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The flow front remains active, and was more than half way across the coastal plain today (July 6). This afternoon, the flow front was roughly 2 km (1.2 miles) from the base of the pali, and 1.3 km (0.8 miles) from the ocean. The front consisted of slow moving pāhoehoe.
As this small channel of lava flows into a depression, its semi-congealed surface twists and wrinkles—forming the ropy surface commonly seen on pāhoehoe flows. Flows on the pali are visible in the background.