Images

Kīlauea

Summit crater lake growth

July 25, 2019 to July 25, 2020

Comparison of images showing growth of Kīlauea's summit water lake over the past year. The left image, taken on August 2, 2019, shows a small green pond that was approximately 6 ft (2 m) deep. The right image, taken on July 21, 2020, shows a lake more than 130 ft (40 m) deep with shades of tan to brown and a sharp color boundary often cutting across the lake.

In the first few minutes of Steamboat's eruptions, it has often been measured well over 300 ft. with a few exceptional eruptions measured by visitors at over 400 ft.!  In this example, done using a rangefinder by a Yellowstone National Park ranger, it comes in at 334.9 ft. For comparison, the Lower Falls of the Yellowstone is about 308 ft.

Image comparison of Kīlauea summit lake on August 2, 2019 and July July 21, 2020

The Raspberry Shake 4D (RS4D) is a personal seismograph with a vertical-component velocity transducer, and three-component (vertical, north-south, and east-west) accelerometer. A Raspberry Pi, which is a computer about the size of a credit card, powers the RS4D unit, which is about the size of a can of Spam.

National Park Service scientist using a camera paired with a GPS receiver to obtain images of Castle Geyser, Yellowstone National Park, in June 2019.

An HVO geologist collects GPS data on the western rim of Kīlauea's summit caldera. The geologist is standing upon a thick sequence of tephra deposits formed during explosive eruptions at Kīlauea's summit between about 1500 CE and the early 19th century.

Comet NEOWISE is seen with the Roosevelt Arch in the foreground at the north Entrance of Yellowstone National Park.  The town of Gardiner, Montana, is in the background.

Panoramic photo of Hayden Valley looking east toward the Yellowstone River from the Mary Mountain trail.

A small stream, Violet Creek, winds its way through Hayden Valley in Yellowstone National Park.

Comparison of photos from Giant and Castle Geysers separated by almost 150 years. These images suggest almost no changes to the geyser structure implying that large geysers form over thousands of years. 

Another view of the Fissure 8 channel, looking upstream. On the right, a lower ledge along the channel wall represents the level of lava in the channel during the later stages of the flow. USGS photo by M. Patrick.

A view into the Absaroka Mountains in northeastern Yellowstone National Park. While the Absarokas of today look a little different due to glacial activity, these are the same mountains that existed over the last 53 million years, well before the arrival of the Yellowstone hot spot.

Hawaiian Volcano Observatory (HVO) electronics technician Steven Fuke stands near a solar panel system that powers a volcano-monitoring station. 

View of the recently cleared Boiling Pots on the Wailuku River in Hilo. The pots, each about 15 m (50 ft) in diameter, are eroded into a 10,000 year old Mauna Loa lava flow. When the water is low, the river does not flow over some of the pot rims but it continues to flow through them. USGS photo.

HVO geologists visited the lower East Rift Zone lava flow field this past week to make measurements and observations, to better understand and reconstruct the dynamics of the Fissure 8 lava flow. This photo shows the channel wall in the braided channel region of the flow.

In the eastern portion of the lake, the dark brown zone had a slightly mottled appearance, but this pattern was transient and gone within about ten minutes.

Geologists from Montana State University study an outcrop of diorite (a silicic igneous rock that cooled slowly beneath the ground). An outcrop of this size is important because it is easier to see any structural relations along with rock composition.

USGS-Cascades Volcano Observatory geophysicist Rebecca Kramer works on station PR05, which is part of the Mount Rainier lahar detection network (Mount Rainier is pictured in the distance). The purpose of the site visit was to upgrade the power system and deploy infrasound equipment. 

The water lake within Halema‘uma‘u crater, at the summit of Kīlauea, continues to slowly rise, with no significant changes in recent weeks. USGS photo by M. Patrick.

The eastern end of the lake, shown here, is slightly warmer than the lake center, and commonly has steam rising from the water surface. USGS photo by M. Patrick.