Images

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.

This telephoto image from January 19, 2017, shows spattering along a down-welling section of Kīlauea Volcano's summit lava lake. The main area of spattering was about 10 m (32 ft) high, but some lava fragments were thrown even higher.

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).

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).

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.

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).

Mount Adams viewed from the south-southeast.

Redoubt Volcano, shown here on April 4, 2009, is just one of the more than 50 historically active volcanoes monitored by the Alaska Volcano Observatory (AVO). Gray ash draping the flanks of the volcano creates a stark contrast to the surrounding snow-covered landscape and white steam rising from Redoubt's summit crater.

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.

A close up view of where approximately 4 acres of old sea cliff fell into the ocean during the delta collapse on December 31. The far eastern end of this collapse (right), is where the old public viewing area was located prior to the collapse.

On the left is a normal photograph of the ocean entry, which produces a robust steam plume and an area of discolored water extending out from the entry point. The thermal image on the right shows how this area of discolored water corresponds to scalding water temperatures.

Another view of the ocean entry, with the plume of hot water extending out from the ocean entry point.

This map shows recent changes to Kīlauea's East Rift Zone lava flow field. The area of the active flow field as of December 14 is shown in pink, while widening and advancement of the active flow as of January 12 is shown in red. Older Pu‘u ‘Ō‘ō lava flows (1983-2016) are shown in gray.

Annotated photograph of Bogoslof Island showing the cumulative effects of 2016-17 eruptive activity. A layer of fine muddy appearing ash drapes most of the landscape and covers pre-existing vegetation. The dashed line indicates the area excavated by explosive eruptive activity so far.