Core storage facility at the the Korean Institute of Geoscience and Mineral Resources in Daejeon, South Korea
Images
Images related to natural hazards.
Core storage facility at the the Korean Institute of Geoscience and Mineral Resources in Daejeon, South Korea
Gas hydrate from offshore Korea courtesy of the Korean Institute of Geoscience and Mineral Resources. Learn more about gas hydrates at https://woodshole.er.usgs.gov/project-pages/hydrates/
Gas hydrate from offshore Korea courtesy of the Korean Institute of Geoscience and Mineral Resources. Learn more about gas hydrates at https://woodshole.er.usgs.gov/project-pages/hydrates/
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
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.
Volcano Watch (no. 7)
Volcano Watch (no. 5)
Scientists predicting lava flow shift from Kupaianaha vent
Scientists predicting lava flow shift from Kupaianaha ventScientists predicting lava flow shift from Kupaianaha vent
Scientists predicting lava flow shift from Kupaianaha vent
Scientists predicting lava flow shift from Kupaianaha ventScientists predicting lava flow shift from Kupaianaha vent
Volcano Watch (no. 4)
Volcano Watch (no. 3)
Volcano Watch (no. 2)
Volcano Watch (no. 1)
Earthquake swarm felt at Lo`ihi seamount
Earthquakes swarm beneath Kīlauea Volcano
Earthquakes swarm beneath Kīlauea Volcano
Kīlauea Volcano divided into lava-risk zones
Kīlauea Volcano divided into lava-risk zones
The Big Island is sinking under weight of volcano
The Big Island is sinking under weight of volcano
Eruption's 10th year begins
Lava continues to flow near Kamoamoa
Lava expected to flow over pali toward Kamoamoa soon
Lava expected to flow over pali toward Kamoamoa soonLava expected to flow over pali toward Kamoamoa soon
Lava expected to flow over pali toward Kamoamoa soon
Lava expected to flow over pali toward Kamoamoa soonLava expected to flow over pali toward Kamoamoa soon
Kīlauea's not Hawaii's only active volcano
Kīlauea's not Hawaii's only active volcano
Lava flow continues in starts and stops
Episode 51 stops, 52 begins at Kīlauea Volcano
Episode 51 stops, 52 begins at Kīlauea Volcano