A Smile From Pele as Lava Continues Flow Into Ocean
Eruptions continue at Kīlauea Volcano’s summit and East Rift Zone, the US Geological Survey’s Hawaii Volcano observatory reported on Friday, Aug. 5, 2016, at 8:58 a.m.
The 61G lava flow, extending southeast of Puʻu ʻŌʻō on Kīlauea’s south flank continues to flow into the ocean at Kamokuna, within the boundary of Hawaii Volcanoes National Park, and has scattered breakouts predominantly on the coastal plain. This new flow is now about 6.5 miles long.
The flow poses no threat to nearby communities, but visitors are advised to use caution.
The length of coast comprising the active entry has ranged between 150 m (492 feet) and 240 m (787 feet) in the past week and the entire area presents a significant hazard to visitors.
Lava Delta Forming: Paradise Helicopters reported that lava has begun to build a delta at the Kamokuna entry point on Thursday, Aug. 4.
Fluid pahoehoe has repeatedly covered the newly completed access road and is now about a quarter-mile wide.
Lava rolled over Pulama Pali a month ago, mostly between Hawaii Volcanoes National Park and the abandoned Royal Gardens subdivision.
Only a handful of visitors made their way on foot this morning, Paradise reported, but three tour boats were on-hand at sunrise to take in the amazing spectacle of hot liquid rock interacting with the Pacific Ocean.
A large crack above the lava delta demonstrates the instability of the area, which could collapse into the sea at any time.
At their own risk, many gawkers stand at the edge of the cliffs to get a glimpse, Paradise reported.
“We visited the vent today as well and once again were able to access the steamy lava lake within the vent to the west,” Paradise reported. “As usual, a great deal of lava is moving quickly through a skylight on the northeast corner, feeding the ocean entry downslope.
Caution to Visitors: The USGS has issued a strong caution to visitors viewing the new ocean entry for Flow 61G, there are additional significant hazards besides walking on uneven surfaces and around unstable, extremely steep sea cliffs.
Venturing too close to an ocean entry exposes you to flying debris created by the explosive interaction between lava and water.
Also, the new land created is unstable because it is built on unconsolidated lava fragments and sand. This loose material can easily be eroded away by surf causing the new land to become unsupported and slide into the sea.
Finally, the interaction of lava with the ocean creates an acidic plume laden with fine volcanic particles that can irritate the skin, eyes and lungs.
Summit Observations: The lava lake at Halemaʻumaʻu Crater continues to be active with a current height of 40 m (131 feet) below the overlook crater rim.Seismicity and deformation rates remain at background levels throughout the volcano. Tiltmeters at Kīlauea’s summit changed from recording deflationary to inflationary tilt at about 4 p.m. HST on Thursday, Aug. 4, consistent with moving from the deflation to inflation portions of a deflation-inflation event. The overall trend for the past several weeks has been slightly inflationary.
Seismicity rates continue to be normal, with tremor fluctuations associated with lava lake spattering. The average daily summit sulfur dioxide emission rate ranged from 4,000 to 6,000 metric tons per day over the past week.
Puʻu ʻŌʻō Observations: Webcam images over the past 24 hours show persistent glow at long-term sources within the crater, indicating no significant changes. Seismicity and tilt records also showed no significant changes in the past day. The sulfur dioxide emission rate from all East Rift Zone vents was about 300 metric tons/day when measured on Aug. 3.