https://youtu.be/wgeH0dXkSUo
This video clip, filmed on August 12, 2016, shows a typical pāhoehoe breakout on KÄ«lauea Volcano’s “61g” lava flow (actual speed). Since the ongoing East Rift Zone (PuÊ»u ʻŌʻō) eruption began in 1983, the net result of countless pāhoehoe flows like this is that 142 square kilometers (55 square miles) of federal, state, and private land on KÄ«lauea Volcano have been covered by lava. Courtesy of USGS/HVO

https://youtu.be/8WogpdNi518
Time-lapse thermal image movie of Halemaumau Overlook Vent. August 18-25, 2016. Images courtesy of USGS/HVO

https://youtu.be/6zVnnhocmJ8
Time-lapse movie of Halemaʻumaʻu Overlook Vent from Hawaiian Volcano Observatory. August 18-25, 2016. Images courtesy of USGS/HVO

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Time-lapse movie of KÄ«lauea Caldera from Hawaiian Volcano Observatory. August 18-25, 2016. Images courtesy of USGS/HVO

KÄ«lauea Volcano’s active lava flow continues to bury more of the emergency access route (Chain of Craters Road) in HawaiÊ»i Volcanoes National Park. Early this morning, slow-moving breakouts were oozing across the road on the west side of the flow. Photo taken Thursday, August 25, 2016 courtesy of USGS/HVO

KÄ«lauea Volcano’s older “61g” lava flows have now inflated (left side of photo), creating jagged terrain that rises as much as 3 m (10 ft) above the road. Today, new lava (right) was covering additional areas of the gravel road. Photo taken Thursday, August 25, 2016 courtesy of USGS/HVO

At the summit of KÄ«lauea, the weather cleared, but inflation turned to deflation and the lava lake level dropped, so the spattering that had been visible from overlooks in HawaiÊ»i Volcanoes National Park the past two days is no longer visible today. But, it was a beautiful day to view HalemaÊ»umaÊ»u Crater from the Jaggar Museum Overlook! Although the lava lake surface was 32 m (105 ft) below the vent rim this morning, it’s still likely that an orange glow from incandescent lava deep within the summit vent will be visible after dark. Photo taken Thursday, August 25, 2016 courtesy of USGS/HVO

(Activity updates are written by scientists at the U.S. Geological Survey’s Hawaiian Volcano Observatory.)

Kīlauea continues to erupt at its summit and East Rift Zone. During the past week, the summit lava lake level varied between about 20 m and 40 m (66–131 ft) below the vent rim within Halema‘uma‘u Crater. On the East Rift Zone, the “61g” lava flow continued to advance across the coastal plain and enter the ocean. The lava flow does not pose an immediate threat to nearby communities.

Mauna Loa is not erupting. Seismicity remains elevated relative to the long-term background rate, but has not changed significantly over the past week. Earthquakes are occurring mostly in the volcano’s south caldera and upper Southwest Rift Zone at depths less than 5 km (3 mi). Global Positioning System (GPS) measurements show deformation related to inflation of a magma reservoir beneath the summit and upper Southwest Rift Zone, with inflation occurring mainly in the southwestern part of the magma storage complex.

Two earthquakes were reported felt on the Island of Hawaiʻi in the past week. On Wednesday, August 24, 2016, at 12:17 p.m., HST, a magnitude-3.8 earthquake occurred 5.1 km (3.2 mi) southeast of Kīlauea Volcano’s summit at a depth of 3.0 km (1.8 mi). At 1:12 p.m. on the same day, a magnitude-3.5 aftershock occurred at a similar location and depth.

Please visit the HVO website (http://hvo.wr.usgs.gov) for past Volcano Watch articles, KÄ«lauea daily eruption updates, Mauna Loa weekly updates, volcano photos, recent earthquakes info, and more; call for summary updates at 808-967-8862 (KÄ«lauea) or 808-967-8866 (Mauna Loa); email questions to askHVO@usgs.gov

https://youtu.be/L-4b3NxXEKE
Time-lapse multi-image movie of Pu’u ‘O’o Crater. August 18-25, 2016. Images courtesy of USGS/HVO

https://youtu.be/1bqhGBz6uIA
Time-lapse movie from images gathered from a temporary thermal camera looking into Pu’u ‘O’o Crater. The temperature scale is in degrees Celsius up to a maximum of 500 Celsius (932 Fahrenheit) for this camera model, and scales based on the maximum and minimum temperatures within the frame. Thick fume, image pixel size and other factors often result in image temperatures being lower than actual surface temperatures. August 18-25, 2016. Images courtesy of USGS/HVO