Videos

As you watch this VIDEO CLIP, note the rocky ledge (yellow arrow) at the bottom of the webcam image. At 6:58 a.m., HST, today, this large slab of the summit vent wall, located directly below HVO's HMcam, collapsed.

VIDEO CLIP captured by HVO webcam: At 11:59 a.m., a rockfall from the south wall of Halema‘uma‘u Crater triggered a small explosive event in the summit lava lake. The explosion threw spatter (fragments of molten lava) onto the rim of the crater, mostly to the west of the former visitor overlook.

This VIDEO CLIP shows a cloud of ash and spatter being thrown from the summit lava lake during today's explosive event. The images were captured by an HVO webcam located on the rim of Halema‘uma‘u Crater, just above the rockfall area.

This video shows activity in the summit lava lake in Halema‘uma‘u Crater. Spattering like this is common in the lake, and this video shows the view from the rim of Halema‘uma‘u (closed to the public due to volcanic hazards). This spattering has recently been visible from the Jaggar Overlook inside Hawai‘i Volcanoes National Park (open to the public).

This video clip shows activity in the summit lava lake in Halema'uma'u Crater. Spattering like this is common in the lake. Today, spattering was active along the east margin of the lake, throwina small bits ot spatter to heights of about 15 m (roughly 50 Meet).

This video shows spattering in two locations of Kīlauea's summit lava lake. In the first segment, spattering is active in a small area in the southern portion of the lake. In the second segment, spattering on the east margin of the lake has created an overhanging ledge with dangling lava stalactites.

This video clip shows the northern portion of the lava lake, where episodic bubbling commonly occurs. The northern margin of the lake is in the upper right portion of the photo. Note how the bubbling occurs in the same general area, regardless of the movement of the crustal plates. The video is shown at 20x speed.

This video clip shows a few of the lava breakouts active on Kīlauea's coastal plain on September 20. The activity consisted of scattered pāhoehoe breakouts. The final segment in this video is shown at x20 speed.

Movie showing spattering near the south edge of Kīlauea's summit lava lake in Halema‘uma‘u.

Kilauea's summit lava lake in Halema'uma'u Crater has been at a high level over the past several days, with the lake surface just 8 meters (26 feet) below the floor of Halema'uma'u this evening. The high level has provided clear views of spatter from the public overlook at Jaggar Museum.

This video clip, filmed on August 12, 2016, shows a typical pāhoehoe breakout on Kīlauea Volcano's "61g" lava flow (actual speed).

This aerial video footage, filmed by USGS in late July 2016, features Kīlauea Volcano's summit vent within Halema‘uma‘u Crater.

The lava flow southeast of Pu'u 'Ō'ō reached the ocean overnight at about 1:15 am. The narrow lobe of lava spilling over the sea cliff has built a tiny delta at the shore, with a weak ocean entry plume.

Stunning 4K aerial and ground b-roll of the Kīlauea Volcano Halemaʻumaʻu Crater Summit Vent Lava Lake taken between July 24 and July 31, 2016. 

The lava flow southeast of Pu'u 'Ō'ō continues to advance downslope, and has crossed roughly half of the coastal plain. Upslope of the flow front there was still some 'a'ā activity, with several small open channels on the pali. The front of the flow was 1.7 km (1.1 miles) from the ocean today.

The lava flow southeast of Pu'u 'Ō'ō continues to advance downslope, and has begun crossing the coastal plain. The leading portion of the flow now consists ot pāhoehoe, shown in this video. Upslope of the flow front there was still some 'a'ā activity, with a few small open channels on the pali.

The lava flow southeast of Pu'u 'Ō'ō continues to advance downslope, and reached the base of the pali yesterday. The leading portion of the flow still consists of narrow channelized 'a'ā streaming down the steep part of the pali.

The lava flow southeast of Pu'u 'Ō'ō continues to advance downslope, and was reaching the base of the pali today. Although the malority of the flow activity is pāhoehoe, the fast-moving flow front IS channe ized 'a'ā. The leading tip of the flow is burning vegetation in a kīpuka.

The lava flow southeast of Pu'u 'Ō'ō continues to advance downslope, and is now progressing down the pali. The flow is following the eastern boundary of Hawai'i Volcanoes National Park, and the western boundary of the abandoned Royal Gardens subdivision. Although the majority of the flow activity is pāhoehoe, the fast-moving flow front is channelized 'a'ā.

The lava lake at Kilauea's summit has risen over the past few days, providing improved views of the lake activity. Spattering along the southern lake margin was vi orous this evening, but within the range of normal activity for the la e. Spatter was thrown as high as the Halema'uma'u Crater floor, about 25 m (80 ft) above the lake surface.

The two breakouts that began at Pu'u 'Ō'ō on May 24 are still active. This morning, the active portions of both flows remained relatively short, extending no more than 1 km (0.6 miles) from their breakout points. The eastern breakout, shown here, was developing a lava tube. A collapse in the roof of the tube provided a view of the lava stream.