Multimedia

Solar panels that power USGS volcano monitoring equipment can be covered with tephra during eruptive episodes at the summit of Kīlauea. These tephra particles can range in size from fine ash to tennis-ball sized and larger.  USGS field engineers visit these stations after eruptive episodes to clean them off and restore power to the stations. USGS photo by M.

On July 10, USGS field engineers visited one of the volcanic gas monitoring stations downwind of the summit of Kīlauea, within the closed area of Hawaiʻi Volcanoes National Park. This area has been blanketed with tephra material during recent eruptive episodes within Halemaʻumaʻu. USGS photo by M. Cappos. 

USGS Hawaiian Volcano Observatory field engineers visited monitoring stations downwind of the Kīlauea summit eruptive vents on July 10. They wore snowshoes as the large footprint keeps the field engineers walking on top of the frothy pumice everywhere, rather than through it. USGS photo by M. Warren. 

During episode 28 of lava fountaining during the ongoing Kīlauea summit eruption, USGS scientists approached the caldera rim to measure volcanic gas emissions with permission from Hawai‘i Volcanoes National Park. This lava fountain on the morning of July 9 was approximately 1000 feet tall (300 meters).

In this view from an eruption monitoring helicopter overflight on Wednesday, July 9, new lava flows can be seen traveling across the Halema‘uma‘u crater floor—these appear as fluid forms with a shiny, silvery crust over incandescent red-hot lava. Older lava flows from previous eruptive episodes have a darker or duller appearance.

During episode 28 lava fountaining on Wednesday, July 9, clasts of fluid, molten lava were ejected to heights of approximately 1000 feet (300 meters) from the vent within Halema‘uma‘u crater and deposited onto the growing tephra hill on the western side of Kaluapele (Kīlauea summit caldera).