Deflation at Kīlauea's summit has caused up to 1.5 meters (about 5 feet) of subsidence, which has stressed the faults around and within Kīlauea Caldera.
Click the image above to read the PDF.
Why so many earthquakes in the Kīlauea summit area?
By Hawaiian Volcano Observatory
May 29, 2018
Deflation at Kīlauea's summit has caused up to 1.5 meters (about 5 feet) of subsidence, which has stressed the faults around and within Kīlauea Caldera.
Related
Why so many earthquakes in the Kīlauea summit area?
Deflation at Kīlauea's summit has caused up to 1.5 meters (about 5 feet) of subsidence, which has stressed the faults around and within Kīlauea Caldera.
Click the image above to read the PDF.
Related
Why so many earthquakes in the Kīlauea summit area?
Deflation at Kīlauea's summit has caused up to 1.5 meters (about 5 feet) of subsidence, which has stressed the faults around and within Kīlauea Caldera.
Click the image above to read the PDF.
Deflation at Kīlauea's summit has caused up to 1.5 meters (about 5 feet) of subsidence, which has stressed the faults around and within Kīlauea Caldera.
Click the image above to read the PDF.