Calm after the storm—a beautiful day on Kīlauea Volcano’s East Rift Zone. Rain from Hurricane Madeline had little impact on Puʻu ʻŌʻō, shown here, or lava flow 61g.
View of the lava pond within the Puʻu ʻŌʻō west pit crater, which is about 50 m (164 ft) across. Weak spattering on the lava pond surface, about 23 m (75 ft) below the crater rim, is visible through the thick volcanic gas cloud
An aerial view of a new breakout (light-colored flow at center of image) from the 61g tube. The breakout began with some vigor on the morning August 29, but today it was sluggish, with only a few scattered pāhoehoe toes still active on the margins of the flow.
View of the 61g flow field, from Puʻu ʻŌʻō (visible on top, left horizon) to the westernmost ocean entry at the coast, where lava spills into the sea, creating a lava delta.
A closer view of where lava is entering the sea along a 1.1-km- (0.7-mi-) wide section of the coastline. There is no evidence that high surf from Hurricane Madeline had any impact on the lava deltas that have formed, and continue to grow, at the ocean entries.