At 08:01 HST 11/05/2026, the North Vent produced what I would call a "wet burp" after the precursory "pistoning" events, small amounts of lava pouring out of the vent for a few seconds to minutes and then everything recedes. There must have been a gas bubble holding thing back because two minutes later the lava started flowing out of the vent in all directions. Then, at 08:25, it stopped. What a tease! I thought this was how Episode 56 started.
About 12 minutes later at 08:38, the North vent once again started overflowing and picked up steam at 08:42. By 09:00, slight doming could be seen in the pool of lava in the vent. Surely this is it!
But, 09:50 and things wind down again. By 09:57 HST there's just fumes coming out of the vent. Phooey.
But then 10:00 comes and the heavy lava flows kick in again. This time seems like the real deal. At 10:30 HST there's little spurts of lava flying up in the air over the vent, but more from gas than a steady fountain of lava. This looks promising!
11:30 HST and the color of the lava is definitely hotter, and the intensity has picked up to a definite dome and precursor to fountaining. The USGS calls Episode 56 as officially starting at 12:10 HST:
Alert Level: WATCH, Color Code: ORANGE 2026-11-05 22:29:12 UTC
HVO/USGS Volcanic Activity Notice
Volcano: Kilauea (VNUM #332010)
Current Volcano Alert Level: WATCH
Current Aviation Color Code: ORANGE
Issued: Thursday, November 5, 2026, 12:29 PM HST
Source: Hawaiian Volcano Observatory
Notice Number: 2026/H514
Location: N 19 deg 25 min W 155 deg 17 min
Elevation: 4091 ft (1247 m)
Area: Hawaii
Summary: Episode 56 of the ongoing Halemaʻumaʻu eruption began at 12:10 PM HST on November 5, 2026.
Volcanic Activity:
Episode 56 of lava fountaining in Halemaʻumaʻu began at the summit of Kīlauea began at 12:10 PM HST on November 5, 2026.
Lava fountain heights are relatively low at about 100 ft (30 meters), but will likely increase. Ground-level sensors near the eruptive vents indicate that winds are blowing from the northeast direction, which suggests that volcanic gas emissions and volcanic material may be distributed to the southwest direction from Halemaʻumaʻu.