July 25: Lavasheds Explained (More or Less)

July 25, 2018. USGS: “Early this morning, several small lobes of lava were oozing out from crusted ‘a‘ā flows along the southern ocean entry.” (Full-sized)
Today’s Eruption Summary

As we approach the 3-month mark— or pass it, since Puʻu ʻŌʻō’s floor collapsed 3 months ago this past Monday— Kīlauea’s 2018 eruption continues with no significant changes. During the USGS morning overflight, the lava’s southwestern margin was holding at less than a tenth of a mile from Pohoiki boat ramp. The vigorous ocean entry continues a few hundred yards to the east. No surges in lava output have been reported at Fissure 8 since Tuesday’s 6:41 am summit collapse.

July 25, 2018. USGS: ” HVO’s overflight early this morning revealed little advancement of the westernmost ocean entry. During the overflight, lava was approximately 145 m (475 ft) from the boat ramp at Isaac Hale Park (near the light-colored structure just left of center in this photo).” (Full-sized)

A deceptive moment of tranquility at the new, extensively remodeled summit:

July 25, 2018. USGS: “Earthquakes shook the ground at Kīlauea’s summit late this afternoon, stirring up rock dust within Halema‘uma‘u and along the caldera walls. This view from the northeast caldera rim looks across at the Keanakāko‘i and South Sulphur Banks areas.” (Full-sized)

Here’s HVO’s Steve Brantley giving the weekly eruption update at last night’s Pahoa community meeting (I’ll be transcribing it tomorrow or Friday).

He explains that complicated “lavashed” map released earlier this week, which predicts where lava is most likely to go if there’s a breakout along particular stretches of Fissure 8’s lava channel. This is an aid to residents living in neighboring areas not affected by lava now, but who are worried about what might happen if the flow diverts.

Continue reading July 25: Lavasheds Explained (More or Less)