Images

Southerly winds offered decent views of the collapse pits on the west flank of Pu`u `Ō `ō. The TEB vent is the heavily fuming vent beyond Pu`u `Ō `ō to the right, and the active tube system extends to the right out of the image frame.

A beautiful example of sulfur crystals that have grown around a small fumarole near the southeast rim of Halema`uma`u crater. The vent is about 0.3 m (1 foot) long.

Although there are no surface flows anywhere on the flow field, lava continues to flow through the Waikupanaha lava tube and enter the ocean.

An aerial view looking north at two active areas of Kīlauea. Pu`u `Ō `ō crater is in the foreground, Mauna Loa (left) and Mauna Kea (right) are in the background. The fume source near the base of Mauna Loa (at Kīlauea's summit) is from the Halema`uma`u Overlook vent.

South winds allow for a different perspective of the Halema`uma`u Overlook vent.

This large rock at the Kīlauea Overlook in Hawai‘i Volcanoes National Park was ejected ballistically in 1790, or soon thereafter, from Kilauea Volcano's summit caldera when it was more than 600 meters (2000 feet) deep.

Aerial view of the Waikupanaha (large plume) and West Waikupanaha ocean entries. The West Waikupanaha entry spans the coastline where the numerous small, wispy plumes are visible. The entries remain active as lava continues to enter the ocean through both lava tubes and surface flows.

Standing at the former time lapse camera site on the rim of Pool 1 of the perched channel, geologists measure the depth of the March 2009 collapse. A hammer head was attached to a steel cable and lowered over the edge until it hit the floor of the collapse pit. When the hammer hit the bottom, the cable was marked, and the depth was measured at 16.5 m (54 ft) deep.

At the Waikupanaha ocean entry (left), three separate steam plumes merge into one as the wind blows the steam offshore. The west Waikupanaha entry is spread out over a larger area with at least 5 separate lava entry points. This photo was taken looking southeast.

Scattered breakouts, like the one shown here, continue to be active on the coastal plain and are situated west of the main Waikupanaha tube and just inland of the west Waikupanaha ocean entry.

This photo is looking east towards the three ocean entry points active today. The most distant, and most vigorous, is the Waikupanaha entry, which has been active since March 2008. In the foreground are two entry points at the west Waikupanaha entry area, which has been active over the past few weeks.

A small open channel of lava was entering the water at one of two entry points at the west Waikupanaha entry area.

Surface activity continued in several small areas above the Kalapana access road, burning more vegetation in the forested kipuka. The trailhead to the county viewing area sits at the end of what remains of the access road, shown here at the top-middle portion of the photograph.

Lava continues to flow into the ocean at the well-established Waikupanaha ocean entry. About 700 m to the west (up the coastline in this photograph), the new ocean entry puts off a small plume that is barely visible from this vantage point.

On the east margin of the entry, lobes were advancing over a small black sand beach.

Breakouts continued near the County lava viewing trail. This breakout, which is burning a downed hala tree, was about 300 m west of the trailhead.

One of the entry points, on the east side of the west Waikupanaha entry.

Several collapses early this morning exposed more of the lava pond deep within the Halema`uma`u vent cavity. For the last several days, glowing and spattering holes (top image) have been active on the floor of the vent cavity, at a depth of about 200 m below the vent rim.

Mount Baker's Carmelo Crater at the summit is breached by Roosevelt Glacier, view to the southeast, Washington.

Scientists from the USGS Alaska Volcano Observatory (AVO) examine deposits on the lobe of the Drift Glacier with the summit of Mount Redoubt and its steaming lava dome in distance.

Soil-temperature measurement at Hot Creek in Long Valley Caldera, California.