Images

Mount Adams viewed from the southeast.

_{CSAV International Program participants from 2011 came from volcano observatories in the Philippines, Democratic Republic of Congo, Costa Rica, Mexico, El Salvador, Colombia, Comoros, and Indonesia.}

USGS Photo, looking north, at what remained of Lake Waiau on September 26, 2013. The water area was just 15 meters (yards) wide at this time. Prior to 2010, the lake occupied the entirety of the now-dry lake bed, which is about 100 meters (yards) wide. The astronomical telescopes at the summit off Mauna Kea are visible on the skyline.

No activity was observed on the Peace Day flow on today's overflight, meaning that the Kahauale‘a 2 flow is now the sole active flow. The Kahauale‘a 2 flow today had reached 6.4 km (4.0 miles) northeast of Pu‘u ‘Ō‘ō, and was burning vegetation around the forest boundary.

Very few surface flows have been observed in Pu‘u ‘Ō‘ō crater over the past month, but the crater today was far from quiet. The spatter cone shown here, in the northern portion of the crater, was producing a loud, continuous jetting sound resulting from gas being forced through a tiny opening at the peak.

Active pāhoehoe breakouts are scattered across portions of the Kahauale‘a 2 flow. This photo shows a nice example of ropy pāhoehoe active near the flow margin.

Much of the Kahauale‘a 2 flow has traveled over ‘A‘ā from Pu‘u ‘Ō‘ō's early activity in the 1980s. This photo shows a lobe of the Kahauale‘a 2 flow advancing over a section of this older ‘A‘ā, burning moss and small trees that have grown on the ‘A‘ā clinker.

Crews test two methods of measuring discharge of the Muddy River near Mount St. Helens, Washington. The computer and tethered orange float create a vertical discharge profile; the hand-held flow tracker confirms the data. Data collection is becoming more electronic-oriented with periodic confirmation of results by physical observations.

Information regarding magma formation, mixing and its ascent to the surface can be deduced from examination of thin sections (thin slices of rock mounted on glass). Science teachers look on as a sample of basalt is viewed under a petrographic microscope.

This thermal image looks southwest towards the vent on Pu‘u ‘Ō‘ō, and shows much of the Kahauale‘a 2 flow. Hotter colors (yellow and white) represent active breakouts, while warm colors (red and purple) show recently active portions of the flow.

pāhoehoe lava on the Kahauale‘a 2 flow invades the forest northeast of Pu‘u ‘Ō‘ō, burning and toppling trees and creating plumes of smoke.

A wider view of the Kahauale‘a 2 flow margin at the forest boundary.

This thermal image looks southwest towards the vent on Pu‘u ‘Ō‘ō, and shows much of the Kahauale‘a 2 flow. Hotter colors (yellow and white) represent active breakouts, while warm colors (red and purple) show recently active portions of the flow.

A close-up view of one of the many breakouts of pāhoehoe on the Kahauale‘a 2 flow.

An HVO geologist shields his face from the intense heat as he takes a sample of active lava on the Kahauale‘a 2 flow. The chemistry of the lava is analyzed through time and used to study changes in the magmatic system.

Repairs are made to an Acoustic Flow Monitor (AFM) located at the confluence of the North Fork Toutle River, Maratta, Castle and Coldwater Creeks, where the most recent lahar occurred in November, 2006. AFMs are installed to "hear" when lahars [muddy debris flows] move down channel so affected communities can be warned of the hazard.

The deep-sea drilling ship Chikyu, which will attempt to drill through the Moho [Image copyrighted by JAMSTEC. Used with permission].

Huckleberry Ridge Tuff deposit exposed on Mt. Everts, near the northern boundary of Yellowstone National Park. The deposit was created by ash falling from the plume early in the eruption sequence, 2.08 million years ago. Photo by Madison Myers, Montana State University.

The Kahauale‘a 2 flow extends to the north and northeast of Pu‘u ‘Ō‘ō. From the edge of the flow, where it first reaches the forest, Pu‘u ‘Ō‘ō still appears to tower above the surrounding plain.

The Kahauale‘a 2 flow extends to the north and northeast of Pu‘u ‘Ō‘ō. From the edge of the flow, where it first reaches the forest, Pu‘u ‘Ō‘ō still appears to tower above the surrounding plain.

Active breakouts on the Kahauale‘a 2 are scattered over a broad area. Here, a breakout near the edge of the forest engulfs trees and burns dead foliage.