Images

An aerial photograph looking west along the coastline of the current flow field. The Ki entry continues to produce a small plume, which is distributed along the newly formed delta. The color change in the ocean near the entry is due to the wave erosion of material from the delta and the lava itself.

Since reaching the water a few weeks ago, the Ki ocean entry has formed a small delta, seen here, with a surface area of about 7 acres. A small steam plume rises above the entry, indicating that relatively little lava is making it into the ocean.

The western side of the delta was the most active, with several small streams of lava pouring off the front of the delta into the water.

Fumes marks the trace of the tube system within the new Quarry flow. The Ki ocean entry, where the lava flowing through the tube system spills into the ocean, is at upper left. The shiny surfaces in the foreground at the center of the image are active lava flows.

Steep view of the Overlook vent from over the south rim of Halema`uma`u. The closed and partly destroyed visitor overlook is visible at the bottom of the image.

Looking south across Halema`uma`u Crater at the gas plume rising from the Overlook vent.

View of HALEMAUMUA Crater during typical tradewind conditions, which blows the gas plume to the southeast. For scale, the Halema‘uma‘u Crater is about 1 km (0.6 mi) across (left to right); the floor of Halema‘uma‘u Crater is about 80 m (260 ft) m below the crater rim.

Seismologists demonstrates how an earthquake's S and P waves travel through the earth at a CVO public open house.

Fume from Pu`u `Ō `ō crater was relatively light today, allowing for nice views into the crater. The Halema`uma`u plume is in the background just below the clouds.

Sometime in the last week, a 2-3 m (yard) skylight opened over the recently formed lava tube that is currently feeding the ocean entry. The terrace on the edge of the lava stream hosts smooth ripple-like features that form during lava level fluctuations, when lava rises up and spills over onto the ledge. Flow direction is from right to left.

View of the current TEB flow field. The ocean entry continues, producing a weak plume scattered along the coastline. The lighter gray colored lava is the recent flow that has entered the vegetation and reached the pavement at the end of Highway 130. Plumes from the TEB shield and Pu`u `Ō `ō crater are on the horizon.

A closer view of the recent flows working their way down the road and through the trees. The viewing area has been moved back once again due to its proximity to the lava flows and potential fire hazards.

Upslope from the west end near the Kalapana access road, scattered breakouts continued to be active.

Flow expansion over the past day also covered most of the former lava viewing area near the Kalapana access road. The County has since relocated the viewing area farther east.

Breakouts continued to be active on the east margin of the flow field, and hit the pavement of the Kalapana access road today creating thick black smoke from the burning asphalt.

Just south of the Kalapana access road, active pahoehoe was pushing through thick vegetation, creating scattered brush fires and small methane bursts.

Flows reached the pavement where the former viewing gate near the Kalapana access road resided.

One of several lava streams on the shore of Kilauea volcano.

The ocean entry that started on April 29 continues, and has expanded in width.

Lava first touched the water at 12:15pm, and this photo shows the first finger of lava approaching the ocean.

View looking back to the north at the terminus of the active flow as it approaches the forested kipuka at the center of the photo. Hwy 130 is at upper right. The old ocean entry viewing area, open from 2008 to early 2010, is visible near the bottom of the photo just to the right of center.