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Explore a diverse collection of engaging videos showcasing the latest research, discoveries, and educational content from the U.S. Geological Survey. Dive into the fascinating world of geology, hydrology, ecology, and natural hazards as we bring science to life. Stay informed and inspired by our visual storytelling that highlights the vital work of USGS scientists and their impact on the planet.
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Florida Keys National Marine Sanctuary
Florida Keys National Marine Sanctuary
Former U.S.
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Florida Keys National Marine Sanctuary
Former U.S.
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PubTalk 6/2010 — Monterey Canyon - Superhighway to the Deep-Sea
PubTalk 6/2010 — Monterey Canyon - Superhighway to the Deep-SeaUSGS-MBARI Cooperative Oceanographic Research
By Charles K. Paull, Senior Scientist Monterey Bay Aquarium Research Institute, Moss Landing, CA
PubTalk 6/2010 — Monterey Canyon - Superhighway to the Deep-Sea
PubTalk 6/2010 — Monterey Canyon - Superhighway to the Deep-SeaUSGS-MBARI Cooperative Oceanographic Research
By Charles K. Paull, Senior Scientist Monterey Bay Aquarium Research Institute, Moss Landing, CA
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 1)
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 1)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.
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 1)
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 1)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.
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 2)
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 2)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.
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 2)
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 2)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.
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 3)
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 3)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.
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 3)
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 3)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.
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 4)
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 4)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.
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 4)
Bedload Transport on the Kootenai River near Bonners Ferry, ID (Part 4)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.
Action within Pu`u `Ō `ō crater
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.
Activity within PuuOo
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.
High Flow on the North Fork Payette River, Idaho
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.
High Flow on the North Fork Payette River, Idaho
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.
Active lava pond within Pu`u `Ō `ō crater
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.
Effects of Urbanization on Stream Ecosystems
Development can have negative effects on streams in urban and suburban areas.
Development can have negative effects on streams in urban and suburban areas.
The Effects of Urbanization on Stream Ecosystems (extended) Part I: Introduction
The Effects of Urbanization on Stream Ecosystems (extended) Part I: IntroductionPart one of a three part series on how development can have negative effects on streams in urban and suburban areas.
The Effects of Urbanization on Stream Ecosystems (extended) Part I: Introduction
The Effects of Urbanization on Stream Ecosystems (extended) Part I: IntroductionPart one of a three part series on how development can have negative effects on streams in urban and suburban areas.
The Effects of Urbanization on Stream Ecosystems (extended) Part II: Study Design
The Effects of Urbanization on Stream Ecosystems (extended) Part II: Study DesignPart two of a three part series on how development can have negative effects on streams in urban and suburban areas.
The Effects of Urbanization on Stream Ecosystems (extended) Part II: Study Design
The Effects of Urbanization on Stream Ecosystems (extended) Part II: Study DesignPart two of a three part series on how development can have negative effects on streams in urban and suburban areas.
The Effects of Urbanization on Stream Ecosystems (extended) Part III: Study Results
The Effects of Urbanization on Stream Ecosystems (extended) Part III: Study ResultsPart three of a three part series on how development can have negative effects on streams in urban and suburban areas.
The Effects of Urbanization on Stream Ecosystems (extended) Part III: Study Results
The Effects of Urbanization on Stream Ecosystems (extended) Part III: Study ResultsPart three of a three part series on how development can have negative effects on streams in urban and suburban areas.
Thermal View of Active Lava Pond within
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.
Looking into the Halema`uma`u vent cavity
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.
Thermal View of Halema'uma'u Vent
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.
PubTalk 5/2010 — The Heat is On: Desert Tortoises & Survival
PubTalk 5/2010 — The Heat is On: Desert Tortoises & SurvivalA New USGS documentary video exploring the world of the mojave desert tortoise
Introduced & discussed by USGS Ecologist Todd Esque & Ken Nussear, Wildlife Biologist
PubTalk 5/2010 — The Heat is On: Desert Tortoises & Survival
PubTalk 5/2010 — The Heat is On: Desert Tortoises & SurvivalA New USGS documentary video exploring the world of the mojave desert tortoise
Introduced & discussed by USGS Ecologist Todd Esque & Ken Nussear, Wildlife Biologist