Hawai'i Volcano Blog

Kīlauea Volcano Update: July 20, 2017

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Clear weather provided good views of the lava lake at Kīlauea Volcano’s summit on July 20, 2017. The activity this evening was typical for the lava lake, with variable spattering along the lake margins. Spattering shown here was in the southeast part of the lake, which is the most common site for spattering. This photo was taken by USGS scientists from the rim of Halema‘uma‘u crater, an area that remains closed to the public due to ongoing volcanic hazards.

This past week, Kīlauea Volcano’s summit lava lake fluctuated in concert with summit inflation and deflation, with levels ranging 82 to 148 feet below the vent rim.

On the East Rift Zone, the 61g flow remained active, with lava entering the ocean near Kamokuna and surface breakouts downslope of Pu‘u ‘Ō‘ō.

The 61g flows do not pose an immediate threat to nearby communities.

ARTICLE CONTINUES BELOW AD
ARTICLE CONTINUES BELOW AD

Mauna Loa is not erupting.

GPS measurements continue to show deformation related to inflation of a magma reservoir beneath the summit and upper Southwest Rift Zone.

No significant changes in volcanic gas emissions were measured.

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During the past week, small-magnitude earthquakes occurred beneath the volcano, primarily in the south caldera and upper Southwest Rift Zone, at depths less than 3 miles.

No earthquakes were reported felt on the Island of Hawaiʻi during the past week.

This map shows recent changes to Kīlauea’s East Rift Zone lava flow field. The area of the active flow field as of June 21 is shown in pink, while widening and advancement of the active flow as of July 10 is shown in red. Older Pu‘u ‘Ō‘ō lava flows (1983–2016) are shown in gray. The yellow line is the trace of the active lava tube. USGS map.

The Volcano Activity Update is a weekly article written by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates.

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Call for summary updates at (808) 967-8862 (Kīlauea) or (808) 967-8866 (Mauna Loa); email questions to [email protected].

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