Beginning the weekend of June 3-4, the Payette rose quickly to above flood stage. The peak of record for this gage is 8,830 cfs, recorded May 11, 1947.
Field measurements at about 4;00 p.m. on Wednesday, June 9, 2010 at gage 13246000, North Fork Payette River near Banks, Idaho. Measured discharge was at 7,500 cfs. Beginning the weekend of June 3-4, the Payette rose quickly to above flood stage. The peak of record for this gage is 8,830 cfs, recorded May 11, 1947.
Field measurements at about 4;00 p.m. on Wednesday, June 9, 2010 at gage 13246000, North Fork Payette River near Banks, Idaho. Measured discharge was at 7,500 cfs. Beginning the weekend of June 3-4, the Payette rose quickly to above flood stage. The peak of record for this gage is 8,830 cfs, recorded May 11, 1947.
Field measurements at about 4;00 p.m. on Wednesday, June 9, 2010 at gage 13246000, North Fork Payette River near Banks, Idaho. Measured discharge was at 7,500 cfs. Beginning the weekend of June 3-4, the Payette rose quickly to above flood stage. The peak of record for this gage is 8,830 cfs, recorded May 11, 1947.
movie shows the active lava pond within Pu`u `Ō `ō crater, imaged with a thermal camera. The video is shown at x60 speed, and covers about 25 minutes. Lava is being supplied to the crater from two vents, one visible in the upper right corner of the image and one out of view in the lower left.
movie shows the active lava pond within Pu`u `Ō `ō crater, imaged with a thermal camera. The video is shown at x60 speed, and covers about 25 minutes. Lava is being supplied to the crater from two vents, one visible in the upper right corner of the image and one out of view in the lower left.
Development can have negative effects on streams in urban and suburban areas.
Development can have negative effects on streams in urban and suburban areas.
Part one of a three part series on how development can have negative effects on streams in urban and suburban areas.
Part one of a three part series on how development can have negative effects on streams in urban and suburban areas.
Part two of a three part series on how development can have negative effects on streams in urban and suburban areas.
Part two of a three part series on how development can have negative effects on streams in urban and suburban areas.
Part three of a three part series on how development can have negative effects on streams in urban and suburban areas.
Part three of a three part series on how development can have negative effects on streams in urban and suburban areas.
This movie shows the active lava pond within PuuOo crater, imaged with a thermal camera. The video is shown at x60 speed, and covers about 25 minutes. Lava is being supplied to the crater from two vents, one visible in the upper right corner of the image and one out of view in the lower left.
This movie shows the active lava pond within PuuOo crater, imaged with a thermal camera. The video is shown at x60 speed, and covers about 25 minutes. Lava is being supplied to the crater from two vents, one visible in the upper right corner of the image and one out of view in the lower left.
video from a thermal camera looking into the vent cavity at Halema`uma`u around 3pm today. The video is shown at x4 speed. At the beginning of the clip, the lava level is at a high stand, with slowly migrating crustal plates and little spattering. Eventually, small scale spattering begins in the northeast corner of the pond, accompanied by vigorous degassing.
video from a thermal camera looking into the vent cavity at Halema`uma`u around 3pm today. The video is shown at x4 speed. At the beginning of the clip, the lava level is at a high stand, with slowly migrating crustal plates and little spattering. Eventually, small scale spattering begins in the northeast corner of the pond, accompanied by vigorous degassing.
This video is from a thermal camera looking into the vent cavity at Halema'uma'u around 3pm today. The video is shown at x4 speed. At the beginning of the clip, the lava level is at a high stand, with slowly migrating crustal plates and little spattering.
This video is from a thermal camera looking into the vent cavity at Halema'uma'u around 3pm today. The video is shown at x4 speed. At the beginning of the clip, the lava level is at a high stand, with slowly migrating crustal plates and little spattering.