Eruptive activity persists on Kilauea’s east rift zone, from the vent, Pu‘u ‘O‘o, to the Kamokuna ocean entry in the Hawaii Volcanoes National Park. Attention is at a high level at the ocean entry due to extreme instability of the cliff side, as cracks shown in the photos below have been quickly increasing in width, leading to a couple sizable collapses yesterday AFTER our overflight. Hopefully, we will have the opportunity to post before & after shots soon. For now, these are images from yesterday morning.
A view of the fracture and one of the skylights that has formed as a result of an increase in width. Rising steam from the crack is an indication of its depth, extending to near or beyond sea level.
A view of the crack at the Kamokuna ocean entry. A skylight gives a peek at a portion of the river of lava before it exits the tube and into the sea.
A lengthy crack had formed at the ocean entry, running parallel to the ocean’s edge, widening over the past few weeks.
The distal tip of the latest breakout on Pu‘u ‘O‘o’s eastern flank. Still not much more than 1/2 mile from its source.
A view of Pu‘u ‘O‘o and its lava pond on the right, and trail of rising gases extending to the Kamokuna ocean entry near the top middle of the image.