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On June 13 at about 6:00 am, there was a new pāhoehoe breakout along the episode 61g tube system approximately 1.1 km (0.7 miles) from the vent. Today (June 21), geologists visiting the site found that the ground had been cracked and uplifted about 2 m (6.6 feet) where the breakout originated (center). This is the closest active breakout to Pu‘u ‘Ō‘ō and the 61g vent, and also the largest on the flow field. Smaller scattered surface flows from the March 5 breakout remain active, but all lava flow activity is on the upper flow field above the pali.
The ocean entry remains active and continues to increase the size of the Kamokuna lava delta. Today, activity was concentrated towards the western side of the delta (left center), and building outward in a narrow lobe. Surface flows on the delta over the past few weeks have covered most of the delta with new lava.