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Four scientists stand around a table in a lab with gray sediment core samples on the table, and they are examining the sediment.
Selecting sediment samples from cores
Selecting sediment samples from cores
Selecting sediment samples from cores

(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.

Why are HVO scientists talking so much about Mauna Loa?...
Why are HVO scientists talking so much about Mauna Loa?
Why are HVO scientists talking so much about Mauna Loa?
Why are HVO scientists talking so much about Mauna Loa?

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.

Why are HVO scientists talking so much about Mauna Loa?...
Why are HVO scientists talking so much about Mauna Loa?
Why are HVO scientists talking so much about Mauna Loa?
Why are HVO scientists talking so much about Mauna Loa?

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.

Sounds we can't hear teach us about lava lakes...
Sounds we can't hear teach us about lava lakes
Sounds we can't hear teach us about lava lakes
Sounds we can't hear teach us about lava lakes

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.

Participants of workshop, about 30 adults, standing in two rows against a tropical backdrop.
UFORIC International Workshop
UFORIC International Workshop
UFORIC International Workshop

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.

Image of Tim Collett talking about Gas Hydrates
USGS in South Korea
USGS in South Korea
USGS in South Korea

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.

Image of Tim Collett
USGS research geologist, Tim Collett
USGS research geologist, Tim Collett
USGS research geologist, Tim Collett

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

Image of Seth Haines
Gas Hydrate and Sediment Pressure Chamber
Gas Hydrate and Sediment Pressure Chamber
Gas Hydrate and Sediment Pressure Chamber

 Seth Haines, USGS research geophysicist, on a Korean Institute of Geoscience and Mineral Resources laboratory tour, which included stops at their gas hydrate and sediment pressure chamber - it's a whopping 320 gallons, dwarfing even Seth, a 6-footer.  The chamber is the silvery ring and the black cylinder beneath it.  It's so big and heavy

 Seth Haines, USGS research geophysicist, on a Korean Institute of Geoscience and Mineral Resources laboratory tour, which included stops at their gas hydrate and sediment pressure chamber - it's a whopping 320 gallons, dwarfing even Seth, a 6-footer.  The chamber is the silvery ring and the black cylinder beneath it.  It's so big and heavy

HVO's Volcano Watch now hosts a complete archive and inspires a new...
HVO's Volcano Watch now hosts a complete archive
HVO's Volcano Watch now hosts a complete archive
HVO's Volcano Watch now hosts a complete archive

Early evening view of the lava lake within Halema‘uma‘u crater at the summit of Kīlauea Volcano on January 30, 2018, when the lake level was 27 m (88 ft) below the crater floor. The bright yellow area of spattering marks the location where the circulating lava descends into the lake, thereby releasing gases trapped beneath the solid black crust on the lake surface.

Early evening view of the lava lake within Halema‘uma‘u crater at the summit of Kīlauea Volcano on January 30, 2018, when the lake level was 27 m (88 ft) below the crater floor. The bright yellow area of spattering marks the location where the circulating lava descends into the lake, thereby releasing gases trapped beneath the solid black crust on the lake surface.

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