Images

Zooming in on the bottom of Halema‘uma‘u, the small puddle between the two greenish ponds is more visible. USGS photo by J. Babb, 08/04/2019.

USGS scientists Rebecca Kramer and Dan Dzurisin install a solar panel and GPS antenna (green square) at a semipermanent GPS station in the southern part of Yellowstone National Park. The work first required digging through 4 feet of snow!

With the help of a powerful telephoto lens, HVO geologists confirmed today that there are two areas of ponded water at the bottom of Halema‘uma‘u. Using a laser range finder from their observation site, they were able to measure the two greenish ponds.

While making observations today, HVO geologists noted a koa‘e kea (white-tailed tropicbird) gliding across the ponded water at the bottom of Halema‘uma‘u. The bird is visible in the top left quarter of the photo. USGS photo by M. Patrick, 08/03/2019.

This image shows an area of greenish fume (near top of photo) east of the water pond (center) at the bottom of Halema‘uma‘u. This fume could suggest another emerging area of ponded water, but this has not yet been confirmed. HVO continues to closely monitor the area, and will report any significant changes.

The water pond deep within Halema‘uma‘u is impossible to see from most areas along the rim of Kīlauea's caldera. But one potential viewpoint on the rim was examined today by HVO geologists, who were able to see the small pond of water at the bottom of the crater, despite poor weather and fleeting views through fog.

A slightly closer view of the water in the bottom of Halema‘uma‘u taken with a telephoto lens during HVO's overflight today (August 1, 2019). USGS photo by S. Conway, 08/01/2019.

Zooming in even closer, an HVO scientist captured this image of the water on the floor of the crater during today's overflight. For more information, please read "Water or no water: that is (or was) the question"—HVO's Aug.

Photographs of Cistern Spring showing the draining behavior that occurs after major water eruptions of Steamboat Geyser. Left: about 2.5 hours after the onset of a major Steamboat eruption. Right: about 19.5 hours after that eruption.

This huge boulder was dropped by a retreating glacier on the north rim of the Grand Canyon of the Yellowstone in Yellowstone National Park, and it is a testament to Yellowstone's icy past.

An HVO geologist walks along the Mauna Loa summit trail, with Mauna Kea visible in the distant background.

HVO staff visited the summit of Mauna Loa on foot to repair the webcam on April 24. The weather was perfectly clear and views of the caldera floor showed nothing unusual.

Rockslide damage to the Golden Gate area near Mammoth Hot Springs, Yellowstone National Park, as a result of the 1959 Hebgen Lake earthquake.

Seismic geyser in eruption in 1970. Photo by John Brandow.

Hebgen Lake fault scarp in 1959. USGS photo by J. R. Stacy.

HVO scientists inspect a seismic station on Mauna Loa to evaluate for a possible equipment upgrade in the near future.

HVO scientists measure a GPS instrument to ensure its stability during a multi-day deployment in the Kahuku Unit of Hawai‘i Volcanoes National Park.

Map of moderate, high and very high threat volcanoes monitored by the California

A close-up of the active fumarole field on the north wall of the pit.

The weather was warm and sunny during a routine visit to the Halema‘uma‘u webcam. No significant changes were observed, and no rockfalls were heard.

As the sun rose above Mauna Kea (background) on July 6, 1975, eruptive fissures along the Northeast Rift Zone of Mauna Loa fed voluminous ‘a‘ā lava flows that quickly moved down the north flank of the volcano. USGS photo by D. Peterson.