Images

Panoramic photo of Pocket Basin, a hydrothermal explosion crater in Yellowstone National Park's Lower Geyser Basin, taken from the northeast rim looking southwest into the crater. Pocket Basin is a U-shaped crater that is dissected on the SW edge by the Firehole River, visible on the far-right of the photo.

HVO geologists made observations of Kīlauea's summit water lake from the east rim of Halema‘uma‘u. This view point is on the large downdropped block that subsided during the 2018 collapse events. From this spot, a view of the entire lake is possible, providing a new perspective on the growth of the lake.

This view shows Kīlauea's water lake from the east side of the crater. On September 23, 2020, the western portion of the lake (top of image) was the most varied in color, with patches of greenish and brown water. The majority of the lake surface, however, was the typical tan hue. USGS photo by M. Patrick.

Small patches of light-colored floating material were seen drifting on the surface of Kīlauea's summit water lake on September 23, 2020. The composition of this material is unknown, but future water sampling missions may provide insight. USGS photo by M. Patrick.

Portions of Crater Rim Drive, within Hawai‘i Volcanoes National Park, appear cracked, offset, and down-dropped in this photo, taken during an overflight of Kīlauea’s summit on September 23, 2020. To the north, Kīlauea’s summit water lake, within Halema‘uma‘u, is visible. USGS photo by K. Mulliken.

Hawaiian Volcano Observatory geologists flew over the Sulphur Banks area and Ha‘akulamanu trail within Hawai‘i Volcanoes National Park on September 23, 2020. Fumaroles in the Sulphur Banks area are sampled approximately every three months by Hawaiian Volcano Observatory gas geochemists to track long-term changes in volcanic gas chemistry at Kīlauea.

The weather was overcast during an overflight of Kīlauea's summit on September 23, 2020. This view shows Wahinekapu (Steaming Bluff) and the Steam Vents area within Hawai‘i Volcanoes National Park. Extensive cracks in the area allow heated groundwater to escape from underground.

On September 23, 2020, Hawaiian Volcano Observatory geophysicists and a geologist conducted a gravity survey of Kīlauea summit, as part of HVO's regular monitoring program. In this photo, scientists are carrying survey equipment westward along the remnants of the Halema‘uma‘u Trail on the down-dropped block of Kīlauea caldera.

During a gravity survey, HVO scientists measure the relative strength of gravity (gravimeter, bottom left corner of photo) between benchmarks. High-precision vertical positions from kinematic Global Positioning System (GPS, tripod and antenna middle of photo) help correct the gravity measurement for the effects of elevation changes.

A gravimeter makes a measurement at a benchmark situated among lava flows erupted in 1919. The strength of gravity varies with both elevation and the amount of mass beneath the instrument. Changes in mass can indicate changes in the amount of magma entering Kīlauea's magma reservoirs. USGS photo by A. Flinders.

An HVO geophysicist takes a gravity measurement at a benchmark near a continuous gravimeter (inside hutch). The continuous gravimeter takes gravity measurements once per second and relays the data via radio back to HVO. During the gravity survey on September 23, 2020, HVO scientists took measurements at multiple locations on the floor of Kīlauea caldera.

Color variations are common at Kīlauea's summit water lake, and are usually dominated by tan and brown hues. Today, the interaction between different color zones produced a large swirl in the center of the lake.

Map of the USGS Hawaiian Volcano Observatory’s current camera network coverage.   Lava-flow hazard zone 1 is outlined in yellow.   Color-shaded areas are visible to at least one camera in the current network.  We would like to expand the network so that it covers the grey-shaded areas in zone 1 as well.  If your property has a good view

GNSS site LKWY, which was visited in September 2020 to install new GNSS equipment and upgrade the communications for improved data quality.  The site is now capable of collecting several times more observation data then was possible with the original older equipment.

The inside of a borehole seismometer equipment enclosure is full of batteries, cables, data communications equipment and data recording instruments.  Some of the geodetic infrastructure in Yellowstone National Park is colocated with seismic equipment.  In this case, the communications downlink radio for the GNSS station is housed with the borehole enc

View of Absaroka Range from Eagle Peak, WY, toward the southwest.

On the surface of Kīlauea's new landscape, a story is told

The Upper Geyser Basin viewed from the Old Faithful webcam. Hot water was piped from Solitary Geyser to the former site of the geyser bathhouse.

Map of thermal areas in Yellowstone (red), as well as lakes (outlined in blue), many of which have thermal areas on their shores or beneath their surfaces.

High-resolution images of Fern Lake from different seasons.  North is up.  Fern Lake is about 1 km across from east to west.  Red arrows in the winter image point to large zones of open water, indicating either nearshore springs or underwater hydrothermal vents, but there are also many smaller zones of open water that are conspicuous. 

Shaded relief map based on high-resolution topographic data from lidar and showing subtle terraces on the north side of Yellowstone Lake (a few example terraces are marked by yellow arrows and traced by dashed and dotted white lines).