Images

A wider view of the ocean entry.

HVO geophysicist shares information at a public outreach event for Volcano Awareness Month at the University of Hawai‘i at Hilo in January 2017.

Yellowstone National Park is the site of Earth's largest concentration of geysers, as well as steam vents, hot springs, and mudpots. These hydrothermal features attest to the region's volcanic history, which spans over two million years and is the reason that the Yellowstone Volcano Observatory was established.

A steady stream of lava exiting the episode 61g lava tube pours into the ocean at the Kamokuna ocean entry. The interaction between the lava and ocean water causes explosive reactions, throwing bits of lava (seen in the photo at the base of the lava stream).

Misty weather created a double rainbow over Pūlama Pali and the 61g flow field. Fume trace from the tube can be seen at bottom center.

Since the delta collapse on December 31, 2016 there has not been any evidence of the lava delta rebuilding. The fume trace of the 61g tube system on the coastal plain is visible up slope from the ocean entry. The cove in the sea cliff (at center) is where the ~4 acre portion of old sea cliff collapsed into the ocean after the delta fell in.

A close up of the lava stream pouring out of the tube and directly into the Pacific Ocean.

This video clip shows the lava stream - about 1-2 m or yards wide - pouring out of the tube into the Pacific Ocean, triggering pulsating explosions that are throwing bits of lava onto the top of the sea cliff.

This thermal image shows the Kamokuna ocean entry. Two plumes of hot (scalding) water branch out from the entry point. The lava stream itself is the very hot feature right of center. Just above the lava stream, about 10 meters (yards) behind the sea cliff, is a narrow line of high temperatures that appears to be a hot crack.

Analysis of shoreline changes at Bogoslof volcano due to eruptive activity between January 11 and 24, 2017. The base image is a Worldview-2 satellite image collected on January 24, 2017. The approximate location of the shoreline on January 11, 2017 is shown by the dashed orange line.

Kīlauea Volcano's summit lava lake level typically rises and falls in concert with summit inflation and deflation, as shown by these two HVO webcam images. The left image was captured a week ago (on Jan. 17, 2017), when the lava level was 52.5 m (172 ft) below the vent rim, the lowest level measured since April 8, 2016. The right image, captured this morning (Jan.

This video clip of Kīlauea Volcano's summit lava lake shows spattering along the southeast margin of the lake.

Kīlauea Volcano's summit lava lake level rose over the past day with steep summit inflation, providing improved views of spattering from visitor overlooks in Hawai‘i Volcanoes National Park.

Mount Shasta, a steep-sided Cascade Range stratovolcano in Northern California, looms above Little Glass Mountain, a thick obsidian flow erupted from the Medicine Lake shield volcano about 1,000 years ago. These are just two of the 19 young volcanic areas monitored by the USGS California Volcano Observatory (CalVO).

A net sedimentation tile (NST) is used by scientists to measure surface sediment deposition in wetlands over short time scales. Scientists installed several NSTs on the surface of the marsh to measure sediment deposition. The samples are retrieved and measured in the lab to identify short-term sediment deposition rates on the marsh surface.

The summit lava lake within Halema‘uma‘u Crater today (Jan. 15, 2017) was about 50.5 m (166 ft) below the crater floor (vent rim). One of the most interesting things exposed by the lower lake level was the clear view of the thick, dark veneer of lava on the eastern vent wall (close-up shown below).

In places, the dark-colored veneer of lava, or bathtub rings, have already collapsed into the lava lake, exposing older, light- or rusty-colored rocks in the vent wall. The lava lake surface is visible in the foreground. The distance from the vent rim to the lake surface is 50.5 m (166 ft).

Telephoto image of the lava veneer on the 50.5 m (166 ft) tall eastern vent wall; the lava lake surface is visible at lower left. The solidified lava coating the vent wall is quite thick.

Mount Adams viewed from the south-southeast.

The November 21 breakout from the episode 61g lava flow remains active. The tip is 2.4 km (1.5 mi) straight-line from the vent, and the furthest active lava is roughly 600 m (660 yd) back from the tip. The breakout, extending to the lower right of the image, can be identified by its light silver color. Pu‘u ‘Ō‘ō is visible in the upper left of the photo.

The Kamokuna ocean entry remains active. On December 31, approximately 21 acres of delta collapsed into the ocean. The remaining ~2.5 acres can be seen at the base of the sea cliff in long narrow sections. On the lower right of the photo, a scarp is visible where a portion of the old sea cliff collapsed.