This large rock at the Kīlauea Overlook in Hawai‘i Volcanoes National Park was ejected ballistically in 1790, or soon thereafter, from Kilauea Volcano's summit caldera when it was more than 600 meters (2000 feet) deep.
Images
Hawaiian Volcano Observatory images of eruptive activity, field work, and more.
This large rock at the Kīlauea Overlook in Hawai‘i Volcanoes National Park was ejected ballistically in 1790, or soon thereafter, from Kilauea Volcano's summit caldera when it was more than 600 meters (2000 feet) deep.
Aerial view of Pu‘u ‘Ō‘ō and surrounding features.
Aerial view of Pu‘u ‘Ō‘ō and surrounding features.
Early morning glow from Overlook vent in Halema‘uma‘u, Kīlauea
Early morning glow from Overlook vent in Halema‘uma‘u, KīlaueaIncandescence from the lava lake surface (out of view) reflects an awesome glow on the gas plume rising from the lake surface.
Early morning glow from Overlook vent in Halema‘uma‘u, Kīlauea
Early morning glow from Overlook vent in Halema‘uma‘u, KīlaueaIncandescence from the lava lake surface (out of view) reflects an awesome glow on the gas plume rising from the lake surface.
Lava from the Pu'u 'Ō'ō-Kupaianaha eruption, active since 1983, enters the ocean on the south flank of Kīlauea Volcano.
Lava from the Pu'u 'Ō'ō-Kupaianaha eruption, active since 1983, enters the ocean on the south flank of Kīlauea Volcano.
USGS Hawaiian Volcano Observatory geologist Janet Babb
USGS Hawaiian Volcano Observatory geologist Janet BabbThe degassing lava lake within Halema‘uma‘u at the summit of Kīlauea was a fitting backdrop in 2009 for USGS Hawaiian Volcano Observatory geologist Janet Babb, who later co-produced a video about the summit eruption.
USGS Hawaiian Volcano Observatory geologist Janet Babb
USGS Hawaiian Volcano Observatory geologist Janet BabbThe degassing lava lake within Halema‘uma‘u at the summit of Kīlauea was a fitting backdrop in 2009 for USGS Hawaiian Volcano Observatory geologist Janet Babb, who later co-produced a video about the summit eruption.
Vog obscures view during slack or no tradewinds at summit of Kīlauea
Vog obscures view during slack or no tradewinds at summit of KīlaueaVog obscures view during slack or no tradewinds at the summit of Kīlauea Volcano, Hawai‘i
Vog obscures view during slack or no tradewinds at summit of Kīlauea
Vog obscures view during slack or no tradewinds at summit of KīlaueaVog obscures view during slack or no tradewinds at the summit of Kīlauea Volcano, Hawai‘i
Side-by-side comparison of the NW wall of Kīlauea Caldera on a clea...
Side-by-side comparison of the NW wall of Kīlauea Caldera on a clea...Side-by-side comparison of the northwest wall of Kīlauea Caldera on a clear day (left) and a day with thick vog (right). HVO observation tower and building can be seen near the center in each photo.
Side-by-side comparison of the NW wall of Kīlauea Caldera on a clea...
Side-by-side comparison of the NW wall of Kīlauea Caldera on a clea...Side-by-side comparison of the northwest wall of Kīlauea Caldera on a clear day (left) and a day with thick vog (right). HVO observation tower and building can be seen near the center in each photo.
Geologist on rim of Halema‘uma‘u downloading camera images, Kīlauea...
Geologist on rim of Halema‘uma‘u downloading camera images, Kīlauea...HVO geologist downloads images collected with infrared cameras set up on the rim of Halema‘uma‘u Crater. The cameras are aimed at an erupting lava lake to conduct a thermal survey of the lake's surface.
Geologist on rim of Halema‘uma‘u downloading camera images, Kīlauea...
Geologist on rim of Halema‘uma‘u downloading camera images, Kīlauea...HVO geologist downloads images collected with infrared cameras set up on the rim of Halema‘uma‘u Crater. The cameras are aimed at an erupting lava lake to conduct a thermal survey of the lake's surface.
HVO on rim of Kīlauea's summit caldera overlooking Halema‘uma‘u, Ha...
HVO on rim of Kīlauea's summit caldera overlooking Halema‘uma‘u, Ha...The U.S. Geological Survey's Hawaiian Volcano Observatory, the first volcano observatory in the United States, is located on the west rim of Kīlauea Volcano's summit caldera in Hawai‘i Volcanoes National Park. A volcanic gas plume rises from a vent that opened in 2008 at the base of the south wall of Halema‘uma‘u Crater. Crater Rim Drive in foreground.
HVO on rim of Kīlauea's summit caldera overlooking Halema‘uma‘u, Ha...
HVO on rim of Kīlauea's summit caldera overlooking Halema‘uma‘u, Ha...The U.S. Geological Survey's Hawaiian Volcano Observatory, the first volcano observatory in the United States, is located on the west rim of Kīlauea Volcano's summit caldera in Hawai‘i Volcanoes National Park. A volcanic gas plume rises from a vent that opened in 2008 at the base of the south wall of Halema‘uma‘u Crater. Crater Rim Drive in foreground.
The USGS Hawaiian Volcano Observatory Monitors Kilauea's Summit Eruption
The USGS Hawaiian Volcano Observatory Monitors Kilauea's Summit EruptionThe USGS Hawaiian Volcano Observatory (foreground) is located on the caldera rim of Kilauea Volcano, Hawai'ithe most active volcano in the world. The observatory's location provides an excellent view of summit eruptive activity, which began in 2008.
The USGS Hawaiian Volcano Observatory Monitors Kilauea's Summit Eruption
The USGS Hawaiian Volcano Observatory Monitors Kilauea's Summit EruptionThe USGS Hawaiian Volcano Observatory (foreground) is located on the caldera rim of Kilauea Volcano, Hawai'ithe most active volcano in the world. The observatory's location provides an excellent view of summit eruptive activity, which began in 2008.
USGS Hawaiian Volcano Observatory Monitors Kilauea's Summit Eruption
USGS Hawaiian Volcano Observatory Monitors Kilauea's Summit EruptionThe USGS Hawaiian Volcano Observatory (foreground) is located on the caldera rim of Kilauea Volcano, Hawai'i—the most active volcano in the world. The observatory's location provides an excellent view of summit eruptive activity, which began in 2008.
USGS Hawaiian Volcano Observatory Monitors Kilauea's Summit Eruption
USGS Hawaiian Volcano Observatory Monitors Kilauea's Summit EruptionThe USGS Hawaiian Volcano Observatory (foreground) is located on the caldera rim of Kilauea Volcano, Hawai'i—the most active volcano in the world. The observatory's location provides an excellent view of summit eruptive activity, which began in 2008.
HVO on rim of Kīlauea's summit caldera overlooking Halema‘uma‘u, Ha...
HVO on rim of Kīlauea's summit caldera overlooking Halema‘uma‘u, Ha...The Hawaiian Volcano Observatory, the first volcano observatory in the United States, is located on the west rim of Kīlauea Volcano's summit caldera in Hawai‘i Volcanoes National Park. A volcanic gas plume rises from a vent that opened in 2008 at the base of the south wall of Halema‘uma‘u Crater. Crater Rim Drive in foreground.
HVO on rim of Kīlauea's summit caldera overlooking Halema‘uma‘u, Ha...
HVO on rim of Kīlauea's summit caldera overlooking Halema‘uma‘u, Ha...The Hawaiian Volcano Observatory, the first volcano observatory in the United States, is located on the west rim of Kīlauea Volcano's summit caldera in Hawai‘i Volcanoes National Park. A volcanic gas plume rises from a vent that opened in 2008 at the base of the south wall of Halema‘uma‘u Crater. Crater Rim Drive in foreground.
The Hawaiian Volcano Observatory perched on the west rim of Kīlauea Volcano's summit caldera, overlooks Halema‘uma‘u Crater, where a new vent that opened in March 2008 emits a volcanic gas plume.
The Hawaiian Volcano Observatory perched on the west rim of Kīlauea Volcano's summit caldera, overlooks Halema‘uma‘u Crater, where a new vent that opened in March 2008 emits a volcanic gas plume.
The USGS Hawaiian Volcano Observatory is perched on the rim of Kilauea Volcano's summit caldera (next to the Thomas A. Jaggar Museum in Hawai'i Volcanoes National Park), providing a spectacular view of the active vent in Halema‘uma‘u Crater.
The USGS Hawaiian Volcano Observatory is perched on the rim of Kilauea Volcano's summit caldera (next to the Thomas A. Jaggar Museum in Hawai'i Volcanoes National Park), providing a spectacular view of the active vent in Halema‘uma‘u Crater.
Nighttime view of tephra-jet explosion, Kīlauea, Hawai‘i
Nighttime view of tephra-jet explosion, Kīlauea, Hawai‘iIncandescent arcs trace the path of lava fragments cast out during a tephra-jet explosion at the Waikupanaha ocean entry in 2008. This is a relatively small explosion, reaching a few tens of meters (yards) height, while one earlier in the day was nearly 70 meters (230 ft) in height.
Nighttime view of tephra-jet explosion, Kīlauea, Hawai‘i
Nighttime view of tephra-jet explosion, Kīlauea, Hawai‘iIncandescent arcs trace the path of lava fragments cast out during a tephra-jet explosion at the Waikupanaha ocean entry in 2008. This is a relatively small explosion, reaching a few tens of meters (yards) height, while one earlier in the day was nearly 70 meters (230 ft) in height.
When lava from the Pu'u 'Ō'ō-Kupaianaha eruption, active since 1983, meets the ocean, large littoral explosions can result.
When lava from the Pu'u 'Ō'ō-Kupaianaha eruption, active since 1983, meets the ocean, large littoral explosions can result.
Talmadge Magno - Hawaii County Civil Defense Administrator and former Chief Ranger at Hawaiʻi Volcanoes National Park
Talmadge Magno - Hawaii County Civil Defense Administrator and former Chief Ranger at Hawaiʻi Volcanoes National ParkTalmadge Magno during his tenure as Chief Ranger at Hawaii Volcanoes National Park in 2008. NPS photo.
Talmadge Magno - Hawaii County Civil Defense Administrator and former Chief Ranger at Hawaiʻi Volcanoes National Park
Talmadge Magno - Hawaii County Civil Defense Administrator and former Chief Ranger at Hawaiʻi Volcanoes National ParkTalmadge Magno during his tenure as Chief Ranger at Hawaii Volcanoes National Park in 2008. NPS photo.
Clear day during tradewind conditions at the summit of Kīlauea
Clear day during tradewind conditions at the summit of KīlaueaClear day during tradewind conditions at the summit of Kīlauea Volcano, Hawai‘i
Clear day during tradewind conditions at the summit of Kīlauea
Clear day during tradewind conditions at the summit of KīlaueaClear day during tradewind conditions at the summit of Kīlauea Volcano, Hawai‘i
Gas plume rising from Halema‘uma‘u, Kīlauea, Hawai‘i
Gas plume rising from Halema‘uma‘u, Kīlauea, Hawai‘iGas plume rising from Halema‘uma‘u Crater, Kīlauea Volcano, Hawai‘i
Gas plume rising from Halema‘uma‘u, Kīlauea, Hawai‘i
Gas plume rising from Halema‘uma‘u, Kīlauea, Hawai‘iGas plume rising from Halema‘uma‘u Crater, Kīlauea Volcano, Hawai‘i
Volcanic-gas plume rises from Halema‘uma‘u, Kīlauea
Volcanic-gas plume rises from Halema‘uma‘u, KīlaueaVolcanic-gas plume rises from Halema‘uma‘u Crater, Kīlauea Volcano, Hawai‘i
Volcanic-gas plume rises from Halema‘uma‘u, Kīlauea
Volcanic-gas plume rises from Halema‘uma‘u, KīlaueaVolcanic-gas plume rises from Halema‘uma‘u Crater, Kīlauea Volcano, Hawai‘i
Volcanic-gas plume rises from Halema‘uma‘u, Kīlauea
Volcanic-gas plume rises from Halema‘uma‘u, KīlaueaA plume of volcanic gases (chiefly water vapor, carbon dioxide, and sulfur dioxide), tiny lava and rock particles, and droplets drifts southwest in the tradewinds from Halema‘uma‘u Crater.
Volcanic-gas plume rises from Halema‘uma‘u, Kīlauea
Volcanic-gas plume rises from Halema‘uma‘u, KīlaueaA plume of volcanic gases (chiefly water vapor, carbon dioxide, and sulfur dioxide), tiny lava and rock particles, and droplets drifts southwest in the tradewinds from Halema‘uma‘u Crater.